Structural Geology: Faults, Folds, And Fabrics 800 AM1200 PM, Colorado Convention Center C109. Structural geology faults,Folds, and Fabrics. John G. Solum and Alexander P. Bump, Presiding. http://gsa.confex.com/gsa/2002AM/finalprogram/session_3329.htm
Extractions: Session No. 13 Sunday, October 27, 2002 8:00 AM-12:00 PM, Colorado Convention Center: C109 Structural Geology: Faults, Folds, and Fabrics John G. Solum and Alexander P. Bump, Presiding Paper # Start Time 8:00 AM HANGINGWALL-TO-DETACHMENT TRANSITION AT A THIN-SKINNED EXTENSIONAL DETACHMENT FAULT IN THE EASTERN BLACK WARRIOR BASIN, ALABAMA : GROSHONG, Richard H. Jr and CATES, Luke M., Department of Geological Sciences, The Univ of Alabama, Tuscaloosa, AL 35487-0338, rhgroshong@cs.com 8:15 AM CHARACTER OF DEFORMATION ADJACENT TO THE SAN ANDREAS FAULT, DURMID HILL, CA : WOJTAL, Steven F., Oberlin, OH 44074, steven.wojtal@oberlin.edu. 8:30 AM TRANSIENT VERSUS LONG-TERM STRAIN ACCUMULATION ON THE BLACKWATER FAULT, EASTERN CALIFORNIA SHEAR ZONE : OSKIN, Michael E., Institute for Crustal Studies, Univ of California, Santa Barbara, 1140 Girvetz Hall, Santa Barbara, CA 93106, oskin@crustal.ucsb.edu. 8:45 AM 1.1 MA MELT PULSES IN PSEUDOTACHYLYTE FROM THE ALPINE FAULT, NZ : VAN DER PLUIJM, Ben A., Geological Sciences, Univ of Michigan, 2534 CC Little Building, Ann Arbor, MI 48109-1063, vdpluijm@umich.edu, WARR, Laurence N., Geologisch-Paläontologisches Institut, Ruprecht-Karls-Universität, Heidelberg, Germany, PEACOR, Donald R., Geological Sciences, Univ of Michigan, Ann Arbor, MI 48109, and HALL, Chris M., Geological Sciences, Univ of Michigan, 4534 CC Little Building, Ann Arbor, MI 48109-1063 9:00 AM FABRICS AND AGE OF CLAY GOUGE IN THE MOAB FAULT, UTAH, USA
STRUCTURAL GEOLOGY AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS STRUCTURAL geology AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS. We describethe kinematics and geometry of faults within the range to constrain the http://gsa.confex.com/gsa/2002AM/finalprogram/abstract_45716.htm
Extractions: Paper No. 191-20 Presentation Time: 8:00 AM-12:00 PM STRUCTURAL GEOLOGY AND TECTONICS OF THE FRANKLIN MOUNTAINS, WEST TEXAS WU, Kaiwen and ANDRONICOS, Chris L., Department of Geological Sciences, Univ of Texas at El Paso, 500 W. University Ave, El Paso, TX 79968, wu@geo.utep.edu 2002 Denver Annual Meeting (October 27-30, 2002)
Faults Strikeslip faults Movement along strike-slip faults is horizontal. Returnto Physical geology Online page. Return to Physical geology GSAMS page. http://www.dc.peachnet.edu/~pgore/geology/geo101/faults.htm
Death Valley Geology Gallery - Faults Death Valley National Park geology Image Gallery faults. Badwater Spring andfault Photo by Martin Miller. Black Mountain front Photo by Martin Miller. http://wrgis.wr.usgs.gov/docs/parks/deva/galfaults.html
SanGIS: GENERALIZED GEOLOGY AND FAULTS (Map DPLU0015) GENERALIZED geology AND faults. Map Number DPLU0015. Map Title GENERALIZED geologyAND faults. Map Purpose Differentiate geologic formation and fault locations. http://www.sangis.org/sangis/mapgal/dplu0015/
Extractions: Map Number: Map Title: GENERALIZED GEOLOGY AND FAULTS Map Purpose: Differentiate geologic formation and fault locations Date Created: Map Scale: no scale Map Size: 44" x 34" Creating Agency: County DPLU Map Contents: Faults and geologic formations in the San Diego County Update Frequency: N/A Removal Date: Description: Map showing the various geologic types and identifying fault
UCD Geology: GEL 20 - Faults And Earthquakes GEL 20 geology of California faults and Earthquakes . Dipslip faults.A. Normal Yellowstone, 1959; Fairview Peak, 1954; Dixie Valley http://www-geology.ucdavis.edu/~GEL20/W99_moores/handouts/faults.html
Structural Geology Notebook - Tear Faults The tear faults may be a result of drastic lateral changes when the Reference Twiss,Robert J. and Moores, Eldridge M.; Structural geology WH Freeman and http://maps.unomaha.edu/Maher/geo330/sandbox/tina3.html
Descriptive Structural Geology Of Faults 8 faults and faulting in van der Pluijm Marshak, 1997, Earth Structure An introduction to structural geology and tectonics. McGraw-Hill. http://maps.unomaha.edu/Maher/GEOL3300/week2/fault.html
Extractions: Description of faults Readings: This figure is from a core drilled into basement rocks of South Carolina and shows a pseudotachylite injection vein (red arrow), a pseudotachylite slip surface with secondary associated, high angle oblique microfaults (violet arrow), and a chloritized fault breccia (yellow arrow). The slip here is parallel to the gneissic layering. Notebook terms for week 2 Fault geometry: idealized as a plane with a vector of slip in it and offset and truncated layers. strike and dip of fault plane.
Major Faults & High-Strain Zones | The Geology Of Virginia Valley Ridge faults. Lowangle thrust faults of Alleghanian age (~300 Ma). Mesozoicfaults. Brittle normal faults of Mesozoic age (~200 Ma). CB- DR-, http://www.wm.edu/geology/virginia/faults.html
Structural Geology How rocks deform, and why, is the study of structural geology. Involves nearsurface to deep crustal processes. 396). Break slip faults (Monroe; fig. http://jersey.uoregon.edu/~mstrick/RogueComCollege/RCC_Lectures/Structural.html
Extractions: Revised 9 / 01 (Monroe 4th ed.) Including... Introduction Introduction to crustal stress Directed stress and crustal deformation Geologic structures ... Directed stress and plate tectonics Introduction Before we start, we need to review the following: There are 2 main earth elevations Above and below sea level There are 2 main earth processes Construction and Destruction Tectonics and surface weathering Over the course of geologic time these 2 are in balance There are 2 main igneous rocks Basalt and granite All three of these are inter-related (DESCRIBE) What we are studying tonight is the reality of tectonics DEFINE: Tectonics Tectonics: the study of earth processes which result in the creation and deformation of magma and rock Constructional processes My favorite part of geology (really should save to last!!) Some are real flashy: get some videodisc frames Volcanoes Earthquakes All involve stress at varying degrees of intensity Mt. St. Helens - good example of stress at the surface
North Cascades Geology: Forming Depressions Along Faults in the fault planes that open up gaps in the crust, or to have the faults discontinuousbut arranged in an en echelon pattern. USGS geology in the Parks home http://www.aqd.nps.gov/grd/usgsnps/noca/sb11faultbasins.html
Extractions: One way to get extension or stretching of the crust while blocks of crust are sliding past each other along large faults is to have irregularities in the fault planes that open up gaps in the crust, or to have the faults discontinuous but arranged in an en echelon pattern North Cascades geology home North Cascades National Park home
Extractions: Earthquakes were probably common in southwestern Indiana when several ancient faults that are found in the bedrock were formed, but no modern earthquakes are known to have been associated with them. Even more intense earthquakes in that region have been related to the New Madrid, Missouri, seismic zone, a major area of earthquake activity in the midcontinent region of North America. In 1811-12 three major earthquakes, centered in that area, were among the greatest in recorded history. The recurrence of such earthquakes could have disastrous consequences in Indiana. Recent mapping by the Indiana Geological Survey has located many of the bedrock faults in southern Indiana and has shown that they have been inactive in recent times. Increased knowledge of these structures will also help in exploring for and developing coal and petroleum that are associated with these faulted rocks. Our Hoosier State Beneath Us: Structural Geology
USDA Forest Service Pacific Southwest Region Forest geology Structure, faults and Folds BACK. CONTENTS Forest geologyby Tom Dibblee Geologic Structure, faults and Folds BACK. http://www.r5.fs.fed.us/lospadres/ecosystem/geology/forest_geology/forest_geo_st
Extractions: @import url(http://www.fs.fed.us/r5/global-websites/styles/screen.css); Skip navigation Forest Service National Links Forest Service Home Employment Fire and Aviation International Forestry Just for Kids Maps and Brochures Passes and Permits Photo and Video Gallery Publications Recreational Activities Research and Development State and Private Forestry Pacific Southwest Home About Us Contact Us Current Conditions ... Contact Web Manager Pacific Southwest Region TTY: 707.562.9130 The requested URL was not found on this server. The page you are looking for might have been removed, had its name changed, or is temporarily unavailable. Please try the following: Please address questions and comments to: Public Affairs The Pacific Southwest Region manages the National Forests in California and assists the State and Private forest landowners in California, Hawaii and the U.S. Affiliated Pacific Islands.
USDA Forest Service Pacific Southwest Region geology Geohazards Earthquakes faults BACK. CONTENTS GeohazardsEarthquakes Faulting BACK. Earthquakes and faults. A fault http://www.r5.fs.fed.us/lospadres/ecosystem/geology/geohazards/earthquakes.html
Extractions: @import url(http://www.fs.fed.us/r5/global-websites/styles/screen.css); Skip navigation Forest Service National Links Forest Service Home Employment Fire and Aviation International Forestry Just for Kids Maps and Brochures Passes and Permits Photo and Video Gallery Publications Recreational Activities Research and Development State and Private Forestry Pacific Southwest Home About Us Contact Us Current Conditions ... Contact Web Manager Pacific Southwest Region TTY: 707.562.9130 The requested URL was not found on this server. The page you are looking for might have been removed, had its name changed, or is temporarily unavailable. Please try the following: Please address questions and comments to: Public Affairs The Pacific Southwest Region manages the National Forests in California and assists the State and Private forest landowners in California, Hawaii and the U.S. Affiliated Pacific Islands.
Page Not Found faults in the Bryant Watershed. faults are breaks in the rock wheremovement of the rocks has occurred. Black lines represent faults. http://www.watersheds.org/blue/earth/faults.htm
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Page Not Found Geologic map of the Bryant Watershed area. Black lines represent faults. Colorsrepresent different rock formations. Back to Rock Structures faults. http://www.watersheds.org/blue/earth/faults01a.htm
Extractions: We're sorry, the page you are looking for could not be found. Due to the restructuring of our site, it may have moved to a new location. If you typed in the url, be sure the address is typed correctly. Search for the page with keywords. Use the search box in the navigation bar above. The navigation bar has links to the main areas on our site. View our site map to find a listing of the topics we have to offer. If you are unable to find what you're looking for, e-mail webkeeper@watersheds.org
Extractions: Figure F3. Simplified regional geology, including offshore faults and depocenters. Small circles locate active volcanoes, including Mt. Lamington (L), Mt. Victory (V), and Dawson Strait (D). The dashed line locates the landward boundary of oceanic crust, and the thin double lines locate the spreading axes. Ticks on normal faults indicate the downthrown side; triangles on reverse faults, the upthrusted side. Islands include Amphlett (A), D'Entrecasteaux (DE), Egum Atoll (E), Lusancay (LC), Misima (MI), Trobriand (T), and Woodlark (W). M = Moresby Strait, MR = Moresby rift, MS = Moresby Seamount.
Geology - North Carolina (1:250,000) Faults - Western North Carolina 1986 Ending_Date 19981201 Source_Currentness_Reference Data creation and editdates Source_Citation_Abbreviation geology faults, CGIA Source_Contribution http://www.lib.ncsu.edu/stacks/gis/regional/westnc/metadata/cgia83/landres/wgeo2
Extractions: Metadata also available as - [ Parseable text NCSU Libraries is responsible for this data set This data was created to assist governmental agencies and others in making resource management decisions through use of a Geographic Information System (GIS). This clipped coverage was created for use in conjunction with the Western North Carolina Region Data System.
Extractions: Title Source Type Format Scale Date Coverage Geologic Regions of North Carolina NCDENR Polygon ARC/INFO NC CGIA: Hydrogeology: NC Piedmont and Blue Ridge NCCGIA Polygon ARC/INFO Chesapeake Watershed Lithogeochemical Map: Lithogeochemical Map Units USGS Polygon Chesapeake Watershed Chesapeake Watershed Lithogeochemical Map: Sulfide Deposits USGS Polygon Chesapeake Watershed Chesapeake Watershed Lithogeochemical Map: Geologic Map Units USGS Polygon Chesapeake Watershed National Atlas: Generalized Geologic Map of the Conterminous US USGS Polygon Shapefile Conterminous US Lithochronologic Units and Mineral Deposits: Lithology USGS Polygon Shapefile/e00/SDTS Appalachian Region Quaternary Sediments: Miscellaneous Geologic Point Features USGS Point Shapefile/SDTS/e00 n/a North-Central US Lithochronologic Units and Mineral Deposits: Normal Thrusts USGS Line Shapefile/e00 Appalachian Region Mineral Resources: Igneous Rocks PLUTO USGS Polygon Shapefile n/a US USGS: Geology USGS Polygon E00/DLG Conterminous US USGS: Legend USGS Text E00/DLG Conterminous US South Carolina Piedmont and Blue Ridge: Geology USGS Polygon Shapefile/e00