Volcanic field

Source: Wikipedia, the free encyclopedia.

The north face of Mount Garibaldi rises above The Table and Garibaldi Lake in the Garibaldi Lake volcanic field

A volcanic field or crater row is an area of Earth's crust that is prone to localized volcanic activity. The type and number of volcanoes required to be called a "field" is not well-defined.[1] Volcanic fields usually consist of clusters of up to 100 volcanoes such as cinder cones. Lava flows may also occur. They may occur as a monogenetic volcanic field or a polygenetic volcanic field.

Description

Alexander von Humboldt observed in 1823 that geologically young volcanoes are not distributed uniformly across the Earth's surface, but tend to be clustered into specific regions. Young volcanoes are rarely found within cratons, but are characteristic of subduction zones, rift zones, or in ocean basins. Intraplate volcanoes are clustered along hotspot traces.[2]

Within regions of volcanic activity, volcanic fields are clusters of volcanoes that share a common magma source.

Scoria cones are particularly prone to cluster into volcanic fields, which are typically 30–80 kilometers (19–50 mi) in diameter and consist of several tens to several hundred individual cones. The unusually large Trans-Mexican Volcanic Belt has nearly 1000 cones covering an area of 60,000 square kilometers (23,000 sq mi).[5]

Examples

Karapınar Field in Turkey
SP Crater in the San Francisco volcanic field is a cinder cone with a basalt lava flow that extends for 4 miles (6 km).
El Muweilih Crater in Sudan with natron-rich clay on the crater floor

Canada

Mexico

United States

Iceland

Africa

Others

See also

References