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A stone stripe, also called a lava stringer, [1] is an elongated concentration of mostly talus-like basalt rock found along a hillside or the base of a cliff. Many stone stripes occur without cliffs. A stone stripe is identified by its lack of vegetative cover. They typically occur in north central Oregon and develop at 900 to 1,100 meter ...
Near the Tri-Cities, rockhounding is popular along the Columbia River, Horse Heaven Hills, Saddle Mountains, Bickleton and the Ginkgo Petrified Forest State Park. Rockhounding on WA DNR-managed land
Gilboa tree fossil ()Gilboa Fossil Forest, New York, United States, is a petrified forest and one of the oldest known forests. [1] [2] Located near the Gilboa Dam in Schoharie County, New York, the region is home to tree trunks from the Devonian period.
One forest of in situ, 24,000-year-old unfossilized upright trees was exposed by excavations for a quarry near Charleston, Illinois. [32] Excavations for a tailings pond about Marquette, Michigan , exposed an in situ forest of unfossilized trees, which are about 10,000 years old, buried in glacial lake and stream sediments.
Species of ebony include Diospyros ebenum (Ceylon ebony), native to southern India and Sri Lanka; D. crassiflora (Gabon ebony), native to western Africa; D. humilis (Queensland ebony), native to Queensland, the Northern Territory, New Guinea and Timor; and D. celebica (Sulawesi ebony), native to Indonesia and prized for its luxuriant, multi-colored wood grain.
Slate – Metamorphic rock - A low grade metamorphic rock formed from shale or silt; Suevite – Rock consisting partly of melted material formed during an impact event – A rock formed by partial melting during a meteorite impact; Talc carbonate – A metamorphosed ultramafic rock with talc as an essential constituent; similar to a serpentinite
Spider Rock Pinnacle Balanced Rock The West and East Mitten Buttes Window Rock. Antelope Canyon; Canyon de Chelly National Monument. Spider Rock; Capitol Butte; Cathedral Rock, Red Rock State Park, Sedona
These deeply-formed rocks were uplifted, eroded, and exposed for eons. By 600 million years ago, North America had been beveled off to a remarkably smooth surface. It is on this crystalline rock surface that the younger, more familiar layered rocks of the Colorado Plateau were deposited. [11]
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