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Bath Glacier

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Journal Article
Published: 01 March 2004
Geological Magazine (2004) 141 (2): 247-248.
... of continental shelf erosion and supply of sediment to continental shelf, slope and deep marine basin environments. This volume is a valuable new addition to the Geological Society Special Publication series, with a range of papers concerned with processes of glacier-influenced slope sedimentation, iceberg...
Journal Article
Published: 01 January 2007
Geological Magazine (2007) 144 (1): 219-220.
...Colm Ó Cofaigh © 2007 Cambridge University Press 2007 Researchers in the fields of geocryology and glaciology often work in isolation from each other even though the interaction between glaciers and permafrost strongly influences a range of erosional and depositional processes, as well...
Journal Article
Published: 01 January 2009
Geological Magazine (2009) 146 (1): 156.
... and ranges in climate from the Atacama Desert in the north to the temperate rainforests and glaciers of the south. The geology of Chile is dominated by the Andean mountain belt caused by the ongoing subduction of the Pacific plate under the South American continent as part of the Pacific ‘ring of fire...
Series: Geological Society, London, Special Publications
Published: 01 January 2017
EISBN: 9781862399655
... on north-, NE- and east-facing slopes (Fig. 7 ). The orientations of the glaciers were classified in two hemispheres along an axis running from NW to SE (315–135°). An orientation analysis was performed on the cirques. The vast majority of cirques in the six regions of Greece were oriented towards...
Journal Article
Published: 18 June 2007
Canadian Journal of Earth Sciences (2007) 44 (5): 707-719.
...T.A. Arsenault; John J. Clague; R.W. Mathewes Abstract Moraine Bog lies just outside the outermost lateral moraine of Tiedemann Glacier in the southern Coast Mountains of British Columbia. A sediment core taken from the wetland was analyzed for pollen, magnetic susceptibility, and loss on ignition...
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Journal Article
Published: 30 November 2004
Canadian Journal of Earth Sciences (2004) 41 (12): 1401-1410.
...Franklin F. Foit, Jr.; Daniel G. Gavin; Feng Sheng Hu Abstract Several mid-late Holocene Glacier Peak tephras along with Mazama and Mount St. Helens Wn and P tephras were found in cores from Cooley and Rockslide lakes in southeastern British Columbia, ∼300 km northeast of Glacier Peak...
FIGURES | View All (4)
Journal Article
Journal: GSA Bulletin
Published: 01 June 2002
GSA Bulletin (2002) 114 (6): 718-730.
... thick and rests with sharp planar contacts on stagnant glacier ice reportedly of Miocene age, older than 8.1 Ma. The age of the ice is based on 40 Ar/ 39 Ar analyses of presumed in situ ash-fall deposits that occur within Granite drift. At odds with the great age of this ice are high-centered polygons...
FIGURES | View All (10)
Journal Article
Published: 01 December 2011
Bulletin of the Seismological Society of America (2011) 101 (6): 2662-2674.
... and statistical properties of the data. We find a significant difference between the magnitude of the largest aftershock and the mainshock. This is analyzed and discussed using the modified Båth’s law. It is observed that the aftershock decay rate can be approximated by the modified Omori law. The distribution...
FIGURES | View All (8)
Journal Article
Published: 17 September 2008
Geological Magazine (2009) 146 (2): 291-299.
... of the overlying Middle Pleistocene Wroxham Crag, probably by routing of sub-glacial, or glacial, melt-waters derived from late Pleistocene glaciers. New geochemical (particularly stable isotope) data shows that cementation of the chalks, although related spatially to the solution features, was not caused...
Journal Article
Published: 01 August 2010
Quarterly Journal of Engineering Geology and Hydrogeology (2010) 43 (3): 333-344.
... was affected by ice sheets and valley glaciers and by periglacial solifluction. During retreat of the Late Devensian valley glacier, terminal moraines were emplaced, with proglacial lakes upstream and, on breaching, strong erosion downstream, particularly in the Bingley area. All of the Airedale slides...
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Journal Article
Published: 28 July 2004
Canadian Journal of Earth Sciences (2004) 41 (7): 881-895.
... of phase with ice in the lowland. This resulted in glacial lakes forming during both advance and retreat phases. However, in contrast to watersheds in the northwestern Fraser Lowland, no definitive evidence of a Coquitlam ice advance was found within the Chehalis valley. Although glaciers in the area were...
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Journal Article
Published: 01 August 1965
Bulletin of the Seismological Society of America (1965) 55 (4): 693-720.
... States west of a line from Glacier National Park to El Paso produces lower seismic amplitudes for teleseismic events of a given magnitude than would be expected. Two other areas of comparatively low signal strength are tentatively located in the Wichita-Ouachita Mountain belt and the eastern portion...
Journal Article
Journal: Geology
Published: 01 October 2003
Geology (2003) 31 (10): 905-908.
... glacier flow. The existence of nunataks at this time opens the possibility for glacial survival of plant species. Geological Society of America 2003 23 06 2003 02 04 2003 12 06 2003 Two angular to subangular blocks of granite from the autochthonous block field yielded ages...
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Series: Geological Society, London, Special Publications
Published: 01 January 2000
DOI: 10.1144/GSL.SP.2000.176.01.08
EISBN: 9781862394247
.... 1984 ; Thorsteinsson et al. 1997 ); this means that the ice becomes progressively harder to compress vertically, and easier to localize the shear horizontally. Abstract Localization of deformation in ice is known to be important at all scales in deforming glaciers. However, relatively little...
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Series: Field Guide
Published: 01 January 2003
DOI: 10.1130/0-8137-0004-3.1
EISBN: 9780813756042
... will be north and west of Missoula to sites along U.S. Highway 93 and State Routes 28, 382, and 200 to view the relationship of valley glaciers and Glacial Lake Missoula, pingo scar terrain, large terminal moraines, Joseph T. Pardee’s classic giant current ripple forms and gulch fills in the Camas Prairie...
FIGURES | View All (9)
Journal Article
Journal: GSA Bulletin
Published: 01 November 2009
GSA Bulletin (2009) 121 (11-12): 1711-1725.
... farther south at the Palmer Deep drill site. Minimum sea-ice cover and warm water conditions occurred between 8.2 and 5.9 ka. From 5.9 to 2.6 ka, there was a gradual cooling and more extensive sea-ice cover in the bay. After 2.6 ka, the climate varied slightly, causing only subtle variation in glacier...
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Journal Article
Published: 01 May 1999
Bulletin de la Société Géologique de France (1999) 170 (3): 413-420.
... Méllègue (confins algéro-tunisiens) sont-ils des diapirs ou des « glaciers de sel » ? » PERTHUIS0T V. et al., Bull. Soc. géol. Fr., 169, p. 53-61, 1998 JEAN-MARIE VILA 1, MüHAMED BEN YOUSSEF2 , SALAH BOUHLEL3 , ANDRÉ CHARRIÈRE 1 , M0NGI CHIKHAOUI4, TAÏEB DALI4, M0HAMED GHANMI4, FÉKRI KAMOUN5, SAMIA KASSAÂ3...
Journal Article
Published: 21 June 2008
Canadian Journal of Earth Sciences (2008) 45 (5): 513-529.
.... Fractions selected for U–Pb analyses were washed in 2 N HNO 3 for 1 h at ca. 50 °C, placed in an ultrasonic bath for 1 min, and then rinsed with distilled H 2 O and acetone prior to weighing with a Mettler UTM2 ultramicrobalance. A measured amount of a calibrated 205 Pb– 235 U tracer solution was added...
FIGURES
Journal Article
Published: 01 September 2005
Geological Magazine (2005) 142 (5): 635.
... H arris , C. & M urton , J. B. 2005. Cryospheric Systems. Glaciers and Permafrost . Geological Society Special Publication no. 242. vii + 161 pp. London, Bath: Geological Society of London. Price £60.00, US $108.00; GSL members’ price £30.00, US $54.00; AAPG/SEPM/GSA/RAS/EFG/PESGB members...
Journal Article
Published: 01 August 1983
Quarterly Journal of Engineering Geology and Hydrogeology (1983) 16 (3): 197-210.
.... Boulton, G. S. 1970a . On the origins and transport of englacial debris in Svalbard glaciers. J. Glaciol. 9 , 213 – 229 . Boulton, G. S. 1970b . The deposition of subglacial and meltout tills at the margins of certain Svalbard glaciers. J. Glaciol. 9 , 231 – 245...