1-11 OF 11 RESULTS FOR

Sturgis Moraine

Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account

Would you like to receive an alert when new items match your search?
Close Modal
Sort by
Image
Location of the Pigeon River meltwater channel south of the <span class="search-highlight">Sturgis</span> <span class="search-highlight">Moraine</span>...
Published: 13 November 2018
Fig. 2. Location of the Pigeon River meltwater channel south of the Sturgis Moraine. On the digital elevation model basemap, lighter greys are higher elevation. Black arrows indicate meltwater flow direction from the Huron-Erie Lobe to the west. The boundary between the Saginaw and Huron-Erie
Published: 30 January 2018
DOI: 10.1130/2017.2530(06)
EISBN: 9780813795300
... streamlined plain ( Fig. 6 ) is a drumlinized tract north of the Sturgis moraine ( Dodson, 1985 ). Dodson’s (1985) morphometric analysis of the landforms distinguished a variety of streamlined forms, ranging from classically shaped drumlins to indistinctly streamlined hills, to lineations visible on air...
FIGURES | View All (15)
Journal Article
Published: 13 November 2018
Canadian Journal of Earth Sciences (2019) 56 (2): 175–182.
...Fig. 2. Location of the Pigeon River meltwater channel south of the Sturgis Moraine. On the digital elevation model basemap, lighter greys are higher elevation. Black arrows indicate meltwater flow direction from the Huron-Erie Lobe to the west. The boundary between the Saginaw and Huron-Erie...
FIGURES | View All (4)
Journal Article
Journal: GSA Bulletin
Published: 01 March 1986
GSA Bulletin (1986) 97 (3): 329–334.
... analyses of more than 200 samples collected from moraines, till plains, and multi-till exposures 2 to 60 km inland suggest that Saugatuck till at the lakeshore is equivalent to till in the Lake Border Valparaiso, and Sturgis-Kalamazoo morainic systems, whereas Ganges till can be traced in the subsurface...
Series: GSA Special Papers
Published: 07 April 2021
DOI: 10.1130/2020.2548(16)
EISBN: 9780813795485
..., and Huron-Erie lobes of the Laurentide ice sheet ( Zumberge, 1960 ; Kehew et al., 1999 ). During final stages of deglaciation, the Lake Michigan and Huron-Erie lobes expanded into broad areas vacated as the Saginaw lobe retreated from the Sturgis moraine ( Kehew et al., 1999 , 2012a , 2012b ). Major...
FIGURES | View All (8)
Journal Article
Published: 01 December 1999
Bulletin of the Seismological Society of America (1999) 89 (6): 1458–1472.
..., Tioga glacial outwash; Qo2, Tahoe glacial outwash; Qm2, Tahoe moraines; Qfo, older alluvial fans; gr, granodiorite; my, metavolcanics. At this location, the Genoa fault offsets outwash terraces along the West Fork of the Carson River, indicating a slip rate of about 1 mm/yr; farther north, the main part...
... Michigan occupies a bedrock high formed by the subcrop of the Mississippian Marshall Sandstone and Coldwater Shale (Fig. 12 ). Glacial drift in this area is some of the thinnest in the Lower Peninsula. Land System 1 Land system 1 consists of the Sturgis moraine, a terminal/recessional moraine...
FIGURES | View All (29)
Journal Article
Published: 14 December 2021
Bulletin of the Seismological Society of America (2022) 112 (2): 704–713.
... sites: CC, Carson City; CH, C‐Hill; ECV, East Carson Valley; FC, Fay Canyon; FW, freeway; IH, Indian Hills; JV, Jacks Valley; KC, Kings Canyon; MC, Mott Canyon; MRF, Mount Rose Fan; ST, Sturgis; WA, Walleys; WC, Whites Creek; WF, Woodfords; WV, Washoe Valley. Area of Figure  2 shown in inset the map...
FIGURES | View All (5)
Journal Article
Published: 19 June 2014
Canadian Journal of Earth Sciences (2014) 51 (8): 737–749.
... – Powell Moraine in northeast Indiana ( Barnett 1985 ; Calkin and Feenstra 1985 ; Glover et al. 2011 ). Once ice receded from the Fort Wayne Moraine, Lake Maumee began forming in lower topography dammed by the receding ice mass and the higher topography to the west, draining through the Fort Wayne outlet...
FIGURES
Journal Article
Published: 01 December 2005
South African Journal of Geology (2005) 108 (4): 557–577.
...-walled trough, 0.1 km deep and ~18 km wide, assuming its axis is oriented roughly transverse to paleoslope contours. The glacial deposits average 80 m in thickness outside the trough, are attenuated on the sides of the trough, and form a steep moraine-like ridge in the trough axis. The ridge rises 600 m...
FIGURES | View All (12)
Series: GSA Field Guide
Published: 01 January 2016
DOI: 10.1130/2016.0043(06)
EISBN: 9780813756431
... was at least modest. It probably was a shallow, protected coast with an abundant supply of sand. The overlying, thin-bedded sandstone shows signs of strong currents, possibly tidal in origin. Figure 4. (A) Scarp in a sandy till in the Johnstown moraine the Gasser Pit. (B) More sandy till in southern...
FIGURES | View All (25)