... Member, has been named formally; it is the unit studied in this paper. The Fort Apache Member of the Supai Formation is well exposed in canyon walls along the Mogollon Rim for the Fort Apache—White River area of the Fort Apache Indian Reservation west to Oak Creek Canyon south of Flagstaff ( Fig...

... of terraces for nine localities (Fig. 1). These are: (1) the Colorado River at Oak Bay, Utah, ~10 km below the San Juan-C olorado River confluence; (2) the Colorado S an Juan River confluence in Glen Canyon, Utah; (3) the lower San Juan River near the Great Bend meander, Utah; (4) the San Juan River from...

...Figure 7. The geology of Surveyor Canyon (site location 8 on Fig. 1 ). (A) Location of Surveyor Canyon, a tributary to Oak Creek Canyon. (B) Area mapped in this study. The black and white line corresponds to the profile location in (C) and (D). The topography and geology along the red and black...

....) in the Simi field. 14 In the Oak Ridge fields, Shiells Canyon, 15 Bardsdale, 16 and South Mountain, 17 most of the production has been from sands in the lower part of the more shaly middle division of the Sespe from 1,500 to 2,700 feet above the top of marine Eocene. A little oil has been...

... with minor damage recorded in Kachina Village and Flagstaff. Rockfalls were reported in Oak Creek Canyon, and several of the aftershocks and one foreshock were also felt in Kachina Village and west Flagstaff ( Arizona Daily Sun, 2014 ). Figure 1. Felt intensities for the 1 December 2014 M w  4.7...

... intimately associated with oil, but in the Wiley Canyon dome, which is barren of oil, identical waters occur. For this reason it seems certain that the character of the waters is not due to reaction with oil. The chemical character of the waters from the Sespe formation, from localities along the Oak...

... Canyon, Los Angeles County, California. Based on their orientation and projection to the surface, we suggest that the imaged fault zones are extensions of the Oak Ridge fault. Geologic mapping by others and correlations with seismicity studies suggest that the Oak Ridge fault is the causative fault...

... Pass. Because of the weathering characteristics of the Tertiary rocks, the contact is everywhere covered with colluvium; however, three-point solutions suggest that the contact dips westward at angles varying from 18°–23° north of Oak Creek Canyon ( fig. 2 , OC ) to 27° or more south of the canyon...

..., 1987 ). The Debeque Canyon Landslide south of Debeque is also larger, but it is composed of a large rock mass similar to the Dotsero analog landslide and the original landslide block at WSC ( White et al., 2003 ). Recall that, because of exposure limitations, we were forced to measure to top...

... Susana Mountains; the central part, between Torrey Canyon, on the east and Sulphur Canyon on the west, is known as Oak Ridge, while the extreme western end is called South Mountain. This range gradually becomes lower toward the west and finally dies out just east of the town of Saticoy, where Santa Clara...

...W. Chase Gerald Fig. 1. Areal Geologic Map of the Post Oak Conglomerate and Related Rocks Wichita Mountains, Oklahoma © 1954 American Association of Petroleum Geologists. All rights reserved 1954 American Association of Petroleum Geologists Introduction. —During the compiling...

... Island; CIP—Channel Islands platform; CT—Channel Islands thrust; DF—Dume fault; EF—Elsinore fault; Go—Goleta; HC—Hueneme Canyon; HF—Hosgri fault; MCF—Malibu Coast fault; MD—Mojave Desert; NIF—Newport-Inglewood fault; NPF—North Channel–Pitas Point fault system; O—Oxnard; ORF—Oak Ridge fault; P—Palos...

.... During deposition, the northeast-dipping Steel Canyon normal fault accommodated uplift of an intrabasinal horst that shed a wedge of Third Creek Member conglomerate eastward into the lake system between ∼10.0 and <9.2 Ma. The Third Creek Member interfingers with a Cache Valley Member lake-margin tufa...

... fault system that separates the western Transverse Ranges from the California Continental Borderland. The white box labeled “S” locates the town of Saticoy. orf means Oak Ridge fault. View is to the west–northwest. Topography is shown with a vertical exaggeration of 1.8. The image incorporates Shuttle...

.... The basal part of the Paleocene Silverado Formation in the Santa Ana Mountains consists of nonmarine conglomerate. In the western Santa Monica Mountains, in Solstice Canyon ( Fig. 3 ), Secs. 21, 22, T1S, R18W, the Paleocene consists of poorly bedded brownish-white cobble conglomerate and coarse...

..., galls of A. schorni , A. polygonalis , and A. cyanomontanus are more similar in form to the Palearctic species Cynips cornifex (Hartig, 1843), on the European white oak Q. pubescens Willdenow, 1796 than they are to X. clavuloides or the undescribed gall on the canyon live oak, Q. chrysolepis...

... and McCollum, 2011 ; Sundberg, 2011 ; Webster, 2011a ). Shaded stars mark the sections investigated: AC, Antelope Canyon; E, Echo Canyon; GR, Groom Range; GS, Grassy Spring; I, Indian Springs Canyon; LC, Log Cabin Mine; M, Montezuma Range; OS, Oak Spring Summit; SM, Split Mountain. White circles represent...