Chapter 3
Volcanism
and Earthquake
--Type of Landform depends on:
>Fluidity & Strength of Magma + types of (cracks+faults+joints) that it penetrates + manner in which it escapes to surface.
--Solidification of Magma =Intrusive landform(called Plutonic rocks) +Extrusive landform(Volcanic rocks)
--Both Plutonic + Volcanic rocks = igneous rock.
Landforms of Igneous Intrusion:
--They come to surface after prolonged erosion unlike extrusive landforms--image ↓(in next to next heading).

--Batholiths:
>Batholiths form the core of huge mountains and may be exposed on surface after erosion.
>These are granitic.
>Wicklow Mountain in Ireland.
>Fluidity & Strength of Magma + types of (cracks+faults+joints) that it penetrates + manner in which it escapes to surface.
--Solidification of Magma =Intrusive landform(called Plutonic rocks) +Extrusive landform(Volcanic rocks)
--Both Plutonic + Volcanic rocks = igneous rock.
Landforms of Igneous Intrusion:
--They come to surface after prolonged erosion unlike extrusive landforms--image ↓(in next to next heading).

--Batholiths:
>Batholiths form the core of huge mountains and may be exposed on surface after erosion.
>These are granitic.
>Wicklow Mountain in Ireland.
--Laccoliths:
> These are large dome-shaped intrusive bodies connected by a pipe-like conduit from below.
> These are basically intrusive counterparts of an exposed domelike batholiths.
> Karnataka plateau is spotted with dome hills of granite rocks. Most of these, now exfoliated, are examples of laccoliths or batholiths.
> These are large dome-shaped intrusive bodies connected by a pipe-like conduit from below.
> These are basically intrusive counterparts of an exposed domelike batholiths.
> Karnataka plateau is spotted with dome hills of granite rocks. Most of these, now exfoliated, are examples of laccoliths or batholiths.
--Lapoliths :
> develops into a saucer shape, concave to the sky .
>Ex- Transval , South Africa.
> develops into a saucer shape, concave to the sky .
>Ex- Transval , South Africa.
--Phacolith :
> wavy mass of intrusive rocks (syncline + Antisyncline).
> wavy materials have a definite conduit to source beneath in the form of magma chambers (subsequently developed as batholiths).
>Cordon Hill in England.
--Sills:
> Horizontal intrusion.
>Thin sheet || thick sills. Ex- Great Whin Sill of N.E. England.
--Dykes.
> Vertical intrusion.
>becoz of narrowness= seldom dominates landscape.
>Can be upstanding wall of shallow trenches (depends on corrosion resistance to nearby rocks)
>most commonly found intrusive forms in the western Maharashtra area. These are considered the feeders for the eruptions that led to the development of the Deccan traps.
> wavy mass of intrusive rocks (syncline + Antisyncline).
> wavy materials have a definite conduit to source beneath in the form of magma chambers (subsequently developed as batholiths).
>Cordon Hill in England.
--Sills:
> Horizontal intrusion.
>Thin sheet || thick sills. Ex- Great Whin Sill of N.E. England.
--Dykes.
> Vertical intrusion.
>becoz of narrowness= seldom dominates landscape.
>Can be upstanding wall of shallow trenches (depends on corrosion resistance to nearby rocks)
>most commonly found intrusive forms in the western Maharashtra area. These are considered the feeders for the eruptions that led to the development of the Deccan traps.
Type of Lava:
--Basic Lava:
> (Fe, Mg) > SiO2 (silica).
>Property = Highly Fluid.
>>as a result = spread to large area(as move fast before solidifies).
>>forms thin layer over great distance.
>Appearance =Gentle slope + wide diameter + Flattened shield or dome.

--Basic Lava:
> (Fe, Mg) > SiO2 (silica).
>Property = Highly Fluid.
>>as a result = spread to large area(as move fast before solidifies).
>>forms thin layer over great distance.
>Appearance =Gentle slope + wide diameter + Flattened shield or dome.

--Acid Lava:
> SiO2 > (Fe, Mg).
>Property= Highly Viscous.
>>as a result= spread less
>>thick layer
>distinct feature:
>>Viscosity ↑ = speed ↓ è rapid Congealing.
> SiO2 > (Fe, Mg).
>Property= Highly Viscous.
>>as a result= spread less
>>thick layer
>distinct feature:
>>Viscosity ↑ = speed ↓ è rapid Congealing.
>>this Congealing sometimes = obstructs out flow.
>>Result = Pyroclast AKA Volcanic Bomb.
>Appearance:
>>sometime Lava solidies within conduit = forming Spine.
>>some spine are very resistive = side by mountain erodes leaving= rising Spine between.
>>Ex- Mt. Pelee in Martinique(Carabean island)

Type of Volcanos:
--Active = Barren Island, India.
--Dormant=Narcondom Island, India.
--Extinct= no one is sure when volcano goes extinct. Mt. Karataku, was thought to be extinct but it erupted.

Extusive landforms:
--Formed by Basic Lava:
>Produces Extensive Lava Plains=Snake basin(USA).
>or Produces Basalt pateau= Deccan trap (India).
>Lava dome or shield Volcane = gentle slope.
>Caldera = swimming pool of Lava with steep wall in the dome.=Kilauea Volcano(Hawai, USA)
(Image ↓)

--Formed by Acidic Lava:
>Less viscous or Fluid
>Pyroclasts = explodes forming= Ash + Cinder cone= forms Crater in middle(like Caldera). (https://www.youtube.com/watch?v=Eqc2zaWS3XA) .
>usually small volcano in groups= height <1000 feet.
--Composite Volcano= repetitive eruption= layers.
>Ex- Mt. Stromboli =bcoz of frequent eruption = known as “Light hous of Mediterranean”.
-Mt Etna in Sicily.
--Crater Vs Caldera:
>If the top of Cone is blown off = Crater
>If Crater enlarges in depression= Caldera.
>Water fill = Crater/Caldera Lake = Ex- Lake Toba in Sumatra.
--Active = Barren Island, India.
--Dormant=Narcondom Island, India.
--Extinct= no one is sure when volcano goes extinct. Mt. Karataku, was thought to be extinct but it erupted.

Extusive landforms:
--Formed by Basic Lava:
>Produces Extensive Lava Plains=Snake basin(USA).
>or Produces Basalt pateau= Deccan trap (India).
>Lava dome or shield Volcane = gentle slope.
>Caldera = swimming pool of Lava with steep wall in the dome.=Kilauea Volcano(Hawai, USA)
(Image ↓)

--Formed by Acidic Lava:
>Less viscous or Fluid
>Pyroclasts = explodes forming= Ash + Cinder cone= forms Crater in middle(like Caldera). (https://www.youtube.com/watch?v=Eqc2zaWS3XA) .
>usually small volcano in groups= height <1000 feet.
--Composite Volcano= repetitive eruption= layers.
>Ex- Mt. Stromboli =bcoz of frequent eruption = known as “Light hous of Mediterranean”.
-Mt Etna in Sicily.
--Crater Vs Caldera:
>If the top of Cone is blown off = Crater
>If Crater enlarges in depression= Caldera.
>Water fill = Crater/Caldera Lake = Ex- Lake Toba in Sumatra.
Some Epic Volcanic
Erruption:
--Mt. Vesuvius= Bay of Naple (Itly) =24 Aug .A.D. 79.
--Mt. Krakatau=Sunda strait (b/w Java and Sumatra), 1883 =Greatest .
>Explosion formed Caldera(Although written in Basic Lava type ↑).
>land was not inhabitated by any one===sound till Australia.
>re-erupted in 1927.
--Mt. Vesuvius= Bay of Naple (Itly) =24 Aug .A.D. 79.
--Mt. Krakatau=Sunda strait (b/w Java and Sumatra), 1883 =Greatest .
>Explosion formed Caldera(Although written in Basic Lava type ↑).
>land was not inhabitated by any one===sound till Australia.
>re-erupted in 1927.
--Mt. Pelee=
West indies, 1902.
Facts for Valcanos:
--Mt. Cameroon = only Active volcano in West Africa.
--Atlantic coast(mostly Alpine fold mountain) has mostly= Dormant Volcano.
>Volcano of Iceland + Azores(autonomous region of Volcano) = Active.
--Mt. Cameroon = only Active volcano in West Africa.
--Atlantic coast(mostly Alpine fold mountain) has mostly= Dormant Volcano.
>Volcano of Iceland + Azores(autonomous region of Volcano) = Active.
Geyeser Vs Hot spring:
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Geyeser
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Hot Spring
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Feature
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Violent eruption
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Just hot water
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Location
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3 Major areas:
1)Iceland 2)Rotorua district of North Island(New Zealand) 3)Yellowstone park(USA) |
All across the globe
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Famous
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Wyoming, in USA (erupts in every 63
minutes avg)
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Japan + Hawaii(USA)
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