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Fort Hays Limestone Member

The Fort Hays Limestone is a member of the Niobrara Formation of the Colorado Group exposed in Colorado, Kansas, Nebraska, and South Dakota and is named for the bluffs near the old Fort Hays, a well-known landmark in western Kansas.[1][2]

Fort Hays Limestone
Stratigraphic range: Cretaceous
Fort Hays Limestone in the K-147 road cut at the Cedar Bluff State Park, Kansas, USA.
TypeFormation Member
Unit ofNiobrara Formation of the Colorado Group
UnderliesSmoky Hill Chalk Member of the Niobrara Formation
OverliesNon-conformably, Codell Sandstone, Blue Hill Shale, or Juana Lopez members of the Carlile Formation
Lithology
PrimaryLimestone
OtherShale partings
Location
RegionMid-continental: Colorado, Kansas, Nebraska, South Dakota
Country United States
Type section
Named forFort Hays
Named byS. W. Williston[1]
LocationHogback ridge just west of old Fort Hays, Kansas
Year defined1893[1]

Defining the southeast border of the High Plains, the towering stone-capped bluffs of the Fort Hays Escarpment are "perhaps the most conspicuous physiographic boundary in Kansas."[3]

The iconic stone blockhouse of Fort Hays is built from the namesake limestone.


The Fort Hays Limestone was a generally practical building stone. However, it deteriorates when in contact with soil (note the repaired foundation on the Old Fort Hays Blockhouse). In contrast, the Fencepost limestone is quite durable in the ground, so, the Fencepost can be seen in foundation course of buildings that are otherwise faced with Fort Hays Limestone. Particularly in Hays and Ellis, where the Fort Hays and Fencepost outcrops are in close geographic proximity, the two limestones are seen in combination in buildings.[4][5]

See also edit

References edit

  1. ^ a b c Daniel F. Merriam (1963). "The Geologic History of Kansas". Kansas Geological Survey Bulletin (162). Kansas Geological Survey. Retrieved 2017-01-22. The term Fort Hays is derived from old Fort Hays, a well-known landmark in western Kansas, and was first used by Samuel Wendell Williston in 1893.
  2. ^ Howard E. Simpson. "Geology of the Yankton Area South Dakota and Nebraska" (PDF). Geological Survey Professional Paper (328). U.S. Department of the Interior.
  3. ^ Grace Muilenburg; Ada Swineford (1975). "Wence the Fence: Geology of the Post Rock". Land of the Post Rock – Its Origins, History, and People. University Press of Kansas, Lawrence. pp. 89–91.
  4. ^ Warren G. Hodson (1965). Geology and Ground-Water Resources of Trego County, Kansas, Kansas Geological Survey, Bulletin 174. University of Kansas Publications, State Geological Survey of Kansas. p. Economic Geology, continued. The Fort Hays Limestone Member of the Niobrara Chalk has been quarried for structural stone at numerous localities in Trego County. The Fort Hays is relatively soft, although it hardens upon weathering. The Fort Hays also tends to absorb water and thus to deteriorate through freeze-and-thaw action and from spalling. Many farm buildings, city dwellings, and business houses in the area constructed of the Fort Hays Limestone seem to stand up well for many years, however. In a report by Risser (1960) the sources and characteristics of building stone in Kansas are discussed.
  5. ^ Alvin R. Leonard and Delmar W. Berry (1961). Geology and Ground-water Resources of Southern Ellis County and Parts of Trego and Rush Counties, Kansas, Kansas Geological Survey, Bulletin 149. University of Kansas Publications, State Geological Survey of Kansas. p. Geography. In addition to fence posts, the [Fencepost] limestone has been used widely in southern Ellis County and elsewhere for foundations and buildings. Among the buildings constructed from this stone are the magnificent Catholic churches at Pfeifer, Victoria, and Liebenthal and the principal buildings at the Fort Hays State College in Hays. Newer buildings constructed from sawed blocks of this stone include the Methodist church and the Ellis County courthouse in Hays. ... The Fort Hays Limestone member of the Niobrara Chalk also has been quarried for structural stone, although it is not as weather-resistant as the "Fencepost" Limestone bed. It is softer than the Greenhorn Limestone and spalls badly when used for foundation stone.


fort, hays, limestone, member, fort, hays, limestone, member, niobrara, formation, colorado, group, exposed, colorado, kansas, nebraska, south, dakota, named, bluffs, near, fort, hays, well, known, landmark, western, kansas, fort, hays, limestonestratigraphic,. The Fort Hays Limestone is a member of the Niobrara Formation of the Colorado Group exposed in Colorado Kansas Nebraska and South Dakota and is named for the bluffs near the old Fort Hays a well known landmark in western Kansas 1 2 Fort Hays LimestoneStratigraphic range CretaceousFort Hays Limestone in the K 147 road cut at the Cedar Bluff State Park Kansas USA TypeFormation MemberUnit ofNiobrara Formation of the Colorado GroupUnderliesSmoky Hill Chalk Member of the Niobrara FormationOverliesNon conformably Codell Sandstone Blue Hill Shale or Juana Lopez members of the Carlile FormationLithologyPrimaryLimestoneOtherShale partingsLocationRegionMid continental Colorado Kansas Nebraska South DakotaCountry United StatesType sectionNamed forFort HaysNamed byS W Williston 1 LocationHogback ridge just west of old Fort Hays KansasYear defined1893 1 Defining the southeast border of the High Plains the towering stone capped bluffs of the Fort Hays Escarpment are perhaps the most conspicuous physiographic boundary in Kansas 3 The iconic stone blockhouse of Fort Hays is built from the namesake limestone The Fort Hays Limestone was a generally practical building stone However it deteriorates when in contact with soil note the repaired foundation on the Old Fort Hays Blockhouse In contrast the Fencepost limestone is quite durable in the ground so the Fencepost can be seen in foundation course of buildings that are otherwise faced with Fort Hays Limestone Particularly in Hays and Ellis where the Fort Hays and Fencepost outcrops are in close geographic proximity the two limestones are seen in combination in buildings 4 5 See also edit nbsp Earth sciences portal nbsp Kansas portal nbsp Paleontology portalList of fossiliferous stratigraphic units in Colorado List of fossiliferous stratigraphic units in Kansas List of fossiliferous stratigraphic units in Nebraska Paleontology in Colorado Paleontology in Kansas Paleontology in NebraskaReferences edit a b c Daniel F Merriam 1963 The Geologic History of Kansas Kansas Geological Survey Bulletin 162 Kansas Geological Survey Retrieved 2017 01 22 The term Fort Hays is derived from old Fort Hays a well known landmark in western Kansas and was first used by Samuel Wendell Williston in 1893 Howard E Simpson Geology of the Yankton Area South Dakota and Nebraska PDF Geological Survey Professional Paper 328 U S Department of the Interior Grace Muilenburg Ada Swineford 1975 Wence the Fence Geology of the Post Rock Land of the Post Rock Its Origins History and People University Press of Kansas Lawrence pp 89 91 Warren G Hodson 1965 Geology and Ground Water Resources of Trego County Kansas Kansas Geological Survey Bulletin 174 University of Kansas Publications State Geological Survey of Kansas p Economic Geology continued The Fort Hays Limestone Member of the Niobrara Chalk has been quarried for structural stone at numerous localities in Trego County The Fort Hays is relatively soft although it hardens upon weathering The Fort Hays also tends to absorb water and thus to deteriorate through freeze and thaw action and from spalling Many farm buildings city dwellings and business houses in the area constructed of the Fort Hays Limestone seem to stand up well for many years however In a report by Risser 1960 the sources and characteristics of building stone in Kansas are discussed Alvin R Leonard and Delmar W Berry 1961 Geology and Ground water Resources of Southern Ellis County and Parts of Trego and Rush Counties Kansas Kansas Geological Survey Bulletin 149 University of Kansas Publications State Geological Survey of Kansas p Geography In addition to fence posts the Fencepost limestone has been used widely in southern Ellis County and elsewhere for foundations and buildings Among the buildings constructed from this stone are the magnificent Catholic churches at Pfeifer Victoria and Liebenthal and the principal buildings at the Fort Hays State College in Hays Newer buildings constructed from sawed blocks of this stone include the Methodist church and the Ellis County courthouse in Hays The Fort Hays Limestone member of the Niobrara Chalk also has been quarried for structural stone although it is not as weather resistant as the Fencepost Limestone bed It is softer than the Greenhorn Limestone and spalls badly when used for foundation stone nbsp This article about a specific stratigraphic formation in Kansas is a stub You can help Wikipedia by expanding it vte nbsp This article related to the Cretaceous period is a stub You can help Wikipedia by expanding it vte Retrieved from https en wikipedia org w index php title Fort Hays Limestone Member amp oldid 1206226728, wikipedia, wiki, book, books, library,

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