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Bullion Mountains - Bristol Lake
This subsection includes alluvial fans, basin floor, volcanic flows, and mountains and hills in a linear depression that stretches from Troy Lake southeastward to Bristol Lake and beyond, plus the lower part of Fenner Valley. It has a very hot arid climate. MLRAs 30g and 30h.
Lithology and Stratigraphy. Quaternary alluvial, lacustrine, and eolian deposits and Cenozoic volcanic rocks predominate in this subsection. The volcanic rocks are mostly Miocene andesite and basalt and Quaternary basalt. The mountains are mostly Mesozoic granitic and Pre-Cenozoic metamorphic rocks.
Geomorphology. This subsection is on very gently to moderately sloping alluvial fans and volcanic flows, nearly level basin floor and dry lake bed, steep mountains, and moderately steep hills. Fenner Valley is aligned toward the northeast. The Sheep Hole and Calumet Mountains south of Bristol Lake and Bullion Mountains (subsection 322An) are aligned toward the northwest to north-northwest and the Ship Mountains in Fenner Valley are oriented toward the north-northeast. Bristol Lake is the largest dry lake bed; others are Troy, Broadwell, Lavic, and Dale Lakes. Two prominent craters on recent basalt flows are Pisgah Crater in the northwest part of the subsection and Amboy Crater on a flow over Bristol Lake. The elevation range is from about 620 feet on Bristol Lake up to 3726 feet in the Calumet Mountains, 4685 feet in the Sheep Hole Mountains, and 3300 feet in the Ship Mountains. Fluvial erosion and deposition, eolian deflation and deposition, and mass wasting are the main geomorphic processes.
Soils. The soils are mostly Lithic Torriorthents and Lithic Haplocambids on mountains and the rocky recent basalt flows, plus Lithic Haplargids on older volcanic flows and on north-facing slopes in granitic terrain. The soils are mostly Typic Torrifluvents, Typic Torripsamments, and Typic Torriorthents on younger fans and Durinodic Haplocalcids and Durinodic Calciargids on older fans. Typic Torripsamments and Arenic Haplargids occur in eolian sand. The soils are well drained, except on poorly drained playas. There are Salorthids on poorly drained playas lacking vascular plants. Soil temperature regimes are mostly thermic on the mountains and hyperthermic on large basin floors and on south-facing slopes at lower elevations. Soil moisture regimes are aridic.
Vegetation. The predominant natural plant communities are Creosote bush series and Creosote bush - white bursage series. Mixed saltbush series is common on basin floor and Iodine bush series and Saltgrass series are present on wet basin-fill and lacustrine deposits.
Grasslands: Alkali sacaton series, Big galleta series, Desert sand verbena series, Indian ricegrass series, Saltgrass series.
Shrublands: Brittlebrush series, Bush seepweed series, Creosote bush series, Creosote bush - white bursage series, Desert-holly series, Fourwing saltbrush series, Greasewood series, Iodine bush series, Joshua tree series, Mixed saltbush series, Scadscale series, White bursage series, Winter fat series.
Forests and woodlands: Blue palo verde - ironwood - smoke tree series, Mesquite series.
Surface Water. Runoff is rapid from mountains and alluvial fans and slow from basin-fill. All drainage is internal, to closed basins in the subsection. Streams are dry most of each year; they may have no water in them some years. There is temporary ponding on playas, or dry lake beds.< previous - Mojave Desert - next >
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Troy dry lake, Newberry Springs, CA
Bristol dry lake, Amboy, CA
Kelso Dunes WildernessWithin this wilderness lie two sweeping valleys: the rolling Bristol Mountain and the Kelso Sand Dunes ...
Bristol Mountains WildernessA portion of the rolling Bristol Mountains and a tilted volcanic plain form this wilderness. The lack of any springs and extreme ...