The Yelta And Paramatta Mines
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In our eReader you can find the full English version of the book. Read The Yelta And Paramatta Mines Online - link to read the book on full screen. Our eReader also allows you to upload and read Pdf, Txt, ePub and fb2 books. In the Mini eReder on the page below you can quickly view all pages of the book - Read Book The Yelta And Paramatta Mines
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This apparent belt of the rock extends from a point six chains west of the railway line for a distance of 14 chains to the west-south-west. Such sedi- mentary rocks are of peculiar interest from a geological point of view, in that they are likely to afford the clue to the structure of the district. The information available with regard to this particular occurrence is, unfortun- ately, inconclusive.
The superficial covering, which completely masks the rocks throughout the area, is of variable t...hickness and composition. In some places the basal rock is found decomposed, in situ, at a depth of only a few inches. In other places the prospecting pits show the presence of several feet of sand, traver- tine, and clay.
The travertine consists for the most part of calcium carbonate, with which are mingled clay, sand, and fragments of the decayed felspathic porphyry. The structure is in almost all cases concretionary. This deposit is formed by the evaporation of the water which circulates through the shallow belt of disintegrated rock lying immediately below the surface.
What to read after The Yelta And Paramatta Mines?
You can find similar books in the "Read Also" column, or choose other free books by L Keith Leonard Keith Ward to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
This apparent belt of the rock extends from a point six chains west of the railway line for a distance of 14 chains to the west-south-west. Such sedi- mentary rocks are of peculiar interest from a geological point of view, in that they are likely to afford the clue to the structure of the district. The information available with regard to this particular occurrence is, unfortun- ately, inconclusive.
The superficial covering, which completely masks the rocks throughout the area, is of variable t...hickness and composition. In some places the basal rock is found decomposed, in situ, at a depth of only a few inches. In other places the prospecting pits show the presence of several feet of sand, traver- tine, and clay.
The travertine consists for the most part of calcium carbonate, with which are mingled clay, sand, and fragments of the decayed felspathic porphyry. The structure is in almost all cases concretionary. This deposit is formed by the evaporation of the water which circulates through the shallow belt of disintegrated rock lying immediately below the surface.
What to read after The Yelta And Paramatta Mines?
You can find similar books in the "Read Also" column, or choose other free books by L Keith Leonard Keith Ward to read onlineMoreLess
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