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Volcanic Landforms: Extrusive and Intrusive, Study notes of Geology

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

2021/2022

Uploaded on 09/27/2022

madbovary
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Volcanic Landforms
Extrusive & Intrusive
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Volcanic Landforms

Extrusive & Intrusive

Introduction to Volcanic landforms

Extrusive (above the

earth's surface)

● Vent eruptions

○ classic volcanoes

● Fissure Eruptions

○ mid-atlantic ridge

● Hot Spots

○ weak point in earth's crust ○ Hawaiian islands

Intrusive (formed in

the earth's crust

● Batholith

○ slow cooling magma in the earth's crust

● Leinster Batholith

○ Wicklow & Dublin Mts ○ Granite batholith exposed by weathering

What are vent eruptions?

● 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 & Dome Shaped Volcanoes

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)

Fissure Eruptions

Antrim Plateau Mid-Atlantic Ridge in Iceland

More on the Antrim Plateau

● Fissure Eruption

● Formed 65 million years ago due to

separating plates (North American &

Eurasian plate separating)

● Basalt Plateau (high flat topped land)

extending over Antrim & Derry

● Basic lava (low silica & gas content) flowed

onto the surface due to plate divergence

● Includes Giant's Causeway - rapid cooling of

lava led to shrinking and formation of

hexagonal shape

Intrusive Landforms

● Intrusive - formed

by magma that

does not reach the

surface

● Main intrusive

landform is a

batholith

● Example: Leinster

Batholith (Granite

Rock)

Leinster Batholith (Granite Rock)

The Leinster Batholith

● 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