Between the Franklin Mountains and the Hueco Mountains (to the east) lies the Hueco Bolson a relatively flat valley which is filled with sand and silts and is the major source of El Paso's water supply. The Rio Grande Valley is aligned from northwest to southeast, but curves prominently between Cerro Cristo Rey and the Southern Franklin Mountains, forming El Paso del Norte. The tectonic style of the Franklin Mountains comprises a north-trending, west-dipping, tilted fault block typical of Basin and Range structure (see Lovejoy, 1980). 2), and the El Paso Group overlies a Precambrian (Red Bluff) crystalline complex. At 9:00 is southern flank of Franklin Mountains, where Bliss Sandstone is overlain by Ordovician strata (Fig. Continue east on I-10 keep in right lane. Proceed north on Santa Fe Street.Ġ.1 Turn right on frontage road (Wyoming) and proceed eastward through 4 traffic lights.Ġ.9 Join I-10, travelJing east, passing Southern Pacific railroad yards.Ģ.2 Pass Southern Pacific railroad yards on right. The underground visit to the manto and breccia-pipe deposits at the Potosí mine, West Camp, Santa Eulalia completes the day.Ġ.0 Buenos dias. The Sierra de Samalayuca, near the community of the same name, has been considered by some to be Early Jurassic or Paleozoic in age, and it consists of weakly-metamorphosed sediments in an anticlinal structure. Of particular interest is the lower Cretaceous in Sierra del Presidio and Banco Lucero, Los Medanos (dune field), Sierra La Candelaria and Sierra El Kilo intrusions, and the Tertiary volcanic stratigraphy of Sierra Gallego (near El Sueco), Sierra El Nido, Sierra de La Campana, and Sierra Sacramento. Numerous ranges are visible from the roadside and some stops are scheduled for description of lithologies and structures, particularly where mapping has been accomplished. Much of the first day's route is spent in travelling in a southerly direction through desert basins to Chihuahua City (Fig.
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