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<br />The geology of the Gore Creek watershed <br />varies from older Precambrian-age basement rocks <br />to Quaternary-age alluvial deposits (Jig. 3). The <br />Precambrian rocks. which are predominantly igneous <br />with some metamorphics. fonn the mountains in the <br />northem and eastern parts of the watershed. The head- <br />waters area of Gore Creek consist~ of predominantly <br />igneous rocks. Fractured Precambrian rocks generally <br /> <br /> <br />yield small quantities of water that are adequate only for <br />domestic supplies. Where the Precambrian rocks are frac- <br />tured. water may discharge from springs. Water from <br />these rocks is suitable for all uses (Voegeli. 1965). <br />Sedimentary rocks of pre-Pennsylvanian Paleozoic. <br />Pennsylvanian. and Pennian age crop out in the southern <br />and western parts of the water~hed. Rocks in the Black <br />Gore Creek watershed are predominantly sedimentary. <br /> <br />01 <br />~ Od <br />\, <br /> <br />EXPLANATIO:>i <br />UNCONSOLIDATED SURFICIAL DEPOSITS AND <br />ROCKS OF QUATERNARY AGE <br />GRAVEL AND AlLUVIUM (PINEDALE AND <br />BULL LAKE AGE)-Indudes Broadway and Lou\'iers Alluviums <br />GLACIAL DRIFT OF PI~EDALE AND BULL LAKE GlAClATIQ!\"S- <br />Includes ).Orne unclassified glacial deposils <br />OLDER GLACIAL DRIFT (PRE-BULL LAKE AGE) <br />LANDSLIDE DEPOSITS-Locally includes talus. rock-glacier. and <br />thick colluvial depo,il' <br />Ar-;'C1EST ALLUVIUM-In isolated palches that may nOl all be of <br />the !>ameage <br />SEDI~1ENTARY ROCKS OF PERMIAN A:\'D PE~~SYLVA;.llA!\ AGE <br />MAROON FORMATIOJ\"-Arkosic sandslon.... sihstone. conglomerate. <br />and locallimeslone <br /> <br />~ <br />~ <br />~ <br />lQiJ <br />Jii!l <br />[fui <br /> <br />[I\m <br /> <br />SEDIME;.lTARY ROCKS OF PENNSYLVANIAf\ AGE <br /> <br />MI~TUR:'Il FORMATION IN WEST-CENTRAL Af\D SOUTH-CENTRAL <br />COLORADO AI'D aTHER Ul\rrS OF MIDDLE PE:-JNSYLVA~IAf\ <br />AGE-Arkosic <,aoostune. eOflgJomerale. shale. and limestone <br /> <br />BlaTlllC Gf\EISS. SCHIST. A1'\D \t1G\1ATITE-I..<x:allv contains minor <br />hornblende gneiss. calc-silicate rock. quartzite. and marble. Derived <br />principally from sedimentary r(K."h <br /> <br />IGNEOUS ROCKS <br /> <br />GRA1\"ITIC ROCKS OF 1.7OQ-r-.1.y. AGE GROUP (1.650-1.7.30 \.ULLlON YEARS)--. <br />Indudc:s Bakers Bridge. Bro","-ns Pass. Powdcrhom. and Tcnmile Granites; <br />Boulder Creek, Denny Creek. Kroenke. and Pill" I\lcmlow Granodiorite,: <br />ero,s Creek Quartz Montnnites; and unnamed granitic rocks <br /> <br />~ <br /> <br />SEDlI\IENTARY ROCKS OF PRE.PEl\l'\SYLVAl'\IAN AGE <br />META\tORPHIC ROCKS Or PRECAMBRIAN AGE <br /> <br />o <br />I <br />o <br /> <br />5 MILES <br /> <br />mil <br /> <br />~ <br /> <br />Figure 3. Geology of the Gore Creek watershed. <br /> <br />2 <br /> <br />3 4 <br /> <br />" <br /> <br />" <br /> <br />2 <br /> <br />4 <br /> <br />5 KILOMETERS <br /> <br />3 <br /> <br />6 Gore Creek Watershed, Colorado-Assessment of Historical and Current Water Quantity. Water Quality, <br />and Aquatic Ecology, 1968-98 <br />