While their activity most often passes outside the scrutiny of humans, the desert ecosystem is diverse. Fauna Of Valley Of Fire State Park Desert bighorn ram in Valley of Fire State Park, Nevada. Many other common desert plants bloom during the spring months, including the indigo bush, desert mallow, and desert marigold. There are several species of cactus in the park, including the beaver tail and cholla. All slow-growing shrubs that are ideally suited for dry, arid regions develop compact leaves and small flowers. The most common plants in the Valley of Fire State Park are creosote bush, burro bush, and brittlebush, which are found widely separated from each other. Flora In Valley Of Fire State Park Beavertail Cactus in Valley of Fire State Park, Nevada. During the summer, the Southwest Monsoon occasionally brings heavy rain showers. The area receives occasional rainfall during the cooler winter months, brought by storms over the Pacific Ocean. Temperatures may fluctuate 20 or 30 degrees between day and night. The park lies within the Mojave Desert and experiences a warm, dry climate with mild winters and hot summers, where temperatures can reach over 46☌. The park is home to petrified trees that are remnants of its days as a fertile region thousands of years ago. Elephant Rock in Valley of Fire State Park. Each type of rock erodes differently, and the multiple and complex changes created the spectacular configurations, including a floor and jagged walls. Along with sandstone, there are deposits of limestones, shale, and other conglomerate minerals, which account for the varying colors of red, gray, and brown. Shifting sands over millions of years brought about a considerable level of erosion, which created uniquely rounded and textured stone formations. The sandstone is actually a remnant of the sands that lined the seafloor. During the Jurassic period, the inland sea began to dry out, and the land began to rise. The unique red sandstone rock formations in Valley of Fire State Park, Nevada. The Lake Mead Fault System also resulted in changes to the surface layer of rock as the ground shifted, with some areas pushed up from the rest into ridges and rock formations. The Shear Zone is segmented, which resulted in a great deal of upheaval across its surface over time. Two faults run within the park, the Las Vegas Valley Shear Zone and the Lake Mead Fault System. Valley of Fire borders the Lake Mead National Recreation Area to the east, just at the confluence of the Virgin River, and is located in a region known as the southeastern Basin and Range. The park lies at an elevation between 402–917 m. Landscape Of The Valley Of Fire State Park Amazing colors and shape of the Fire Wave Rock in Valley of Fire State Park, Nevada. A 16.9 km section of Valley of Fire Road, which runs through the Park from the east to west entrances, was officially designated as a Nevada Scenic Byway in 1995. Nevada’s oldest state park, the Valley of Fire State Park, was designated a National Natural Landmark in 1968. The Park grew over the decades to its present-day size. The Park opened in 1934 and was given its official designation in 1935. In 1931, about 8,760 acres of federal land were transferred to the state of Nevada to create the Park. The Park is situated about 26 km south of Overton and 80km northeast of Las Vegas in Clark County of the US State of Nevada. In the setting sunlight, these irregular sandstone formations often appear to glow, a phenomenon that gave the Park its name. Valley of Fire State Park covers just under 46,000 acres, with a distinctive terrain of red or Aztec sandstone.
0 Comments
Leave a Reply. |
AuthorWrite something about yourself. No need to be fancy, just an overview. ArchivesCategories |