Partial Report for Crooked Creek fault (Class B) No. 1032
citation for this record: Crone, A.J., compiler, 1998, Fault number 1032, Crooked Creek fault, in Quaternary fault and fold database of the United States: U.S. Geological Survey website, http://earthquakes.usgs.gov/hazards/qfaults, accessed 03/08/2014 05:00 AM.
|Synopsis||This feature is classified as a Class B feature because of the uncertainty concerning the cause of the subsurface deformation. As discussed below, it is uncertain if the stratigraphic offset related to the Crooked Creek fault is solely the result of dissolution of soluble subsurface strata or is related to genuine, deep-seated tectonic movements (Frye and Hibbard, 1941 #2810). The fault is defined largely on the basis of drill-hole data (Izett and Honey, 1995 #2812) and anomalous geomorphic features above the subsurface structure. No exposures of the fault are known. Deformation associated with the feature has resulted in a structural depression in the subsurface and an elongate topographic trough (Smith, 1940 #2813).|
|County(s) and State(s)||FORD COUNTY, KANSAS |
MEADE COUNTY, KANSAS
|Physiographic province(s)||GREAT PLAINS |
|Reliability of location||Poor|
Compiled at 1:24,000 scale.
|Geologic setting||The oldest exposed rocks in the Meade County area are Lower Permian sedimentary rocks, although older Paleozoic rocks are present in the subsurface. Shallow seas covered the region periodically during Paleozoic time, and in Permian time, there was a progressive transition to non-marine sedimentation. At times during this transition, extensive evaporation of isolated inland seas resulted in the deposition of salt and gypsum (Hutchinson Salt Member of the Wellington Formation; estimated to be about165 m thick based on geophysical logs shown in Figure 3 of Izett and Honey, (1995 #2812). Non-deposition and erosion during much of the Mesozoic created an unconformity between Paleozoic rocks and the overlying Tertiary sediments (Frye, 1942 #2809). The Miocene-age, silty sandstone and gravel that comprise the Ogallala Formation are the most widespread Tertiary rocks in southwestern Kansas. In the area of the Crooked Creek fault in Meade County, the Ogallala Formation is overlain by claystone, siltstone, sand, and gravels of the Pliocene Rexroad Formation and Stump Arroyo Member, and the Pliocene/Pleistocene Crooked Creek Formation (Izett and Honey, 1995 #2812). All of these materials are generally undeformed and nearly flat lying.|
|Length (km)||44 km.|
|Sense of movement||No data|
|Geomorphic expression||An abrupt, anomalous change in the course of Crooked Creek in Meade County, an area of unusual artesian flow of groundwater, and unusual surficial depressions (sinkholes) first drew attention to the area of the Crooked Creek fault. The prevailing topographic slope in southwestern Kansas is about 2.37 m/km in a southeasterly direction (Gutentag and others, 1981 #2811). The upper 30-40 km of Crooked Creek flows in a generally east to southeasterly direction, but at the eastern border of Meade County about 10 km north of the town of Fowler, the stream valley turns abruptly to the southwest, and maintains this flow direction for about 45 km before it turns abruptly and again flows to the southeast. The anomalous southwesterly flowing reach of the stream coincides with the area of artesian aquifers and the area of sinkholes. The spatial coincidence of these unusual geomorphic features and the groundwater condition suggest a common explanation. |
The exact cause of the unusual geomorphology in the area still remains uncertain. Haworth (1896 #2814) first suggested that these features could be related to faulting, whereas other authors contend that dissolution of subsurface evaporites and subsequent collapse of overlying strata have played a major role in the area's geomorphology (Frye, 1942 #2809). Gutentag and others (1981 #2811) and Izett and Honey (1995 #2812) report that the stratigraphic offsets are only the result of dissolution of subsurface evaporites.
|Age of faulted surficial deposits||The age of the youngest faulted deposits is uncertain. If the stratigraphic offsets are solely caused by dissolution, then Holocene deposits are "faulted" because sinkholes have formed during historical time (Frye, 1942 #2809). The geological history related to the Crooked Creek fault is poorly known, but Smith (1940 #2813) suggests that the late stages of movement history included ". . . renewal of downward movement along the southern part of the trough in early Pleistocene time, leading to the deposition of the Odee formation; and continued movement in later Quaternary time, outlining the details of the present topography . ." Frye and Hibbard (1941 #2810 p. 397) state that "The latest movement along the Crooked Creek fault occurred in the Recent epoch, displacing the Pleistocene formations and again giving surface expression to the basin."|
|Most recent prehistoric deformation|
|Slip-rate category||Insufficient data|
|Date and Compiler(s)||1998|
Anthony J. Crone, U.S. Geological Survey
|References||#2809 Frye, J.C., 1942, Geology and ground-water resources of Meade County, Kansas: Bulletin of the University of Kansas, State Geological Survey of Kansas 45, 152 p.|
#2810 Frye, J.C., and Hibbard, C.W., 1941, Pliocene and Pleistocene stratigraphy and paleontology of the Meade basin, southwestern Kansas, in 1941, Reports of studies: State Geological Survey of Kansas Bulletin 38, p. 390-424.
#2811 Gutentag, E.D., Lobmeyer, D.H., and Slagle, S.E., 1981, Geohydrology of southwestern Kansas: Kansas Geological Survey Irrigation Series 7, 73 p., 3 pls.
#2814 Haworth, E., 1896, Local deformation of strata in Meade County, Kansas and adjoining territory (preliminary): American Journal of Science, v. 2, p. 368-373.
#2812 Izett, G.A., and Honey, J.G., 1995, Geologic map of the Irish Flats NE quadrangle, Meade County, Kansas: U.S. Geological Survey Miscellaneous Investigations Map I-2498, scale 1:24,000.
#2813 Smith, H.T.U., 1940, Geological studies in southwestern Kansas: Bulletin of the University of Kansas, State Geological Survey of Kansas 34, 212 p.