maar

The three maars near Daun- 50°10′30″N 6°50′41″E / 50.175057°N 6.844783°E / 50.175057; 6.844783

A maar is a broad, low-relief volcanic crater that is caused by a phreatomagmatic eruption, an explosion caused by groundwater coming into contact with hot lava or magma. A maar characteristically fills with water to form a relatively shallow crater lake. The name comes from the local Palatinate German dialect of Daun, where it is in turn derived from Latin mare (sea). Maars are shallow, flat-floored craters that scientists interpret as having formed above diatremes as a result of a violent expansion of magmatic gas or steam; deep erosion of a maar presumably would expose a diatreme. Maars range in size from 60 to 8,000 m (200 to 26,200 ft) across and from 10 to 200 m (33 to 660 ft) deep, and most are commonly filled with water to form natural lakes. Most maars have low rims composed of a mixture of loose fragments of volcanic rocks and rocks torn from the walls of the diatreme.

Examples

Hole-in-the-Ground, in Oregon, a maar crater

The largest known maars are found on the Seward Peninsula in northwest Alaska. These maars range in size from 4,000 m (13,100 ft) to 8,000 m (26,200 ft) in diameter and a depth up to 300 m (980 ft). Their large size is due to the explosive reaction that occurs when magma come in contact with permafrost. Examples of the Seward Peninsula maars include North Killeak Maar, South Killeak Maar, Devil Mountain Maar and Whitefish Maar.^[1]

Maars occur in western North America, Patagonia in South America, the Eifel region of Germany (where they were originally described), and in other geologically young volcanic regions of Earth. Elsewhere in Europe La Vestide du Pal provides a spectacular example of a maar easily visible from the ground or air. Kilbourne Hole and Hunt's Hole, near El Paso, Texas, are maars. The notorious, carbon dioxide-saturated Lake Nyos in Africa is another example. An excellent example of a maar is Zuni Salt Lake in New Mexico, a shallow saline lake that occupies a flat-floored crater about 6,500 ft (2,000 m) across and 400 ft (120 m) deep. Its low rim is composed of loose pieces of basaltic lava and wall rocks (sandstone, shale, limestone) of the underlying diatreme, as well as random chunks of ancient crystalline rocks blasted upward from great depths. Maars in Canada are found in the Wells Gray-Clearwater volcanic field of east-central British Columbia and in kimberlite fields throughout Canada. A notable field of maars is found in the Pali Aike Volcanic Field in Patagonia, South America.^[2]

One of the most notable craters misidentified as a maar is Arizona's Meteor Crater; for many years this was thought to be of volcanic rather than meteoric origin.^[3]

Gallery

Ukinrek Maars, Alaska; the result of a 10-day volcanic eruption in 1977. The maar is about 300 m (980 ft) in diameter

Weinfelder Maar, one of the three maars originally described

The maar at Birkat Ram, the Golan Heights

Notes

References

• USGS Photo glossary of volcano terms: Maar
• USGS: Maars and Tuff Cones

External links

• List of Maar Volcanoes