![]() ![]() ![]() The Todilto Formation is the older unit and forms a thin, white to gray, resistant cap on top of the Entrada Sandstone. The Jurassic Todilto and Summerville formations overlie the Entrada Sandstone. The sand dunes were cemented by silica andĬalcite from ground water and compacted to form the massive rock cliffs seen today. High-angle crossbeds or layers are seen in the sandstone. The Slick Rock Member forms the spectacular cliffs and consists of 100-400 ft of reddish-orange well-cemented, thick-bedded, well-rounded sandstones, typical ofĪncient sand dunes. The Dewey Bridge Member consists of 40-60 ft of reddish-brown, reddish-orange silty sandstone and siltstone that form slope the base of the massive cliffs. The Entrada Sandstone is divided into two members, Dewey Bridge Member and overlying Slick Rock Member. The spectacular massive cliffs forming background for the public facilities in the park belong mostly to the Jurassic Entrada Sandstone. Older rocks, the Triassic river deposits of the Chinle Group, are exposed in the plains to the south of the park and younger Cretaceous rocks form the high ridges north of the park. Gallup offers a unique array of happenings and events to discover throughout the year. Middle to Upper Jurassic (175-145 million years old) and Quaternary ( less than 1 m.y.) rocks are exposed in Red Rock Park (Figures 2 and 3). Figure 3 – Jurassic section exposed along or visible from the trail to Church Rock (Lucas et al., 2003). (Green and Jackson, 1975 Lucas et al., 2003). Upper-midscale, smoke-free hotel near I-40 8.5 miles from Red Rock Park 4 floors, 69 rooms and suites Indoor swimming pool is closed until March 2023. Main campground, historic Outlaw Trading Post, and U.S. Red rock 10 gallup nm free#This 103-room hotel has conveniences like free breakfast. Museum, convention hall, arena complex, 2. Red Roof Inn Gallup places you within a 10-minute drive of Historic District and El Morro Theatre. Geology Figure 2 – Geologic map of Red Rock Park with public facilities. The park is located 10 miles east of Gallup in McKinley County, north of I-40 via NM-566 ( Figure 1). Gallup-McKinley County Chamber of Commerce Directory search results for: bible.ph-The One Bible. Red Rock Park opened in 1972 as a state park at a cost of $6 million (McLemore, 1989), but in 1989 the park was turned over to the Navajo Nation. The 640-acre park offers excellent scenery for balloonists, hikers, campers, and other visitors. ![]() Church Rock, or Navaho Church, is a prominent landmark in the park. Red Rock Park takes its name from the spectacular red sandstone cliffs surrounding an impressive array of public facilities, including a rodeo arena, convention center, museum, and campgrounds. Introduction Figure 1 – Index map showing location of Red Rock Park (formerly Red Rock State Park). McLemore, V.T., 2003, Red Rock Park, New Mexico Geological Society Guidebook 54, p. McLemore, V.T., 1989, Red Rock State Park: New Mexico Geology, v.
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