- published: 30 May 2013
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Basalt (pronounced /bəˈsɔːlt/, /ˈbæsɒlt/, /ˈbæsɔːlt/, or /ˈbeɪsɔːlt/) is a common extrusive igneous (volcanic) rock formed from the rapid cooling of basaltic lava exposed at or very near the surface of a planet or moon. Flood basalt describes the formation in a series of lava basalt flows.
By definition, basalt is an aphanitic (fine-grained) igneous rock with generally 45-55% silica (SiO2) and less than 10% feldspathoid by volume, and where at least 65% of the rock is feldspar in the form of plagioclase. It is the most common volcanic rock type on Earth, being a key component of oceanic crust as well as the principal volcanic rock in many mid-oceanic islands, including Iceland, Réunion and the islands of Hawaii. Basalt commonly features a very fine-grained or glassy matrix interspersed with visible mineral grains. The average density is 3.0 gm/cm3.
Basalt is defined by its mineral content and texture, and physical descriptions without mineralogical context may be unreliable in some circumstances. Basalt is usually grey to black in colour, but rapidly weathers to brown or rust-red due to oxidation of its mafic (iron-rich) minerals into hematite and other iron oxides and hydroxides. Although usually characterized as "dark", basaltic rocks exhibit a wide range of shading due to regional geochemical processes. Due to weathering or high concentrations of plagioclase, some basalts can be quite light-coloured, superficially resembling andesite to untrained eyes. Basalt has a fine-grained mineral texture due to the molten rock cooling too quickly for large mineral crystals to grow; it is often porphyritic, containing larger crystals (phenocrysts) formed prior to the extrusion that brought the magma to the surface, embedded in a finer-grained matrix. These phenocrysts usually are of olivine or a calcium-rich plagioclase, which have the highest melting temperatures of the typical minerals that can crystallize from the melt.
The Columbia River is the largest river in the Pacific Northwest region of North America. The river rises in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the US state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is 1,243 miles (2,000 km) long, and its largest tributary is the Snake River. Its drainage basin is roughly the size of France and extends into seven U.S. states and a Canadian province.
By volume, the Columbia is the fourth-largest river in the United States; it has the greatest flow of any North American river draining into the Pacific. The river's heavy flow and its relatively steep gradient gives it tremendous potential for the generation of electricity. The 14 hydroelectric dams on the Columbia's main stem and many more on its tributaries produce more hydroelectric power than those of any other North American river.
Thomas Foster is a fictional comic book superhero published by Marvel Comics, and is the fifth person to hold the mantle of Goliath. He was created by Reginald Hudlin, Greg Pak and Koi Turnbull, he first appeared in Black Panther vol. 3 #23 (December 2006).
Tom Foster made his first appearance in Black Panther #23. He subsequently succeeded in gaining superpowers and becoming Goliath in World War Hulk: Aftersmash #1, before appearing to join Damage Control in the same issue.
On the creation of Foster, Pak stated:
Tom Foster was introduced in Black Panther #23, when he and his family were visited by King T'Challa and Queen Ororo of Wakanda, following the murder of his uncle Bill Foster during the superhero civil war. Angry at the pro-registration forces for his uncle's death, Tom swore to continue his legacy by replicating the Pym Particles which give Bill his powers. To this end, T'Challa swore to assist him in any way he could, once Tom finished his studies at M.I.T.
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Formation of Columnar Basalt is quickly described in this 2 Minute Geology episode. Columnar Basalt is the result of cooling and cracking of an unusually thick basaltic lava flow. Columns are often 50 feet high or more! The Columbia River Basalt Group of Washington and Oregon (USA) is a stack of more than 300 individual lava flows. The flows issued forth from deep fissures that began forming 17 million years ago in southeast Washington and northeast Oregon. Columns are well-developed in some of the flows and non-existant in many others. The Roza Flow is the most famous Columbia River Basalt flow for column formation. Notable columns around the world include Devil's Tower in Wyoming and Giant's Causeway in Ireland. This episode begins with Nick at the foot of some Columnar Basalt in ...
Basaltic magma
Geologist explains basaltic pillow lava formation (pillow basalt). Expand description for more details about pillow lavas or visit http://HUGEfloods.com Use High-Definition (HD) option to improve video quality. Pillow lavas form when basaltic lava encounters water. Active pillows have been video recorded in Hawaii as the ongoing Kilauea eruption sends active basalt lava flows into the Pacific Ocean. In continental settings, pillows are formed when flood basalts bury landscapes dominated by large freshwater lakes and streams. The Columbia River Basalt Group of Washington and Oregon (USA) is a stack of more than 300 individual lava flows. The flows issued forth from deep fissures that began forming 17 million years ago in southeast Washington and northeast Oregon. Some of the flows ha...
bm lumajang original 087776326324
The properties of basalt, which is found under the oceanic crust, include mostly dark material, such as hornblende, as well as dark silicate minerals. Find out how to identify basalt stone with information from a geology professor in this free video on rocks. Expert: Jeffrey K. Wagner Bio: Jeffrey K. Wagner is an associate professor of astronomy and geology. He has been a faculty member of Bowling Green State University Firelands since 1981. Filmmaker: Bradley Walton
Best viewed at larger size. Discrete element simulation of mixing in a basaltic mush during magma reintrusion. The particles are olivine crystals with the correct contact dynamics for viscous fluids. Faults, shear bands and schlieren, form. Support from NSF and NETL is gratefully acknowledged.