Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min
Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min
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In our eReader you can find the full English version of the book. Read Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min 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 Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min
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They consist mostly of sand and gravel. These facts are apparent from the following statement of materials passed through in boring the existing well.
At depth Intervening of thickness.
FEET. FEET.
9 Soil and gravel.
9 9 Clay and gravel.
18 18 Sand and gravel.
36 54 Quicksand.
90 1 Coarse sand.
91 C Clay. At 93 feet, a piece of grapevine with bark.
97 38 Sand, varying from quicksand to coarse sand. At 114 feet, sand filled the pipe 12 feet ; at 125 feet, it filled 5 feet.
135 45 Gravel, quicksa...nd, and coarse sand. At 144 feet the pipe filled 10 feet. At 168 feet another piece of grapevine.
180 7 Blue Clay.
187 13 Rock fragments.
200 2 Gravel. Brine stood 18 by salometer.
202 8 Shelly rock.
210 Bed-rock said to be a sand stone probably Potsdam sandstone (see diagram. ) Here is a favorable bed of materials to serve as a reservoir for any brines wliick might escape from the outcrops of any of the contiguous strata ; and some surface indications of brine have long been known ; but, in boring into these deposits no brine seems to have been reached of sufficient strength for practical purposes.
What to read after Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min?
You can find similar books in the "Read Also" column, or choose other free books by Winchell, Alexander, 1824-1891 to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
They consist mostly of sand and gravel. These facts are apparent from the following statement of materials passed through in boring the existing well.
At depth Intervening of thickness.
FEET. FEET.
9 Soil and gravel.
9 9 Clay and gravel.
18 18 Sand and gravel.
36 54 Quicksand.
90 1 Coarse sand.
91 C Clay. At 93 feet, a piece of grapevine with bark.
97 38 Sand, varying from quicksand to coarse sand. At 114 feet, sand filled the pipe 12 feet ; at 125 feet, it filled 5 feet.
135 45 Gravel, quicksa...nd, and coarse sand. At 144 feet the pipe filled 10 feet. At 168 feet another piece of grapevine.
180 7 Blue Clay.
187 13 Rock fragments.
200 2 Gravel. Brine stood 18 by salometer.
202 8 Shelly rock.
210 Bed-rock said to be a sand stone probably Potsdam sandstone (see diagram. ) Here is a favorable bed of materials to serve as a reservoir for any brines wliick might escape from the outcrops of any of the contiguous strata ; and some surface indications of brine have long been known ; but, in boring into these deposits no brine seems to have been reached of sufficient strength for practical purposes.
What to read after Report of a Geological Survey of the Vicinity of Belle Plaine Scott County Min?
You can find similar books in the "Read Also" column, or choose other free books by Winchell, Alexander, 1824-1891 to read onlineMoreLess
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