Rock City, Kansas

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Rock City
Rock City

Rock City is a park, which is owned by a non-profit corporation, located on hillsides overlooking the Solomon River in Ottawa County, Kansas. It is located 3.6 miles south of Minneapolis, Kansas off of Kansas Highway 106. In a patch of prairie about 500 meters (1600 feet) long and 40 meters (130 feet) wide, Rock City contains three clusters of large spherical boulders. These three clusters contain a total of 200 spherical boulders. This park has a visitor center and picnic tables. A small admission fee, which is used to maintain this park, is charged for access to it. It has been designated as a National Natural Landmark. More information about Rock City can be obtained from the Chamber of Commerce, 213 West Second, Minneapolis, KS 67467, (785) 392-3068.

The remarkable size and spherical shape of these boulders was first noted by Bell (1901). Later, these boulders were either noted or described by Gould (1901), Landes (1935), Schoewe (1937), Shaffer (1937), Ward (1939), and Swineford (1947). Shaffer (1937) was the first to map the distribution of these boulders at Rock City and investigate their petrography in detail (McBride and others 2006).

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[edit] Physical Characteristics

Large spherical boulders, which occur in Rock City, are giant calcite-cemented concretions, which are typically called "cannonball concretions" because of their subspherical to spherical shape. They range in diameter from 3 to 6 meters (10 to 20 feet) with the average diameter being 3.6 meters (12 feet). These concretions lie 2 to 8 meters (6.6 to 26 feet) apart (McBride and others 2006). Similar giant calcite-cemented concretions have also been found in a quartzite quarry within Lincoln County and in exposures of the the similar age sandstones in Utah and Wyoming (McBride and others 2003, 2006).

These boulders consist of well-sorted, medium-grained sandstone, which is tightly cemented by calcite. The sandstone consists or more than 95 percent quartz sand. About 20 percent of the original sandstone, mostly feldspar grains, has been replaced by the calcite. Pyrite, which is now oxidized to goethite, occurs within the calcite cement of these concretions as microscopic crystals and very small, knobby concretions. The pyrite concretions typically are about 30 cm (1 foot) in diameter. Also, included within these calcite concretions are smaller calcite concretions, which have been engulfed by the growth of the larger concretions (McBride and others 2006).

The host rock, which contained these spherical boulders, consists of well-sorted, medium-grained, highly porous, and friable sandstone. Being only weakly indurated by small amounts of iron oxide, sometimes seen as Liesegang rings (banding) at Rock City, it is considerably softer and very much more easily eroded than the calcite concretions. The sand comprising it accumulated within a river channel, which is part of the Dakota Sandstone, which accumulated within a low-lying coastal plain. Differential cementation and later erosion of cross-bedding inherited from the riverine sand, in which these concretions occur, created the "ornamentation", which these concretions exhibit (McBride and others 2006).

[edit] Origin

As discussed in detail by McBride and others (2006), these spherical boulders are giant calcite-cemented concretions. In the past, the origin of the spherical boulders found at Rock city had been erroneously interpreted as glacial boulders, corals, concretionary masses of limestone, and normal erosional remnants of sandstone. Shaffer (1937) was the first to recognize them as calcite-cemented concretions. From a detailed examination of the mineralogy of these concretions and the carbon and oxygen isotopes of the calcite cement comprising them, McBride and others (2006) concluded that they formed as the result of diffusion of calcium through and precipitation of calcite within the sandstone containing them after being deeply buried. The carbon and calcium comprising these concretions came either from marine limestone, shells, anhydrite, or some combination of these in addition to bicarbonate derived from oxidized methane from strata outside of, but hydrologically connected to, the Dakota Sandstone. After the formation of the concretions, differential erosion of the considerably softer sandstone surrounding them exposed as free-standing boulders (McBride and others 2006).

[edit] References Cited

  • Bell, W.T., 1901, The remarkable concretions of Ottawa County, Kansas, American Jounral of Science, 4th Series, v. 11, p. 315-316.
  • Gould, C.N., 1901, The Dakota Cretaceous of Kansas and Nebraska, Kansas Academy of Science, v. 17, p. 122-178.
  • Landes, K.K., 1935, Scenic Kansas, Geological Survey of Kansas Bulletin, no. 36, 55 p.
  • McBride, E.F., and K.L. Milliken, 2006, Giant calcite-cemented concretions, Dakota Formation, central Kansas, USA, Sedimentology, v. 53, n. 5, p. 1161–1179.
  • Shaffer, H.L., 1937, Concretions in the Dakota Sandstone, Compass, v. 17, p. 87-90.
  • Swineford, A., 1947, Cemented sandstones of the Dakota and Kiowa formations in Kansas, Geological Survey of Kansas Bulletin, no. 79, p. 53–104.
  • Ward, H.K., 1938, Concretions of Rock City. Mineralogist, v. 6, p. 23-24.

[edit] External links

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