The Ramon Crater is hosued in Israel’s largest National Park. Here, you can enjoy local geology, flora, and fauna, in addition to learning about the erosion rainwater has caused on this desert. The 1500-foot “Crater” itself was actually caused by erosion, and not by falling meteorites, as its name would suggest. Its formation began hundreds of millions years ago, when the ocean that covered the Negev Desert began to recede. About 5 million years ago, the rivers changed their course, carving out the crater in their movement. As the crater deepened, lower (and older) strata of rocks were exposed. The colors and shape of some are simply splendid; at the bottom, the rocks are up to 200 million years old.
The Ramon Crater is a stunning nature reserve with hiking for both experienced desert survival enthusiasts and the casual visitor. Before any level hike, however, every visitor should stop to see the magnificent view from the Mitzpe Ramon Visitors’ Center, which is situated on the edge of crater. Large models explain about the site’s geography and geology; an audio-visual production describes the Negev’s formation, its craters, flora and fauna and even illustrates the history of settlement there. For another great view, visitors should stop at the “Bird Balcony” that hangs out from the middle of the promenade. Once the promenade trail ends, a path continues down along the crater’s edge leading to a camel shaped rock with a small observation platform. Here, the Bio Ramon complex will present a rich collection of desert plans and animals in both indoor and outdoor environments.
The most spectacular section of the crater is Wadi Nikarot (Hebrew for “Grotoo Riverbed”), which originates in the northern Sinai Desert. Erosion has gouged out softer portions of the rock and left rows of fascinating overhangs and crevices.