Travels Through the Bannat of Temeswar Transylvania And Hungary in the Year 1
Travels Through the Bannat of Temeswar Transylvania And Hungary in the Year 1
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Y accordingly brownifh or yellovvifli. Sometimes thefe colours may be owing to a ftronger irony- mixrure of the rock, or to the yellow brown- ifh clay-Qate, which is not uncommon in thefe parts. Thefe forts of clay, the white as well as the yellow, turn red in fire, the white lefs than the yellow, which evidences its being lefs impreg- nated with iron than the latter. The yellow clay is ufed as common loam in walh. Jn a great part of the circle of Pilfen^ and on the frontier mountains towards i...heUpper Palaiinate ixud Bavaria, the vegetable mould, or the upper ilrata of the ground, are extremely loamy. Unlefs they be accumulated by river-inundations, they may be properly confidered as produced by folutions and decays of the adjacent granite and other argillaceous hills, which v^ill, I am confident, granite-pebbles and rocks, which are fo frequent in thefe fandy plains, feem to favour fuch an opinion ; and as among the peb- bles of the fca-ßiores, befides thefe granite-pieces, a great va- riety of the harder remains of the more ancient mountains, nay of different fecundary ones, are to be found, fuch as jafper, porphyry, various coloured hcrnftone, quartz-lumps, gneifs, horndate, marble, limeftones and ßint, wliich prove that nothing- Hands proof of age and time ; this opinion Grains fome credit, and this the more fo, as hitherto no fort of rock has been difcovered, in which a greater quantity of vifible quartz be contained.
What to read after Travels Through the Bannat of Temeswar Transylvania And Hungary in the Year 1?
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To quickly assess the difficulty of the text, read a short excerpt:
Y accordingly brownifh or yellovvifli. Sometimes thefe colours may be owing to a ftronger irony- mixrure of the rock, or to the yellow brown- ifh clay-Qate, which is not uncommon in thefe parts. Thefe forts of clay, the white as well as the yellow, turn red in fire, the white lefs than the yellow, which evidences its being lefs impreg- nated with iron than the latter. The yellow clay is ufed as common loam in walh. Jn a great part of the circle of Pilfen^ and on the frontier mountains towards i...heUpper Palaiinate ixud Bavaria, the vegetable mould, or the upper ilrata of the ground, are extremely loamy. Unlefs they be accumulated by river-inundations, they may be properly confidered as produced by folutions and decays of the adjacent granite and other argillaceous hills, which v^ill, I am confident, granite-pebbles and rocks, which are fo frequent in thefe fandy plains, feem to favour fuch an opinion ; and as among the peb- bles of the fca-ßiores, befides thefe granite-pieces, a great va- riety of the harder remains of the more ancient mountains, nay of different fecundary ones, are to be found, fuch as jafper, porphyry, various coloured hcrnftone, quartz-lumps, gneifs, horndate, marble, limeftones and ßint, wliich prove that nothing- Hands proof of age and time ; this opinion Grains fome credit, and this the more fo, as hitherto no fort of rock has been difcovered, in which a greater quantity of vifible quartz be contained.
What to read after Travels Through the Bannat of Temeswar Transylvania And Hungary in the Year 1?
You can find similar books in the "Read Also" column, or choose other free books by Ignaz Born to read onlineMoreLess
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