FORCE PMC234 module card stock

FORCE PMC234 module card stock

Technical data of product parameters

Precipitation is the source of the water in the bedrock aquifers in the Colorado Plateau.
The normal annual precipitation on the plateau ranges from less than 6 to more than 40 inches. but on most of the plateau the precipitation is less than 12 inches (fig. 2).
The High Plateaus section has the greatest precipitation and more than 16 inches falls on PMC23
most of the section. In addition to providing recharge to the aquifers. there is sufficient precipitation to maintain the flow of several perennial streams that are tributary to the Colorado
River or that flow into the Great Basin.
In the Canyon Lands section. peaks in the Henry, La Sal, and Abajo Mountains receive
more than 30 inches of percipitation. These areas are very small in comparison to the vast
area of the Canyon Lands, however, al’1d less than 10 inches falls on most of the section. Few
perennial streams head in the section.
In the Uinta Basin section, high areas along the south flank and on the west end receive PMC23
more than 30 inches of precipitatio\1; but these areas are small in comparison to the size of
the basin. Less than 12 inches falls on most of the basin. A large part of the Uinta Mountains north of the Uinta Basin receives more than 30 inches of precipitation. These mountains
contribute a large amount of water to the bedrock aquifers along the north edge of the basin,
and several perennial streams head in the mountains and flow into the basin.The water from oil wells, abandoned oil tests converted to water wells, and springs in
the Weber Sandstone ranges from about 400 t-o 2.600 ppm of dissolved solids (fig. 5 and table
2). The source of the water in the Weber is from recharge to areas of outcrop in Split PMC23
Mountain and along the south flank of the Uinta Mountains.
Oil wells in the Ashley Valley oil field produce water from the Weber Sandstone. but
some of the water possibly comes from limestone of Pennsylvanian and Mississippian ages
which underlies the Weber (Goode and Feltis. 1962. p. 12). Normal faults in the oil field,
described by Peterson (1957, p. 191), could {:Ossibly form conduits between the underlying
limestones and the Weber. Some of the wells in the Ashley Valley oil field are open to
both the Weber and the overlying Phosphoria Formation. and the range in dissolved solids
in water from these wells is about 500 to 2.600 ppm (fig. 5 and table 2).

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