Origin of a washboard moraine of the Des Moines Lobe inferred from sediment properties

[1]  B. Lowery,et al.  Physical Tests for Monitoring Soil Quality , 2015 .

[2]  C. Harding,et al.  Origin of washboard moraines of the Des Moines Lobe: Spatial analyses with LiDAR data , 2015 .

[3]  Ó. Ingólfsson,et al.  The Eyjabakkajokull glacial landsystem, Iceland: Geomorphic impact of multiple surges , 2014 .

[4]  R. Alley,et al.  Exploring till bed kinematics using AMS magnetic fabrics and pebble fabrics: the Weedsport drumlin field, New York State, USA , 2012 .

[5]  David J. A. Evans,et al.  An assessment of surge-induced crevassing and the formation of crevasse squeeze ridges , 2011 .

[6]  N. Iverson,et al.  Deformation of the Batestown till of the Lake Michigan lobe, Laurentide ice sheet , 2009, Journal of Glaciology.

[7]  N. Iverson,et al.  Magnetic fabrics of the Douglas Till of the Superior lobe: exploring bed-deformation kinematics , 2009 .

[8]  John B. Anderson,et al.  Submarine glacial landforms and rates of ice-stream collapse , 2008 .

[9]  N. Iverson,et al.  Magnetic fabric of sheared till: A strain indicator for evaluating the bed deformation model of glacier flow , 2008 .

[10]  N. Iverson,et al.  The experimental basis for interpreting particle and magnetic fabrics of sheared till , 2008 .

[11]  P. Möller,et al.  Ribbed moraine formed by subglacial folding, thrust stacking and lee‐side cavity infill , 2008 .

[12]  J. Attig,et al.  Surging of the southwestern part of the Laurentide Ice Sheet , 2008 .

[13]  David J. A. Evans,et al.  Subglacial till: Formation, sedimentary characteristics and classification , 2006 .

[14]  Carrie E. Jennings,et al.  Terrestrial ice streams—a view from the lobe , 2006 .

[15]  P. Möller,et al.  Marginal formation of De Geer moraines and their implications to the dynamics of grounding‐line recession , 2005 .

[16]  John B. Anderson,et al.  Retreat signature of a polar ice stream: sub-glacial geomorphic features and sediments from the Ross Sea, Antarctica , 2002, Geological Society, London, Special Publications.

[17]  N. Iverson,et al.  Flow mechanism of the Des Moines lobe of the Laurentide ice sheet , 2002, Journal of Glaciology.

[18]  S. Tulaczyk,et al.  Estimates of effective stress beneath a modern West Antarctic ice stream from till preconsolidation and void ratio , 2001 .

[19]  J. Attig,et al.  Minor end moraines of the Wisconsin Valley Lobe, north‐central Wisconsin, USA , 2001 .

[20]  N. Iverson,et al.  Clast-fabric development in a shearing granular material: Implications for subglacial till and fault gouge , 2000 .

[21]  David J. A. Evans,et al.  Glaciers and Glaciation , 1997 .

[22]  C. J. Patterson.  Southern Laurentide ice lobes were created by ice streams: Des Moines Lobe in Minnesota, USA , 1997 .

[23]  David J. A. Evans,et al.  The interpretation and classification of subglacially-deformed materials , 1996 .

[24]  D. Benn.  Fabric signature of subglacial till deformation, Breidamerkurjokull, Iceland , 1995 .

[25]  D. Benn.  Fabric Shape and the Interpretation of Sedimentary Fabric Data , 1994 .

[26]  M. Hambrey,et al.  The structural geology of a surge-type glacier , 1994 .

[27]  P. Clark,et al.  Subglacial drainage, eskers, and deforming beds beneath the Laurentide and Eurasian ice sheets , 1994 .

[28]  P. Clark.  Unstable Behavior of the Laurentide Ice Sheet over Deforming Sediment and Its Implications for Climate Change , 1994, Quaternary Research.

[29]  E. A. Christiansen,et al.  Preconsolidation of tills and intertill clays by glacial loading in southern Saskatchewan, Canada , 1993 .

[30]  D. H. Tarling,et al.  The magnetic anisotropy of rocks , 1993 .

[31]  P. Clark.  Surface form of the southern Laurentide Ice Sheet and its implications to ice-sheet dynamics , 1992 .

[32]  J. Lundqvist.  Rogen (ribbed) moraine—identification and possible origin , 1989 .

[33]  R. Stewart,et al.  Nature and origin of corrugated ground moraine of the Des Moines lobe, Story County, Iowa , 1988 .

[34]  C. Burras,et al.  Basin Properties and Postglacial Erosion Rates of Minor Moraines in Iowa , 1987 .

[35]  M. Sharp.  “Crevasse-Fill” Ridges—A Landform Type Characteristic of Surging Glaciers? , 1985 .

[36]  A. Lutenegger,et al.  Origin and Properties of Glacial Till and Diamictons , 1983 .

[37]  L. Clayton,et al.  Chronology of late wisconsinan glaciation in middle North America , 1982 .

[38]  L. Clayton,et al.  A GLACIAL PROCESS-FORM MODEL , 1982 .

[39]  W. D. Kovacs,et al.  An Introduction to Geotechnical Engineering , 1981 .

[40]  Joseph E. Bowles,et al.  Engineering Properties of Soils and Their Measurement , 1978 .

[41]  D. Mickelson,et al.  Till Ridges Presently Forming above and below Sea Level in Wachusett Inlet, Glacier Bay, Alaska , 1974 .

[42]  D. M. Mark.  Analysis of Axial Orientation Data, Including Till Fabrics , 1973 .

[43]  R. Palmquist,et al.  Possible Subglacial Origin for "Minor Moraine" Topography , 1969 .

[44]  D. Lawrence,et al.  Periodicity of Deglaciation in North America Since the Late Wisconsin Maximum , 1953 .

[45]  C. S. Gwynne.  MINOR MORAINES IN SOUTH DAKOTA AND MINNESOTA , 1951 .

[46]  C. S. Gwynne.  Swell and Swale Pattern of the Mankato Lobe of the Wisconsin Drift Plain in Iowa , 1942, The Journal of Geology.