Intrusive and Extrusive Activity

Description

A-Levels Plate Tectonics Mind Map on Intrusive and Extrusive Activity, created by hannah_louisa on 16/05/2013.
hannah_louisa
Mind Map by hannah_louisa, updated more than 1 year ago
hannah_louisa
Created by hannah_louisa almost 11 years ago
133
0

Resource summary

Intrusive and Extrusive Activity
  1. Intrusive
    1. Batholith
      1. large chambers of magma cool underground and form domes of igneous rock
      2. Dykes and sills
        1. magma flows into gaps in the surrounding rock, cools and forms vertical dykes and horizontal sills
        2. Cooling Cracks
          1. cracks may form as the magma cools
        3. Extrusive
          1. Lava Eruptions
            1. Basaltic lava - Constructive
              1. temperature of eruption over 950
                1. flows easily and gas can escape easily. eruptions aren't violent, usually frequently and long periods
                2. Andesitic and Rhyolitic - Destructive
                  1. 750-950 degrees eruption. rhyolitic is less than 750
                    1. flow less easily and often have blockages. gases can't escape so pressure build and the blockage is cleared by a violent eruption. short lived and intermittent
                  2. Volcanos
                    1. Dome- Destructive. lava is rhyolitic or andesitic. thick lava causes steep sides as it flows shorter distances
                      1. Caldera- Destructive. andesitic and rhyolitic. central part collapses as the magma chamber below empties
                        1. Shiled- Constructive. Basaltic lava. long linear vent can be several km long
                        2. Hot Springs
                          1. places where groundwater emerges at the surface. if the source is close to an area of recent intrusive activity the water is heated and becomes a hot spring
                            1. temperature varies from 20-90 degrees. tourist attractions
                            2. Geysurs
                              1. type of hot spring here hot water and steam are ejected from the surface in a fountain.
                                1. groundwater is heated above boiling point by magma in the crust
                                  1. hot water becomes pressurised and forces its way to the surface
                                  2. Boiling mud pool
                                    1. another hot spring, form in areas with fine grained soil, water mixes with the soil to make a hot muddy pool
                                  Show full summary Hide full summary

                                  Similar

                                  Plate Tectonics
                                  eimearkelly3
                                  GCSE Chemistry: The Crust
                                  Landon Valencia
                                  Plate Tectonics
                                  sarah.lalaz
                                  Plate Tectonics
                                  eimearkelly3
                                  Plate Margins
                                  RachelBean
                                  Physical Geography
                                  hayleyelizabeth9
                                  C1.7 revision
                                  Josh Steer
                                  Plate Tectonics For CE
                                  Oliver Hall
                                  Plate Tectonics
                                  Adam......
                                  Plate Tectonics
                                  eimearkelly3
                                  Unit 2 Geological Oceanography
                                  Jennifer Tuxford