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Keri­


Keri­
Photo Information
Copyright: Kristmundur Roman (zakharii) (66)
Genre: Landscapes
Medium: Color
Date Taken: 2009-04-17
Categories: Mountain, River
Camera: Canon PowerShot A60
Exposure: f/2.8, 1/160 seconds
More Photo Info: [view]
Photo Version: Original Version
Date Submitted: 2009-06-01 0:52
Viewed: 4191
Points: 0
[Note Guidelines] Photographer's Note
Keri­ (occasionally Anglicized as Kerith or Kerid) is a volcanic crater lake located in the GrÝmsnes area in south Iceland, on the popular tourist route known as the Golden Circle. It is one of several crater lakes in the area, known as Iceland's Western Volcanic Zone, which includes the Reykjanes paninsular and the Langj÷kull Glacier, created as the land moved over a localized hotspot, but it is the one that has the most visually recognizable caldera still intact. The caldera, like the other volcanic rock in the area, is composed of a red (rather than black) volcanic rock. The caldera itself is approximately 55 m (180 ft) deep, 170 m (560 ft) wide, and 270 m (890 ft) across. Keri­ĺs caldera is one of the three most recognizable volcanic craters because at approximately 3,000 years old, it is only half the age of most of the surrounding volcanic features. The other two are Sey­ishˇlar and Kerhˇll.

While most of the crater is steep-walled with little vegetation, one wall is sloped more gently and blanketed with a deep moss, and can be descended fairly easily. The lake itself is fairly shallow (7-14 metres, depending on rainfall and other factors), but due to minerals from the soil, is an opaque and strikingly vivid aquamarine.

Although vulcanologists originally believed Keri­ was formed by a huge volcanic explosion, as is the accepted norm with volcanic craters, more thorough studies of the GrÝmsnes region failed to find any evidence of such an explosion in Keri­. It is now believed that Keri­ was a cone volcano which erupted and emptied its magma reserve. Once the magma was depleted, the weight of the cone collapsed into the empty magma chamber. The current pool of water at the bottom of the crater is at the same level as the water table and is not caused by rainfall.


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