Cathedral Gorge State Park
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Cathedral Gorge State Park is a Nevada State Park covering 1,608 acres (7.19 km²). It is located in Central/Eastern Nevada 1 mile (2 km) north of the intersection of U.S. Route 93 and State Route 319, near Panaca. Cathedral Gorge was first established as one of the four original Nevada State Parks in 1935. The park sits at an elevation of 4,800 feet (1,500 m) above sea level, and is typically arid with very hot summers, and very cold winters. In the summer, temperatures usually range from 95 degrees Fahrenheit (35 degrees Celsius) in mid-day to roughly 55 °F (13 °C) at night. Rainfall is variable, and thunderstorms are prevalent. At one time, Shakespearian plays were performed with the clay formations in the backdrop. The various naturally formed crevices were used as dressing rooms, and as a backstage where actors and actresses would prepare, awaiting their cue.
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[edit] Natural history
[edit] Geology
A majority of Meadow Valley (which lies along U.S. Route 93 from the towns of Caliente to Panaca) was covered by a freshwater lake nearly 1 million years ago during the Pliocene Era. The richly colored canyons of Cathedral Gorge (called the Panaca Formation) are remnants of this ancient lakebed. Over centuries, the lake began to gradually drain. Erosion began working away at the exposed portions of sediment and gravel that once composed the lake bottom. Rainwater and melting snow carved rivulets in the soft siltstone and clay shale, splitting tiny cracks and fissures into larger and larger gullies and canyons.
[edit] Plants
In areas below the eroded escarpment (dubbed the "Badland") it is difficult for plantlife to take root in the constantly eroding clay. However, away from the clay, the park's diverse soil types allow various plant associations to grow. Fragile sand dunes are held firm thanks to a wide array of wildflowers and grasses, such as Dune Primroses and Indian Rice Grass. Within the valley center, clay, sand, and gravel have melded to form a rich, granulated soil that encourages the growth of the following species: narrowleaf yucca, juniper trees, Barberry sagebrush, greasewood, white sage, shadscale, four-winged saltbush. Rabbitbrush finds sanctuary in disturbed areas, such as roadsides and walkways. Very few species of cactus can tolerate the climate in Cathedral Gorge, where temperatures in winter can fall below freezing, and rise above 100 °F (40 °C) in summer.
Other trees, not native to the park, have been planted around the campground to provide shade.
[edit] Animals
Small mammals form a majority of the park's animal population: black-tailed jackrabbits, cottontail rabbits, coyotes, gophers, kangaroo rats kit foxes, mice, and skunks. Deer can be observed infrequently near Miller Point during the late fall and winter.
Birds are seen frequently around camp areas, and near dense patches of shrubs. The natives include, blackbirds, black-throated sparrows, finches, American kestrels, small hawks, ravens, roadrunners, American robins, sapsuckers, and introduced European starlings. Migratory birds include, bluebirds, cedar waxwings, hummingbirds, and warblers.
Various species of non-poisonous snakes and lizards are abundant. In the summer, the Great Basin rattlesnake may be spotted.
