Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland.

































































































































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The small extent of the valley, and the proximity of the high
mountains of Avila and the Silla, give a - Page 629
Personal Narrative Of Travels To The Equinoctial Regions Of America During The Years 1799-1804 - Volume 1 - By Alexander Von Humboldt And Aime Bonpland. - Page 629 of 779 - First - Home

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The Small Extent Of The Valley, And The Proximity Of The High Mountains Of Avila And The Silla, Give A Gloomy And Stern Character To The Scenery Of Caracas; Particularly In That Part Of The Year When The Coolest Temperature Prevails, Namely, In The Months Of November And December.

The mornings are then very fine; and on a clear and serene sky we could perceive the two domes

Or rounded pyramids of the Silla, and the craggy ridge of the Cerro de Avila. But towards evening the atmosphere thickens; the mountains are overhung with clouds; streams of vapour cling to their evergreen slopes, and seem to divide them into zones one above another. These zones are gradually blended together; the cold air which descends from the Silla, accumulates in the valley, and condenses the light vapours into large fleecy clouds. These often descend below the Cross of La Guayra, and advance, gliding on the soil, in the direction of the Pastora of Caracas, and the adjacent quarter of Trinidad. Beneath this misty sky, I could scarcely imagine myself to be in one of the temperate valleys of the torrid zone; but rather in the north of Germany, among the pines and the larches that cover the mountains of the Hartz.

But this gloomy aspect, this contrast between the clearness of morning and the cloudy sky of evening, is not observable in the midst of summer. The nights of June and July are clear and delicious. The atmosphere then preserves, almost without interruption, the purity and transparency peculiar to the table-lands and elevated valleys of these regions in calm weather, as long as the winds do not mingle together strata of air of unequal temperature.

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