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Whipple Mountains

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Forming the easternmost portion of California and relatively isolated by the Colorado River as well as by the desert washes to the west, this range supports an interesting flora.  A sparse creosote bush scrub on the rocky substrate covers most of the range.  There are, however, some riparian and desert-wash associations.

Here is one of the few places that the giant saguaro, Carnegiea gigantea, is found in the State.  While the blue palo verde, Cercidium floridum, is common here and elsewhere in the State, this is one of the few known localities where the foothills palo verde, Cercidium microphyllum, occurs in California.  In these mountains the fishhook cactus, Mammillaria milleri, is at or near its western distribution limit.  There is a stand of the California fan palm, Washingtonia filifera, which, though it occurs in several locales in Arizona, is here at the northeastern limit of its distribution.

Animals are relatively abundant in the mountains. Bighorn, Ovis canadensis, are found here, as are desert tortoises, Gopherus agassizi.  In the riparian portions the Colorado River toad, Bufo alvarius, and the tree lizard, Urosaurus ornatus, are at the northern and western limits, respectively, of their ranges.  There are important bat populations in the region.

The basic rock complex is Pre-Cambrian igneous and metamorphics with some Tertiary volcanics.  There are numerous faults.  In some areas it is possible to observe gravity slide blocks of Tertiary rhyolite resting on Pre-Cambrian granitics.

There are a number of indurated packrat, Neotoma sp., middens in the range.  These middens contain plant microfossils, pollen, bones, insect remains, etc., and are being analyzed to develop data on the climate, flora, etc., of the area.  They date from a few hundred years to more than 40,000 B.P. and, with few exceptions, record the existence of woodland or forest plant communities in the modern, hot desert – woodlands that persisted until some 8,000 years ago.

Integrity:  Though there is some development along the Colorado River and a few trails and an aqueduct run through the area, most of the range is virtually undisturbed; however, there are some effects of overgrazing by wild burros.

Use:  Research, educational, observational, Some private.

Ref:  Van Devender, T. R.  1976.  Biota of the Hot Deserts of North America During the Last Glaciation: the Packrat Midden Record.  Abst. Amer. Quat. Assn. Oct. 1976 meeting.

December 1976  

San Bernardino
Inventory of California Natural Areas
Revision © 2005 Steven Louis Hartman

 

 

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Last modified: December 06, 2005