Carol A Finn, Ph.D. (Former Employee)
Science and Products
Filter Total Items: 131
A report of field surveys for the Transantarctic Mountains Aerogeophysical Research Activities (TAMARA) Program A report of field surveys for the Transantarctic Mountains Aerogeophysical Research Activities (TAMARA) Program
No abstract available.
Authors
Carol A. Finn, Detlef Damaske, Terry Wilson
Aeromagnetic evidence for a volcanic caldera(?) complex beneath the divide of the West Antarctic Ice Sheet Aeromagnetic evidence for a volcanic caldera(?) complex beneath the divide of the West Antarctic Ice Sheet
A 1995–96 aeromagnetic survey over part of the Sinuous Ridge (SR) beneath the West Antarctic Ice Sheet (WAIS) divide shows a 70-km diameter circular pattern of 400–1200-nT anomalies suggesting one of the largest volcanic caldera(?) complexes on earth. Radar-ice-sounding (RIS) shows the northern part of this pattern overlies the SR, and extends south over the Bentley Subglacial Trench...
Authors
John C. Behrendt, C. A. Finn, D. Blankenship, R.E. Bell
Something old, something new, something borrowed, something blue: A new perspective on seismic hazards in Washington using aeromagnetic data Something old, something new, something borrowed, something blue: A new perspective on seismic hazards in Washington using aeromagnetic data
No abstract available.
Authors
Carol A. Finn, W. D. Stanley
Preliminary merged aeromagnetic map of Oregon Preliminary merged aeromagnetic map of Oregon
No abstract available.
Authors
C. W. Roberts, R.J. Blakely, C. A. Finn
Seismic reflection images beneath Puget Sound, western Washington State: The Puget Lowland thrust sheet hypothesis Seismic reflection images beneath Puget Sound, western Washington State: The Puget Lowland thrust sheet hypothesis
Seismic reflection data show that the densely populated Puget Lowland of western Washington state is underlain by subhorizontal Paleogene and Neogene sedimentary rocks deformed by west and northwest trending faults and folds. From south to north beneath the Lowland, features seen on the seismic data include: the horizontally-stratified, 3.5 km thick Tacoma sedimentary basin; the Seattle...
Authors
T. L. Pratt, S. Johnson, C. Potter, W. Stephenson, Carol A. Finn
Patterns of late Cenozoic volcanic and tectonic activity in the West Antarctic rift system revealed by aeromagnetic surveys Patterns of late Cenozoic volcanic and tectonic activity in the West Antarctic rift system revealed by aeromagnetic surveys
Aeromagnetic surveys, spaced ≤5 km, over widely separated areas of the largely ice- and sea-covered West Antarctic rift system, reveal similar patterns of 100- to 1700-nT, shallow-source magnetic anomalies interpreted as evidence of extensive late Cenozoic volcanism. We use the aeromagnetic data to extend the volcanic rift interpretation over West Antarctica starting with anomalies over...
Authors
John C. Behrendt, R. Saltus, D. Damaske, A. McCafferty, C. A. Finn, D. Blankenship, R.E. Bell
Science and Products
Filter Total Items: 131
A report of field surveys for the Transantarctic Mountains Aerogeophysical Research Activities (TAMARA) Program A report of field surveys for the Transantarctic Mountains Aerogeophysical Research Activities (TAMARA) Program
No abstract available.
Authors
Carol A. Finn, Detlef Damaske, Terry Wilson
Aeromagnetic evidence for a volcanic caldera(?) complex beneath the divide of the West Antarctic Ice Sheet Aeromagnetic evidence for a volcanic caldera(?) complex beneath the divide of the West Antarctic Ice Sheet
A 1995–96 aeromagnetic survey over part of the Sinuous Ridge (SR) beneath the West Antarctic Ice Sheet (WAIS) divide shows a 70-km diameter circular pattern of 400–1200-nT anomalies suggesting one of the largest volcanic caldera(?) complexes on earth. Radar-ice-sounding (RIS) shows the northern part of this pattern overlies the SR, and extends south over the Bentley Subglacial Trench...
Authors
John C. Behrendt, C. A. Finn, D. Blankenship, R.E. Bell
Something old, something new, something borrowed, something blue: A new perspective on seismic hazards in Washington using aeromagnetic data Something old, something new, something borrowed, something blue: A new perspective on seismic hazards in Washington using aeromagnetic data
No abstract available.
Authors
Carol A. Finn, W. D. Stanley
Preliminary merged aeromagnetic map of Oregon Preliminary merged aeromagnetic map of Oregon
No abstract available.
Authors
C. W. Roberts, R.J. Blakely, C. A. Finn
Seismic reflection images beneath Puget Sound, western Washington State: The Puget Lowland thrust sheet hypothesis Seismic reflection images beneath Puget Sound, western Washington State: The Puget Lowland thrust sheet hypothesis
Seismic reflection data show that the densely populated Puget Lowland of western Washington state is underlain by subhorizontal Paleogene and Neogene sedimentary rocks deformed by west and northwest trending faults and folds. From south to north beneath the Lowland, features seen on the seismic data include: the horizontally-stratified, 3.5 km thick Tacoma sedimentary basin; the Seattle...
Authors
T. L. Pratt, S. Johnson, C. Potter, W. Stephenson, Carol A. Finn
Patterns of late Cenozoic volcanic and tectonic activity in the West Antarctic rift system revealed by aeromagnetic surveys Patterns of late Cenozoic volcanic and tectonic activity in the West Antarctic rift system revealed by aeromagnetic surveys
Aeromagnetic surveys, spaced ≤5 km, over widely separated areas of the largely ice- and sea-covered West Antarctic rift system, reveal similar patterns of 100- to 1700-nT, shallow-source magnetic anomalies interpreted as evidence of extensive late Cenozoic volcanism. We use the aeromagnetic data to extend the volcanic rift interpretation over West Antarctica starting with anomalies over...
Authors
John C. Behrendt, R. Saltus, D. Damaske, A. McCafferty, C. A. Finn, D. Blankenship, R.E. Bell
*Disclaimer: Listing outside positions with professional scientific organizations on this Staff Profile are for informational purposes only and do not constitute an endorsement of those professional scientific organizations or their activities by the USGS, Department of the Interior, or U.S. Government