M2 Subtopic 3 Flashcards

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1
Q

These are the geological processes that originate within the Earth and result from the energy stored in its interior. These processes are responsible for shaping the Earth’s surface through the creation and modification of landforms

A

Endogenic Processes

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2
Q

Endogenic Processes Include:

A

Metamorphism and Magma Generation and Intrusion
Tectonic Activity
Volcanism
Earthquakes
Isostasy

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3
Q

the thermal energy that was generated during the formation and early evolution of the Earth.

A

Primordial Heat from Planetary Formation

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4
Q

The process of planet formation involves the collision and aggregation of smaller bodies (planetesimals). The kinetic energy from these collisions was converted into heat

A

Accretion

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5
Q

As the Earth formed, gravitational forces caused it to compress. The conversion of gravitational potential energy into thermal energy generated significant heat

A

Gravitational Compression

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6
Q

The decay of short-lived radioactive isotopes (such as aluminum-26) during the early stages of Earth’s formation contributed to the initial heat

A

Radioactive Decay

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7
Q

also known as gravitational contraction or self-compression, is the process by which a celestial body generates heat due to the conversion of gravitational potential energy into thermal energy

A

Gravitational Compression

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8
Q

Generated by the movement of tectonic plates

A

Heat from Friction Due to Plate Movements

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9
Q

One plate being forced under another generates significant friction and heat

A

Subduction zones

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10
Q

Heat moves through solid materials like rocks; Heat moving from Earth’s hot core to the cooler mantle and crust

A

Conduction

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11
Q

Heat transfer through the movement of semi-fluid rock in the mantle

A

Convection

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12
Q

Localized Heat Sources: Areas of volcanic activity not directly associated with plate boundaries.

A

Hotspots

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13
Q

Conditions Required for Magma Formation

A

Heat, Pressure, Volatiles

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14
Q

For rocks to melt and form magma, temperatures must be high enough to overcome the bonds holding the minerals together.

A

Heat

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15
Q

As it increases with depth, it raises the melting point of rocks. However, under certain conditions, a decrease can lead to melting.

A

Pressure

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16
Q

Primarily water, and carbon dioxide, lower the melting point of rocks.
When they are are introduced into the mantle, they reduce the temperature at which rocks begin to melt, facilitating magma formation.

A

Volatiles

17
Q

Processes Leading to Magma Formation

A

Decompression Melting
Flux Melting
Heat-induced Melting

18
Q

Occurs when there is a decrease in pressure as mantle rocks ascend. This process is common at divergent plate boundaries, such as mid-ocean ridges, where tectonic plates move apart. As the pressure decreases, the mantle material rises and partially melts, forming basaltic magma

A

Decompression Melting

19
Q

Happens when volatiles like water and carbon dioxide are added to the mantle, reducing the melting temperature of the rocks

A

Flux Melting

20
Q

occurs when the temperature of the mantle or crust increases due to tectonic processes such as mantle plumes or hotspots

A

Heat-induced melting

21
Q

These chambers act as storage areas where magma can evolve before potentially leading to volcanic eruptions

A

Magma Chambers

22
Q

When magma cools and solidifies below the Earth’s surface, it forms intrusive igneous rocks

A

Intrusive Pathway

23
Q

When magma reaches the surface, it erupts through volcanic vents, forming extrusive igneous rocks like basalt, andesite, and rhyolite

A

Extrusive Pathways

24
Q

Formed by low-viscosity basaltic lava that flows easily and spreads widely

A

Shield Volcanoes

25
Q

Characterized by alternating layers of lava and pyroclastic material, resulting from explosive and effusive eruptions.

A

Stratovolcanoes/composite

26
Q

Large, basin-shaped depressions formed when a volcano collapses following a massive eruption

A

Calderas

27
Q

As magma cools, early-forming minerals crystallize and settle out of the melt, removing specific elements and altering the composition of the remaining liquid. This process can create layered intrusions with distinct mineral bands

A

Fractional Crystallization

28
Q

Magma can incorporate surrounding rock material as it ascends, altering its composition. It can lead to the formation of hybrid magmas with mixed characteristics.

A

Assimilation

29
Q

When magmas from different sources or depths come into contact, they can mix, forming a new magma with intermediate properties. This process can produce complex igneous rock formations with varied textures and compositions

A

Magma Mixing

30
Q

Types of Metamorphism

A

Contact Metamorphism
Regional Metamorphism
Dynamic Metamorphism

31
Q

Caused by mechanical deformation along fault zones, leading to changes primarily due to pressure. This can create rocks like mylonite

A

Dynamic Metamorphism