Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841Gardner, George
History
Travels in the Interior of Brazil: Principally through the northern provinces, and the gold and diamond districts, during the years 1836-1841
Gardner, George
Brazil -- Description and travel; Mines and mineral resources -- Brazil
The whole of the country around Rio is essentially granitic, all the
rocks being of that nature to which the name of Gneiss-granite has been
applied, from their possessing decided marks of stratification. The
mountains generally run in chains having no particular direction, and are
of all sizes, from slight eminences to mountains which rise from 2,000 to
3,000 feet above the level of the sea. The loftier of these mountains,
such as the Peak of Tejuca, the Corcovado, and the Gavea, have their
south-east sides bare and precipitous, while those to the northward have
a gradual ascent, and are wooded to their summit. Notwithstanding the
enormous length of time which the sides of these mountains have been
covered with their mighty forests, the alluvial layer of soil which rests
on them is very thin. This, however, may be accounted for by the heavy
rains washing it, as well as the materials from which it is formed, down
into the valleys, where the alluvium is often found to be many feet
deep. Hence it is that the deep valleys which intersect the mountain
ranges are the principal seats of agricultural industry; and some of
them, particularly in the vicinity of the city, are thickly studded with
habitations, surrounded with plantations of Coffee, Oranges, Bananas,
and Mandioca. Many of the lower hills near the city are now also cleared
and planted with Coffee, but the plantations were too young when I
left to form any idea of their success at so low a level. Beneath the
alluvium there is a bed of reddish-coloured clay, which is very tenacious
when wet. It is often from thirty to forty feet in thickness, and is
not peculiar to the province, as I have met with it in every part of
Brazil where I have travelled. It frequently contains numerous boulders,
consisting of rounded, as well as angular, fragments of Gneiss, Granite,
and Quartz, and is often inter-stratified with various beds of sand
and gravel. It is obvious then from these observations, that the soil
around Rio itself is not generally rich. Indeed, the first thing which
strikes a stranger on his arrival, is the apparent poverty of the soil
contrasted with the richness of the vegetation. But for the humidity of
the atmosphere, the heavy dews of the dry season, and the rains of the
wet, combined with the heat of a tropical sun, the greater part of the
country immediately surrounding Rio would not be worthy of cultivation.
The very small quantity of soil which suffices for some plants is
quite astonishing to a European. Rocks, on which scarcely a trace of
earth is to be observed, are covered with _Vellozias_, _Tillandsias_,
_Melastomaceæ_, _Cacti_, _Orchideæ_, and _Ferns_, and all in the vigour
of life.
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account