King Coals Levee Or Geological Etiquette With Explanatory Notes And the C
King Coals Levee Or Geological Etiquette With Explanatory Notes And the C
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Compact Quartz is largely disseminated through most rocks in veins and beds ; and is so met with on Skiddaw, in Cumberland. The rounded milk-white Pebbles, found on the sea-shore, and in gravel, are of Quartz.
Felspar, the other constituent of Granite, will be hereafter mentioned.
85. Gneiss is composed of precisely the same mate- rials as Granite, but is slaty in its structure* owing to the comparatively large quantity of Mica it contains. And from this slaty structure perhaps it arises that t...he Felspar is very liable to decomposition. It is of very rare occurrence in England, but abounds in the primitive moun- tains of Scotland and Ireland.
103. Clay Slate. The appearance of Slate is familiar to us under the form of common roofing and 48 \ VERSE schoolboy's Slates'; but no accurate line has yet been drawn by which Clay Slate can be distin- guished from the finer varieties of Grauwack Slate; nor is it agreed whether Clay Slate con- tains organic remains or not, or is to be con- sidered primitive or secondary.
What to read after King Coals Levee Or Geological Etiquette With Explanatory Notes And the C?
You can find similar books in the "Read Also" column, or choose other free books by John Scafe to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Compact Quartz is largely disseminated through most rocks in veins and beds ; and is so met with on Skiddaw, in Cumberland. The rounded milk-white Pebbles, found on the sea-shore, and in gravel, are of Quartz.
Felspar, the other constituent of Granite, will be hereafter mentioned.
85. Gneiss is composed of precisely the same mate- rials as Granite, but is slaty in its structure* owing to the comparatively large quantity of Mica it contains. And from this slaty structure perhaps it arises that t...he Felspar is very liable to decomposition. It is of very rare occurrence in England, but abounds in the primitive moun- tains of Scotland and Ireland.
103. Clay Slate. The appearance of Slate is familiar to us under the form of common roofing and 48 \ VERSE schoolboy's Slates'; but no accurate line has yet been drawn by which Clay Slate can be distin- guished from the finer varieties of Grauwack Slate; nor is it agreed whether Clay Slate con- tains organic remains or not, or is to be con- sidered primitive or secondary.
What to read after King Coals Levee Or Geological Etiquette With Explanatory Notes And the C?
You can find similar books in the "Read Also" column, or choose other free books by John Scafe to read onlineMoreLess
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