USGS ScienceSearch

Geology topics

Research about Transverse Ranges

Source-linked reports with geographic coverage including Transverse Ranges.

2 recordsLinked to original sources

Newly documented population extends geographic range and genetic diversity for the Leaf-toed Gecko (Phyllodactylus nocticolus) into the Transverse Ranges of southern California

Between 19 – 30 May 2018, one of us [AW] discovered a disjunct population of Peninsula leaf-toed geckos, Phyllodactylus nocticolus (Phyllodactylidae) on the northern edge of the Coachella Valley in the Little San Bernardino Mountains of the Transverse Ranges (Fig. 1a). The previously northernmost location for the species is Tahquitz Canyon, Riverside Co. (MVZ 212205) in the Peninsular Ranges 20 km to the south. Southern California has many herp enthusiasts and it is possible that this population is of anthropogenic origin through accidental or misguided purposeful introduction. The apparent barrier to dispersal suggests that, if of natural origin, the dispersal may have occurred at a time when the aeolian sand barrier was less severe. Thus, if this newly discovered population is of natural origin, we expect the genetic data of the disjunct Transverse Ranges population to differ from that of any population sampled in the Peninsular Ranges. Herein we describe this newly discovered population of P. nocticolus, we analyze genetic diversity from the new population, and we compare it with genetic data gathered from populations of P. nocticolus throughout southern California to help determine if this isolated gecko population was of natural dispersal or the result of human intervention. This is particularly noteworthy given the apparent strength of the Coachella Valley’s sand fields as a barrier to dispersal of highly saxicolous lizard faunas.

California

Lower crustal deformation beneath the central Transverse Ranges, southern California: Results from the Los Angeles Region Seismic Experiment

We present a P wave velocity model derived from active source seismic data collected during the 1994 Los Angeles Region Seismic Experiment. Our model extends previously published upper crustal velocity models to mantle depths. Our model was developed by both ray tracing through a layered model and calculating travel times through a gridded model. It includes an 8-km-thick crustal root centered beneath the surface trace of the San Andreas fault, north of the highest topography in the San Gabriel Mountains. A simple mass balance calculation suggests that ∼36 km of north-south shortening across the San Andreas fault in the central Transverse Ranges could have formed this root. If north-south compression began when the “Big Bend” in the San Andreas fault formed at ∼5 Ma, 36 km of shortening implies a north-south contraction rate of ∼7.1 mm/yr across the central Transverse Ranges. If, instead, north-south compression began when the Transverse Ranges formed at 3.4–3.9 Ma, 36 km of shortening implies a contraction rate of 9.2–10.6 mm/yr. North of the San Andreas fault, the Mojave Desert crust has a low-velocity (6.3 km/s) mid and lower crust and a 28-km-deep Moho. South of the San Andreas fault, beneath the Los Angeles and San Gabriel Valley basins, there is a fast (6.6–6.8 km/s), thick (10–12 km) lower crust with a 27-km-deep Moho. Farther south still, the lower crust of the Continental Borderland is fast (6.6–6.8 km/s) and thin (5 km) with a shallow (22 km deep) Moho.

California