froggy
Full Member
Devonian Corals.
Gold occurs in the large quartz lode of the Southern Belle Canyon not far from Coral Ridge, where there are reefs of petrified marine shells and corals in Devonian limestone.
DEVONIAN ROCKS Between the Southern Belle Canyon and Pepper Sauce Wash a long ridge extending eastward, called Coral Ridge, is made up of quartzite, limestone and shaly limestones, in which there is a bed of corals and shells of the Devonian age. The fossils are of especial interest because of their wonderful preservation in every detail of structure. This is due to the permeation of the rock by silicious waters, which have changed the organized structure from carbonate of lime to silica, and have left the surrounding limestone unchanged. The weathering of the rock has left these fossils standing out in bold relief. A fine section of the stratified rock formation is found in Southern Belle Canyon. The strata are uplifted and extend southward at an angle of fifteen degrees. The section consists of regular strata of red sandstone, shale, quartzite, sandstones and limestones, resting upon diorite. At the eastern end of the section, strata of sandstone and limestone abut upon granite.
Ideas of where to look?
Gold occurs in the large quartz lode of the Southern Belle Canyon not far from Coral Ridge, where there are reefs of petrified marine shells and corals in Devonian limestone.
DEVONIAN ROCKS Between the Southern Belle Canyon and Pepper Sauce Wash a long ridge extending eastward, called Coral Ridge, is made up of quartzite, limestone and shaly limestones, in which there is a bed of corals and shells of the Devonian age. The fossils are of especial interest because of their wonderful preservation in every detail of structure. This is due to the permeation of the rock by silicious waters, which have changed the organized structure from carbonate of lime to silica, and have left the surrounding limestone unchanged. The weathering of the rock has left these fossils standing out in bold relief. A fine section of the stratified rock formation is found in Southern Belle Canyon. The strata are uplifted and extend southward at an angle of fifteen degrees. The section consists of regular strata of red sandstone, shale, quartzite, sandstones and limestones, resting upon diorite. At the eastern end of the section, strata of sandstone and limestone abut upon granite.
Ideas of where to look?