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An introduction to volcanic landforms, discussing both extrusive and intrusive types. Extrusive landforms include cone-shaped and dome-shaped volcanoes, vent eruptions, and fissure eruptions. Intrusive landforms, on the other hand, are formed in the earth's crust and include batholiths. The document also covers specific examples of each type, such as Mount Vesuvius, Antrim Plateau, and the Leinster Batholith.
Typology: Study notes
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○ classic volcanoes
○ mid-atlantic ridge
○ weak point in earth's crust ○ Hawaiian islands
○ slow cooling magma in the earth's crust
○ Wicklow & Dublin Mts ○ Granite batholith exposed by weathering
● Eruptions through a vent ● Occur at destructive boundaries (subduction zones) ● Volcano made of lava and ash ● Crater on top - filled with water or cooled rock (^) Crater on Mount Vesuvius
Cone Shaped Volcanoes ● Made up of layers of lava and ash & cinders ● Lava glues with ash & cinders ● Steep cone shape builds up ● Mount Vesuvius
Cone Shaped Volcano in the Philippines
Dome Shaped Volcanoes ● Mound shaped volcano - made of slow moving lava that cannot flow far ● Slow moving lava due to high viscosity (very thick & high silica content)
Dome Shaped Volcano - Mt St Helens (USA)
Antrim Plateau Mid-Atlantic Ridge in Iceland
Leinster Batholith (Granite Rock)
● Large area - includes Dublin & Wicklow Mts ● Formed 400 million years ago as magma was injected into crust ● Magma cooled slowly to form granite ● Heat from magma changed surrounding rocks into metamorphics (Quartzite & Schist) ● Weathering & Erosion over millions of years of the over-lying rock have exposed this granite ● Leinster Batholith now form the granite Wicklow & Dublin Mts
Diagram of Batholith
Slow cooling magma in earth's crust