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1999-03-08_PERMIT FILE - M1999025
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1999-03-08_PERMIT FILE - M1999025
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Last modified
3/16/2021 11:16:46 AM
Creation date
11/26/2007 8:12:21 AM
Metadata
Fields
Template:
DRMS Permit Index
Permit No
M1999025
IBM Index Class Name
Permit File
Doc Date
3/8/1999
Doc Name
CONSTRUCTION MATERIALS REGULAR 112 OPERATION RECLAMATION PERMIT APPLICATION FORM
Media Type
D
Archive
No
Tags
DRMS Re-OCR
Description:
Signifies Re-OCR Process Performed
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• <br />1997 <br /> <br />GRAND JUNCTION, <br />t COLORADO <br />Grand Junction is located at the junction of the <br />t Colorado and Gunnison Rivers. It is on the wes= <br />slope of the Rockies, in a large mountain valley. <br />The area has a clima_e marked by the wide seasonal <br />range usual to interior localities at this <br />' lot etude. Thanks, however, to the protective <br />topography of the vicinity, sudden and severe <br />weather changes are very infrequent. The valley <br />floor slopes from 9,800 feet near Palisade [o <br />4,900 feet at the west end near Fru it a. Mountains <br />are on all sides at distances of Erom 10 to 60 <br />miles and reach heights of 9,000 to over 12,000 <br />feet. <br />This mountain valley location, with attendant <br />' valley breezes, provides protection from spring <br />and fall frosts. This results in a growing season <br />averaging 191 days in the city. This varies <br />considerably in the outlying districts. IL is <br />' about the same in the upper valley around <br />?alisade, and 3 to 9 weeks shorter near the river <br />west of Grand Junction. The growing season is <br />suffice ent ly long co permit commercial growth of <br />almost all Eru its except citrus varieties. Summer <br />' grazing of cattle and sheep on nearby mountain <br />ranges is extensive. <br />The interior, co nCinental location, ringed by <br />' mountains on ail sides, results in quite law <br />precipitation ~n all seasons. Consequently, <br />ag ri cu lCUre a dependent on irrigatron. Adequate <br />supplies of water are available from mountain <br />snows and ra=ns. Summer ra irs occur chiefly as <br />t <br /> <br /> <br /> <br /> <br /> <br /> <br /> <br />(GJT) <br />scattered light showers and thunderstorms which <br />develop over nearby mountain S. Wl rater snOw'S die <br />fairly frequent, but are mostly light and quick to <br />melt. Even [he infrequent snows of from 9 to 8 <br />inches seldom remain on the ground for prolonged <br />periods. Bl rz zard conditions in the valley are <br />extremely rare. <br />Temperatures above 100 degrees are infrequent, and <br />about one-third of the winters have no readings <br />below zero. Summer days with maximum temperatures <br />in the middle 90s and minimums rn the low 60s <br />are common. Rel at.ve humrd icy is very low during <br />the summer, with values similar to ocher dry <br />locations such as the southern parts of New Mexico <br />aad Arizona. Spells of Cold wrnLer weather are <br />somet rmes prolonged due Lo cold air becomtng <br />trapped in the valley. Winds are usually very <br />light during the coldest weather. Changes in <br />winter are normally gradual, and abrupt changes <br />are much less frequent than in eastern Colorado. <br />Cold waves are rare. Sunny days predominate in all <br />seasons. <br />The prevailing wind is from the east-southeast due <br />co the valley breeze effect. The strongest <br />winds are assoc faced with thunderstorms or with <br />pre-frontal weather. They usually are from the <br />south or southwest. <br /> <br />
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