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Madison River

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Journal Article
Journal: AAPG Bulletin
Published: 01 May 1981
AAPG Bulletin (1981) 65 (5): 894.
... pipelines, coal gasification, shale retorting, or even in many places enlarged municipal water systems. The U.S. Geological Survey is, therefore, promoting the water resource potential of the Madison Group and Red River Formation. Such water is to be produced from depths of 2, 500 to 7, 500 ft (762 to 2...
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1980
AAPG Bulletin (1980) 64 (5): 674.
...A. H. Balch; M. W. Lee; J. J. Miller Abstract Intensive energy development activity in the Powder River basin of eastern Wyoming has placed heavy demands on the water resources of the state. The U.S. Geological Survey is therefore investigating the water resource potential of the Madison Group...
Journal Article
Journal: AAPG Bulletin
Published: 01 April 2004
AAPG Bulletin (2004) 88 (4): 405–432.
... are typically influenced by original facies heterogeneity, the early diagenetic environment, and later stage diagenetic overprint. The heterogeneities in the Mississippian Madison Formation in the Wind River basin of Wyoming are a complex interplay between these three factors whereby differences from the facies...
FIGURES | View All (19)
Journal Article
Journal: AAPG Bulletin
Published: 01 April 1967
AAPG Bulletin (1967) 51 (4): 529–557.
...W. J. Sando ABSTRACT The Madison Limestone of west-central Wyoming forms a wedge-shaped body of carbonate strata that tapers unevenly from a thickness of approximately 900 feet at the northern end of the Wind River Mountains to about 500 feet at Wind River Canyon and less than 200 feet...
FIGURES | View All (9)
Journal Article
Journal: AAPG Bulletin
Published: 01 May 1951
AAPG Bulletin (1951) 35 (5): 1107.
...M. E Denson, Jr.; S. Morrisey Norman Abstract Studies of both surface and subsurface sections of the Madison group in the Big Horn and Wind River basins, Wyoming, indicate that persistent units can be recognized by means of field data and insoluble residue analysis. From top to base the major units...
Image
Multiyear mean <span class="search-highlight">Madison</span> <span class="search-highlight">River</span> discharge (dashed curve and open circles) and ...
Published: 01 June 2008
Figure 2. Multiyear mean Madison River discharge (dashed curve and open circles) and Old Faithful eruption intervals (solid curve and filled circles) for the period 1937–1956. Old Faithful data are based on Yellowstone National Park ranger observations (Stephens, 2002). Number in parentheses
Journal Article
Published: 01 April 1962
Bulletin of the Seismological Society of America (1962) 52 (2): 163–180.
... of major faulting of the lake bottom. A part of the Madison Valley, west of Hebgen Lake, also subsided, though not as much, and a segment of the Madison Range fault was reactivated. At least part of the highway through Madison River Canyon, which cuts directly across the Madison Range between Hebgen Lake...
Journal Article
Published: 15 November 1994
Journal of Sedimentary Research (1994) 64 (4b): 542–559.
.... Detailed investigations of the morphology and deposits of asymmetric meander belts of the Madison River and its South Fork, southwestern Montana (using topographic mapping, ground-penetrating radar profiling, coring, sonar, and radiocarbon dating) have been undertaken in an attempt to show how...
Series: DNAG, Centennial Field Guides
Published: 01 January 1987
DOI: 10.1130/0-8137-5402-X.89
EISBN: 9780813754086
... Abstract The Hebgen Lake Earthquake Area, in southwestern Montana, extends westward from the east edge of Hebgen Lake through the Madison River Canyon, a narrow, deep gorge cut through the Madison Range, to Missouri Flats, west of the range. Hebgen Lake, about 8 mi (13 km) north of West...
Journal Article
Journal: Geology
Published: 01 March 1995
Geology (1995) 23 (3): 245–248.
... and Madison River valley, southwestern Montana, were affected during late Quaternary time by varying degrees of tectonic activity as well as by climate change through multiple glaciations; we are thus able to evaluate the impact of tectonism and climate on fan evolution. Two primary fan deposits were...
Journal Article
Journal: AAPG Bulletin
Published: 01 February 1987
AAPG Bulletin (1987) 71 (2): 135–155.
... of approximately 20 km 2 (8 mi 2 ) in the Madison Range of southwestern Montana. The Sphinx consists of more than 1,000 m (3,300 ft) of synorogenic boulder and cobble conglomerate derived from a Late Cretaceous Laramide uplift that was located in the area presently occupied by the Madison River valley...
FIGURES | View All (15)
Journal Article
Journal: GSA Bulletin
Published: 01 August 1970
GSA Bulletin (1970) 81 (8): 2287–2298.
... courses were influenced by the slope of the plain, barriers to northerly drainage, exhumed Tertiary valleys, and lowering of base level brought about by the Madison River. Tertiary topography was partially exhumed. 15 7 1969 27 2 1970 Copyright © 1970, The Geological Society of America...
Journal Article
Published: 01 May 1990
Journal of the Geological Society (1990) 147 (3): 461–467.
...J. ALEXANDER; M. R. LEEDER Abstract The valley and alluvial cone of the antecedent Madison River in the Missouri Flats area of SW Montana lie in a half-graben bounded by a prominent prehistoric fault scarp. Footwall-sourced alluvial fans and fans derived from a major transfer zone have prograded...
Journal Article
Journal: Geology
Published: 01 June 2008
Geology (2008) 36 (6): 451–454.
...Figure 2. Multiyear mean Madison River discharge (dashed curve and open circles) and Old Faithful eruption intervals (solid curve and filled circles) for the period 1937–1956. Old Faithful data are based on Yellowstone National Park ranger observations (Stephens, 2002). Number in parentheses...
FIGURES | View All (4)
Journal Article
Journal: GSA Bulletin
Published: 01 December 1984
GSA Bulletin (1984) 95 (12): 1413–1424.
... creep. Both the potential and the limitations of morphologic dating are demonstrated via measurements of a sequence of terrace scarps along the Madison River. The calculated relative ages are in agreement with the known relative ages, despite the fact that the gradient of the youngest scarp...
Journal Article
Published: 01 April 1962
Bulletin of the Seismological Society of America (1962) 52 (2): 153–162.
..., and landsliding of various types. None of the 28 fatalities resulted from failure of works of man-two were killed by a rolling boulder, the other 26 were buried by a 43 million cubic yard rockslide in the Madison River gorge six miles below Hebgen Dam. The aftershock record, although limited by the scarcity...
Image
Geospatial map of the Green <span class="search-highlight">River</span> Basin for the <span class="search-highlight">Madison</span> Limestone showing t...
Published: 01 January 2010
Figure 10. Geospatial map of the Green River Basin for the Madison Limestone showing the variation in TDS relative to well locations.
Image
—Correlation of sections of the <span class="search-highlight">Madison</span> Limestone in Wind <span class="search-highlight">River</span> Mountains. ...
Published: 01 April 1967
Fig. 3. —Correlation of sections of the Madison Limestone in Wind River Mountains. 1, Buck Spring; 2, Sweetwater Canyon; 3, Little Popo Agie Canyon; 4, Sinks Canyon (North); 5, Washakie Reservoir; 6, Bull Lake Creek; 7, Dinwoody Canyon; 8, Warm Spring Canyon. Sacajawea Member used in sense
Image
—Thickness map of <span class="search-highlight">Madison</span> Limestone in Wind <span class="search-highlight">River</span> basin.
Published: 01 November 1965
FIG. 7. —Thickness map of Madison Limestone in Wind River basin.
Image
—Stratigraphic sections of <span class="search-highlight">Madison</span> Group in Sun <span class="search-highlight">River</span> Canyon area, Montana,...
Published: 01 November 1962
Fig. 3. —Stratigraphic sections of Madison Group in Sun River Canyon area, Montana, with carbonate analyses and positions of faunal collections.