Structure of the Tarkio Limestone along the Humboldt Fault zone in southeastern Nebraska
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Structure of the Tarkio Limestone along the Humboldt Fault zone in southeastern Nebraska

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Published by Conservation and Survey Division, Institute of Agriculture and Natural Resources, University of Nebraska--Lincoln in [Lincoln] .
Written in English

Subjects:

Places:

  • Nebraska,
  • Richardson Co.,
  • Pawnee Co.

Subjects:

  • Limestone -- Nebraska -- Richardson Co.,
  • Limestone -- Nebraska -- Pawnee Co.,
  • Geology, Stratigraphic -- Pennsylvanian.,
  • Geology -- Nebraska -- Richardson Co.,
  • Geology -- Nebraska -- Pawnee Co.

Book details:

Edition Notes

Bibliography: p. 10.

StatementR. R. Burchett and J. L. Arrigo.
SeriesReport of investigations - Nebraska Geological Survey ; no 4, Report of investigations (Nebraska Geological Survey) ;, no. 4.
ContributionsArrigo, J. L., joint author.
Classifications
LC ClassificationsQE471.15.L5 B85
The Physical Object
Pagination112 p. :
Number of Pages112
ID Numbers
Open LibraryOL4069110M
LC Control Number79622632

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Stanford Libraries' official online search tool for books, media, journals, databases, government documents and more. Buy Structure of the Tarkio Limestone along the Humboldt Fault zone in southeastern Nebraska (Report of investigations - Nebraska Geological Survey ; no 4) by Burchett, Raymond R (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : Raymond R Burchett. Structure of the Tarkio Limestone Along the Humboldt Fault Zone in Southeast Nebraska (GSI-4) $ Thickness and Structure Maps of the Pennsylvanian and Permian Rocks Across Southern Nebraska (GSI-7) Twelve Maps Summarizing the Geologic Framework of Southeastern Nebraska (GSI-1) $ Add to Cart. Structure of the Tarkio Umestone along the Humboldt Fault Zone in southeastern Nebraska: University of Nebraska-Uncoin, Conservation and Survey Division Jan p.

Option 2: In the image below the red lines are structure contours on a fault, showing the elevation in feet above sea level of the Tarkio limestone. This is in the area of the Humboldt fault zone, SE Nebraska. Hand contour the data, also interpreting where you think the faults may lie.   The Humboldt Fault Zone was first recognized as a series of discontinuous fault segments east of the Nemaha Anticline near the Nebraska border (Condra, ). The Humboldt Fault Zone is now known as a major north–northeast-trending basement fault zone related to the Ga. Midcontinent Rift System (Berendsen, ). Failed rifts and ancient suture zones can provide weak zones suitable for reactivation in successive deformation events. The amount and type of reactivated movement occurring on any given fault is primarily a function of the stress ratio on the fault, the coefficient of friction of the rock (that is, the slip tendency), and the dip of the weak plane within the rock mass [14,15,16]. Book. Jan ; Fabien Lesguer Structure of the Tarkio Limestone Along the Humboldt Fault Zone in Southeast Nebraska tectonic structure and geomorphological setting are reviewed in the.

Start studying Geology Exam 2. Learn vocabulary, terms, and more with flashcards, games, and other study tools. An earthquake is caused by the sudden release of slowly accumulating strain energy along a fault within the earth's crust. Areas of surface or underground fracturing that can experience earthquakes are known as earthquake fault zones. Some 15 percent of the world's earthquakes occur in Latin America, concentrated in the western cordillera. Raymond R. Burchett has written: 'Structure of the Tarkio Limestone along the Humboldt Fault zone in southeastern Nebraska' -- subject(s): Geology, Limestone, Stratigraphic Geology 'Inventory of. A through G identify rock layers and Q represents a fault. Lines W, X, Y, and Z are locations of unconformities. The rocks have not been overturned. The movement of bedrock along fault Q most probably produced A. gaps in the rock record B. an earthquake C. a volcanic lava ow D. zones .