[XXVII-3] The same may be said, though in a less degree, of the northern and eastern coast of Hond. from Omoa to Gracias á Dios.
[XXVII-4] La Union, San Miguel, Acajutla, Sonsonate, etc., owing to local causes.
[XXVII-5] The average temperature at Tegucigalpa, Comayagua, Juticalpa, and Gracias is about 74°. Squier's Notes on Cent. Am., 25-7; Belly, A travers l'Amér. Cent., i. 53-4.
[XXVII-6] Cold and salubrious on the table-lands in the interior, the thermom. ranging from 65° to 75° Fahr. Molina, Bosq. Costa R., 28. The climate of Costa R. varies from 50° to 60° Fahr., according to elevation. Galindo, in Journ. Royal Geog. Soc. of London, vi. 134; Laferrière, De Paris à Guatém., 47-8.
[XXVII-7] This is by far the pleasanter season, the forenoons being usually cloudless, with a clear, elastic, and balmy atmosphere. Owing to local influences in some portions of the eastern coasts it rains more or less the whole year. Crowe's Gospel, 1-12.
[XXVII-8] Consisting of three groups; viz, the Costa Rican traversing that republic and Panama, the Honduran and Nicaraguan, and the Guatemalan.
[XXVII-9] Some of the summits are 17,000 ft high. Several spurs from the Sierra Madre—the main ridge—cut the plains at right angles, and sometimes reach the sea-shore.
[XXVII-10] All the volcanoes of Cent. Am. are on the Pacific coast, almost in a line, and running due north-west and south-east, beginning with the Cartago or Irazú, in Costa Rica, which is 11,480 ft high, and has left traces of violent eruptions before the historic period; the only proof of its present activity being a small rill of smoke visible from the foot of the mountain. There are hundreds of other volcanic peaks and extinct craters on the line, the most notable being the Turrialba, which was in active eruption in 1866, the ashy matter from it having been beneficial to the coffee plantations; Chirripó, Blanco, Závalo, Barba, Los Votos 9,840 ft high, also in Costa R. Abogado, Cerro Pelado, Tenorio, Cucuilapa, Miravalles, Rincon de la Vieja, La Hedionda, Orosi, Madera, Ometepec, Zapatera, Guanapepe, Guanacaure, Solentinami, Mombacho, Chiltepe, Masaya or Nindirí; this last said to have been in a state of eruption upwards of 250 years ago, and still continues active; it had a small eruption Nov. 10, 1858; Managua; Momotombo, 6,500 ft high, near the Managua or Leon Lake, about which the Indians had a tradition of a tremendous eruption some 100 years before the coming of the Spaniards, the lava running into the lake and destroying all the fish; the latter part of the story seems to be incorrect, there being evidence that the lava did not reach the lake shore; it partially revived in 1852; Las Pilas, Asososca, Orota, Telica, Santa Clara, El Viejo 6,000 ft high; El Chonco; Cosigüina, whose first eruption was Jan. 20, 1835, believed to have been the most violent ever recorded in history; and Joltepec—all in Nic. El Tigre, Nacaome, and Amapala, or Conchagua, in Hond. In the republic of Salv. are several; namely, the San Salvador, which had not broken out in upwards of three centuries; but in old times it ejected immense masses of lava and scoriæ to a distance of more than 18 miles. It is of great depth, computed by Weems, an American who descended it, at about 5,000 varas; the bottom is occupied by a lake; San Miguel, about 15,000 ft high. In old times it ejected large quantities of cinders and half-melted stones of immense size. The country for 30 miles or more, including the site of San Miguel, one of the oldest towns in Am., being covered with lava and scoriæ; San Vicente; Izalco, which broke out about 100 years ago, is in constant activity, but has not caused any serious damage; Paneon, and Santa Ana. In Guat. are the Pacaya; the Volcan de Agua; the Volcan de Fuego constantly smoking with occasional explosion and shocks, its last eruption being in 1880; Encuentro, Acatenango; Atitlan so remarkable at one time for frequent and violent eruptions, the last ones being in 1828 and 1833, which caused much destruction on the coast of Suchitepequez; Tesamielco, Zapotitlan, Amilpas, Quezaltenango, and Cerro Quemado whose last eruption was in 1785. There are many other nameless ones. Near a number of the active and extinct volcanoes are small and almost circular openings in the ground, through which is ejected smoke or steam. The natives call them ausoles or infiernillos, little hells. Dunlop's Cent. Am., 3, 13-17, 52-5, 91-2, 118-20, 284-90; Squier's Trav., ii. 101-19; Squier's Cent. Am., 359-61, 492-8. Other authorities speaking of the volcanoes of Cent. Am. are: Stout's Nic., 143; Silliman's Journal, xxviii. 332; Levy, Nic., 75-85, 147-53; Guat., Gaceta, Feb. 10, 1854; Diario de Avisos, Nov. 22, 1856; Nic., Gaceta, June 5, Aug. 7, 1869; March 18, 1871; Salv., Diario Oficial, Oct. 11, Nov. 15, 1878; Overland Monthly, xiii. 324; La Voz de Méj., March 17, 1866; Pim and Seemann's Dottings, 39-40; Baily's Cent. Am., 75-8; Wells' Hond., 231-2; Harper's Mag., xix. 739; and the Encyclopædias; Guat., Revista Observatorio Meteor., i. 21-3.
[XXVII-11] About 300 have been recorded in 3½ centuries, which are probably the hundredth part of the actual number.
[XXVII-12] Hist. Cent. Am., ii. 719-21, this series.