The Mineralogy of the Chicago Area
The Mineralogy of the Chicago Area
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In our eReader you can find the full English version of the book. Read The Mineralogy of the Chicago Area 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 Mineralogy of the Chicago Area
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Fig. 9.
repeated in stair-like arrangement. In the lower figure of PL V, fig. 2 are globular masses, very often occurring in unworn and undecomposed specimens. The one at the right is on Niagara limestone. The round velvety looking masses are composed of bunches of crystals of different lengths which extended into the mother solution. The advancing front of such a growing crystal group would naturally be globular, since such a form would give each crystal the largest area of solution from which... to draw material. The persistency of the spherical habit of these concretions is illustrated in PL VI, fig. I. When found on the lake shore these concretions may easily be mistaken for ordinary pebbles, but when a trace of the origi- nal crystal shape remains, as seen in the left hand lower specimen, the true nature of the sample is recognized. Fur- ther, these seeming common stone pebbles are much heavier than an ordinary pebble. Upon being broken open, the yellow metallic luster and the common radiate structure shown in PL VI, fig.
What to read after The Mineralogy of the Chicago Area?
You can find similar books in the "Read Also" column, or choose other free books by A R Alja Robinson Crook to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Fig. 9.
repeated in stair-like arrangement. In the lower figure of PL V, fig. 2 are globular masses, very often occurring in unworn and undecomposed specimens. The one at the right is on Niagara limestone. The round velvety looking masses are composed of bunches of crystals of different lengths which extended into the mother solution. The advancing front of such a growing crystal group would naturally be globular, since such a form would give each crystal the largest area of solution from which... to draw material. The persistency of the spherical habit of these concretions is illustrated in PL VI, fig. I. When found on the lake shore these concretions may easily be mistaken for ordinary pebbles, but when a trace of the origi- nal crystal shape remains, as seen in the left hand lower specimen, the true nature of the sample is recognized. Fur- ther, these seeming common stone pebbles are much heavier than an ordinary pebble. Upon being broken open, the yellow metallic luster and the common radiate structure shown in PL VI, fig.
What to read after The Mineralogy of the Chicago Area?
You can find similar books in the "Read Also" column, or choose other free books by A R Alja Robinson Crook to read onlineMoreLess
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