Violent eruptions create welded tuff
Welded tuff forms during violent volcanic eruptions when an eruption column collapses forming a pyroclastic flow. Pyroclastic flows are sometimes described as a stone wind that can travel great distances from a volcano's vent.
Three samples of welded tuff
Ignimbrite forms during violent volcanic eruptions when an eruption column collapses forming a pyroclastic flow. The pyroclastic flow carries hot gases and other pyroclastic material down the slopes of a volcano at hurricane speeds. The super hot gases and debris in the pyroclastic flow cools in three layers called ignimbrite.
The top and bottom layers form a soft rock called tuff. Tuff forms a top and bottom layer of soft rock because the air and ground beneath the pyroclastic material is much cooler than the inside of the flow deposit.
Center layer of ignimbrite
The center layer remains hot enough to "weld" the ash, pumice and other debris into a hard rock. Glassy rock fragments that make up much of the material deposited by pyroclastic flow deforms readily from the heat.
Pieces of pumice is flattened and deformed during the welding process forming flattened shapes. You can see pieces of pumice in the rocks because it is a slightly different color and usually has a curved or oval shape.
Layers of tuff at Yellowstone
Most tuff forms during eruptions of rhyolite lava. Rhyolite lava is associated with super volcanoes and their eruptions. Welded tuff can be seen at Yellowstone Park on the hillsides where the Lava Creek Tuff is exposed.
Lava Creek Tuff
The Lava Creek Tuff is 1000 times larger than the deposits formed during the eruption of Mount Saint Helens on May 18, 1980. Large deposits of these rocks formed during the Alaskan eruption of Novarupta Volcano in 1912. The rocks can be found in the Valley of Ten Thousand Smokes where Knife Creek cuts through the pyroclastic flow deposits.
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