Ludlow/Amboy is situated in the eastern Mojave Desert of southern California. The area is characterized most recently by expansive flows of late Cenozoic basanites (feldspathoid-bearing basalt) and several pyroclastic cones. Dish Hill, one of the pyroclastic cones, is known locally as a source for Olivine (var. Forsterite), Iddingsite and Kaersutite.
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Map Reference: 34°43'N , 116°10'W
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