William F. Cannon
William (Bill) Cannon is a Scientist Emeritus with the USGS Geology, Energy & Minerals (GEM) Science Center in Reston, VA.
Science and Products
Filter Total Items: 15
Filter Total Items: 105
Mineral-resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin
The Iron River 1° x 2° quadrangle contains identified resources of copper and iron. Copper-rich shale beds in t1n north part of the quadrangle contain 12.2 billion pounds (5.5 billion kg) of copper in well-studied deposits including 9.2 billion pounds (4.2 billion kg) that are economically mineable by 1980 standards. At least several billion pounds of copper probably exist in other parts of the sa
Authors
W. F. Cannon
Mineral resources of the Rainbow Lake Wilderness Area and the Flynn Lake Wilderness Study Area, Bayfield County, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, A. E. Grosz, M. L. Dunn, Gertrude C. Gazdik, J. J. Hill
Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, J. S. Klasner, A. E. Grosz, B. B. Williams
The potential for diamond-bearing kimberlite in northern Michigan and Wisconsin
Between 1876 and 1913, diamonds were found in at least seven localities in southern and central Wisconsin. All were found in Pleistocene glacial deposits or Holocene river gravel. The bedrock kimberlite source for the diamonds is unknown but has been presumed to be in northern Canada, the only area north of Wisconsin previously known to contain kimberlites. Recently, a kimberlite pipe, here named
Authors
William F. Cannon, M.G. Mudrey
Preliminary map of manganese provinces in the conterminous United States
No abstract available.
Authors
Edwin Wilson Tooker, William F. Cannon
Mineral resources of the Sturgeon River Wilderness Study Area, Houghton and Baraga counties, Michigan
No abstract available.
Authors
William F. Cannon, E. R. King, J. J. Hill, P. C. Mory
Bedrock geologic map of parts of Baraga, Dead River and Clark Creek basins, Marquette County, Michigan
No abstract available.
Authors
J. S. Klasner, W. F. Cannon, M. R. Brock
Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, J. S. Klasner, A. E. Grosz, B. B. Williams
The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan
Partly serpentinized peridotite of early Keweenawan age crops out in two places along a 20-kilometer-long zone of positive aeromagnetic anomalies in northern Marquette County, Michigan. Most of the area is mantled by Pleistocene drift with few bedrock exposures.Petrographic and electron microprobe studies show that the peridotite was originally a plagioclase lherzolite containing 40 to 50 percent
Authors
John S. Klasner, David W. Snider, W. F. Cannon, John F. Slack
Geologic map of the Iron River 1? X 2? Quadrangle, Michigan and Wisconsin
No abstract available.
Authors
William F. Cannon
Summary of the estimated iron resources of the Marquette and Gogebic Iron Ranges of Michigan
The U. S. Geological Survey in cooperation with the Geological Survey Division of the Michigan Department of Natural Resources has recently completed detailed studies of iron-bearing rocks in the Marquette and Gogebic iron ranges in the northern peninsula of Michigan. The study included mapping the surface distribution of the iron-bearing rocks over a period of nearly 20 years. During that time, m
Authors
William F. Cannon
Science and Products
Filter Total Items: 15
Filter Total Items: 105
Mineral-resource assessment of the Iron River 1° x 2° quadrangle, Michigan and Wisconsin
The Iron River 1° x 2° quadrangle contains identified resources of copper and iron. Copper-rich shale beds in t1n north part of the quadrangle contain 12.2 billion pounds (5.5 billion kg) of copper in well-studied deposits including 9.2 billion pounds (4.2 billion kg) that are economically mineable by 1980 standards. At least several billion pounds of copper probably exist in other parts of the sa
Authors
W. F. Cannon
Mineral resources of the Rainbow Lake Wilderness Area and the Flynn Lake Wilderness Study Area, Bayfield County, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, A. E. Grosz, M. L. Dunn, Gertrude C. Gazdik, J. J. Hill
Mineral-resource evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, J. S. Klasner, A. E. Grosz, B. B. Williams
The potential for diamond-bearing kimberlite in northern Michigan and Wisconsin
Between 1876 and 1913, diamonds were found in at least seven localities in southern and central Wisconsin. All were found in Pleistocene glacial deposits or Holocene river gravel. The bedrock kimberlite source for the diamonds is unknown but has been presumed to be in northern Canada, the only area north of Wisconsin previously known to contain kimberlites. Recently, a kimberlite pipe, here named
Authors
William F. Cannon, M.G. Mudrey
Preliminary map of manganese provinces in the conterminous United States
No abstract available.
Authors
Edwin Wilson Tooker, William F. Cannon
Mineral resources of the Sturgeon River Wilderness Study Area, Houghton and Baraga counties, Michigan
No abstract available.
Authors
William F. Cannon, E. R. King, J. J. Hill, P. C. Mory
Bedrock geologic map of parts of Baraga, Dead River and Clark Creek basins, Marquette County, Michigan
No abstract available.
Authors
J. S. Klasner, W. F. Cannon, M. R. Brock
Mineral resources evaluation of the Round Lake Wilderness Study Area, Price and Vilas counties, Wisconsin
No abstract available.
Authors
William F. Cannon, C. C. Cameron, J. S. Klasner, A. E. Grosz, B. B. Williams
The Yellow Dog peridotite and a possible buried igneous complex of lower Keweenawan age in the northern peninsula of Michigan
Partly serpentinized peridotite of early Keweenawan age crops out in two places along a 20-kilometer-long zone of positive aeromagnetic anomalies in northern Marquette County, Michigan. Most of the area is mantled by Pleistocene drift with few bedrock exposures.Petrographic and electron microprobe studies show that the peridotite was originally a plagioclase lherzolite containing 40 to 50 percent
Authors
John S. Klasner, David W. Snider, W. F. Cannon, John F. Slack
Geologic map of the Iron River 1? X 2? Quadrangle, Michigan and Wisconsin
No abstract available.
Authors
William F. Cannon
Summary of the estimated iron resources of the Marquette and Gogebic Iron Ranges of Michigan
The U. S. Geological Survey in cooperation with the Geological Survey Division of the Michigan Department of Natural Resources has recently completed detailed studies of iron-bearing rocks in the Marquette and Gogebic iron ranges in the northern peninsula of Michigan. The study included mapping the surface distribution of the iron-bearing rocks over a period of nearly 20 years. During that time, m
Authors
William F. Cannon