scholarly journals Patterns in Shoreline Vegetation and Soils Around Lake Mohave, Nevada and Arizona: Implications for Management

2011 ◽  
Vol 71 (3) ◽  
pp. 374-387 ◽  
Author(s):  
Nita Tallent ◽  
Maliha Nash ◽  
Chad L. Cross ◽  
Lawrence R. Walker
Keyword(s):  
2005 ◽  
Author(s):  
VeeAnn A. Cross ◽  
David S. Foster ◽  
David C. Twichell

1967 ◽  
Vol 32 (3) ◽  
pp. 345-353 ◽  
Author(s):  
Emma Lou Davis
Keyword(s):  

AbstractAlso, Heizer questions the existence of a period of climate moister than that of today at the time when makers of the Lake Mohave lithic complex camped about high shorelines.The following article attempts to do two things:(1) Distinguish descriptively between sand-wear and wave-wear so that other archaeologists can use these criteria.(2) Show that a widespread cultural co-tradition existed in the Inter-Montane West about 7000 B.C. during a period of moister climate. Artifact inventories are submitted. This co-tradition was characterized by sparsity or lack of stone-on-stone milling, by a number of unique implements, and by a practice of frequenting the shores of now-dry water sources. This widely distributed orientation toward fossil water implies a generally wetter climate at that time.This co-tradition was characterized by sparsity or lack of stone-on-stone milling, by a number of unique implements, and by a practice of frequenting the shores of now-dry water sources. This widely distributed orientation toward fossil water implies a generally wetter climate at that time.


1962 ◽  
Vol 28 (2) ◽  
pp. 172-180 ◽  
Author(s):  
William J. Wallace

AbstractArchaeological remains from the southern Californian desert region, spanning a period from 7000 B.C. to historic times, are segregated into four broad cultural horizons. The earliest certain evidences of human occupation consist of stone tools and weapons from the shore line of ancient Lake Mohave. The Lake Mohave artifacts comprise types designed primarily for hunting and related activities. Next in sequence are the lithic materials from Pinto Basin and other localities that demonstrate a mixed hunting-gathering economy. The third or Amargosa period is inadequately known. Triangular arrowpoints, pottery, and numerous seed-grinding implements distinguish the closing aboriginal phase. The major research needs are indicated.


1938 ◽  
Vol 4 (2) ◽  
pp. 154-155
Author(s):  
Robert McCormick Adams

Archaeological reconnaisance work along the ancient shore lines of desiccated Lake Mohave, located south of Death Valley in California, has been interpreted by Mr. and Mrs. Campbell and their associates. Groups of implements were found along the old beach line located above the present playa. These were found at approximately the same vertical elevation. Most geologists, including D. G. Thompson, O. E. Meinzer, and E. Antevs, are concurrent in the belief that the desiccation of this lake took place in late Pleistocene times; although Thompson believes the antiquity to be uncertain. The age of the lake, together with neighboring lake beds which are also desiccated, was interpreted by geologists before archaeologists became interested in the problem; however, it is possible that the groups of implements found exposed in the beaches might be considerably younger than the Pleistocene phase of the lake's existence. The presence of modern camp sites containing materials typologically different than those mentioned above was determined at the southern portion of the lake near existing or recent springs.


1967 ◽  
Vol 32 (2) ◽  
pp. 168-185 ◽  
Author(s):  
Claude N. Warren

AbstractThe confusing terminology surrounding the San Dieguito complex is reviewed, and a critical evaluation of the content of this complex is undertaken. The San Dieguito complex is redefined and includes Lake Mohave, Death Valley I, and Playa I and II complexes. An age of greater than 6000 B.C. is shown for at least one component of the complex and a date of 7000 to 8000 B.C. is suggested for the complex as a whole.The hypothesis is developed that the San Dieguito complex is distinct from the Desert culture and represents a generalized hunting tradition which moved into the area along a north-south belt in the western Great Basin.


<em>Abstract</em>.—The striped bass <em>Morone saxatilis </em>was introduced into the lower Colorado River in the late 1950s and into Lake Mead, Nevada and Arizona, in the late 1960s. The unintended immigration of striped bass into Lake Mohave, Nevada and Arizona, on the main stem, and Lake Pleasant, a tributary reservoir in central Arizona, has resulted in changing management practices. Striped bass entered Lake Mohave via downstream emigration from Lake Mead through Hoover Dam at various life stages, and the newly established population quickly became the primary sport fish in the reservoir. Predation from the striped bass population in Lake Mohave coincided with elimination of threadfin shad <em>Dorosoma petenense </em>and a rapid decline in the survival of stocked rainbow trout <em>Oncorhynchus mykiss</em>. Striped bass are also believed to be hindering ongoing efforts to reestablish the native endangered species razorback sucker <em>Xyrauchen texanus </em>and bonytail chub <em>Gila elegans</em>. Striped bass gained access to Lake Pleasant via Lake Havasu, California and Arizona, by way of the Central Arizona Project (CAP) Canal. Operation of the CAP Canal began in 1985 and the canal was fully connected to Lake Pleasant in 1992. In 1986 and 1989, striped bass population densities in the CAP Canal were estimated at 70 ± 37 fish/ha and 3 ± 1 fish/ha, respectively. Striped bass were first captured in Lake Pleasant in 1998 during a gill-netting survey. Catch per unit effort increased almost yearly from 0.13 fish/net-night in 1998 to 6.74 fish/net-night in 2005. Since their unintended introduction into both reservoirs, striped bass have established viable reproducing populations. Management efforts have emphasized promoting harvest and minimizing the impacts of striped bass on existing fisheries. These experiences provide guidance for evaluating unintended dispersion of striped bass elsewhere.


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