SALVADOR OF THE TWENTIETH CENTURY
CHAPTER I
Discovery of Salvador—Scenery—Volcanoes—Topographical features—Mountain ranges—Natural fertility—Lake Ilopango—Earthquake results—Remarkable phenomena—Disappearance of islands—Public roads improvement and construction under Figueroa government.
It was in the year 1502 that Christopher Columbus, that remarkable and noble-minded Genoese, undeterred by the shameful treatment meted out to him by his adopted countrymen in Spain, sailed away to the East Indies in search of a new passage; and it was in consequence of the mutiny among his ruffianly followers that, putting into Hispaniola, Salvador was discovered. For something over 300 years Spain ruled, and ruled brutally; the history of her government here—as elsewhere through Latin America—being one long series of oppressions, cruelties and injustices practised upon the unfortunate natives and the Spanish residents alike. The ill-treatment extended to Columbus is but a case in point.
Lying on the Pacific Ocean, between the parallels of 13° and 14° 10' N. latitude, and the meridians of 87° and 90° W. longitude, Salvador has a coast-line of about 160 miles, extending from the Bay of Fonseca to the River Paz, which is one of the boundaries between this Republic and the neighbouring State of Guatemala. While Salvador is the smallest of the five different countries forming the Central American group, boasting of but 9,600 square miles, it not alone possesses some of the richest and most beautiful territory, but has the densest population as well as the most considerable industry and the most important commerce.
Very remarkable are the topographical features of Salvador, and very profound is the impression created upon the traveller's mind as he approaches it for the first time through the beautiful Bay of Fonseca, with its wealth of tropical scenery, the romantic islands and the background of noble mountains, afforested to the tops of their numerous peaks, and filling the mind with awe at the memory of their numerous destructive eruptions through the centuries.
The coast here presents, for the greater part, a belt of low-lying, richly wooded alluvial land, varying in width from ten to twenty miles. Behind this, and displaying an abrupt face seawards, rises a noble range of coast mountains—or rather a broad plateau—having an average elevation of 2,000 feet, and relieved by numerous volcanic peaks. It is not the height of these mountains that lends so much dignity and beauty, for, as mountains go, they would be considered as anything but remarkable. It is their extraordinary formation, their almost terrible proximity, and their long and terrifying history, which challenge the attention of the individual who gazes upon them for the first time.
Between the range and the great primitive chain of the Cordilleras beyond, lies a broad valley varying in width from twenty to thirty miles, and being over 100 miles in length. Very gently the coastal plateau subsides towards this magnificent valley, which is drained and abundantly watered by the River Lempa, and is unsurpassed for natural beauty and fertility by any equal extent of country in the tropics.
The northern border of this terrestrial paradise—so far as the eye can judge it—rests upon the flank of the mountains of Honduras, which tower skywards about it to the height of 6,000 to 8,000 feet, broken and rugged to the very summits. To the south of the Lempa, however, the country rises from the immediate and proper valley of the river, first in the form of a terrace with a very abrupt face, and afterward by a gradual slope to the summit of the plateau.