Extrusive Activity Flashcards

1
Q

(1) where does the cascade mountain range lie?

A

Along the western coast of the US extending from Northern California, through Oregon and Washington into British Columbia, Canada.

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2
Q

(1) what is the cascade mountain range?

A

A continental mountain arc formed due to the subduction of an offshore oceanic plate (Juan de Fuca) beneath the continental crust (North American plate).

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3
Q

(2) lava plateaux - when did the Columbia river lava plateaux form?

A

12-17 million years ago

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4
Q

(2) lava plateaux - how big is the Columbia river lava plateaux?

A

It is regional in scale and covers 130,000 Km squared of the states of Washington and Oregon

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5
Q

(2) lava plateaux - what did a fissure eruption result in?

A

Hundreds of separate effusive basalt flows - reach total thickness of 2000m

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6
Q

(2) lava plateaux - what are basalt lavas?

A

Very ‘runny’ and take a long time to cool

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7
Q

(2) lava plateaux - what is the form of volcanism in areas within plates associated with?

A

Mantle plumes or hot spots

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8
Q

(2) lava plateaux - the plateaux is…….

A

Very distinctive and remains stable as a landscape over time

However it is gradually denuded and sculpted by erosion from wind, rain and rivers which incise into the plateaux

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9
Q

(3) shield volcanoes - what are shield volcanoes made of?

A

Also made of fluid lava flows however unlike fissure eruptions the effusive lava erupts from a central vent, flowing in all directions.

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10
Q

(3) shield volcanoes - there are various shield volcanoes along the cascade range, what do these include?

A

Belknap,
three fingered jack,
Mount Washington,
Mount bachelor

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11
Q

(3) shield volcanoes - what does Belknap shield volcano and its surrounding lava flows cover?

A

98 sq. kilometres

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12
Q

(3) shield volcanoes - when did Belknaps explosive phase begin?

A

Over 2900 years ago

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13
Q

(3) shield volcanoes - Belknap is one of the cascades what?

A

Youngest volcanoes with lava flows as young as 1,400 years

Therefore is a dynamic landscape with potential to be rescaled in future as it receives fresh flows of lava from the central vent

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14
Q

(4) cinder cones - how do cinder cones form?

A

From the build up of pyroclastic materials ejected from a single vent

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15
Q

(4) cinder cones - what are cinder cones!

A

Explosive and geologically younger features which often from on the flanks of larger volcanoes

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16
Q

(4) cinder cones - describe lava butte cinder cone in Oregon

A

It rises 500ft above the ground and has view over the cascade range. It formed 7000 years ago covering 9 miles with lava.

17
Q

(4) cinder cones - what is wizard islands?

A

A small cinder cone formed more recently which rises out of the lake that now occupies the crate lake caldera

18
Q

(5) calderas - what is crater lake caldera?

A

An example of a large caldera crater more recently filled with water

19
Q

(5) calderas - when did crater lake caldera form?

A

Around 6000 years ago

It is the remnant of a high volcano called Mount Mazama which lost its top as the lava beneath the mountain drained out in violent explosions and the top collapsed inwards.

20
Q

(5) calderas - what are calderas often distinctively characterised by?

A

Geothermal activity such as geysers and secondary features such as hot springs and earthquakes are often common

21
Q

(5) calderas - where is Yellowstone national park, Wyoming, situated?

A

Within a caldera, accounting for its many geothermal features.
Seismic unrest in the park has recently been detected which could indicate a period of further activity.

22
Q

(5) calderas - calderas are very large in scale, what does this mean?

A

They are less distinctive from the ground but more easily viewed by satellite.

23
Q

(6) stratovolcanoes and lava domes - what are stratovolcanoes?

A

Extrusive landforms often related to explosive volcanic activity at subduction zones

24
Q

(6) stratovolcanoes and lava domes - what are stratovolcanoes often characterised by?

A

A conduit system with a crater at the summit containing a central vent bringing magma up to the surface from a chamber below

25
Q

(6) stratovolcanoes and lava domes - where do parasitic cones often form?

A

On the flanks of composite volcanoes where lava may flow from fissures.
Strengthening of the cone may occur when magma solidifies in dykes (vertical intrusions cutting across bedding planes)

26
Q

(6) stratovolcanoes and lava domes - Mount St. Helens volcano is…..

A

40,000 years old, 2549m high and still potentially active today

Remained dormant from 1857-1980

27
Q

(6) stratovolcanoes and lava domes - during the five month period following the 1980 Mount St. Helens eruption what happened?

A

There were 5 small explosive eruptions which along with 16 small eruptions in 1986 created a lava dome in the crater formed in the 1980 eruption

28
Q

(6) stratovolcanoes and lava domes - what did the lava dome do to Mount St. Helens?

A

Plugged the vent and trapped gases leading to the build up of pressure and a subsequent explosive eruption shattering the dome and transforming the landscape.

29
Q

(7) EVALUATION - what is the cascade range?

A

A distinctive landscape produced by volcanic and seismic activity at an active subduction zone

30
Q

(7) EVALUATION - what is the cascade range a result of?

A

Activity that started 16 million years ago but has been shaped by subsequent activity up to the present day.

31
Q

(7) EVALUATION - some features of extrusive landscapes have the potential to what?

A

Change dramatically and periodically after millions of years of being shaped by denudation.

32
Q

(7) EVALUATION - the 1980 Mount St. Helens eruption triggered what?

A

The collapse of the North side of the volcano which brought secondary effects such as a land slide, superheated pyroclastic debris flows and Lahars.

33
Q

(7) EVALUATION - other landforms appear what?

A

Less dynamic e.g. Belknap shield volcano, but still have the potential to be shaped by the future tectonic activity

34
Q

(7) EVALUATION - lava plateaux in e range however are what?

A

Stable features which erode slowly over long periods of geological time.