Garry L. Running

University of Wisconsin–Eau Claire

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Phillip H. Larson

Minnesota State University, Mankato

Tammy M. Rittenour

Utah State University

Douglas J. Faulkner

University of Wisconsin–Eau Claire

Randall J. Schaetzl

Michigan State University

Karen G. Havholm

University of Wisconsin–Eau Claire

Harry M. Jol

University of Wisconsin–Eau Claire

Luke Burds

University of Wisconsin–Eau Claire

Richard J. Mataitis

University of Wisconsin–Eau Claire

Ronald C. Schirmer

Minnesota State University, Mankato

Mark W. Bowen

Minnesota State University, Mankato

Cooperative Institutions

United States Geological Survey

Denver Federal Center

Chinese Academy of Sciences

Geosciences and Environmental Change Science Center

Pacific Island Ecosystems Research Center

University of Wisconsin–Eau Claire

University of Calgary

University of Illinois Urbana-Champaign

Institute of Earth Environment

University of Arizona

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Geomorphic Investigations of Newly Identified Linear Dunes in Western Wisconsin, USA

Garry L. Running Erica C. Jansen Kayla Coonen

Source

Cite

Citations (0)

DEFINING THE GEOMORPHOLOGY OF CLIFF-TOP DUNES: CASE STUDY OF THE CHIPPEWA RIVER VALLEY, WI, USA

Abstracts with programs - Geological Society of America (2019)

Phillip H. Larson Jason Millett Luke Burds Richard J. Mataitis Garry L. Running

Cliff

10.1130/abs/2019am-338638

Cite

Citations (0)

GEOMORPHOLOGY OF AEOLIAN SAND STRINGERS IN WESTERN WISCONSIN AND SOUTHEASTERN MINNESOTA

Abstracts with programs - Geological Society of America (2020)

Kenzie L. Shandonay Richard J. Mataitis Luke Burds Phillip H. Larson Mark W. Bowen

10.1130/abs/2020nc-347354

Cite

Citations (0)

Stratigraphy, sedimentology, and environmental significance of late mid-Holocene dunes, Lauder Sand Hills, glacial Lake Hind Basin, southwestern Manitoba

Canadian Journal of Earth Sciences (2005)

Karen G. Havholm Garry L. Running

Mid-Holocene eolian dune and sand-sheet deposits, rare in the northern Great Plains, are buried under a meter or more of younger sediment in the glacial Lake Hind Basin, southwestern Manitoba. Six facies observed in three cut-bank exposures allow reconstruction of sedimentary processes and resulting landscape at the study site in the basin center around 6100 cal (calibrated) BP. A mosaic of parabolic dunes with interdune and dune-marginal lightly vegetated sand sheets developed in the Souris River flood plain that was least partly covered with woodlands and wetlands. During floods, nearby interdune areas were inundated. Dune foreset orientation and stratification indicate a more easterly sand transport direction, lending support to the hypothesis that more pervasive westerly "zonal" flow contributed to mid-Holocene aridity evident elsewhere in the northern Great Plains. More arid conditions during the mid-Holocene may have helped trigger eolian activity. However, with the exception of a more active eolian component, the flood-plain environment may have been similar to that of the late Holocene. Mid-Holocene Gowen (Mummy Cave Complex) artifacts, the first found in Manitoba, indicate that people inhabited the resource-rich environment where eolian and flood-plain landforms occurred together. Protection of mid-Holocene dune and sand-sheet strata during late Holocene phases of eolian reactivation is attributed to rapid rise in the local water table soon after deposition.

10.1139/e05-019

Cite

Citations (12)

Autogenic incision and terrace formation resulting from abrupt late-glacial base-level fall, lower Chippewa River, Wisconsin, USA

Geomorphology (2016)

Douglas J. Faulkner Phillip H. Larson Harry M. Jol Garry L. Running Henry M. Loope

Outwash plain

Meltwater

Terrace (agriculture)

Alluvial fan

10.1016/j.geomorph.2016.04.016

Cite

Citations (50)

AEOLIAN GEOMORPHOLOGY AND GEOARCHEOLOGY OF THE KIWANIS SITE, CHIPPEWA RIVER VALLEY, WISCONSIN

Abstracts with programs - Geological Society of America (2020)

Luke Burds Phillip H. Larson Ronald C. Schirmer Garry L. Running Douglas J. Faulkner

10.1130/abs/2020nc-347758

Cite

Citations (0)

Reconstructing a Prairie-Woodland Mosaic on the Northern Great Plains: Risk, Resilience, and Resource Management

Plains Anthropologist (2006)

Matt Boyd Scott Hamilton Garry L. Running

AbstractRecent geological evidence of high-amplitude, short-term, climatic variability on the northern Plains in the late Holocene implies that significant fluctuations in resource availability may have regularly occurred on the scale of human generations. In this region, evidence of high mobility, low population density, and storage are generalized responses of hunter-gatherer populations to the effects of environmental variability on resourcepredictability. In order to achieve more sophisticated understanding of the relationship between risk, environment, and land-use for the last few thousand years, we suggest that multidisciplinary reconstruction of detailed landscape histories is necessary. This is so because landscape histories may encode: (1) spatial and temporal variability in habitat diversity (i.e., patchiness); (2) geographical differences in ecosystem resilience and resistance to short-term macro climatic variability; and (3) enhancement of resource predictability or diversity through lnanagement practices such as anthropogenic burning. Modern vegetation surveys, presettlement landcover reconstructions, and recent geomorphic and paleo vegetation data from the Oak Lake Sandhills, Manitoba, Canada, are assembled to illustrate these points.Keywords: landscape reconstructionhistorical ecologyhunter-gatherer land useanthropogenic burningnorthern Great Plains

10.1179/pan.2006.024

Cite

Citations (4)

GPR survey of a Holocene aeolian/fluvial/lacustrine succession, Lauder Sandhills, Manitoba, Canada

Geological Society London Special Publications (2003)

Karen G. Havholm N. D. Bergstrom Harry M. Jol Garry L. Running

Abstract A stream cut-bank at Flintstone Hill, Lauder Sandhills, Glacial Lake Hind Basin, southwestern Manitoba, exposes an extensive Holocene sedimentary sequence. Ground penetrating radar (GPR) is used to determine lateral continuity of four major stratigraphic units (wetland complex, Mid-Holocene aeolian dune, sandsheet/fluvial, Late Holocene aeolian dune) and to image primary sedimentary features within the dune strata. Depth of GPR signal penetration is only about 5 m. Signal attenuation is attributed to the presence of primarily pedogenic silts/clays and carbonate- and iron sesquioxide-rich horizons within the sandier units. Nevertheless, the stratigraphic units are shown by GPR, and confirmed by core data, to be laterally continuous within the survey area. Finer-scale dune strata are not well displayed in the aeolian units. Signal attenuation above the Mid-Holocene unit and relatively high iron sesquioxide concentrations within the unit limit imaging of well-preserved dune foreset strata. In the Late Holocene unit, depositional strata are poorly preserved and GPR primarily images soil A-horizons formed on surfaces of temporary stabilization within the dune sediment.

10.1144/gsl.sp.2001.211.01.04

Cite

Citations (20)

Archaeological geology of the Rustad Quarry site (32RI775): An early archaic site in Southeastern North Dakota

Geoarchaeology (1995)

Garry L. Running

Abstract At The Rustad Quarry Site (32RI775), in southeastern North Dakota, Early Archaic artifacts, bison bone, and hearth features were found in the lowest of three Boroll‐like buried soils formed in alluvial fan sediments. Alluvial fan sediments were deposited from 8000 to 4925 B.P., and were then buried by eolian sand. The alluvial fan sediments (mudflows) bury lacustrine sediments (Sherack Formation deposited from 9900 to 9500 B.P. in Glacial Lake Agassiz II), both of which overlie a Moorhead Phase fluvial terrace deposited from 10,900 to 9,900 B.P. Cultural remains were associated with five radiocarbon ages, three on archaeological charcoal (7180 B.P., 7240 B.P., and 7550 B.P.) and two on organic carbon from two welded A‐horizons containing the cultural remains (7370 B.P. and 7675 B.P.). A well‐developed Aquoll‐like soil formed in the lacustrine sediments from 9500 to 8000 B.P. Soil morphology and chemistry of the Boroll‐like fan soils, the Aquoll‐like lacustrine soil, and other Boroll‐like soils formed in eolian and deltaic sediments nearby suggest a subhumid, cool continental climate with riparian woodland and mixed prairie vegetation at the site and surrounding area from 11,400 B.P. to the present. This partially contradicts paleoenvironmental reconstruction from pollen sites nearby that suggest the area was covered by a closed canopy spruce forest from terminal late‐Pleistocene to 10,000 B.P. Alluvial fan formation and eolian activity on the adjacent Sheyenne Delta occurred from 8000 to 5000 B.P., which indicates greater landscape instability and drier conditions during the mid‐Holocene (Altithermal).

10.1002/gea.3340100303

Cite

Citations (11)

QUA volume 89 issue 3 Cover and Back matter

Quaternary Research (2018)

Randall J. Schaetzl E. Arthur Bettis Onn Crouvi Kathryn E. Fitzsimmons David A. Grimley

An abstract is not available for this content so a preview has been provided. As you have access to this content, a full PDF is available via the ‘Save PDF’ action button.

Content (measure theory)

10.1017/qua.2018.44

Cite

Citations (0)