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Volcanic Landforms
Volcanic landforms
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Geography
Secondary Education
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Volcanic landforms
Slide 1 - Tekstslide
Volcanic landforms
Intrusive: Lava solidifies within the Earth's crust.
Extrusive: Lava solidifies outside the crust.
Slide 2 - Tekstslide
https:
Slide 3 - Link
Slide 4 - Tekstslide
Batholith
They form the base of the mountain.
Large and coarse grained.
A part of the magma chamber also forms batholith.
Huge in size.
Slide 5 - Tekstslide
How did the Batholith come to the Earth's surface?
Slide 6 - Open vraag
https:
Slide 7 - Link
Laccoliths
Lava Sill, that solidifies slowly and gives a dome shape.
Slide 8 - Tekstslide
https:
Slide 9 - Link
Observe this picture
Slide 10 - Tekstslide
How can we connect this with Lopoliths?
Slide 11 - Woordweb
Lopoliths
Lava solidifies in a shallow saucer shaped basin.
Slide 12 - Tekstslide
Slide 13 - Tekstslide
Phacoliths
Lava solidifies on an anticline or base of a syncline.
Slide 14 - Tekstslide
https:
Slide 15 - Link
2
Slide 16 - Video
00:21
Dykes
Magma solidifies in vertical columns to form Dykes
Slide 17 - Tekstslide
00:34
Slide 18 - Tekstslide
Batholith
Laccolith
Sill
Dyke
Lopolith
Slide 19 - Sleepvraag
Extrusive Forms
Slide 20 - Tekstslide
Types
Ash and cinder cones
Lava domes
Lava Shields
Composite cones
Slide 21 - Tekstslide
Slide 22 - Video
Paricutín cinder cone volcano.
Slide 23 - Tekstslide
Lava Domes
Formed when acidic lava solidifies quickly forming steep sided cones.
Slide 24 - Tekstslide
Lava Shield
Formed when basic lava solidifies.
Broader than domes.
Slide 25 - Tekstslide
Composite volcano
Slide 26 - Tekstslide
Stratovolcano
Alternating layer of Lava and pyroclastic material.
More than one vent
Ejects out lava and rock material.
Eg: Vesuvius, Fuji
Slide 27 - Tekstslide
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