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Conkling Cavern UTEP 90

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NM: Doña Ana Co.: 1399 m

General Description.—Vertical section (from museum model) shown in Conkling (1932). He mentions that the cavern was filled completely to within about 8 ft. "from the chimney-like neck at the entrance." "Examination of the cave deposit indicates that some of the material is of the nature of wind-blown dune sand redeposited in old river beds." In his list, he has fresh water shells and some plant material (root of Algaroba or Mesquite tree; plant leaves; branch Sotol Plant).

The cave site is near the eastern side of Bishop's Cap; Shelter Cave is high on the western side.

Age.—Howard and Miller (1933) point out the difficulty of trying to tell what is Pleistocene and what is not. Conclude that Conkling Cavern older than Shelter Cave and that at least material below the water-lain stratum is Pleistocene, and that in all probability some of the Shelter Cave deposits are Pleistocene.

Comments.—In comparing Conkling Cavern and Shelter Cave, note that in CC, great numbers of Coragyps occidentalis (47 specimens according to Conkling 1932) are present while Cathartes aura is scarce (one specimen according to Conkling 1932), while the first is absent and the second abundant in SC. Note that Conkling's identifications are based on lists supplied by Stock for mammals and Howard for birds— both were very preliminary and shouldn't be taken too seriously.

Publications.—*(Brattstom 1964); Bryan 1929; (*Conkling 1932); Harris 1985; Howard 1968; Howard and Miller 1933; Nowak 1979; Rea 1980; Smartt 1977; Stewart 1951; Stock 1936; Van Devender et al. 1976.

Fauna.—

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Last Update: 10 Mar 2008