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         Faults Geology:     more books (100)
  1. Geology of Mexico: Celebrating the Centenary of the Geological Society of Mexico (Special Paper (Geological Society of America))
  2. Faults and Subsurface Fluid Flow in the Shallow Crust (Geophysical Monograph)
  3. Active faults of Pakistan: Map sheets and inventories (Special publication)
  4. Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali Fault Systems of Southwestern Sichuan and Central Yunnan, China (Special Paper (Geological Society of America))
  5. An Excursion Guide to the Moine Geology of the Scottish Highlands by I. Allison, F. May, 1988-02
  6. It's Your Fault: The San Jacinto Valley Faults by K. Scott Bullock, 1992
  7. Exhumation Associated With Continental Strike-Slip Fault Systems (Special Paper (Geological Society of America))
  8. Active Tectonics of the Devils Mountain Fault and Related Structures, Northern Puget Lowland and Eastern Strait of Juan De Fuca Region, Pacific (U.S. Geological Survey Professional Paper, 1643)
  9. Structural Geology in Reservoir Characterization (Special Publication No. 127) by M. P. Coward, S. Daltaban, et all 1998-01-01
  10. The Geometry of Normal Faults (Geological Society Special Publication) by A. M. Roberts, G. Yielding, 1991-01
  11. Earthquake Proof Design and Active Faults
  12. The Seismogenic Zone of Subduction Thrust Faults (MARGINS Theoretical and Experimental Earth Science Series)
  13. Seismic Interpretation of Contractional Fault-Related Folds: An AAPG Seismic Atlas (AAPG Studies in Geology) by John H. Shaw, 2004-08-01
  14. The Internal Structure of Fault Zones: Implications for Mechanical & Fluid-Flow Properties - Special Publication no 299 by Geological Society Publishing House, 2008-07-15

21. Faults (Geology) (Open Library)
Publishing History This is a chart to show the publishing history of editions of works about this subject. Along the X axis is time, and on the y axis is the count
http://openlibrary.org/subjects/faults_(geology)

22. Alibris: Faults Geology,
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23. Faults And Folds
FORCES, FAULTS AND FOLDS. Forces, ultimately from plate tectonics, act on rock and cause it to break (fault) or fold (fold). FORCES
http://wc.pima.edu/~bfiero/tucsonecology/setting/geology_faults.htm
rock types faults/folds real faults/folds geological concepts ... Tucson geology
FORCES, FAULTS AND FOLDS
Forces, ultimately from plate tectonics , act on rock and cause it to break (fault) or fold (fold). FORCES Tension : pulling apart Compression : pushing together Shear (Lateral) : sliding past FAULTS: when rocks break due to force. Put mouse cursor in image to see force applied to it. Normal Fault
Caused by tension Reverse Fault
Caused by compression Strike-Slip Fault
Caused by shear (lateral) forces FOLDS: when rocks bend due to force. Put mouse cursor in image to see force applied to it. Anticline
Caused by compression
Folded up like an "A" Syncline
Caused by compression
Folded down like a "U" Now, are you ready to apply your new knowledge on the real thing
Email Me
Site Map Pima Community College

24. Nature: Earthquakes & Volcanoes: Faults (geology) Books
Faults (geology) Books. Discount prices on, MesoScale Shear Physics in Earthquake and Landslide Mechanics, Post-Miocene Right Separation on the San Gabriel and Vasquez Creek
http://www.allbookstores.com/Nature/Earthquakes_and_Volcanoes/Faults_(Geology).h
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25. Fault (geology) -- Britannica Online Encyclopedia
fault (geology), in geology, a planar or gently curved fracture in the rocks of the Earth’s crust, where compressional or tensional forces cause relative displacement of the
http://www.britannica.com/EBchecked/topic/202708/fault
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fault
Table of Contents: fault Article Article Related Articles Related Articles External Web sites External Web sites Citations ARTICLE from the fault in geology, a planar or gently curved fracture in the rocks of the , where compressional or tensional forces cause relative displacement of the rocks on the opposite sides of the fracture. Faults range in length from a few centimetres to many hundreds of kilometres, and displacement likewise may range from less than a centimetre to several hundred kilometres along the fracture surface (the fault plane). In some instances, the movement is distributed over a fault zone composed of many individual faults that occupy a belt hundreds of metres wide. The geographic distribution of faults varies; some large areas have almost none, others are cut by innumerable faults. Faults may be vertical, horizontal, or inclined at any angle. Although the angle of inclination of a specific

26. Faults (geology) An-Najah Libraries
AnNajah Libraries
http://libraries.najah.edu/books/all/Faults (geology)

27. Sedona Geology
INTRODUCTION TO SEDONAAREA GEOLOGY Sedona Rocks. Sedona’s rocks are red because they contain iron oxide (hematite). Most of the red rock layers are sandstones whose red color
http://www.naturescience.org/naturalhistory_sed/sedonageology.html
INTRODUCTION TO SEDONA-AREA GEOLOGY Sedona Rocks
  • Sedona is built on the soft shale of the Hermit Formation.
Stage 1: 1,800-1,700, then 515-251, then 251-65 Million Years Ago

Southwest Northeast Three Eras, Three Sets of Layers
The Yavapai Supergroup (bottom layers) formed by plate tectonic processes as volcanic mountains collided with western North America. After a billion years of erosion, the mountains were reduced to a flat layer of schist (gray), granite (pink), and volcanic rocks containing rich copper deposits (black). Above these mountain roots Paleozoic sedimentary layers (blue, red, tan) and Mesozoic layers (green) formed. Most of these layers accumulated on top of a slowly subsiding western margin of North America. Stage 2: 80-40 Million Years Ago Uplift
Stage 3: 28-15 Million Years Ago Erosion
Near the Central Arizona Highlands, erosion removed rock strata, stripping everything away down to the Hermit Shale. Inch by inch, removal of the easily-eroded, soft shale undermined the harder cliffs above. This caused the overhanging strata to cave in. As this process progressed, a cliff formed, the ancestral Mogollon Rim, and the cliff slowly retreated toward the north.
Stage 4: 15 Million Years Ago to Present Lava Flows and Faulting
This most recent stage started with volcanoes and lava flows. These are still visible today at the tops of cliffs near Sedona (red-orange layer). A little later the Verde Fault, along the west side of the Verde Valley, caused a large lake to form there. This fault also exposed the copper deposits of Jerome. A smaller fault occurred along the future path of Oak Creek Canyon, promoting erosion and development of the canyon.

28. Alibris: Thrust Faults Geology,
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29. Table Of Contents For Tectonic Faults
Stephen A. Miller, Claudio L. Rosenberg, Janos Urai, and Bruce W.D. Yardley Author Index Subject Index Library of Congress Subject Headings for this publication Faults (Geology).
http://catdir.loc.gov/catdir/toc/ecip072/2006033362.html
Table of contents for Tectonic faults : agents of change on a dynamic Earth / Mark R. Handy, Greg Hiath, Niels Hovius.
Bibliographic record and links to related information available from the Library of Congress catalog. Note: Contents data are machine generated based on pre-publication provided by the publisher. Contents may have variations from the printed book or be incomplete or contain other coding.
Library of Congress Subject Headings for this publication: Faults (Geology).
Geodynamics.

30. Butler County, Ohio - Geology
Geology. The county is located in the till plain region of the state. Bedrock underlying the county is primarily ordovicianage interbedded limestone and shale.
http://www.rootsweb.ancestry.com/~ohbutle2/geology.html
Search billions of records on Ancestry.com
Geology
  • The county is located in the "till plain" region of the state. Bedrock underlying the county is primarily ordovician-age interbedded limestone and shale. The area was covered with Wisconsinan ground moraine glaciers approximately 14,000 to 24,000 years ago. Karst openings (sinkholes and caves resulting from erosion of the bedrock) are relatively uncommon despite the limestone and shale bedrock. The three most common soil series types in Butler County are Miamian, Kokomo, and Eldean soils. Butler County is located in Ohio soil region 4. Characteristics of the soils in this region are:
      98% of the soil in this region is greater than 40 inches deep over the underlying bedrock. In 17% of the soil, the seasonal high water table lies less than a foot below the surface of the soil 22% of the soil has a clay content of more than 27% in the topsoil 20% of the soil has more than 3% organic matter in the upper 10 inches (good for agriculture) 19% of the soil has more than 8% slope (this is not good for farming or building)
    Seismographic events are relatively uncommon in the area. On January 11, 1983 at 9:41 pm, an earthquake centered near Hamilton! registered 2.0 on the Richter scale but was not felt by residents.

31. Finding Faults
A Seismic Jigsaw Puzzle Takes Shape. Jeff Babcock should have heard his future calling him back in grade school. When the teacher told
http://explorations.ucsd.edu/faults/
A Seismic Jigsaw Puzzle Takes Shape San Diego At Risk Hi-Ho Hi-Ho It's Off To Sea We Go The L-Cheapo World Tour A Seismic Jigsaw Puzzle Takes Shape Jeff Babcock should have heard his future calling him back in grade school. When the teacher told the class it was free drawing time, he was the kid sketching volcanoes. Robert Gordon Sproul as Babcock maps in detail an offshore earthquake fault system. He uses an innovative seismometer developed by his team at Scripps. On this October day, Babcock, fellow geophysicists Graham Kent and Alistair Harding, and graduate students Renee Bulow and Jeff Dingler are retrieving eight of the instruments from the ocean floor. Scientists have tended to stop at such boundaries, but the unknown fault might harbor even more destructive power than realized. Just as the IGPP team, which includes institute Director John Orcutt, was getting funding to build the seismographs, other scientists suggested that the Oceanside Fault could produce quakes with magnitudes exceeding 7.0 on the Richter scale, the same size as temblors that damaged San Francisco in 1989 and Northridge, California, in 1994.

32. Seismology/ Geology Glossary
aftershock. Any earthquake which occurs after a larger earthquake (a mainshock) within one rupturelength of the original fault rupture and before the seismicity rate in that area
http://www.data.scec.org/glossary.html
aftershock
    Any earthquake which occurs after a larger earthquake (a mainshock ) within one rupture-length of the original fault rupture and before the seismicity rate in that area has returned to the background (pre-mainshock) level is generally considered an aftershock. For some earthquakes, a specific "aftershock zone" may be defined, in lieu of the one-rupture-length rule given above.
afterslip
    Aseismic slip, very similar to creep , that occurs along a fault ruptured by a large earthquake in the months following that event.
alluvium
    Loose material clay, silt, sand, gravel, and larger rocks washed down from hills and mountains and deposited in low areas.
Alquist-Priolo Act
Basin and Range
    An area of the southwestern United States characterized by roughly parallel mountain ranges and valleys, formed by a series of tilted fault blocks, and brought about by tectonic extension of the region. As is true of any region experiencing crustal extension, normal faulting is common here. (This name can apply generally to any zone of similar landforms and tectonics.)
blind thrust fault
    A shallow-dipping reverse fault which terminates before it reaches the surface. When it breaks, therefore, it may produce uplift, but never any clear surface rupture. Many still-unknown blind thrust faults may exist in southern California. Two examples of known blind thrust faults: the Elysian Park Thrust, which runs underneath downtown Los Angeles and the Northridge Thrust Fault, which ruptured in the 1994 Northridge quake.

33. Faults (Geology) Geology Remote Sensing. Rifts (Geology
Faults (Geology) Geology Remote sensing. Rifts (Geology) Africa, Eastern. Rifts (Geology) Botswana Okavango Rift Zone.
http://scholarsmine.mst.edu/thesis/pdf/kinabo_09007dcc8048de9a.pdf

34. - Alaska Division Of Geological & Geophysical Surveys
News feed; Seismic hazards Denali Fault Earthquake Information. On November 3, 2002 an impressive, magnitude 7.9 earthquake ruptured several faults along the Denali fault system.
http://www.dggs.dnr.state.ak.us/?menu_link=engineering&link=denali_fault

35. GIS Datasets - New York State Museum -
Geographic Information System The datasets of the NYS Museum which are posted here are made freely available. Use of this data implies you understand the disclaimer
http://www.nysm.nysed.gov/gis/
Calendar GIS Shop Outreach ... Search
Navigation
Geographic Information System
The datasets of the NYS Museum which are posted here are made freely available.
  • Use of this data implies you understand the associated with it. Our Metadata references are available from the NYS GIS Clearinghouse
Data Format Information:
  • File Format: Data is distributed in ARC/INFO® EXPORT format (with ".e00") extension or ArcInfo Shapefile (".shp"). File Type: The EXPORT files are stored in DOS ASCII format. File Compression: Files are compressed with PKZIP 2.04g. File Decompression: Once downloaded to your site, the files can be decompressed using the software programs PKUNZIP in the DOS or Windows environment, or GUNZIP in the UNIX environment. UNIX users must change the ".zip" extension to ".e00.gz" before running GUNZIP on the files. UNIX users also have the option of using other UNIX shareware tools (such as ZIP for UNIX) to decompress the ".zip" file.
Dataset Guide:
The NYS Museum Dataset Guide has pertinent information on data files, including version and date of last update. This information is also available by viewing the metadata for each individual coverage in the

36. Geology Worksheets And Printable Activities
Geology for kids and students of all ages, from minerals and rocks, to volcanoes, earthquakes and tsunamis, tons of activities for the yound geologist on KBTeachers
http://www.kbteachers.com/geology-worksheets/

37. Linked Sequence Stratigraphic And Structural Evolution Of Prop-agating Normal Fa
Authors R. L. Gawthorpe, I. Sharp, J. R. Underhill, S. Gupta. Citations 13 Linked sequence stratigraphic and structural evolution of propagating normal faults Geology
http://academic.research.microsoft.com/Paper/3331830.aspx
var SiteRoot = 'http://academic.research.microsoft.com'; SHARE Author Conference Journal Year Look for results that meet for the following criteria: since equal to before
Publication
Linked sequence stratigraphic and structural evolution of prop-agating... Edit Linked sequence stratigraphic and structural evolution of prop-agating normal faults: Geology Citations: 13 R. L. Gawthorpe I. Sharp J. R. Underhill ... S. Gupta Published in 1997. Citation

38. Reverse Fault (geology) -- Britannica Online Encyclopedia
reverse fault (geology), Email is the email address you used when you registered. Password is case sensitive.
http://www.britannica.com/EBchecked/topic/500445/reverse-fault
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Table of Contents: reverse fault Article Article Related Articles Related Articles Citations LINKS Related Articles Aspects of the topic reverse fault are discussed in the following places at Britannica.
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MLA Style: reverse fault http://www.britannica.com/EBchecked/topic/500445/reverse-fault APA Style: reverse fault . (2010). In http://www.britannica.com/EBchecked/topic/500445/reverse-fault

39. CSU Libraries: Digital Repository: Results - Full
Strikeslip faults (Geology) Wyoming Wind River Basin. Thrust faults (Geology) Wyoming Wing River Basin. ix, 118 p. ill., maps (some col.), col. photos
http://digitool.library.colostate.edu/dtl_publish/18/84933.html

40. Books Books Books By Subject Nature Earthquakes & Volcanoes Faults (Geology) At
Faults (Geology) Rifts (Geology) Seismic prospecting; Seismology; Tsunamis; Ecology; Environmental Conservation Protection; Essays; Fish; Flowers; Forests Forestry
http://www.deepdiscount.com/books_books_books-by-subject_nature_earthquakes-volc

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