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Iceland: Mid-Atlantic Ridge |
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The purple zones are the Rift regions... Iceland lies along the crack
in the middle of the Atlantic, and is part of the Atlantic Rift
Ridge... the European and North American Plates are slowly pulling
apart, at a rate of 2-6 inches per year.
Volcanoes in the region are different than in other areas... they
normally erupt out of a crack in the earth that rips open during a
volcano, and stream hot, runny, lava all along the crack.
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This is one of the rift lines in the separation zone. This crack
widens a couple of inches every year.... In some places, during an
earthquake, it has moved as much as 9 meters in one day!
The majority of the movement happens in 10 year intervals, on
average, with the last interval in 2000.
Below, a bridge crosses from the European plate to the North American
Plate, at the mid point of the rift Zone.
The region around the bridge was covered in lava during an eruption
from a rift rip in the mid 1700's... the crack the bridge crosses
formed in the time since then.
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This valley is part of the "Rift Zone", and the river you see is at
the tail end of a large lake that covers canyons hundreds of feet
deep.
An interesting thing is that the bridge in this picture extends to an
island, called Þingvellir (the Þ is sort of a th sound), where the first
council of Iceland, the Althing met. Its considered to be the
first democratic assembly in history.
For really important stuff, the current parliament still meets there,
out of tradition.
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Several large cracks can be seen snaking across the valley, itself a
large crack in the Earth's Crust. Many hundreds of earthquakes
happen in the rift zone each year.
This is a close-up of the crack shown above... the roadway crosses
the crack. They have a grate covering the expansion zone that has
to be replaced every few years with a larger one.
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The roadway snakes across a valley floor covered with lava deposits,
a sign of recent activity. Pockets of team rise out the ground in
areas, signs that hot magma isn't far below the surface... the crust
is quite thin in this region.
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The lake in the rift valley, Thingvallavatn, is the
largest natural lake in Iceland. The river coming out of the lake
is more than 5 times the volume of the small rivers flowing into it...
most of the water flows into the lake under the lava beds, well below
ground.
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The edges of the valley are lined with walls that have huge rifts
along them... its a very unique sight... imagine the power it would take
to pull the ground apart like this... its incredible!
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< Back to Iceland |
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