Spatial distribution and geomorphology of lunette dunes on the High Plains of Western Kansas: implications for geoarchaeological and paleoenvironmental research

被引:7
作者
Bowen, Mark W. [1 ]
Johnson, William C. [2 ]
King, Dylan A. [1 ]
机构
[1] Univ Wisconsin, Dept Geog & Urban Planning, Oshkosh, WI 54901 USA
[2] Univ Kansas, Dept Geol & Atmospher Sci, Lawrence, KS 66045 USA
关键词
Digital raster graphics; geospatial database; GIS; LiDAR; playa wetlands; Quaternary; CENTRAL GREAT-PLAINS; SOUTHERN HIGH-PLAINS; PLEISTOCENE-HOLOCENE TRANSITION; UNITED-STATES; PLAYA WETLANDS; NEW-MEXICO; USA; RECORD; LOESS; EVOLUTION;
D O I
10.1080/02723646.2017.1319683
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The High Plains are a vast, low relief landscape that contains thousands of upland-embedded depressional playa wetlands. Lunettes are isolated dunes that form from prolonged periods of aeolian deposition along the downwind margin of some larger playas. Playa-lunette systems are important landscape elements that have the potential to preserve high-resolution records of past environments, and several archeological sites have been associated with playalunette systems throughout the High Plains. While a comprehensive playa wetland geospatial database has been developed for the High Plains, lunettes have only been mapped for the Southern High Plains of Texas and New Mexico. The purpose of this research was to map and characterize the geomorphology of all lunettes associated with playas in the High Plains and bordering regions of western Kansas. Results indicate 129 lunettes are associated with 104 playas in Kansas. All lunettes are associated with playas larger than 5 ha, and about 10% of these larger playas have a lunette. Lunette height ranges from approximately 1.5-12 m, with a median height of 3 m. Most lunettes (60%) are in Finney, Gray, Lane, and Scott counties, which have broad, flat uplands with few major drainages upwind of playas and lunettes.
引用
收藏
页码:21 / 37
页数:17
相关论文
共 48 条
[1]   Late Quaternary evolution of a lunette in the central Great Plains: Wilson Ridge, Kansas [J].
Arbogast, AF .
PHYSICAL GEOGRAPHY, 1996, 17 (04) :354-370
[2]  
Blackmar JeannetteM., 2006, Kansas Archaeology, P46
[3]   Holocene records of environmental change in High Plains playa wetlands, Kansas, US [J].
Bowen, Mark W. ;
Johnson, William C. .
HOLOCENE, 2015, 25 (11) :1838-1851
[4]   Late Quaternary environmental reconstructions of playa-lunette system evolution on the central High Plains of Kansas, United States [J].
Bowen, Mark W. ;
Johnson, William C. .
GEOLOGICAL SOCIETY OF AMERICA BULLETIN, 2012, 124 (1-2) :146-161
[5]   A GIS-based Approach to Identify and Map Playa Wetlands on the High Plains, Kansas, USA [J].
Bowen, Mark W. ;
Johnson, William C. ;
Egbert, Stephen L. ;
Klopfenstein, Scott T. .
WETLANDS, 2010, 30 (04) :675-684
[6]  
EPA, 2013, LEV 3 4 EC CONT US
[7]   LOESS ACCUMULATION AND SOIL FORMATION IN CENTRAL KANSAS, UNITED-STATES, DURING THE PAST 400,000 YEARS [J].
FENG, ZD ;
JOHNSON, WC ;
SPROWL, DR ;
LU, YC .
EARTH SURFACE PROCESSES AND LANDFORMS, 1994, 19 (01) :55-67
[8]  
Fenneman N.M., 1931, PHYSIOGRAPHY W US
[9]  
Frye J. C., 1956, STRATIGRAPHY OGALLAL
[10]   STRATIGRAPHY OF THE LATE PLEISTOCENE LOESSES OF KANSAS [J].
FRYE, JC ;
LEONARD, AB .
JOURNAL OF GEOLOGY, 1951, 59 (04) :287-&