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marmots

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Diagrams of burrow systems of living <b>marmots</b> ( Marmota  spp.) after various...
in > PALAIOS
Published: 01 November 2013
Fig. 16.— Diagrams of burrow systems of living marmots ( Marmota spp.) after various authors. A – G) Plan and lateral views of generalized burrow systems of woodchuck ( Marmota monax ), after Fischer (1893) . Note the simple burrow systems compared with other marmotines and three closely
Series: GSA Reviews in Engineering Geology
Published: 01 January 2013
DOI: 10.1130/2013.4121(14)
EISBN: 9780813758213
... is proportional to the rate of bank erosion, E r . We proposed earlier that the rate of erosion in a breached reservoir might decelerate with time after dam breach, as was observed with the Marmot Dam removal on the Sandy River in Oregon ( Major et al., 2008 , 2012 ). All cross section ( n = 25), bank pin ( n...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2012
DOI: 10.1144/SP368.16
EISBN: 9781862396166
... of these organically enriched deglacial sediments comprises shales and dolostones deposited following the Sturtian glaciation in the Centralian Superbasin of Australia, an amalgam of basins that extends almost continent-wide across Australia. Data from the Marmot MMDD-1 drill core on the Stuart Shelf in the southern...
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Journal Article
Published: 01 May 1962
Journal of Paleontology (1962) 36 (3): 540–556.
... similarity to living spermophiles, particularly to the subgenus Spermophilus. It could be considered a primitive member of this group of ground squirrels except for the large size of the upper and lower fourth premolars, a generic character of modern marmots. The large fourth premolars are exceptions...
Journal Article
Published: 01 April 1990
Rocky Mountain Geology (1990) 28 (1): 31–37.
Journal Article
Published: 01 September 1968
Bulletin of Canadian Petroleum Geology (1968) 16 (3): 414–415.
... of excavation would elim- inate extensive supplementary rock bolting. It is further suggested that the excavation of a semi-elliptical arch in thinly-bedd.ed sedimentary rocks is inadvisable. GEOLOGICAL AND GROUNDWATER INVESTIGATIONS IN THE MARMOT CREEK EXPERIMENTAL BASIN OF SOUTHWESTERN ALBERTA, CANADA...
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A)  Location map of the overthrust belt in western Alberta and eastern Brit...
Published: 01 December 2010
, are exposed in the Canadian Rocky Mountains (after Geldsetzer 1989 ; Mountjoy 1989 ; Switzer et al. 1994 ). Key to stratigraphic sections: MC = Marmot Crack, A/C = Thornton Cr., AB = Poachers Cr., KC = Klapper Cr., KP = Kakwa Park. See Figures 3 and 4 for the location of stratigraphic sections AB
Journal Article
Published: 01 September 1968
Bulletin of Canadian Petroleum Geology (1968) 16 (3): 414.
... of excavation would elim- inate extensive supplementary rock bolting. It is further suggested that the excavation of a semi-elliptical arch in thinly-bedd.ed sedimentary rocks is inadvisable. GEOLOGICAL AND GROUNDWATER INVESTIGATIONS IN THE MARMOT CREEK EXPERIMENTAL BASIN OF SOUTHWESTERN ALBERTA, CANADA...
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Primitive mantle-normalized multi-element plots of mafic rock units. (A) Ke...
in > Geosphere
Published: 08 May 2019
that overlie the Cambrian Tshinakin limestone ( Paradis et al., 2006 ). The Selwyn basin units include the Marmot Formation ( Leslie, 2009 ), Menzie Creek formation ( Pigage, 2004 ), and Crow, Rabbitkettle, and Sunblood Formations ( Pigage et al., 2015 ). (B) Cretaceous syn- to post-breakup volcanic rocks
Image
(A) Location map of the overthrust belt in western Alberta, showing the loc...
Published: 01 May 2012
—Maligne Formation, P—Perdrix Formation, H—Mount Hawk Formation. Key to stratigraphic sections: MC—Marmot Crack, A/C—Thornton Creek, AB and W4—Poachers Creek, KC—Klapper Creek.
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Localities containing  Homotherium serum  in Canada and the United States. ...
Published: 26 September 2017
1987 Gilliland Local Fauna Texas Irvingtonian Graham and Lundelius 2010 Laubach Cave No. 2 Texas Late Wisconsinan Graham and Lundelius 2010 Marmot Quarry Texas Blancan Graham and Lundelius 2010 Slaton Quarry Local Fauna Texas Rancholabrean Graham and Lundelius 2010
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Representative distribution of latest Proterozoic and Paleozoic magmatic ro...
Published: 24 October 2005
to dacitic tuff, ∼363 Ma ( Richards et al. 2002 ); 16, foliated tonalite in Dorsey assemblage (= Yukon–Tanana terrane), 349.9 ± 4.2 Ma, Nelson et al. ( 1998 ). Lower Ordovician to Middle Devonian: 17, Middle Ordovician to Middle Devonian Marmot Formation (Misty Creek Embayment) alkalic basalt (WPB), Cecile
Journal Article
Published: 01 January 2004
Seismological Research Letters (2004) 75 (1): 96.
... of the high-performance, very broadband, network-aware, and ultralow-power Q330-based data-acquisition modules, each equipped with GPS receivers. Each data acquisition block will run Antelope Marmot data-acquisition software that provides blocks of data acquisition, extended buffering, and command...
FIGURES
Journal Article
Published: 01 November 2005
Journal of Paleontology (2005) 79 (6): 1239–1240.
... at δ 13 C and δ 18 O isotopes and the latter examines tooth morphology in marmots hoping to obtain paleoclimatic data. Unfortunately, perhaps due to the behavior of marmots, no effects were seen. Shabel et al. provide an analysis of the Badger Room fauna, which was collected as a bulk sample from...
Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2007
DOI: 10.1144/GSL.SP.2007.273.01.19
EISBN: 9781862395213
... ‘possible relationship to a living descendant’, impressive insights for a pre-scientific culture ( Spalding 1999 , pp. 22–23). Fig. 11. Hoary marmot, a large rodent that inhabits the northern Rockies. Alaska, and the Yukon. The Gitxsan place name for a set of dinosaur tracks in British Columbia...
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Journal Article
Published: 01 March 1978
Bulletin of Canadian Petroleum Geology (1978) 26 (1): 164–166.
.... J. Earth Sci., v. 5, p. 1455-1466. - - , 1973a, Surflcial geology of the Kananaskis Research Forest and Marmot Creek Basin region of Alberta: Geol. Surv. Canada, Paper 72-51., 25p. , 1973b, Surficial geology of the Drumheller area, Alberta: Geol. Surv. Canada, Mem. 370, 122p. , and Harrison, J. E...
Journal Article
Journal: PALAIOS
Published: 01 November 2013
PALAIOS (2013) 28 (11): 793–824.
...Fig. 16.— Diagrams of burrow systems of living marmots ( Marmota spp.) after various authors. A – G) Plan and lateral views of generalized burrow systems of woodchuck ( Marmota monax ), after Fischer (1893) . Note the simple burrow systems compared with other marmotines and three closely...
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Series: AAPG Memoir, AAPG Memoir
Published: 01 January 2004
DOI: 10.1306/M80924C13
EISBN: 9781629810478
... ; Hopkins, 1972 ). At the stratigraphic level of the Arcs Member, the platform increases in width by an additional 5–10 km ( Mountjoy, 1989 ). Nearly continuous outcrops at Marmot Cirque (Figure 4 ) and adjacent areas (Slide Creek and Poachers Creek) expose the platform margin and basin architecture...
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Series: Geological Society, London, Special Publications, Geological Society, London, Special Publications
Published: 01 January 2005
DOI: 10.1144/GSL.SP.2005.247.01.16
EISBN: 9781862394957
.... Other rodents are also habitat-specific: the beaver Castor lives near the water, and marmots show a preference for rocky, open and/or alpine habitats. In contrast, the porcupine Hystrix is a temperate to tropical large rodent that lives today in open, wet and warm areas. The field mouse Apodemus...
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Series: GSA Field Guide
Published: 01 January 2009
DOI: 10.1130/2009.fld015(11)
EISBN: 9780813756158
... stored behind Marmot Dam, ~20 km upstream. The dam was removed on 19 October 2007. Multiple levels of Old Maid degradation terraces and the deposits composing them. “Ghost forests” of trees that had been buried by rapid deposition by lahars and floods during the Timberline and Old Maid eruptive...