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Based off this usgs report is there bigger gold that needs to be found??? read below tell me what you think
Placer gold was discovered Blank name Creek in 1913 and mining occurred almost every year up to and possibly after WW II (Hoare and Cobb, 1977). The creek has not been glaciated. Gravels in the narrow flood plain, up to 300 feet wide, were 14 feet thick at the mouth and thinned upstream to thicknesses of 1 to 4 feet (Maddren, 1915). About 2.5 miles of the creek were mined, mostly by crude hand methods that, before WWII, included ripping up and washing individual bedrock slabs. The recovered gold was coarse and included flat, pumpkin-seed-size nuggets. The grade ran from 0.06 to 0.12 ounce of gold per square foot of bedrock. Panning of the tailings after WW II recovered much fine gold (Hoare and Cobb, 1977, p. 6). An alluvial bench, with gravels up to 10 feet thick, is present along the east side of the creek. Gold is reported to be present throughout the bench gravels (Hoare and Cobb, 1977). Bedrock in the drainage is mostly clastic sedimentary rocks of the mid-Cretaceous Kuskokwim Group. These rocks are intruded and thermally metamorphosed by an Upper Cretaceous felsic stock in the headwaters of the creek; dikes and sills are present locally elsewhere (Hoare and Cobb, 1977; Box and others, 1993).
Placer gold was discovered Blank name Creek in 1913 and mining occurred almost every year up to and possibly after WW II (Hoare and Cobb, 1977). The creek has not been glaciated. Gravels in the narrow flood plain, up to 300 feet wide, were 14 feet thick at the mouth and thinned upstream to thicknesses of 1 to 4 feet (Maddren, 1915). About 2.5 miles of the creek were mined, mostly by crude hand methods that, before WWII, included ripping up and washing individual bedrock slabs. The recovered gold was coarse and included flat, pumpkin-seed-size nuggets. The grade ran from 0.06 to 0.12 ounce of gold per square foot of bedrock. Panning of the tailings after WW II recovered much fine gold (Hoare and Cobb, 1977, p. 6). An alluvial bench, with gravels up to 10 feet thick, is present along the east side of the creek. Gold is reported to be present throughout the bench gravels (Hoare and Cobb, 1977). Bedrock in the drainage is mostly clastic sedimentary rocks of the mid-Cretaceous Kuskokwim Group. These rocks are intruded and thermally metamorphosed by an Upper Cretaceous felsic stock in the headwaters of the creek; dikes and sills are present locally elsewhere (Hoare and Cobb, 1977; Box and others, 1993).