Report On the Second Year's Progress of the Survey of the Oil Lands of Japan
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The only fossils (except one calamite) that have yet heen found ai e in the highly metamorphosed limestone ; and the only recognised ones at Akasaka in Mino, and are said hy Dr. K.
Nauinann to be of carboniferous age (fusulina 'and ciinoids).
The syenite of the mountains has much white feldspar, a good deal of very daik brown mica, hornblende crystals about a sixtenth of an inch long and a little glassy quartz slightly smoky in round grains, and the whole rock in some places (as near Toono) is ...crumbling into gray sand.
In all the syenites observed the quartz is in like manner in "crystals or in rounded crystalline grains," as Riclitho- f'en says it is in granitic rhyolite ; "while," he says, " in granite it usually permeates the interstices between the other component minerals ;" a passage that by a miscon- ception on my part formerly confirmed me in a probably iiicorieei. iiupiessiou in regaid to some syenites near Chi- kubutomuushi high up on the east coast of Yesso, which I took to belong to the old volcanic rooks.
What to read after Report On the Second Year's Progress of the Survey of the Oil Lands of Japan?
You can find similar books in the "Read Also" column, or choose other free books by Benjamin Smith Lyman to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
The only fossils (except one calamite) that have yet heen found ai e in the highly metamorphosed limestone ; and the only recognised ones at Akasaka in Mino, and are said hy Dr. K.
Nauinann to be of carboniferous age (fusulina 'and ciinoids).
The syenite of the mountains has much white feldspar, a good deal of very daik brown mica, hornblende crystals about a sixtenth of an inch long and a little glassy quartz slightly smoky in round grains, and the whole rock in some places (as near Toono) is ...crumbling into gray sand.
In all the syenites observed the quartz is in like manner in "crystals or in rounded crystalline grains," as Riclitho- f'en says it is in granitic rhyolite ; "while," he says, " in granite it usually permeates the interstices between the other component minerals ;" a passage that by a miscon- ception on my part formerly confirmed me in a probably iiicorieei. iiupiessiou in regaid to some syenites near Chi- kubutomuushi high up on the east coast of Yesso, which I took to belong to the old volcanic rooks.
What to read after Report On the Second Year's Progress of the Survey of the Oil Lands of Japan?
You can find similar books in the "Read Also" column, or choose other free books by Benjamin Smith Lyman to read onlineMoreLess
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