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<br />of today. Water and wind shaped the major topographic features of <br />the area as valleys deepened and younger streams were superimposed <br />on the older, underlying rock. <br /> <br />Fruita lies at an elevation of approximately 4,500 feet <br />southern part of the Grand Valley, a wide, gently sloping <br />corridored by high, rocky cliffs. To the north, the <br />gradually ascends for several miles to the base of Book <br />which rise abruptly to more than 8,000 feet. Approximately <br />south of town, the steep sandstone and shale formations <br />Colorado National Monument (or the Uncompahgre Uplift) <br />Frui ta is part of the Canyon Lands, a subdi vi s ion of a <br />physiographic region known as the Colorado Plateaus. <br /> <br />in the <br />valley <br />valley <br />Cliffs, <br />2 mi les <br />of the <br />begin. <br />larger <br /> <br />The climate of Fruita is classified as arid to semiarid. The <br />mountainous regions around Frui ta are subject to moderately heavy <br />precipitation. Elevation greatly influences the precipitation <br />amounts. Annual preclpltation at Fruita averages approximately <br />9 inches. The higher mesas (headwaters and primary drainage areas <br />of Little Salt Wash) receive from 10 to 20 inches, while the <br />mountainous regions (headwaters of the Colorado River) average <br />approximately 40 inches. Convection-type cloudburst storms of <br />small aerial extent and general rainfall over large areas normally <br />make August, September, and October the wettest months of the year. <br />Most wintertime precipitation occurs as snow, and a deep snowpack <br />normally accumul.ates at the higher elevations. Average snowfall <br />ranges from approximately 19 inches at Fruita to approximately 72 <br />inches in the mountainous regions surrounding Fruita. Snowfall is <br />generally dominated by a few large storms. Snowpack ordinarily <br />begins in late October. Snowmelt generally begins in late April <br />and continues through early July. <br /> <br />The temperature extremes at Frui ta are evidenced by mean maximums <br />ranging from approximately 38'F in January to approximately 94'F in <br />July, and by mean minimums ranging from approximately 150F in <br />January to 62'~' in July. Cooler temperatures prevail in higher <br />mountain areas. Record low and high temperatures are -34'F and 64'F <br />for January and 380F and 111'F for July, respectively. The growing <br />season usually extends for approximately 190 days. <br /> <br />The soils in the <br />infiltration rate <br />degree of runoff. <br /> <br />Fruita area have a <br />and characteristically <br /> <br />low to <br />allow a <br /> <br />moderately <br />somewhat <br /> <br />low <br />high <br /> <br />The natural vegetation of the Grand Valley, where not disturbed by <br />human encroachment, consists of desert shrubs (such as winterfat <br />and sagebrush), cottonwood trees, willow trees, and an understory <br />of hardy grasses. Agricultural operations in the valley consist <br />mainly of fruit, vegetable, and livestock feed crops. Between <br />elevations of 5,000 and 8,000 feet (headwaters of Little Salt Wash <br />and primary drainage area of the Colorado River upstream of <br />Fruita), pinon pine, juniper, oak, big sagebrush, serviceberry, and <br />Douglas fir trees are prominent. From an elevation of 8,,000 feet <br />to timberline (headwaters of Colorado River), vegetation consists <br /> <br />5 <br />