Chile

Physiography.—For purposes of general topographical description Chile may be divided into three regions: the desert region of the north, the central agricultural region between the provinces of Coquimbo and Llanquihue, and the heavily-forested rainy region south of lat. 41° S. The desert region is an elevated arid plateau descending gradually from the Andes towards the coast, where it breaks down abruptly from elevations of 800 to 1500 ft. From the sea this plateau escarpment has the appearance of a range of flat topped hills closely following the coast line. The surface is made up of extensive plains covered with sand and deposits of alkaline salts, broken by ranges of barren hills having the appearance of spurs from the Andes, and by irregular lateral ranges in the vicinity of the main cordillera enclosing elevated saline plateaus. This region is rainless, barren and inhospitable, absolutely destitute of vegetation except in some small river valleys where irrigation is possible, and on the slopes of some of the snow-covered peaks where the water from the melting snows nourishes a scanty and coarse vegetation before it disappears in the thirsty sands. It is very rich in mineral and saline deposits, however. The eastern parts of this region lie within the higher ranges of the Andes and include a large district awarded to Chile in 1899 (see Argentina and Atacama). This arid, bleak area is apparently a continuation southward of the great Bolivian altaplanicie, and is known as the Puna de Atacama. Its average elevation is estimated at 11,000 to 12,000 ft. A line of volcanoes crosses it from north to south, and extensive lava beds cover a considerable part of its surface. Large shallow saline lakes are also characteristic features of this region. From 28° S. the spurs from the cordillera toward the coast are more sharply defined and enclose deeper valleys, where the cultivation of the soil becomes possible, at first through irrigation and then with the aid of light periodical rains. The slopes of the Andes are precipitous, the general surface is rough, and in the north the higher ground and coast are still barren. Beginning with the province of Aconcagua the coast elevations crystallize into a range of mountains, the Cordillera Maritima, which follows the shore line south to the province of Llanquihue, and is continued still farther south by the mountain range of Chiloé and the islands of the western coast, which are the peaks of a submerged mountain chain. Lying between this coast range and the Andes is a broad valley, or plain, extending from the Aconcagua river south to the Gulf of Ancud, a distance slightly over 620 m. with an average width of about 60 m. It is sometimes called the “Vale of Chile,” and is the richest and most thickly-populated part of the republic. It is a highly fertile region, is well watered by numerous streams from the Andes, has a moderate rainfall, and forms an agricultural and grazing region of great productiveness. It slopes toward the south, and its lower levels are filled with lakes and with depressions where lakes formerly existed. It is an alluvial plain for the greater part, but contains some sandy tracts, as in Ñuble and Arauco; in the north very little natural forest is found except in the valleys and on the slopes of the enclosing mountain ranges, but in the south, where the rainfall is heavier, the plain is well covered with forest. South of 41° S. the country is mountainous, heavily-forested and inhospitable. There are only a few scattered settlements within its borders, and a few nomadic tribes of savages eke out a miserable existence on the coast. The deeply-indented coast line is filled with islands which preserve the general outline of the continent southward to the Fuegian archipelago, the outside groups forming a continuation of the Cordillera Maritima. The heavy and continuous rainfall throughout this region, especially in the latitude of Chiloé, gives rise to a large number of rivers and lakes. Farther south this excessive precipitation is in the form of snow in the Cordilleras, forming glaciers at a comparatively low level which in places discharge into the inlets and bays of the sea. The extreme southern part of this region extends eastward to the Atlantic entrance to the Straits of Magellan, and includes the greater part of the large island of Tierra del Fuego with all the islands lying south and west of it. There are some comparatively level stretches of country immediately north of the Straits, partly forested and partly grassy plains, where sheep farming has been established with some degree of success, but the greater part of this extreme southern territory is mountainous, cold, wet and inhospitable. The perpetual snow-line here descends to 3500 to 4000 ft. above sea-level, and the forest growth does not rise above an altitude of 1000 to 1500 ft.

It has been officially estimated that the arable lands of Chile comprise about twenty-five millions of acres (slightly over 39,000 sq. m.), or very nearly one-eighth of its total area. Mountains. The desert regions of the north include comparatively large areas of plains and gently sloping surfaces, traversed by ranges of barren hills. The remainder of the republic, probably more than three-fifths of its surface, is extremely mountainous. The western slopes of the Andes, with its spurs and lateral ranges, cover a broad zone on the eastern side of the republic, and the Cordillera Maritima covers another broad zone on its western side from about lat. 33° to the southern extremity of Chiloé, or below lat. 43°. This maritime range is traversed by several river valleys, some of which, like the Bio-Bio, are broad and have so gentle a slope as to be navigable. The Andes, however, present an unbroken barrier on the east, except at a few points in the south where the general elevation is not over 5000 to 6000 ft., and where some of the Chilean rivers, as the Palena and Las Heras, have their sources on its eastern side. From the 52nd to about the 31st parallel this great mountain system, known locally as the Cordillera de los Andes, apparently consists of a single chain, though in reality it includes short lateral ranges at several points; continuing northward several parallel ranges appear on the Argentine side and one on the Chilean side which are ultimately merged in the great Bolivian plateau. The Chilean lateral range, which extends from the 29th to the 19th parallels, traverses an elevated desert region and possesses several noteworthy peaks, among which are Cerro Bolson, 16,017 ft., and Cerro Dona Ines, 16,706 ft. It is broken to some extent in crossing the province of Antofagasta, the southern division being known as the Sierra de Huatacondo. At the southern frontier of Bolivia the main chain, which has served as the boundary line between Argentina and Chile, divides into two great ranges, the principal one continuing almost due north along the eastern side of the great Bolivian alta-planicie, and the other forming its western rim, where it is known as the Cordillera Silillica, and then following the trend of the coast north-westward into Peru becomes the Cordillera Occidental. The western slopes of the Andes are precipitous, with short spurs enclosing deep valleys. The whole system is volcanic, and a considerable number of volcanoes are still intermittently active, noticeably in central and southern Chile. The culminating point of the Chilean Andes is Aconcagua, which rises to a height of 23,097 ft.

In southern Chile the coast is highly mountainous, but the relation of these elevations to the Andes has not been clearly determined. The highest of these apparently detached groups are Mt. Macá (lat. 45° S.), 9711 ft., and Mt. Arenales (about 47° S. lat.), 11,286 ft. Cathedral Peak on Wellington Island rises to a height of 3838 ft. and the highest point on Taytao peninsula to 3937 ft. The coast range of central Chile has no noteworthy elevations, the culminating point in the province of Santiago being 7316 ft. Between central Chile and the northern desert region there is a highly mountainous district where distinct ranges or elongated spurs cross the republic from the Andes to the coast, forming transverse valleys of great beauty and fertility. The most famous of these is the “Vale of Quillota” between Valparaiso and Santiago. The Chilean Andes between Tacna and Valdivia are crossed by 24 passes, the majority of them at elevations exceeding 10,000 ft. The best-known of these is the Uspallata pass between Santiago and the Argentine city of Mendoza, 12,870 ft. above sea-level. The passes of central and southern Chile are used only in the summer season, but those of northern Chile are open throughout the whole year.

The volcanic origin of the Andes and their comparatively recent elevation still subject Chile, in common with other parts of the western coast region, to frequent volcanic and seismic disturbances. In some instances since European occupation, violent earthquake shocks have resulted in considerable elevations of certain parts of the coast. After the great earthquake of 1835 Captain Robert FitzRoy (1805-1865) of H.M.S. “Beagle” found putrid mussel-shells still adhering to the rocks 10 ft. above high water on the island of Santa Maria, 30 m. from Concepción, and Charles Darwin declares, in describing that disaster, that “there can be no doubt that the land round the bay of Concepción was upraised two or three feet.” These upheavals, however, are not always permanent, the upraised land sometimes settling back to its former position. This happened on the island of Santa Maria after 1835. The existence of sea-shells at elevations of 350 to 1300 ft. in other parts of the republic shows that these forces, supplemented by a gradual uplifting of the coast, have been in operation through long periods of time and that the greater part of central and southern Chile has been raised from the sea in this way. These earthquake shocks have two distinct characteristics, a slight vibration, sometimes almost imperceptible, called a temblor, generally occurring at frequent intervals, and a violent horizontal or rotary vibration, or motion, also repeated at frequent intervals, called a terremoto, which is caused by a fracture or displacement of the earth’s strata at some particular point, and often results in considerable damage. When the earthquake occurs on the coast, or beneath the sea in its vicinity, tidal waves are sometimes formed, which cause even greater damage than the earthquake itself. Arica has been three times destroyed by tidal waves, and other small towns of the north Chilean coast have suffered similar disasters. Coquimbo was swept by a tidal wave in 1849, and Concepción and Talcahuano were similarly destroyed in 1835. The great earthquake which partially destroyed Valparaiso in 1906, however, was not followed by a tidal wave. These violent shocks are usually limited to comparatively small districts, though the vibrations may be felt at long distances from the centre of disturbance. In this respect Chile may be divided into at least four great earthquake areas, two in the desert region, the third enclosing Valparaiso, and the fourth extending from Concepción to Chiloé. A study of Chilean earthquake phenomena, however, would probably lead to a division of southern Chile into two or more distinct earthquake areas.

The coast of Chile is fringed with an extraordinary number of islands extending from Chiloé S. to Cape Horn, the grouping of which shows that they are in part the summits of a submerged Coast. mountain chain, a continuation southward of the Cordillera Maritima. Three groups of these islands, called the Chiloé, Guaytecas and Chonos archipelagoes, lie N. of the Taytao peninsula (lat. 45° 50′ to 46° 55′ S.), and with the mainland to the E. form the province of Chiloé. The largest of these is the island of Chiloé, which is inhabited. Some of the smaller islands of these groups are also inhabited, though the excessive rainfall of these latitudes and the violent westerly storms render them highly unfavourable for human occupation. Some of the smallest islands are barren rocks, but the majority of them are covered with forests. These archipelagoes are separated from the mainland in the north by the gulfs of Chacao (or Ancud) and Corcovado, 30 to 35 m. wide, which appear to be a submerged part of the great central valley of Chile, and farther south by the narrower Moraleda channel, which terminates southward in a confusing network of passages between the mainland and the islands of the Chonos group. One of the narrow parts of the Chilean mainland is to be found opposite the upper islands of this group, where the accidental juxtaposition of Magdalena island, which indents the continent over half a degree at this point, and the basin of Lake Fontana, which gives the Argentine boundary a sharp wedge-shaped projection westward, narrows the distance between the two to about 26 m. The Taytao peninsula, incorrectly called the Tres Montes on some maps, is a westward projection of the mainland, with which it is connected by the narrow isthmus of Ofqui, over which the natives and early missionaries were accustomed to carry their boats between the Moraleda Channel and Gulf of Peñas. A short ship canal here would give an uninterrupted and protected inside passage from Chacao Channel all the way to the Straits of Magellan, a distance of over 760 m. A southern incurving projection of the outer shore-line of this peninsula is known as Tres Montes peninsula, the most southern point of which is a cape of the same name. Below the Taytao peninsula is the broad open Gulf of Peñas, which carries the coast-line eastward fully 100 m. and is noticeably free from islands. The northern entrance to Messier Channel is through this gulf. Messier, Pitt, Sarmiento and Smyth’s Channels, which form a comparatively safe and remarkably picturesque inside route for small steamers, about 338 m. in length, separate another series of archipelagoes from the mainland. These channels are in places narrow and tortuous. Among the islands which thickly fringe this part of the coast, the largest are Azopardo (lying within Baker Inlet), Prince Henry, Campaña, Little Wellington, Great Wellington and Mornington (of the Wellington archipelago), Madre de Dios, Duke of York, Chatham, Hanover, Cambridge, Contreras, Rennell and the Queen Adelaide group of small barren rocks and islands lying immediately north of the Pacific entrance to the Straits of Magellan. The large number of English names on this coast is due to the fact that the earliest detailed survey of this region was made by English naval officers; the charts prepared from their surveys are still in use and form the basis of all subsequent maps. None of these islands is inhabited, although some of them are of large size, the largest (Great Wellington) being about 100 m. long. It has likewise been determined, since the boundary dispute with Argentina called attention to these territories and led to their careful exploration at the points in dispute, that Skyring Water, in lat. 53° S., opens westward into the Gulf of Xaultegua, which transforms Ponsonby Land and Cordoba (or Croker) peninsula into an island, to which the name of Riesco has been given. The existence of such a channel was considered probable when these inland waters were first explored in 1829 by Captain FitzRoy, but it was not discovered and surveyed until three-quarters of a century had elapsed. Belonging to the Fuegian group south of the Straits of Magellan are Desolation, Santa Ines, Clarence, Dawson, Londonderry, Hoste, Navarin and Wollaston islands, with innumerable smaller islands and rocks fringing their shores and filling the channels between them. Admirable descriptions of this inhospitable region, the farthest south of the inhabited parts of the globe, may be found in the Narrative of the Surveying Voyages of His Majesty’s Ships “Adventure” and “Beagle” between the years 1826 and 1836 (3 vols., 1839).

The western and larger part of Tierra del Fuego (q.v.) belongs to Chile. About 63 m. S.W. of Cape Horn, in lat. 56° 25′ S., is the Diego Ramirez group of small, rocky islands, the most southern possession of the republic. Its westernmost possessions are Sala-y-Gomez and Easter islands, the former in about 27° S., 105° W., and the latter, the easternmost inhabited Polynesian island, in 27° 6′ S., 109° 17′ W. Much nearer the Chilean coast (396 m.), lying between the 33rd and 34th parallels, are the three islands of the Juan Fernandez group, and rising apparently from the same submerged plateau about 500 m. farther north of the latter are the rocky islets of San Ambrosio and San Felix, all belonging to Chile. North of Chiloé there are few islands in close proximity to the coast. The more important of these are La Mocha, off the southern coast of Arauco, in lat. 38° 20′ S., which is 8 m. long and rises to an elevation of 1240 ft. above the sea; Santa Maria, 30 m. south-west of Concepcion, which partially encloses the Bay of Arauco and is well cultivated; and Quiriquina, lying off the port of Talcahuano in the entrance to Concepción bay. There are a few barren islands on the desert coast, the largest of which are between Coquimbo and Caldera. Since the removal of their guano deposits they have become practically worthless, except where they serve to shelter anchorages.

The coast of northern and central Chile is singularly deficient in good harbours. Those of the desert region are only slight indentations in a remarkably uniform coast-line, sheltered on one side by a point of land, or small island. The landings Harbours. are generally dangerous because of the surf, and the anchorages are unsafe from storms on the unprotected side. Among the most frequented of these are Valparaiso, Coquimbo, Caldera, Iquique and Arica. There are some small harbours for coasting vessels of light draught along the coast of central Chile, usually at the partially obstructed mouths of the larger rivers, as San Antonio near the mouth of the Maipó, Constitución at the mouth of the Maule, and Llico on the outlet of Lake Vichuquen, but there is no harbour of importance until Conceptión (or Talcahuano) Bay is reached. There are three harbours on this bay, El Tomé, Penco and Talcahuano (q.v.), the last being the largest and best-protected port on the inhabited part of the Chilean coast. Immediately south of this bay is the large Bay of Arauco, into which the Bio-Bio river discharges, and on which, sheltered by the island of Santa Maria, are the ports of Coronel and Lota. The next important harbour is that of El Corral, at the mouth of the Valdivia river and 15 m. below the city of Valdivia. The Bay of San Carlos on the northern coast of Chiloé, which opens upon the narrow Chacao channel, has the port of Ancud, or San Carlos, and is rated an excellent harbour for vessels of light and medium draught. Inside the island of Chiloé the large gulfs of Chacao (or Ancud) and Corcovado are well protected from the severe westerly storms of these latitudes, but they are little used because the approach through the Chacao channel is tortuous and only 2 to 3 m. wide, and the two gulfs, though over 30 m. wide and 150 m. long, are beset with small rocky islands. At the north end of the first is the Reloncavi, a large and nearly landlocked bay, on which stands Puerto Montt, the southern terminus of the Chilean central railway. The large Gulf of Peñas, south of Taytao peninsula, is open to the westerly storms of the Pacific, but it affords entrance to several natural harbours. Among these are the Gulfs of Tres Montes and San Estevan, and Tarn Bay at the entrance to Messier Channel. The next 300 m. of the Chilean coast contain numerous bays and inlets affording safe harbours, but the mainland and islands are uninhabited and the climate inhospitable. Behind Rennell Island in lat. 52° S., however, is a succession of navigable estuaries which penetrate inland nearly to the Argentine frontier. The central part of this group of estuaries is called Worsley Sound, and the last and farthest inland of its arms is Last Hope Inlet (Ultima Esperanza), on which is situated the Chilean agricultural colony of Puerto Consuelo. The Straits of Magellan, about 360 m. in length, lie wholly within Chilean territory. Midway of them is situated Punta Arenas, the most southern town and port of the republic.

Except in the extreme south the hydrography of Chile is of the simplest description, all the larger rivers having their sources in the Andes and flowing westward to the Pacific. Their courses Rivers. are necessarily short, and only a few have navigable channels, the aggregate length of which is only 705 m. Nearly all rivers in the desert region are lost in the sands long before reaching the coast. Their waterless channels are interesting, however, as evidence of a time when climatological conditions on this coast were different. The principal rivers of this region are Sama (which forms the provisional boundary line with Peru), Tacna, Camarones, Loa, Copiapó, Huasco, Elqui, Limari and Choapa. The Loa is the largest, having its sources on the slopes of the Cordillera south of the Minho volcano, between 21° and 21° 30′ S. lat., and flowing south on an elevated plateau to Chiuchiu, and thence west and north in a great curve to Quillaga, whence its dry channel turns westward again and reaches the Pacific in lat. 21° 28′ S., a few miles south of the small port of Huanillos. Its total length is estimated at 250 m. The upper courses of the river are at a considerable elevation above the sea and receive a large volume of water from the Cordilleras. The water of its upper course and tributaries is sweet, and is conducted across the desert in pipes to some of the coast towns, but in its lower course, as in all the rivers of this region, it becomes brackish. The Copiapó, which once discharged into the sea, is now practically exhausted in irrigating a small fertile valley in which stands the city of that name. The Copiapó and Huasco have comparatively short courses, but they receive a considerable volume of water from the higher sierras. The latter is also used to irrigate a small, cultivated valley. The rivers of the province of Coquimbo—the Elqui or Coquimbo, Limari and Choapa—exist under less arid conditions, and like those of the province of Aconcagua—the Ligua and Aconcagua—are used to irrigate a much larger area of cultivated territory. The central agricultural provinces are traversed by several important rivers, all of them rising on the western slopes of the snow-clad Andes and breaking through the lower coast range to the Pacific after being extensively used to irrigate the great central valley of Chile. These are the Maipó (Maypó or Maipú), Rapel, Mataquito, Maule, Itata, Bio-Bio, Imperial, Tolten, Valdivia or Calle-Calle, Bueno and Maullin. With the exception of the first three, these rivers have short navigable channels, but they are open only to vessels of light draught because of sand-bars at their mouths. The largest is the Bio-Bio, which has a total length of 220 m., 100 of which are navigable. These rivers have been of great service in the agricultural development of this part of Chile, affording means of transportation where railways and highways were entirely lacking. Some of the larger tributaries of these rivers, whose economic value has been equally great, are the Mapocho, which flows through Santiago and enters the Maipó from the north; the turbulent Cachapoal, which joins the Rapel from the north; the Claro, which waters an extensive part of the province of Talca and enters the Maule from the north; the Ñuble, which rises in the higher Andes north of the peaks of Chillan and flows entirely across the province of Ñuble to join the Itata on its western frontier; the Laja, which rises in a lake of the same name near the Argentine frontier in about lat. 35° 30′ S. and flows almost due west to the Bio-Bio; and the Cautin, which rises in the north-east corner of Cautin and after a tortuous course westward nearly across that province forms the principal confluent of the Imperial. The unsettled southern regions of Chiloé (mainland) and Magallanes are traversed by a number of important rivers which have been only partially explored. They have their sources in the Andes, some of them on the eastern side of the line of highest summits. The Puelo has its origin in a lake of the same name in Argentine territory, and flows north-west through the Cordilleras into an estuary (Reloncavi Inlet) of the Gulf of Reloncavi at the northern end of the Gulf of Chacao. Its lower course is impeded in such a manner as to form three small lakes, called Superior, Inferior and Taguatagua. A large northern tributary of the Puelo, the Manso, has its sources in Lake Mascardi and other lakes and streams south-east of the Cerro Tronador, also in Argentina, and flows south-west through the Cordilleras to unite with the Puelo a few miles west of the 72nd meridian. The Reloncavi Inlet also receives the outflow of Lake Todos los Santos through a short tortuous stream called the Petrohue. The Comau Inlet and river form the boundary line between the provinces of Llanquihue and Chiloé, and traverse a densely wooded country in a north-westerly direction from the Andes to the north-eastern shore of the Gulf of Chacao. Continuing southward, the Yelcho is the next important river to traverse this region. It drains a large area of Argentine territory, where it is called the Rio Fetaleufu or Fetalauquen, its principal source being a large lake of the same name. It flows south-west through the Andes, and then north-west through Lake Yelcho to the Gulf of Corcovado. The Argentine colony of the 16th of October, settled principally by Welshmen from Chubut, is located on some of the upper tributaries of this river, in about lat. 43° S. The Palena is another river of the same character, having its source in a large frontier lake called General Paz and flowing for some distance through Argentine territory before crossing into Chile. It receives one large tributary from the south, the Roo Pico, and enters an estuary of the Gulf of Corcovado a little north of the 44th parallel. The Frias is wholly a Chilean river, draining an extensive Andean region between the 44th and 45th parallels and discharging into the Puyuguapi channel, which separates Magdalena island from the mainland. The Aisen also has its source in Argentine territory near the 46th parallel, and drains a mountainous region as far north as the 45th parallel, receiving numerous tributaries, and discharging a large volume of water into the Moraleda channel in about lat. 45° 20′ S. The lower course of this river is essentially an inlet, and is navigable for a short distance. The next large river is the Las Heras, or Baker, through which the waters of Lakes Buenos Aires and Pueyrredon, or Cochrane, find their way to the Pacific. Both of these large lakes are crossed by the boundary line. The Las Heras discharges into Martinez Inlet, the northern part of a large estuary called Baker or Calen Inlet which penetrates the mainland about 75 m. and opens into Tarn Bay at the south-east corner of the Gulf of Peñas. Azopardo (or Merino Jarpa) island lies wholly within this great estuary, while at its mouth lies a group of smaller islands, called Baker Islands, which separate it from Messier Channel. The course of the Las Heras from Lake Buenos Aires is south and south-west, the short range of mountains in which are found the Cerros San Valentin and Arenales forcing it southward for an outlet. Baker Inlet also receives the waters of still another large Argentine-Chilean lake, San Martin, whose far-reaching fjord-like arms extend from lat. 49° 10′ to 48° 20′ S.; its north-west arm drains into the Tero, or La Pascua, river. Lake San Martin lies in a crooked deeply cut passage through the Andes, and the divide between its southern extremity (Laguna Tar) and Lake Viedma, which discharges through the Santa Cruz river into the Atlantic, is so slight as to warrant the hypothesis that this was once a strait between the two oceans. After a short north-westerly course the Toro discharges into Baker Inlet in lat. 48° 15′ S., long. 73° 24′ W. South of the Toro there are no large rivers on this coast, but the narrow fjords penetrate deeply into the mountains and bring away the drainage of their snow-capped, storm-swept elevations. A peculiar network of fjords and connecting channels terminating inland in a peculiarly shaped body of water with long, widely branching arms, called Worsley Sound, Obstruction Sound and Last Hope Inlet, covers an extensive area between the 51st and 53rd parallels, and extends nearly to the Argentine frontier. It has the characteristics of a tidewater river and drains an extensive region. The sources of the Argentine river Coile are to be found among the lakes and streams of this same region, within Chilean territory. A noteworthy peculiarity of southern Chile, from the Taytao peninsula (about 46° 50′ S. lat.) to Tierra del Fuego, is the large number of glaciers formed on the western and southern slopes of the Cordilleras and other high elevations, which discharge direct into these deeply cut estuaries. Some of the larger lakes of the Andes have glaciers discharging into them. The formation of these icy streams at comparatively low levels, with their discharge direct into tidewater estuaries, is a phenomenon not to be found elsewhere in the same latitudes.

The lakes of Chile are numerous and important, but they are found chiefly in the southern half of the republic. In the north the only lakes are large lagoons, or morasses, on the upper Lakes. saline plateaus between the 23rd and 28th parallels. They are fed from the melting snows and periodical storms of the higher Andes, and most of them are completely dry part of the year. Their waters are saturated with saline compounds, which in some cases have considerable commercial value. In central Chile above the Bio-Bio river the lakes are small and have no special geographical interest, with the exception perhaps of the Laguna del Maule, in 36° 7′ S., and Laguna de la Laja, in 37° 20′, which lie in the Andes near the Argentine frontier and are sources of the two rivers of the same names. Below the Bio-Bio river there is a line of large picturesque lakes extending from the province of Cautin, south through that of Llanquihue, corresponding in character and position to the dry lacustrine depressions extending northward in the same valley. They lie on the eastern side near the Cordilleras, and serve the purpose of great reservoirs for the excessive precipitation of rain and snow on their western slopes. With one exception they all drain westward into the Pacific through short and partly navigable rivers, and some of the lakes are also utilized for steamship navigation. These lakes are Villarica on the southern frontier of Cautin, Rinihue and Ranco in Valdivia, and Puyehue, Rupanco, Llanquihue and Todos los Santos in Llanquihue. The largest of the number are Lakes Ranco and Llanquihue, the former with an estimated area of 200 sq. m. and the latter of 300 sq. m. Lake Todos los Santos is situated well within the Andean foothills north-east of Puerto Montt and at an elevation of 509 ft., considerably above that of the other lakes, Lake Ranco being 230 ft. above sea-level. The great Andean lakes of General Paz (near the 44th parallel), Buenos Aires (in lat. 46° 30′ S.), Pueyrredon, or Cpchrane (47° 15′ S.) and San Martin (49° S.), lie partly within Chilean territory. In the extreme south are Lagoa Blanca, a large fresh-water lake in lat. 52° 30′ S., and two large inland salt-water sounds, or lagoons, called Otway Water and Skyring Water, connected by FitzRoy Passage.

Geology.—Chile may be divided longitudinally into two regions which differ from each other in their geological structure. Along the coast lies a belt of granite and schist overlaid unconformably by Cretaceous and Tertiary deposits; inland the mountains are formed chiefly of folded Mesozoic beds, together with volcanic rocks of later date. The great longitudinal valley of Chile runs approximately, but only approximately, along the boundary between the two zones. Towards the north the coastal zone disappears beneath the sea and the Andean zone reaches to the shore. The ancient rocks which form the most characteristic feature of the former do indeed occur upon the coast of Peru, but in the north of Chile they are found only in isolated masses standing close to the shore or, as at Mejillones, projecting into the sea. South of Antofagasta the old rocks form a nearly continuous band along the coast, extending as far as Cape Horn and Staten Island, and occupying the greater part of the islands of southern Chile. Lithologically they are crystalline schists, together with granite, diorite, gabbro and other igneous rocks. They are known to be pre-Jurassic, but whether they are Palaeozoic or Archaean is uncertain. They are strongly folded and are overlaid unconformably by Cretaceous and Tertiary deposits. In the north both the Cretaceous and Tertiary beds of this zone are limited in extent, but towards the south Mesozoic beds, which are at least in part Cretaceous, form a band of considerable width. The Tertiary beds include both marine and terrestrial deposits, and appear to be chiefly of Miocene and Pliocene age. The whole of the north part of Tierra del Fuego is occupied by plateaus of horizontal Tertiary strata.

The Chilean Andes correspond with the Western Cordillera of Bolivia and Peru, and consist almost entirely of Jurassic and Cretaceous beds, together with the products of the Tertiary eruptions. The Mesozoic beds are thrown into a series of parallel folds which run in the direction of the chain and which are generally free from any complications such as overthrusting or overfolding. The Cretaceous beds form a synclinal upon the eastern side of the chain (and, in general, beyond the Chilean boundary), while the Jurassic beds are thrown into a number of folds which form the axis and the western flank. Through the Mesozoic beds are intruded granitic and other igneous rocks of Tertiary age, and upon the folded Mesozoic foundation rise the volcanic cones of Tertiary and later date. The Trias is known only at La Ternera near Copiapó, where coal-seams with Rhaetic plants have been found; but the rest of the Mesozoic series, from the Lias to the Upper Cretaceous, appears to be represented without a break of more than local importance. The deposits are marine, consisting mainly of sandstone and limestone, together with tuffs and conglomerates of porphyry and porphyrite. These porphyritic rocks form a characteristic feature of the southern Andes, and were at one time supposed to be metamorphic; but they are certainly volcanic, and as they contain marine fossils they must have been laid down beneath the sea. They are not confined to any one horizon, but occur irregularly throughout the Jurassic and occasionally also amongst the Cretaceous strata. They form, in fact, a special facies which may frequently be traced laterally into the more normal marine deposit of the same age. The fauna of the Mesozoic beds is very rich, and includes forms which are found in northern Europe, others which occur in central Europe, and others again which are characteristic of the Mediterranean region. It lends no support to Neumayr’s theory of climatic zones. A large part of the chain is covered by the products of the great volcanoes which still form the highest summits of the Chilean and Argentine Andes. The rocks are liparites, dacites, hornblende and pyroxene andesites. The recent lavas of the still active volcanoes of the south are olivine-bearing hypersthene-andesite and basalt.1

Climate.—The climate of Chile varies widely, from the tropical heat and extreme arid conditions of the northern coast to the low temperatures and extreme humidity of western Tierra del Fuego and the southern coast. The high altitudes of the Andean region also introduce vertical zones of temperature, modified to some extent by the rainless plateaus of the north, and by the excessive rainfall of the south. In general terms it may be said that the extremes of temperature are not so great as in corresponding latitudes of the northern hemisphere, because of the greater expanse of water in comparison with the land areas, the summers being cooler and the winters warmer. The cold antarctic, or Humboldt, current sweeps northward along the coast and greatly modifies the heat of the arid, tropical plateaus. The climate of northern and central Chile is profoundly affected by the high mountain barrier on the eastern frontier and by the broad treeless pampas of Argentina, which raise the easterly moisture-laden winds from the Atlantic to so high an elevation that they sweep across Chile without leaving a drop of rain. At very rare intervals light rains fall in the desert regions north of Coquimbo, but these are brought by the prevailing coast winds. With this exception these regions are the most arid on the face of the globe, highly heated by a tropical sun during the day and chilled at night by the proximity of snow-covered heights and a cold ocean current. Going south the temperature slowly falls and the rainfall gradually increases, the year being divided into a short rainy season and a long, dry, cloudless season. At Copiapó, in 27° 22′ S., 1300 ft. above the sea, the mean annual temperature is 60° and the rainfall about 1 in., but at Coquimbo, in 29° 56′ S., the temperature is 59.2° and the rainfall 1½ in. At Santiago, in 33° 27′ S., 1755 ft. above the sea, the mean temperature is 54° and the annual rainfall 16½ in., though the latter varies considerably. The number of rainy days in the year averages about 21. At Talca, in 35° 36′ S. and 334 ft. above sea-level, the mean annual temperature is nearly one degree above that of Santiago, but the rainfall has increased to 19.7 in. The long dry season of this region makes irrigation necessary, and vegetation has something of a subtropical appearance, palms growing naturally as far south as 37°. The climate is healthy and agreeable, though the death-rate among the common people is abnormally high on account of personal habits and unsanitary surroundings. In southern Chile the climate undergoes a radical change—the prevailing winds becoming westerly, causing a long rainy season with a phenomenal rainfall. The plains as well as the western slopes of the Andes are covered with forest, the rivers become torrents, and the sky is covered with heavy clouds a great part of the year. At Valdivia, in 39° 49′ S. and near the sea-level, the mean annual temperature is 52.9° and the annual rainfall 108 to 115 in., with about 150 rainy days in the year. These meteorological conditions are still more accentuated at Ancud, at the north end of the island of Chiloé, in 41° 46′ S., where the mean annual temperature is 50.7° and the annual rainfall 134 in. The equable character of the climate at this point is shown by the limited range between its summer and winter temperatures, the mean for January being 56.5° and the mean for July 45.9°. The almost continual cloudiness is undoubtedly a principal cause, not only of the low summer temperatures, but also of the comparatively high winter temperatures. Frosts are infrequent, and snow does not lie long. The climate is considered to be healthful notwithstanding the excessive humidity. The 600 m. of coast from the Chonos Archipelago south to the Fuegian islands have a climate closely approximating that of the latter. It is wet and stormy all the year through, though the rainfall is much less than that of Ancud and Valdivia. The line of perpetual snow, which is 6000 ft. above sea-level between lat. 41° and 43°, descends to 3500 (to 4000) ft. in Tierra del Fuego, affording another indication of the low maximum temperatures ruling during the summer. At the extreme south, where Chilean territory extends across to the Atlantic entrance to the Straits of Magellan, a new climatic influence is encountered in the warm equatorial current flowing down the east coast of South America, which gives to eastern Tierra del Fuego a higher temperature than that of the western shore. The Andes, although much broken in these latitudes, also exert a modifying influence on these eastern districts, sheltering them from the cold westerly storms and giving them a drier climate. This accounts for the surprising meteorological data obtained from Punta Arenas, in 53° 10′ S., where the mean annual temperature is 43.2° and the annual rainfall only 22.5 in. Other observations reduce this annual precipitation to less than 16 in. According to observations made by the Swedish Antarctic Expedition (1901-1903), at Orange Bay, Hoste Island, in lat. 55° 31′ S., long. 68° 05′ W., which is more exposed to the westerly storms, the mean temperature for 11 months was 41.98° and the total precipitation (rain and snow) 53.1 in. The mean maximum temperature was 49.24°, and the mean minimum 35.83°. The observations showed 284 days with rain or snow, of which 70 were with snow.

Flora.—The indigenous flora of Chile is less extensive and less interesting than those of Argentina and Brazil, but contains many peculiar genera and species. A classification of this flora necessitates its division into at least three general zones—the desert provinces of the north, central Chile, and the humid regions of the south. The first is an arid desert absolutely barren along part of the coast, between Tacna and Copiapó, but with a coarse scanty vegetation near the Cordilleras along watercourses and on the slopes where moisture from the melting snows above percolates through the sand. In the valleys of the Copiapó and Huasco rivers a meagre vegetation is to be found near their channels, apart from what is produced by irrigation, but the surface of the plateau and the dry river channels below the sierras are completely barren. Continuing southward into the province of Coquimbo a gradual change in the arid conditions may be observed. The higher summits of the Cordilleras afford a larger and more continuous supply of water, and so dependent are the people in the cultivated river valleys on this source of water supply that they watch for snowstorms in the Cordilleras as an indication of what the coming season is to be. The arborescent growth near the mountains is larger and more vigorous, in which are to be found the “algarrobo” (Prosopis siliquastrum) and “chañar” (Gourliea chilensis), but the only shrub to be found on the coast is a species of Skytanthus. Near the sierras where irrigation is possible, fruit-growing is so successful, especially the grape and fig, that the product is considered the best in Chile. In regard to the indigenous flora of this region John Ball2 says: “The species which grow here are the more or less modified representatives of plants which at some former period existed under very different conditions of life.” Proceeding southward cacti become common, first a dwarfed species, and then a larger columnar form (Cereus quisco). The streams are fringed with willows; fruit trees and alfalfa fields fill the irrigated valleys, and the lower mountain slopes are better covered with a thorny arborescent growth. The divides between the streams, however, continue barren as far south as the transverse ranges of mountains across the province of Aconcagua.

To some degree the flora of central Chile is of a transition character between the northern and southern zones. It is much more than this, however, for it has a large number of genera and species peculiarly its own. A large majority of the 198 genera peculiar to the South American temperate regions belong exclusively to central Chile. This zone extends from about the 30th to the 36th parallel, perhaps a little farther south to include some characteristic types. The evergreens largely predominate here as well as in the extreme south, and on the open, sunburnt plains the vegetation takes on a subtropical aspect. One of the most characteristic trees of this zone is the peumo (Cryptocarya peumus), whose dense evergreen foliage is everywhere conspicuous. The quillay (Quillaja saponaria) is another characteristic evergreen tree of this region, whose bark possesses saponaceous properties. In earlier times the coquito palm (Jubaea spectabilis) was to be found throughout this part of Chile, but it has been almost completely destroyed for its saccharine sap, from which a treacle was made. One of the most striking forest trees is the pehuen or Chilean pine (Araucaria imbricata), which often grows to a height of 100 ft. and is prized by the natives for its fruit. Three indigenous species of the beech—the roble (Fagus obliqua), coyhue (F. Dombeyi), and rauli (F. procera)—are widely diffused and highly prized for their wood, especially the first, which is misleadingly called roble (oak). Most of the woods used in construction and manufactures are found between the Bio-Bio river and the Taytao peninsula, among which are the alerce (Fitzroya patagonica), ciprés or Chiloé cypress (Libocedrus tetragona), the Chilean cypress (L. Chilensis), lingue (Persea lingue), laurel (Laurus aromatica), avellano (Guevina avellana), luma (Myrtus luma), espino (Acacia cavenia) and many others. Several exotic species have been introduced into this part of Chile, some of which have thriven even better than in their native habitats. Among these are the oak, elm, beech (F. sylvatica), walnut, chestnut, poplar, willow and eucalyptus. Through the central zone the plains are open and there are forests on the mountain slopes, but in the southern zone there are no plains, with the exception of small areas near the Straits of Magellan, and the forests are universal. In the variety, size and density of their growth these forests remind one of the tropics. They are made up, in great part, of the evergreen beech (Fagus betuloides), the deciduous antarctic beech (F. antarctica),3 and Winter’s bark (Drimys Winteri), intermingled with a dense undergrowth composed of a great variety of shrubs and plants, among which are Maytenus magellanica, Arbutus rigida, Myrtus memmolaria, two or three species of Berberis, wild currant (Ribes antarctica), a trailing blackberry, tree ferns, reed-like grasses and innumerable parasites. On the eastern side of the Cordillera, in the extreme south, the climate is drier and open, and grassy plains are found, but on the western side the dripping forests extend from an altitude of 1000 to 1500 ft. down to the level of the sea. A peculiar vegetable product of this inclement region is a small globular fungus growing on the bark of the beech, which is a staple article of food among the Fuegians—probably the only instance where a fungus is the bread of a people.

It is generally conceded that the potato originated in southern Chile, as it is found growing wild in Chiloé and neighbouring islands and on the adjacent mainland. The strawberry is also indigenous to these latitudes on both sides of the Andes, and Chile is credited with a species from which the cultivated strawberry derives some of its best qualities. Maize and quinoa (Chenopodium quinoa) were known in Chile before the arrival of Europeans, but it is not certain that they are indigenous. Species of the bean and pepper plant are also indigenous, and the former is said to have been cultivated by the natives. Among the many economic plants which have been introduced into Chile and have become important additions to her resources, the more prominent are wheat, barley, hemp and alfalfa (Medicago sativa), together with the staple European fruits, such as the apple, pear, peach, nectarine, grape, fig, olive and orange. The date-palm has also been introduced into the southern provinces of the desert region. Among the marine productions on the southern coast, a species of kelp, Macrocystis pyrifera, merits special mention because of its extraordinary length, its habit of clinging to the rocks in strong currents and turbulent seas, and its being a shelter for innumerable species of marine animals. Captain FitzRoy found it growing from a depth of 270 ft.

Fauna.—The fauna of Chile is comparatively poor, both in species and individuals. A great part of the northern deserts is as barren of animal life as of vegetation, and the dense humid forests of the south shelter surprisingly few species. There are no large mammals in all this extensive region except the Cetacea and a species of the Phocidae of southern waters. Neither are there any dangerous species of Carnivora, which are represented by the timid puma (Felis concolor), three species of wildcats, three of the fox, two of Conepatus, a weasel, sea-otter and six species of seal. The rodents are the most numerously represented order, which includes the coypu or nutria (Myopotamus coypus), the chinchilla (Chinchilla laniger), the tuco-tuco (Ctenomys brasiliensis), a rabbit, and 12 species of mice—in all some 12 genera and 25 species. The coypu, sometimes called the South American beaver, inhabits the river-banks, and is highly prized for its fur. It is also found along the river-courses of Argentina. The ruminants are represented by a few species only—the guanaco (Auchenia huanaco), vicuna (A. vicugna), huemul (Cervus chilensis), which appears on the Chilean escutcheon, and the pudu deer, a small and not very numerous species. There are two species of the Edentata, Dasypus and Pichiciego, the latter very rare, and one of the opossums. European animals, such as horses, cattle, sheep, swine and goats, have been introduced into the country and do well. Sheep-raising has also been inaugurated with some degree of success in the vicinity of the Straits of Magellan. The avifauna, with the exception of waterfowl, is also limited to comparatively few species. Birds of prey are represented by the condor, vulture, two species of the carrion-hawk (Polyborus), and owl. The Chilean slopes of the Andes appear to be a favourite haunt of the condor, where neighbouring stock-raisers suffer severe losses at times from its attacks. The Insessores are represented by a number of species. Parrots are found as far south as Tierra del Fuego, where Darwin saw them feeding on seeds of the Winter’s bark. Humming-birds have a similar range on this coast, one species (Mellisuga Kingii) being quite numerous as far south as Tierra del Fuego. A characteristic genus is that of Pteroptochus, of which there are three or four species each characterized by some conspicuous peculiarity. These are P. megapodius, called El Turco by the natives, which is noticeable for its ungainly appearance and awkward gait; the P. albicollis, which inhabits barren hillsides and is called tapacollo from the manner of carrying its tail turned far forward over its back; the P. rubecula, of Chiloé, a small timid denizen of the gloomy forest, called the cheucau or chuca, whose two or three notes are believed by the superstitious natives to be auguries of impending success or disaster; and an allied species (Hylactes Tarnii, King) called the guid-guid or barking bird, whose cry is a close imitation of the yelp of a small dog. The southern coast and its inland waters are frequented by several species of petrel, among which are the Procellaria gigantea, whose strength and rapacity led the Spaniards to call it quebranta huesos (breakbones), the Puffinus cinereus, which inhabits the inland channels in large flocks, and an allied species (Puffinuria Berardii) which inhabits the inland sounds and resembles the auk in some particulars of habit and appearance. There are numerous species in these sheltered channels, inlets and sounds of geese, ducks, swans, cormorants, ibises, bitterns, red-beaks, curlew, snipe, plover and moorhens. Conspicuous among these are the great white swan (Cygnus anatoides), the black-necked swan (Anser nigricollis), the antarctic goose (Anas antarctica) and the “race-horse” or “steamer duck” (Micropterus brachypterus).

The marine fauna is less known than the others, but it is rich in species and highly interesting in its varied forms and characteristics. The northern coast has no sheltered waters of any considerable extent, and the shore slopes abruptly to a great depth, which gives it a marine life of no special importance. In the shoal waters about Juan Fernandez are found a species of codfish (possibly Gadus macrocephalus), differing in some particulars from the Newfoundland cod, and a large crayfish, both of which are caught for the Valparaiso market. The sheltered waters of the broken southern coast, however, are rich in fish and molluscs, especially in mussels, limpets and barnacles, which are the principal food resource of the nomadic Indian tribes of those regions. A large species of barnacle, Balanus psittacus, is found in great abundance from Concepción to Puerto Montt, and is not only eaten by the natives, by whom it is called pico, but is also esteemed a great delicacy in the markets of Valparaiso and Santiago. Oysters of excellent flavour are found in the sheltered waters of Chiloé. The Cetacea, which frequent these southern waters, are represented by four species—two dolphins and the sperm and right whale—and the Phocidae by six species, one of which (Phoca lupina) differs but little from the common seal. Another species (Macrorhinus leoninus), popularly known as the sea-elephant, is provided with short tusks and a short trunk and sometimes grows to a length of 20 ft. Still another species, the sea-lion (Otaria jubata), furnishes the natives of Tierra del Fuego with an acceptable article of food, but like the Phoca lupina it is becoming scarce.

Of Reptilia Chile is singularly free, there being recorded only eleven species—five saurians, four ophidians, one frog and one toad—but a more thorough survey of the uninhabited territories of the south may increase this list. There are no alligators in the streams, and the tropical north has very few lizards. There are no poisonous snakes in the country, and, in a region so filled with lakes and rivers as the rainy south, only two species of batrachians. The insect life of these strangely associated regions is likewise greatly restricted by adverse climatic conditions, a considerable part of the northern desert being absolutely barren of animal and vegetable life, while the climate of Tierra del Fuego and the southern coast is highly unfavourable to terrestrial animal life, for which reason comparatively few species are to be found. Writing of a journey inland from Iquique, Charles Darwin says (Journal of Researches, &c., p. 444): “Excepting the Vultur aura, ... I saw neither bird, quadruped, reptile, nor insect.” Of his entomological collection in Tierra del Fuego, which was not large, the majority were of Alpine species. Moreover, he did not find a single species common to that island and Patagonia. These conditions subsist with but few modifications, if any, from the Straits northward to the 42nd parallel, the extreme humidity, abnormal rainfall and dark skies being unfavourable to the development of insect life, while the Andes interpose an impassable barrier to migration from the countries of the eastern coast. The only venomous species to be found in central Chile is that of a spider which frequents the wheat fields in harvest time.

Divisions and Towns.—Chile contains 23 provinces and one territory, which are subdivided into 75 departments, 855 subdelegations and 3068 districts. The territory north of the Bio-Bio was originally divided into 13 provinces, besides which the Spaniards held Chiloé, Juan Fernandez and Valdivia, the latter being merely a military outpost. During the years which have elapsed since the War of Independence the territory south of the Bio-Bio has been effectively occupied and divided into six provinces, Chiloé and the neighbouring islands and mainland to the east became a province, and four provinces in the northern deserts were acquired from Bolivia and Peru. In addition to this, Chile claimed Patagonia and the adjacent islands, and has finally secured not only the forested strip of territory west of the Andes, but also a large piece of the Patagonian mainland, south of lat. 52° S., the larger part of Tierra del Fuego, and all the western islands. This extensive region, comprising an area of 71,127 sq. m., has been provisionally organized as the territory of Magallanes. For a list of provinces, their areas, reduced from official returns, their populations, and the names and populations of their capitals, see the bottom of this page.

In addition to the provincial capitals there are few towns of importance. Among these may be mentioned:—

The population is not concentrated in large cities, but is well distributed through the cultivated parts of the country. The large number of small towns, important as ports, market towns, or manufacturing centres, is a natural result. Many of the foregoing towns are only villages in size, but their importance is not to be measured in this way. Arica is one of the oldest ports on the coast, and has long been a favoured port for Bolivian trade because the passes through the Cordilleras at that point are not so difficult. Moreover, the railway from Arica to La Paz will still further add to its importance, though it may not greatly increase its population. Another illustration is that of Vichuquen, province of Curicó, situated on a tide-water lake on the coast, which is the centre of a large salt-making industry. Still another instance is that of Castro, the oldest settlement and former capital of Chiloé, which after a century of decay is increasing again through the efforts to develop the industries of that island.

Communications.—Railway construction in Chile dates from 1850, when work was begun on a short line between Copiapó and the port of Caldera, in the Atacama desert region. Since then lines have been built by private companies from the coast at several points to inland mining centres. One of these, running from Antofagasta to the Caracoles district, was afterwards extended to Oruro, Bolivia, and has become a commercial route of international importance, with a total length of 574 m., 224 of which are in Chile. It should be remembered that many of these railway enterprises of the desert region originated at a time when the territory belonged to Bolivia and Peru. The first railway to be constructed in central Chile was the government line from Valparaiso to Santiago, 115 m. in length, which was opened to traffic in 1863. About the same time the government began the construction of a longitudinal trunk line running southward from Santiago midway between the Andes and the Coast range, and connecting with all the provincial capitals and prominent ports. This is the only railway “system” it is possible for Chile to have. The civil war of 1891 called attention to the need of a similar inland route through the northern provinces. A branch of the Valparaiso and Santiago line runs to Los Andes, and its extension across the Andes connects with the Argentine lines from Buenos Aires to Mendoza and the Chilean frontier—all sections together forming a transcontinental route about 850 m. in length. The Transandine section of this route crosses the Cordillera through the Uspallata pass. A further Transandine scheme provides for a line through the Pino Hachado pass (38° 30′ to 39° S.), and the Argentine Great Southern Company obtained a concession in 1909 to extend its Neuquen line to the frontier of Chile. The railways of the republic had a total mileage at the end of 1906 of 2950 m., of which 1495 m. were owned by the state, and 1455 m. belonged to private companies. The private lines are located in the northern provinces and are for the most part built and maintained for the transportation of mining products and supplies.

In addition to her railway lines Chile has about 21,000 m. of public roads of all descriptions, 135 m. of tramways, and 705 m. of navigable river channels, besides a very considerable mileage of lake and coast navigation. Telegraphic communication between all the important towns of the republic, initiated in 1855 with a line between Santiago and Valparaiso, is maintained by the state, which in 1903 owned 9306 m. of line in a total of 11,080 m. Cable communication with Europe by way of Buenos Aires was opened in 1875, and is now maintained by means of two underground cables across the Andes, 32 m. in length. A West Coast cable also connects with Europe and North American states by way of Panama. There were 15,853 m. of telephone wires in the republic in 1906, all the principal cities having an admirable service. Modern postal facilities date from 1853. The Chilean post-office is administered by a director-general at Santiago, and has a high degree of efficiency and liberality, compared with those of other South American states. The postal rates are low, and newspapers and other periodical publications circulate free, as a means of popular instruction. The postal revenues for 1904 amounted to 2,775,730 pesos and the expenditures to 2,407,753 pesos. Chile is a member of the International Postal Union, and has arrangements with the principal commercial nations for the exchange of postal money values.

The sea has been the only means of communication with distant parts of the country, and must continue to be the chief transportation route. There are said to be 56 ports on the Chilean coast, of which only 12 are prominent in foreign trade. Many of the so-called ports are only landing-places on an open coast, others are on shallow bays and obstructed river-mouths, and some are little-known harbours among the channels and islands of the south. The prosperity of Chile is intimately connected with her ocean-going trade, and no elaborate system of national railway lines and domestic manufactures can ever change this relationship. These conditions should have developed a large merchant marine, but the Chileans are not traders and are sailors only in a military sense. In 1905 their ocean-going merchant marine consisted of only 148 vessels, of which 54 were steamers of 42,873 tons net, and 94 were sailing vessels of 39,346 tons. Nineteen of the 54 steamers belonged to a subsidized national line whose West Coast service once extended to San Francisco, California, and a large part of the others belongs to a Lota coal-mining and copper-smelting company which employs them in carrying coal to the northern ports and bringing back metallic ores for smelting. The navigable rivers and inland lakes employ a number of small steamers. The foreign commerce of the republic is carried chiefly by foreign vessels, and the coasting trade is also open to them. Three or four foreign companies maintain a regular steamship service to Valparaiso and other Chilean ports. The shipping entries at all Chilean ports during the year 1904, both national and foreign, numbered 11,756, aggregating 17,723,138 tons, and the clearances 11,689, aggregating 17,370,763 tons. Very nearly one-half this tonnage was British, a little over 18% German, and about 29% Chilean.

Commerce.—In the aggregate, the commerce of Chile is large and important; in proportion to population it is exceeded among South American states only by Argentina, Uruguay and the Guianas. Unlike those states, it depends in great part on mining and its allied occupations. The values of imports and exports (including bullion, specie and re-exports) in pesos of 18d. during the five years 1901- 1905 were as follows:—

The principal imports comprise live animals, fish, coffee, maté (Ilex paraguayensis), tea, sugar, wood and its manufactures, structural iron and steel, hardware and machinery, railway and telegraph supplies, lime and cement, glass and earthenware, cotton, woollen and silk manufactures, coal, petroleum, paints, &c. Import duties are imposed at the rates of 60, 35, 15, 5 and 25%, and certain classes of merchandise are admitted free. The higher rates are designed chiefly to protect national industries, while wines, liquors, cigars and tobacco are admitted at the lowest rate. The 25% rate covers all articles not mentioned in the schedules, which number 2260 items. The duty free list includes raw cotton, certain descriptions of live animals, agricultural machinery and implements, metal wire, fire engines, structural iron and steel, and machinery in general. The tariff is nominally ad valorem, but as the rates are imposed on fixed official valuations it is essentially specific. The duties on imports in 1905 amounted to 91,321,860 pesos, and in 1906 to 103,507,556 pesos. The principal exports are gold, silver, copper (bars, regulus and ores), cobalt and its ores, lead and its ores, vanadium ores, manganese, coal, nitrate of soda, borate of lime, iodine, sulphur, wheat and guano. Nitrate of soda forms from 70 to 75% of the exports, and the royalty received from it is the principal source of national revenue, yielding about £4,000,000 per annum. In 1904 mineral products made up fully seven-eighths of the exports, while agricultural and pastoral products did not quite reach one-eighth.

Agriculture.—According to the census returns about one-half the population of Chile lives in rural districts, and is engaged nominally in agricultural pursuits. What may be called central Chile is singularly well adapted to agriculture. The northern part of this region has a sub-tropical climate, light rainfall and a long, dry summer, but with irrigation it produces a great variety of products. Alfalfa, or lucerne (Medicago sativa), is grown extensively for shipment to the mining towns of the desert provinces. There were no less than 108,384 acres devoted to it in 1904, a considerable part of which was in the irrigated river valleys of Coquimbo and Aconcagua. Considerable attention is also given to fruit cultivation in these subtropical provinces, where the orange, lemon, fig, melon, pineapple and banana are produced with much success. Some districts, especially in Coquimbo, have gained a high reputation for the excellence of their preserved fruits. The vine is cultivated all the way from Atacama and Coquimbo, where excellent raisins are produced, south to Concepción, where some of the best wines of Chile are manufactured. In 1904 there were 93,370 acres devoted to grape production in this region, the product for that year being 30,184,704 gallons of wine and 212,366 gallons of brandy. The universal beverage of the people—chicha—is made from Indian corn. Although wheat is produced in the northern part of this region, it is grown with greater success in the south, where the rainfall is heavier and the average temperature is lower. There were 1,044,025 acres devoted to this cereal in 1903, which produced 17,910,614 bushels, or an average of 17 bushels (of 60 lb) to the acre. In 1904 the production was increased to 19,999,324 bushels, but in 1905 it fell off to 15,771,477 bushels. At one time Chile supplied Argentina and the entire West Coast as far north as California with wheat, but Argentina and California have become wheat producers and exporters, and Chile has been driven from all her old consuming markets. Great Britain is now her best customer, and Brazil takes a small quantity for milling mixtures. Chile has been badly handicapped by her crude methods of cultivation, but these are passing away and modern methods are taking their place. Formerly wheat was grown chiefly in the region of long rainless summers, and the ripened grain was thrown upon uncovered earth floors and threshed by horses driven about over the straw, but this antiquated process was not suited to the climate and enterprise of the more southern provinces, and the modern threshing-machine has been introduced. Barley is largely produced, chiefly for home consumption. Maize (Indian corn) is grown in every part of Chile except the rainy south where the grain cannot ripen, and is a principal article of food. The green maize furnishes two popular national dishes, choclos and humitas, which are eaten by both rich and poor. Potatoes also are widely cultivated, but the humid regions of the south, particularly from Valdivia to Chiloé, produce the greatest quantity. The total annual production exceeds three million bushels. The kidney bean (Phaseolus vulgaris) is another staple product in every part of the country, and is perhaps the most popular article of food among all classes of Chileans. Peas are largely cultivated south of the Maule. Walnuts have become another important product and are exported, the average annual produce being 48,000 to 50,000 bushels. The olive was introduced from Spain in colonial times and is widely distributed through the north central provinces, but its economic importance is not great. Of the European fruits introduced into the southern provinces, the apple has been the most successful. It grows with little care and yields even better than in its original home. The peach, apricot, plum, quince and cherry are also cultivated with success. Wild strawberries are found on both sides of the Andes; the cultivated varieties are unsurpassed, especially those of the province of Concepción.

The pastoral industries of Chile have been developed chiefly for the home market. The climate is admirably suited to cattle-raising, as the winters are mild and pasture is to be found throughout the whole year, but the proximity of the Argentine pampas is fatal to its profitable development. The government has been trying to promote cattle-breeding by levying duties (as high as 16 pesos a head) on cattle imported from Argentina, but with no great success. The importation, which formerly numbered about 140,000 per annum, still numbers not far from 100,000 head. There are some districts in central Chile where cattle-raising is the principal occupation, but the long dry summers limit the pasturage on the open plains and prevent the development which perhaps would otherwise result. As in Argentina, beef is generally dried in the sun to make charqui (jerked beef), in which form it is exported to the desert provinces. Horse and mule breeding are carried on to a limited extent, and since the opening of the far South more attention has been given to sheep. Goats and swine are raised in small numbers on the large estates, but in Chiloé swine-raising is one of the chief occupations of the people. Some attention has been given to the production of butter and cheese, but the industry has attained no great importance. A new industry which has made noteworthy progress, however, is that of bee-keeping, which is greatly favoured by the mild climate and the long season and abundance of flowers.

Manufactures.—The manufacturing interests of Chile have become influential enough to force a high tariff policy upon the country. They have been restricted principally to articles of necessity—food preparations, beverages, textiles and wearing apparel, leather and leatherwork, woodwork, pottery, chemicals, ironware, &c. In earlier days, when Chile had less competition in the production of wheat, flour mills were to be found everywhere in the wheat-producing provinces, and flour was one of the leading exports. Concepción, Talca, and other provincial capitals developed important milling industries, which were extended to all the chief towns of the newer provinces south of the Bio-Bio. There are over 500 large flour mills in Chile, the greater part of which are equipped with modern roller-process machinery. The development of the coal deposits in the provinces of Concepción and Arauco has made possible other industries besides those of smelting mineral ores, and numerous small manufacturing establishments have resulted, especially in Santiago, Valparaiso, Copiapó and other places where no permanent water power exists. Tanning leather is an important industry, especially in the south, some of the Chilean trees, notably the algarrobilla (Balsamocarpon brevifolium) and lingue (Persea lingue) being rich in tannin. To provide a market for the leather produced, factories have been established for the manufacture of boots and shoes, harness and saddles, and under the protection of a high tariff are doing well. Brewing and distilling have made noteworthy progress, the domestic consumption of their products being very large. The breweries are generally worked by Germans and are situated chiefly in the south, though there are large establishments in Santiago and Valparaiso. Small quantities of their products are exported. Furniture and carriage factories, cooperages, and other manufactories of wood are numerous and generally prosperous. There are likewise a large number of factories for canning and preserving fruits and vegetables. Foundries and machine shops have been established, especially for the manufacture of railway material. The sugar beet has been added to the productions of Chile, and with it the manufacture on a small scale of beet sugar. There is one large refinery at Viña del Mar, however, which imports raw cane sugar from Peru for refining. The manufacture of textiles is carried on at Santiago and El Tomé, and numerous small factories are devoted to clothing of various descriptions. The great mining industries have led to a noteworthy development in the production of chemicals, and a considerable number of factories are engaged in the production of pharmaceutical preparations, perfumeries, soaps, candles, &c.

Mining.—The most important of all the national industries, however, is that of mining. In 1903 there were 11,746 registered mines, on which mining dues were paid, the aggregate produce being valued at 178,768,170 pesos. These mines gave employment to 46,592 labourers, of whom 24,445 were employed by the nitrate companies, 13,710 in various metalliferous mines, 6437 in coal mines, and 2000 in other mines. Gold is found in nearly all the provinces from Antofagasta to Concepción, and in Llanquihue, Chiloé and Magallanes territory, but the output is not large. There are a great many placer washings, among which are some extensive deposits near the Straits of Magellan. Silver is found principally on the elevated slopes and plateaus of the Andes in the desert provinces of the north. The second most important mining industry in Chile, however, is that of copper, which is found in the provinces of Antofagasta, Atacama, Coquimbo, Aconcagua, Valparaiso, Santiago, O’Higgins, Colchagua, Curicó and Talca, but the richest deposits are in the three desert provinces. Chile was once the largest producer of copper in the world, her production in 1860-1864 being rated at 60 to 67% of the total. Low prices afterwards caused a large shrinkage in the output, but she is still classed among the principal producers. Iron mining has never been developed in Chile, although extensive deposits are said to exist. Manganese ores are mined in Atacama and Coquimbo, and their export is large. The other metals reported in the official returns are lead, cobalt and vanadium, of which only small quantities are produced. Bolivian tin is exported from Chilean ports. Among the non-metallic minerals are nitrate of soda, borate of lime, coal, salt and sulphur, together with various products derived from these minerals, such as iodine, sulphuric acid, &c. Guano is classed among the mineral products and still figures as an export, though the richest Chilean deposits were exhausted long before the war with Peru. Of non-metallic products nitrate of soda is by far the most important. Extensive deposits of the salt (called caliche in its crude, impure state) in the provinces of Tacna, Tarapacá, Antofagasta and Atacama owe their existence to the rainless character of the climate. Those of the first-named province have been discovered since the war between Chile and Peru, and have greatly extended the prospective life of the industry. The nitrate fields, which lie between 50 and 100 m. from the coast and at elevations exceeding 2000 ft. above sea-level, have been officially estimated at 89,177 hectares (344 sq. m.) and to contain 2316 millions of metric quintals (254,760,000 short tons). The first export of nitrates was in 1830, and in 1884 it reached an aggregate of 550,000 tons, and in 1905 of 1,603,140 tons. The latter figure is apparently about the production agreed upon between the Chilean government and the nitrate companies to prevent overproduction and a resulting decline in price. Nearly all the oficinas, or working plants, are owned and operated by British companies, and the railways of this desolate region are generally owned by the same companies and form a part of the working plant. Borate of lime also furnishes another important export, though a less valuable one than nitrate of soda. Extensive deposits of borax and common salt have been found in the same region, which with several other products of these saline deposits, such as iodine, add considerably to its exports. The coal deposits of Chile are found chiefly in the provinces of Concepción and Arauco, the principal mines being on the coast of the Bay of Arauco at Coronel and Lota. Coal is found also in Valdivia, on the island of Chiloé, and in the vicinity of Punta Arenas on the Straits of Magellan. Sulphur is found in the volcanic regions of the north, but the principal mines are in the provinces of Talca.

The relative magnitude and value of these mineral products may be seen in the following abstract from the official returns of 1903:—

Justice.—The judicial power consists of a Supreme Court of Justice of seven members located in the national capital, which exercises supervisory and disciplinary authority over all the law courts of the republic; six courts of appeal, in Tacna, Serena, Valparaiso, Santiago, Talca and Concepción; tribunals of first instance in the department capitals; and minor courts, or justices of the peace, in the sub-delegacies and districts. The jury system does not exist in Chile, and juries are unknown except in cases where the freedom of the press has been abused. All trials, therefore, are heard by one or more judges, and appeals may be taken from a lower to a higher court. The government is represented in each department by a public prosecutor. The police officials, who are under the direct control of the minister of interior, also exercise some degree of judicial authority. This force is essentially military in its organization, and consisted in 1901 of 500 officers, 934 non-commissioned officers and 5400 police soldiers. Small forces of local policemen are supported by various municipalities. The judges of the higher courts are appointed by the national executive, and those of the minor tribunals by the federal official governing the political division in which they are located.

Army.—For military purposes the republic is divided into five districts, the northern desert provinces forming the first, the central provinces as far south as the Bio-Bio the second and third, and the southern provinces and territory the fourth and fifth. Large sums of money have been expended in arms, equipment, guns and fortifications. The army is organized on the German model and has been trained by European officers who have been employed both for the school and regiment. Though the president and minister of war are the nominal heads of the army, its immediate direction is concentrated in a general staff comprising six service departments, at the head of which is a chief of staff. After the triumph of the revolutionists in the civil war of 1891, the army was reorganized under the direction of Colonel Emil Körner, an accomplished German officer, who subsequently served as chief of the general staff. In 1904 the permanent force consisted of 12 battalions of infantry, 6 regiments of cavalry, 4 regiments of mountain artillery, 1 regiment of horse artillery, 2 regiments of coast artillery, and 5 companies of engineers—aggregating 915 officers and 4757 men. To this nucleus were added 6160 recruits, the contingent for that year of young men twenty-one years of age compelled to serve with the colours. Under the law of the 5th of September 1900, military service is obligatory for all citizens between eighteen and forty-five years, all young men of twenty-one years being required to serve a certain period with the regular force. After this period they are transferred to the 1st reserve for 9 years, and then to the 2nd reserve. The military rifle adopted for all three branches of the service is the Mauser, 1895 model, of 7 mm. calibre, and the batteries are provided with Krupp guns of 7 and 7.5 cm. calibre. Military instruction is given in a well-organized military school at Santiago, a war academy and a school of military engineering.

Navy.—The Chilean navy is essentially British in organization and methods, and all its best fighting ships were built in British yards. In 1906 the effective fighting force consisted of 1 battle ship, 2 belted cruisers, 4 protected cruisers, 3 torpedo gunboats, 6 destroyers and 8 modern torpedo boats. In addition to these there are several inferior armed vessels of various kinds which bring the total up to 40, not including transports and other auxiliaries. The administration of the navy, under the president and minister of war and marine, is confided to a general naval staff, called the “Direccion jeneral de la Armada,” with headquarters at Valparaiso. Its duties also include the military protection of the ports, the hydrographic survey of the coast, and the lighthouse service. The personnel comprises about 465 officers, including those of the staff, and 4000 petty officers and men. There is a military port at Talcahuano, in Concepción Bay, strongly fortified, and provided with arsenal and repair shops, a large dry dock and a patent slip. The naval school, which occupies one of the noteworthy edifices of Valparaiso, is attended by 90 cadets and is noted for the thoroughness of its instruction.

Education.—Under the old conservative régime very little was done for the public school outside the larger towns. As a large proportion of the labouring classes lived in the small towns and rural communities, they received comparatively little attention. The increasing influence of more liberal ideas greatly improved the situation with reference to popular education, and the government now makes vigorous efforts to bring its public school system within the reach of all. The constitution provides that free instruction must be provided for the people. School attendance is not compulsory, however, and the gain upon illiteracy (75%) appears to be very slow. The government also gives primary instruction to recruits when serving with the colours, which, with the increasing employment of the people in the towns, helps to stimulate a desire for education among the lower classes. Education in Chile is very largely under the control of the national government, the minister of justice and public instruction being charged with the direction of all public schools from the university down to the smallest and most remote primary school. The system includes the University of Chile and National Institute at Santiago, lyceums or high schools in all the provincial capitals and larger towns, normal schools at central points for the training of public school teachers, professional and industrial schools, military schools and primary schools. Instruction in all these is free, and under certain conditions text-books are supplied. In the normal schools, where the pupils are trained to enter the public service as primary teachers, not only is the tuition free, but also books, board, lodging and everything needed in their school work. The national university at Santiago comprises faculties of theology, law and political science, medicine and pharmacy, natural sciences and mathematics, and philosophy. The range of studies is wide, and the attendance large. The National Institute at Santiago is the principal high school of the secondary grade in Chile. There were 30 of these high schools for males and 12 for females in 1903, with an aggregate of 11,504 matriculated students. The normal schools for males are located at Santiago, Chillán and Valdivia; and for females at La Serena, Santiago and Concepción. The mining schools at Copiapó, La Serena and Santiago had an aggregate attendance of 180 students in 1903, and the commercial schools at Iquique and Santiago an attendance of 214. The more important agricultural schools are located at Santiago, Chillán, Concepción and Ancud, the Quinta Normal de Agricultura in the national capital having a large attendance. The School of Mechanic Arts and Trades (Escuela de Artes y Oficios) of Santiago has a high reputation for the practical character of its instruction, in which it is admirably seconded by a normal handicraft school (Slöyd system) and a night school of industrial drawing in the same city, and professional schools for girls in Santiago and Valparaiso, where the pupils are taught millinery, dress-making, knitting, embroidery and fancy needlework. The government also maintains schools for the blind and for the deaf and dumb. The public primary schools numbered 1961 in 1903, with 3608 teachers, 166,928 pupils enrolled, and an average attendance of 108,582. The cost of maintaining these schools was 4,146,574 pesos, or an average of £2:17:3 per pupil in attendance. In addition to the public schools there are a Roman Catholic university at Santiago, which includes law and civil engineering among its regular courses of study; numerous private schools and seminaries of the secondary grade, with a total of 11,184 students of both sexes in 1903; and 506 private primary schools, with an attendance of 29,684. The private schools usually conform to the official requirements in regard to studies and examinations, which facilitates subsequent admission to the university and the obtainment of degrees; probably they do better work than the public schools, especially in the German settlements of the southern provinces. A Consejo de Instrucción Pública (council of public instruction) of 14 members exercises a general supervision over the higher and secondary schools. There are schools of music and fine arts in Santiago. The national library at Santiago, with 116,300 volumes in 1906, and the national observatory, are both efficiently administered. At the beginning of the 20th century there were 41 public libraries in the republic, including public school collections, with an aggregate of 240,000 volumes.

Charities.—According to the returns of 1903 there were 88 hospitals in the republic, which reported 79,051 admissions during the year, and had 6215 patients under treatment at its close; 628,536 patients received gratuitous medical assistance at the public dispensaries during the year; there were 24 foundling hospitals with 5570 children; and there were 3092 persons in the various hospicios or asylums, and 1478 in the imbecile asylums.

Religion.—The Roman Catholic religion is declared by the constitution to be the religion of the state, and the inaugural oath of the president pledges him to protect it. A considerable part of its income is derived from a subsidy included in the annual budget, which makes it a charge upon the national treasury like any other public service. The secular supervision of this service is entrusted to a member of the president’s cabinet, known as the minister of worship and colonization. The executive and legislative powers intervene in the appointments to the higher offices of the Church. The greater part of the population remains loyal to the established faith. The law of 1865 gives the privilege of religious worship to other faiths, and the laws of 1883 made civil marriage and the civil registry of births, deaths and marriages obligatory, and secularized the cemeteries. Under the reform of 1865 full religious freedom is practically accorded, and it is provided that the services of religious organizations other than the Roman Catholic may be held in private residences or in edifices owned by private individuals or corporations. Of the 72,812 foreigners residing in Chile in 1895, about 16,000 were described as Protestants. Notwithstanding the opposition of some political elements to the Church, the Chileans themselves may all be classed as Roman Catholics. The ecclesiastical organization includes one archbishop, who resides at Santiago, three bishops residing at La Serena, Concepción and Ancud, and two vicars residing in Antofagasta and Tarapacá. These benefices are filled by appointments from lists of three prepared by the council of state and sent to Rome by the president, and in the case of an archbishop or bishop the appointment must also receive the approval of the Senate. The Chilean clergy are drawn very largely from the higher classes, and their social standing is much better than in many South American states. The Church also possesses much property of its own, and is therefore able to maintain itself on a comparatively small subsidy from the public treasury, which was 985,910 pesos (£73,943) in 1902. The Church maintains seminaries in all cathedral towns, and these also receive a subsidy from the government.

Finance.—For a long time Chile was considered one of the poorest states of Spanish America, but the acquisition of the rich mineral-producing provinces of the north, together with the development of new silver and copper mines in Atacama and Coquimbo, largely increased her revenues and enabled her to develop other important resources. During the decade 1831-1840 the annual revenues averaged about 2,100,000 pesos (of 48d.), which in the decade 1861-1870 had increased to an average of only 8,200,000 pesos—and this during a period of considerable agricultural activity on account of wheat exports to California and Australia. After 1870 the revenues increased more rapidly owing to the development of new mining industries, the receipts in 1879 amounting to 15,300,000 pesos, and in 1882 to 28,900,000 pesos. The revenues from the captured Peruvian nitrate fields then became an important part of the national income, which ten years later (1902) reached an aggregate of 138,507,178 pesos (of i8d.), of which 105,072,832 pesos were in gold. In 1906 the receipts from all sources were estimated at 149,100,000 pesos, of which 62,200,000 pesos gold were credited to the tax on nitrate, 39,800,000 pesos gold to import duties, and 23,500,000 pesos currency to railway receipts. During these years of fiscal prosperity the country suffered much from financial crises caused by industrial stagnation, an excessive and depreciated paper currency and political disorder. To ensure an income that would meet its foreign engagements, the government collected the nitrate and iodine taxes and import duties in gold. As a considerable part of the expenditures were in gold, the practice was adopted of keeping the gold and currency accounts separate. In 1895 a conversion law was passed in which the sterling value of the peso was reduced to 18d., at which rate the outstanding paper should be redeemed. A conversion fund was also created, and, although the government afterwards authorized two more large issues, the beneficial effects of this law were so pronounced that the customs regulations were modified in 1907 to permit the payment of import duties in paper. The national revenue is derived chiefly from the nitrate taxes, customs duties, alcohol tax, and from railway, postal and telegraph receipts. There is no land tax, and licence or business taxes are levied by the municipalities for local purposes. The national expenditures are chiefly for the interest and amortization charges on the public debt, official salaries, military expenses in connexion with the army and navy, public works (including railway construction, port improvements, water and sewage works), the administration of the state railways, telegraph lines and post office, church subsidies, public instruction and foreign representation.

The ordinary and extraordinary receipts and expenditures for the five years 1899-1903, in gold and currency, in pesos of 18d., were as follows:—

For 1906 the expenditures were fixed at 149,000,000 pesos, and the revenues were estimated to produce 149,100,000 pesos, which included 62,200,000 pesos gold from nitrate taxes, 39,800,000 pesos gold and 200,000 pesos paper from import duties, 23,500,000 pesos paper from the state railways, 2,500,000 pesos paper from postal and telegraph receipts, and 15,000,000 pesos gold from loans. How the revenues are expended is shown in the estimates for 1907, in which the total expenditures were estimated at 134,830,532 pesos paper and 58,796,780 pesos gold, the principal appropriations being 16,192,780 pesos paper and 99,733 gold for the war department, 10,460.781 paper and 6,315,731 gold for the marine department, 40,934,273 paper and 16,984,671 gold for railways, and 6,324,817 paper for public works. In addition to these the budget of 1906 provided for gold expenditures in 1907 of 7,000,000 pesos on sanitary works and 8,000,000 pesos on the Arica-La Paz railway. The custom of dividing receipts and expenditures into ordinary and extraordinary, of treating the receipts from loans as revenue, of adding six months to the fiscal year for closing up accounts, and of dividing receipts and expenditures into separate gold and currency accounts, leads to much confusion and complication in the returns, and is the cause of unavoidable discrepancies and contradictions.

In May 1906 the external debt of the republic aggregated £21,700,000, including the loans of 1905 and 1906, amounting to £5,700.000, for sanitary works and railway construction. At the same time the internal debt was 107,000,000 pesos (£8,025,000), which increases the funded indebtedness to £29,725,000. Like Brazil, Chile has been careful to preserve her foreign credit, and though an average indebtedness of about £10 per capita may seem large for a nation with so much absolute poverty among its people, the government is finding no difficulty in negotiating new loans, the mineral resources of the country and the conservative instincts of the people being considered satisfactory guarantees. According to official returns, the real-estate valuations in 1903-1904 aggregated 1,777,217,704 pesos, of which 1,020,609,215 pesos were in urban and 754,608,489 pesos in rural property. Of the total returned, 1,775,217,704 is described as taxable, and 262,626,576 pesos as non-taxable. The large and steadily increasing receipts from import duties, amounting to 91,321,860 pesos in 1905, and 103,507,556 pesos in 1906, appears to indicate an encouraging state of prosperity in the country, although an average of 34½ pesos a year (nearly £2 : 12s.), in addition to the increased prices paid for home manufactures, seems to be a very heavy indirect tax upon so poor a people.

Currency.—The monetary circulation in Chile consists almost wholly of paper currency, nominally based on a gold standard of 18d. per peso. The conversion law of 1895 made the currency convertible at this rate, although the gold peso was rated at 48d. previous to that date; but the financial crisis of 1898 caused the suspension of specie payments, and a forced issue of additional paper led to a further postponement of conversion and the prompt withdrawal of specie from circulation. The paper circulation consists of national and bank issues. The former owes its existence very largely to the war with Peru, the civil war of 1891, and the financial troubles of 1898. On the 1st of January 1890 the national issues stood at 22,487,916 pesos, and the bank issues at 16,679,790 pesos, making a total of 39,167,706 pesos currency in circulation. This total was largely increased by President Balmaceda in 1891. On the 31st of July 1898 the conversion of paper notes, under the law of 1st June 1895, was suspended, and the government issued 27,989,929 pesos to the banks of issue, which was described as a loan at 2%, and raised their outstanding circulation to 40,723,089 pesos, and at the same time issued on its own account 17,693,890 pesos and assumed responsibility for 1,193,641 pesos which had been illegally put into circulation before 1896. This gave an aggregate registered circulation of 86,045,166 pesos in 1898. In 1904 another issue of 30,000,000 pesos was authorized and the date of conversion was still further postponed, and in 1907 a more general act provided that the maximum paper circulation should not exceed 150,000,000 pesos of the value of 18d. per peso, and that new issues should be made only through the issue department and against deposits of gold, which deposits would be returned to depositors on the presentation of the currency issued. The redemption of this issue was guaranteed by a conversion fund of 100,000,000 pesos, and by an authorization to issue a loan of 50,000,000 pesos to redeem the balance, if necessary. The conversion fund under the act of 1895 stood at 77,282,257 pesos (£5,796,170) on the 31st of May 1907. There are 23 joint-stock banks of issue, with an aggregate registered capital of 40,689,665 pesos (£3,051,724). Their circulating notes are secured by deposits in the national treasury of gold, government notes and other approved securities. There is no state bank, though the Bank of Chile, with its numerous agencies and its paid-up capital of 20,000,000 pesos, may be said to fill the place of such an institution. Besides these, there are four non-issue banks, two foreign banks and their agencies, and three mortgage banks, with agencies at the important provincial centres, which loan money on real-estate security and issue interest bearing hypothecary notes to bearer. There are 8 savings banks in the republic, whose aggregate deposits on the 31st of December 1906 were 14,799,728 pesos.

The monetary unit, the gold peso, does not form a part of the actual coinage. The gold coins authorized by this law are the condor of 20 pesos, the medio condor, or doblon, of 10 pesos, and the escudo of 5 pesos. The silver coins are the peso of 100 centavos and its fractional parts of 20, 10 and 5 centavos. The bronze coins are of 2½, 2, 1, and ½ centavos.

The metric system of weights and measures is the legal standard in Chile, but the old Spanish standards are still widely used, especially in handling mining and farm produce. Nitrate of soda is estimated in Chilean quintals (101.41 lb) in the field, and metric quintals (220.46 lb) at the port of shipment. In silver and copper mining the marc (8 oz.) is commonly used in describing the richness of the ores. Farm produce is generally sold by the arroba or fanega; the vara is used in lineal measurement, and the cuadra is used by country people in land measurement.

Bibliography.—General History.—The most valuable authority is D. Barros Arana’s Historia jeneral de Chile (15 vols., Santiago, 1884), from the earliest days up to 1830. Smaller handbooks covering the whole period are: A.U. Hancock, a History of Chile (Chicago, 1893), the only general history in English, and containing a bibliography; Gaspar Toro, Compendio de la historia de Chile (Santiago, 1879), a good clear abstract of Chilean history; and F. Valdes Vergara, Historia de Chile (Valparaiso, 1898), written primarily for schools, but containing useful sketches of leading figures in Chilean history.

Works on Special Periods.—Colonial Period: M.L. Amunátequi, Descubri miento y conquista de Chile (Santiago, 1885), a valuable detailed account of the Spanish conquest; by same author, Los Precursores de la independencia de Chile (Santiago, 1870), a clear useful description of the evils of the Spanish colonial system; Horacio Lara, Cronica de la Araucania (Santiago, 1889), a history of the Araucanian Indians right up to recent dates; Abbé Eyzaguirre, Histoire du Chili (Lille, 1855), mainly dealing with the position of the Church during the colonial period. Perez Garcia’s Historia del reino de Chile (Santiago, 1900), an old history by a Spanish officer written about 1780, and Molina’s History of Chili in the English translation (London, 1809), will also be found useful. Useful material for research exists in J.T. Medina’s Coleccion de documentos para la historia de Chile (Santiago, 1888), a collection of despatches and official documents; his Cosas de la colonia (Santiago, 1889), an accumulation of undigested information about life in the colonial period; and Historiadores de Chile (21 vols., Santiago, 1861), a collection of ancient chronicles and official documents up to the early part of the 17th century.

Revolutionary Period.—A. Roldan, Las Primeras Asambleas nacionales (Santiago, 1890), an account of the struggles in the first national assemblies; A. Valdes, Revolucion Chilena y campañas de la independencia (Santiago, 1888), an account of the early fighting and rivalry of the revolutionary leaders; W. Pilling, Emancipation of South America (London, 1893), a translation of B. Mitre’s life of San Martin, describing the fighting in the wars of independence; Lord Cochrane, Narrative of Services in Chile, Peru and Brazil (London, 1859), an autobiography describing the naval exploits that helped to secure the expulsion of the Spaniards; B. Vicuña Machenna, Vida de O’Higgins (Santiago, 1882), giving a useful account of the revolutionary struggle and the main actors; and the same author’s Historia jeneral de la republica de Chile, a collection of essays on the early republican history by various writers.

Later History.—R. Sotomayor Valdes, Historia de Chili, 1831-1871, a detailed account of the period (Santiago, 1875); the same author’s Campaña del ejercito Chileno en 1837 (Santiago, 1896), describing the fighting of the first Peruvian War; B. Vicuña Machenna, D. Diego Portales (Valparaiso, 1863), a good account of the life and time of Portales, the famous minister of the Conservative party; P.B. Fiqueroa, Historia de la revolution constituyente 1858-59 (Santiago, 1889), an account of the revolution at the end of Montt’s presidency; F. Fonch, Chile in der Gegenwart (Berlin, 1870), a description of Chile at the time; Statement on Behalf of Chile (in the Chilean-Argentine Boundary Arbitration) (6 vols., London, 1901-1902); Sir Thomas Holdich, Countries of the King’s Award (1904); Beltran y Rospido, Los Pueblos hispano-americanos en el siglo XX. (Madrid, 1904); P.F. Martin, Through Five Republics of South America (London, 1906); Wright, The Republic of Chile (London, 1905); G.F. Scott Elliot, Chilé (London, 1907); Sir W.M. Conway, Aconcagua and Tierra del Fuego (London, 1902); “Chile-Argentine Arbitration” in the Geog. Journal (January 1903); C.M. Pepper, Panama to Patagonia (London, 1907); C.E. Akers, History of South America, 1854-1904 (London, 1904); M. Hume, Lecture on the Republic of Chile (London, 1902).