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Litaneutria obscura, commonly known as the obscure ground mantis, is a species of praying mantis in North America. It is native to Arizona, southern California, ...
Ground mantis is a common name given to various species of praying mantis believed to hunt on or near ground level rather than high amid foliage. Examples native to North America include: Litaneutria minor — minor ground mantis [1] Litaneutria skinneri — Skinner's ground mantis [2] Yersiniops solitaria — horned ground mantis [3]
July 2024 was the hottest month ever recorded in Death Valley, with a mean daily average temperature over the month of 108.5 °F (42.5 °C). [34] Four major mountain ranges lie between Death Valley and the ocean, each one adding to an increasingly drier rain shadow effect, and in 1929, 1953, and 1989, no rain was recorded for the whole year. [20]
When directly threatened, many mantis species stand tall and spread their forelegs, with their wings fanning out wide. The fanning of the wings makes the mantis seem larger and more threatening, with some species enhancing this effect with bright colors and patterns on their hindwings and inner surfaces of their front legs.
Little is known about the history of the oldest exposed rocks in the area due to extensive metamorphism.This somber, gray, almost featureless crystalline complex is composed of originally sedimentary and igneous rocks with large quantities of quartz and feldspar mixed in. [1] The original rocks were transformed to contorted schist and gneiss, making their original parentage almost unrecognizable.
Zabriskie Point is a part of the Amargosa Range located east of Death Valley in Death Valley National Park in California, United States, noted for its erosional landscape. It is composed of sediments from Furnace Creek Lake, which dried up 5 million years ago—long before Death Valley came into existence.
Manly Beacon and Red Cathedral viewed from Zabriskie Point. The Amargosa Chaos is a series of geological formations located in the Black Mountains in southern Death Valley.In the 1930s, geologist Levi F. Noble studied the faulting and folding in the area, dubbing it the "Amargosa chaos" due to the extreme warping of the rock.
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