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Flood basalt

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Multiple flood basalt flows of the Columbia River Basalt Group. The photograph shows the step-like character of these formations, called traps. The upper basalt is the Roza Member, while the lower canyon exposes Frenchmen Springs Member basalt
A cliff at the Paraná Magmatic Province, Brazil. Part of a huge lava flow 128 to 138 million years ago. Parts of this event can be seen in the Etendeka traps in Namibia and Angola. These areas were touching in Pangaea

A flood basalt or trap basalt is the result of a giant volcanic eruption or series of eruptions that coats large stretches of land or the ocean floor with basalt lava.

Flood basalts have covered areas as large as a continent in prehistory, creating great plateaus and mountain ranges. Flood basalts have erupted at various times throughout Earth history. They are clear evidence that the Earth has periods of higher activity rather than being in a uniform steady state.[1]

One explanation for flood basalts is that they are caused by the combination of continental rifting and its associated melting. Then a mantle plume produces vast quantities of a basaltic magma. These have a low viscosity, which is why they 'flood' rather than form taller volcanoes.

Flood basalts start at between 100 and 400 km depth, in the asthenosphere. To get a partial melting as large as that of the traps, expelling huge quantities of lava, it is necessary to have a large heat input. Such melting can take place near a hotspot, resulting in a mixture of magma from the depths of the hotspot with superficial magma produced by a mantle plume.

Lava plateaux[change | change source]

A lava plateau is a flat, wide surface (plateau) that is formed when lava comes out of the ground and spreads out very quickly. The layers of lava can build up over time to form a lava plateau. Here are the general properties of lava plateaux:

  • They are very large areas of basaltic lava with a layered structure.
  • Lava makes the plateau bigger, and higher, with each eruption.
  • They tend to be flat.
  • Mid-ocean ridge eruptions make large plains on the sea floor.
  • The lava of these plateaux are thin and runny.
  • These plateaux may take millions of years to form.
  • Overtime a number of fissure eruptions in the same area can build up a high plateau.

Examples[change | change source]

The Emeishan Traps in southwestern China, around Sichuan province, the Deccan Traps of central India, the Siberian Traps, and the Columbia River Plateau of western North America are four large regions covered by prehistoric flood basalts. The two largest flood basalt events in historic time have been at Eldgjá and Lakagigar, both in Iceland. The largest and best-preserved continental flood basalt terrain on Earth is part of the Mackenzie Large Igneous Province in Canada.[2] The maria on the Moon are additional, even more extensive, flood basalts. Flood basalts on the ocean floor produce oceanic plateaus.

The surface covered by one eruption can vary from around 200,000 km² (Karoo) to 1,500,000 km² (Siberian Traps). The thickness can vary from 2000 metres (Deccan Traps) to 12,000 m (Lake Superior). These are smaller than the original volumes due to erosion.

Another example of a lava plateau is the Giant's Causeway, in County Antrim, Northern Ireland. This is was originally part of a great volcanic plateau called the Thulean Plateau.

References[change | change source]

  1. Mahoney J.J. & Coffin M.F. Large igneous provinces: continental, oceanic, and planetary flood volcanism. Geophysical Monograph 100. Washington, DC: American Geophysical Union. [1]
  2. "Muskox Property - The Muskox Intrusion". Archived from the original on 2009-04-08. Retrieved 2010-10-17.