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7 Cards in this Set

  • Front
  • Back
'Ropey lava'
Free flowing basaltic lava. when surface cools it forms a skin which wrinkles as lava continues to flow beneath
'Blocky Lava'
Free flowing basaltic lava forms a skin. volcanic gas breaks through the skin separating it.
'Flow-banded lava'
Viscous rhyolite. as partly solidified lava moves, crystals line up in direction of flow.
Pillow lava
When lava flows into water a thick skin is quickly formed.
Vesicular lava
When volcanic gases are trapped during cooling, leaving small round cavaties in the rock
Amygdaloidal lava
after vesicular lava has cooled, water may seep into the cavaties in the rock. water may evaporate leaving precipitate of minerals behind.
Columnar jointing
Cooling and contraction of thick flows. the contraction cause cracks to develop.