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Seattle, Washington: August 22, 1994: EXTINCT [5] in 2011 58: Orcas off the San Juan Islands: Seattle, Washington: August 22, 1994: EXTINCT [5] in 2011 59: Gray Whales off Oregon Coast: Newport, Oregon: August 29, 1994 60: Spyhopping Gray Whale: San Francisco, California: September 5, 1994: Across from Pier 39 61: Grays off the San Francisco ...
Location of Seattle in King County and Washington. This is a list of the National Register of Historic Places listings in Seattle, Washington. This is intended to be a complete list of the properties and districts on the National Register of Historic Places in the city of Seattle, Washington, United States. Latitude and longitude coordinates ...
The Arctic Club Building is a ten-story hotel in Seattle, Washington located at the Northeast corner of Third Avenue and Cherry Street. Built in 1914 for the Arctic Club, a social group established by wealthy individuals who experienced Alaska's gold rush (Klondike Gold Rush), [3] it was occupied by them from construction until the club's dissolution in 1971.
Baraboo Quartzite is a Precambrian geological formation [1] of quartzite, found in the region of Baraboo, Wisconsin. While pure quartzite is usually white or gray, Baraboo Quartzite is typically dark purple to maroon in color, due to the presence of iron ( hematite ) and other impurities. [ 2 ]
Cliff-forming quartzite, the principle part of the Eureka, is composed of more than 99 percent quartz, which includes both the sand grains and the cement that binds them. [6] The quartz cement accounts for its outstanding hardness and resistance to erosion. Minor constituents are grains of zircon and tourmaline and a trace of feldspar. [6]
The Mesoproterozoic Dripping Spring Quartzite is a resistant, purple quartzite formation found in central and southeast Arizona, USA. It is a cliff-forming purplish unit found in the lower sections of the Apache Group , units of originally sedimentary layers, but later metamorphosed.
The Monkton Quartzite preserves many primary sedimentary features, including wave-action ripples, rain-drop imprints, trilobite tracks, and burrows. [2] The unit contains shallowing upward cycles of subtidal sand shoals overlain by intertidal beds of sand and silt.
Quartz diorite is an igneous, plutonic rock, of felsic composition, with phaneritic texture. Feldspar is present as plagioclase (typically oligoclase or andesine ) with 10% or less potassium feldspar.
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