

Because they are within the 29 Palms Marine Base. Halfway up, there’s a dark hill called Sunshine Crater Cinder Cone distinctly older than Pisgah Crater, which is off-limits. It is believed that most of the present cinder cone consists of pyroclastic material that originated from this final eruption.

The second phase produced similarly extensive flows, while the third eruption produced substantial amounts of tephra. It is believed the cinder cone was formed during this time. Therefore, the first eruption was a basaltic flow that created extensive lava fields and evidence of intrusive structures. It looks like a lady lying on her back with her long dark hair trailing off to the east. The Pisgah Lave Field is located in a valley, with the Cady Mountains (Sleeping Beauty Mountains) to the north. The lava found around the volcano consists of a’a and pahoehoe, with considerable concentrations of olivine, plagioclase, and rich amounts of gypsum that can be found coating rocks near the cinder cone. Moreover, the volcano erupted at least three times, producing porphyritic basalt, and rocks from the first eruptive phase are almost aphanitic. Geological survey activity also occurs at the mountain every so often.
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This volcano is a very popular geology research site, not uncommon to find university classes and professional seminar groups around the mountain. A similar nearby Amboy Crater is interbedded with Bristol Playa sediments that are somewhere 100,000 years old. The volcano is basaltic, a reliable commonly used potassium-argon for dating purposes would be difficult anyway. Though, many others believe the last eruption could occur around 30,000 to 50,000 years ago.

But many geologists, believe, that Pisgah Volcano is the youngest vent of four cinder cones, and may have been active more than 2,000 years ago. However, no authentic data was available on when Pisgah Crater last erupted. Furthermore, the mountain contains a large number of lava tubes, which are frequented by cavers, these lava tubes in the area are a bit popular and with no trouble accessible destination for caving. The base diameter of the Pisgah Crater is 488 meters and stands 98 meters above the surrounding high desert terrain. Due to natural erosion and mining operations, the crater has lost its original cinder cone shape.

Moreover, the mountain top has been removed and scoured into an irregular shape. The site of the Mount Pisgah Volcanic Cinders Mine, which produced pumice for commercial use and various cinder products, and sand was used to depict the black sands of Iwo Jima in the film Letters from Iwo Jima. A Canadian-based company “Can-Cal Resources Limited” presently owned the mountain and specializes in the exploration of precious minerals in California. Although, mining activities have reduced the peak lit bit, but had a severe environmental impact. The volcanic peak is about 2.5 miles, and had a historic elevation of 2,638 feet. Pisgah Crater is in the Craters category for San Bernardino County in the state of California. Pisgah Crater or Pisgah Volcano is a volcanic cinder cone in the Mojave Desert between Barstow and Needles, California United States.
