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BUTTerwICK & dANIeL: FLOrA OF SOUTHerN BLACK MTS., ArIzONA 275<br />
The yuman peoples used many additional plant resources, not only for food but also for fiber,<br />
construction, implements, basketry, water proofing, adhesives, dyes, medicine and fuel, among<br />
other uses (Stone 1987). we documented the following plant species, which serve as sources for<br />
many of these uses, in the flora area: Allium nevadense, Baccharis salicifolia, Celtis reticulata,<br />
Chenopodium berlandieri, Chenopodium fremontii, Chilopsis linearis, Fouquieria splendens,<br />
Fraxinus anomala, Larrea tridentata, Mentzelia albicaulis, Physalis crassifolia, Pluchea sericea,<br />
Populus fremontii, Rhus aromatica, Salix exigua, Salix gooddingii, Salvia columbariae, Typha latifolia,<br />
and Vitis arizonica.<br />
The Hualapai in the Black Mountains interacted frequently with the Mohave people, trading<br />
wild products for agricultural produce from the floodplain of the Colorado river (Stone 1987). The<br />
Mohave practiced a generalized settlement-subsistence pattern, which included farming, fishing,<br />
hunting, and gathering wild plants. Their settlements shifted in arrangement, composition, and<br />
location from year to year and season to season to cope with the unpredictable variations in the timing<br />
and volume of annual floods (Bee 1981). Crops they cultivated included corn, beans, squash,<br />
melons, and grasses. However, gathered resources were not mere supplements to cultivated crops<br />
but constituted a diverse and important component of the Mohavean diet. According to Castetter<br />
and Bell (1951:179–180), mesquite beans continued to be a staple resource into the 20 th century<br />
and was “more important than maize . . . and virtually supplied the living through the winter and<br />
until the next cultivated crop was ready.” Because large game was scarce along the river, fish, such<br />
as the humpbacked sucker and Colorado salmon or squawfish, and small game were the major<br />
sources of protein. during winter, small hunting parties pursued deer and bighorn sheep in the<br />
desert mountain ranges, including the Black Mountains. An annual lean period of reduced supplies<br />
occurred in the spring, when few wild plant resources were available and fish were relatively<br />
scarce. The duration and severity of this lean time depended on the amount and rate of consumption<br />
of stored foods from the previous seasons (Stone 1987).<br />
The remote and rugged terrain of the Black Mountains provided the yuman peoples respite<br />
from the effects of early Spanish contact. However, by the 1800s Anglo-American explorers ventured<br />
into the area. The California gold rush in the 1850s led to increased travel and settlement in<br />
western Arizona. In 1863 gold was first discovered in the Black Mountains at the Moss vein northwest<br />
of Oatman (gray et al. 1990b; ransome 1923). Varying levels of mineral production continued<br />
in the Oatman mining district until 1942. Numbers of feral burros, originally released by the<br />
miners working in the area, increased significantly, resulting in degradation of the vegetation and<br />
perennial springs and competition with the desert bighorn sheep for limited resources. After the<br />
introduction of cattle in Mohave County, army officers consistently reported that livestock grazing<br />
reduced the quantity of wild game and the supply of edible seed (United States Senate 1936). davis<br />
(1973) documented that Sacramento Valley, now desertscrub dominated by Larrea tridentata and<br />
Ambrosia dumosa, was once an open grassland. In 1865 the Colorado river Indian reservation<br />
was established, thereby providing the Mohave people with only a portion of their former prime<br />
farming and gathering lands. In 1883 the Hualapai Indian reservation was established at the north<br />
end of the Hualapai people’s historic area of occupation. A profound impact to the Mohave people’s<br />
way of life resulted from construction of major dams on the Colorado river between 1930<br />
and 1970. These changed the water flows and aquatic temperature, tamed the annual floods, and<br />
reduced transport of sediment, all of which contributed to the loss of marshes and mesquite bosques<br />
as well as the native fish populations (Cole 1981). given the magnitude of changes within the past<br />
century, it is difficult to see how a traditional subsistence economy could be sustained under current<br />
conditions in and around the Black Mountains.