Water Resources Survey: Hill County, Montana 1967
Water Resources Survey: Hill County, Montana 1967
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Aquifer depths are 25 feet to 70 feet below the surface, and reported rates of withdrawal are 4 to 20 gpm pumping. Benches of ice-contact terraces rising slightly above the flood plain are reported near the town of Box Elder and water at a depth of 11 feet, in T. SON— R. 13E, where Barney's Coulee intersects the flood plain may be in one of these benches. The aquifer is re- ported as "coarse gravel entire depth," with a "supply of water unlimited." An estimate of withdraw- als from one well is ...given as 360,000,000 gallons per year, which is equivalent to an average of ahnost 1,000,000 gallons daily or approximately 700 gpm. Under the flood plain are valley fill sands and gravels in the preglacial Missouri valley from depths of about 50 feet to 200+ feet, which are fair aquifers. West of the town of Havre are several wells, 76 to 131 feet deep in sand and gravel; these are reportedly capable of small flow-yields and individually pump 125 to 300 gpm. Near the town of Box Elder valley-fill gravel from a depth of 172-198 feet is pumped for 7 gpm, but probably has a greater potential.
What to read after Water Resources Survey: Hill County, Montana 1967?
You can find similar books in the "Read Also" column, or choose other free books by Montana State Water Conservation Board to read onlineMoreLess
To quickly assess the difficulty of the text, read a short excerpt:
Aquifer depths are 25 feet to 70 feet below the surface, and reported rates of withdrawal are 4 to 20 gpm pumping. Benches of ice-contact terraces rising slightly above the flood plain are reported near the town of Box Elder and water at a depth of 11 feet, in T. SON— R. 13E, where Barney's Coulee intersects the flood plain may be in one of these benches. The aquifer is re- ported as "coarse gravel entire depth," with a "supply of water unlimited." An estimate of withdraw- als from one well is ...given as 360,000,000 gallons per year, which is equivalent to an average of ahnost 1,000,000 gallons daily or approximately 700 gpm. Under the flood plain are valley fill sands and gravels in the preglacial Missouri valley from depths of about 50 feet to 200+ feet, which are fair aquifers. West of the town of Havre are several wells, 76 to 131 feet deep in sand and gravel; these are reportedly capable of small flow-yields and individually pump 125 to 300 gpm. Near the town of Box Elder valley-fill gravel from a depth of 172-198 feet is pumped for 7 gpm, but probably has a greater potential.
What to read after Water Resources Survey: Hill County, Montana 1967?
You can find similar books in the "Read Also" column, or choose other free books by Montana State Water Conservation Board to read onlineMoreLess
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