Test 2 (lecture Recording 1) Flashcards

1
Q

Rock Cycle

A

-Processes involved in the formation of igneous, sedimentary, and metamorphic rocks.
-Connection between magma,
igneous rocks, sediments, sedimentary rocks, and metamorphic rocks.
-Erosion sources for sediments.

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2
Q

Formation of Rocks

A

-Cooling and crystallization for igneous rocks.
-Weathering, erosion, and sediment transport for sedimentary rocks.
-Metamorphism for metamorphic rocks.

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3
Q

Lithification and Diagenesis

A

Explanation of the processes involved in forming sedimentary rocks.

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4
Q

Tectonic Environments

A

-Different tectonic settings where igneous rocks can form.
-Brief overview of large igneous provinces.

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5
Q

Ways Rocks Melt to Form Magma

A

1-Decompression melting
2-Heat transfer melting
3-Flux melting

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6
Q

Decompression melting:

A

decrease in pressure leading to melting.

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7
Q

Flux melting:

A

addition of volatiles like water and CO2.

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8
Q

Heat transfer melting

A

transfer of heat from hotter magma to cooler rocks.

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9
Q

Igneous Rocks:

A

Rocks formed from the cooling and solidification of magma.

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10
Q

Sediments:

A

Small pieces of rocks, minerals, and organic materials that are transported and deposited.

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11
Q

Sedimentary Rocks:

A

Rocks formed from the lithification of sediments through compaction and cementation.

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12
Q

Metamorphic Rocks:

A

Rocks formed from the alteration of existing rocks due to changes in temperature and pressure.

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13
Q

Lithification:

A

The process of compacting and cementing sediments to form sedimentary rocks.

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14
Q

Diagenesis:

A

Another term for the process of lithification.

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15
Q

Metamorphism:

A

The process through which existing rocks undergo changes in temperature and pressure to form metamorphic rocks.

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16
Q

Subduction Zones:

A

Areas where one tectonic plate moves under another.

17
Q

Divergent Boundaries:

A

Areas where tectonic plates move away from each other.

18
Q

Hotspots:

A

Areas where magma from the mantle rises to the Earth’s surface.

19
Q

Magma Formation:

A

1-Decompression Melting: Melting that occurs when rocks experience a decrease in pressure, typically at divergent boundaries.
2-Flux Melting: Melting caused by the addition of volatiles like water and CO2, often associated with subduction zones.
3-Heat Transfer Melting: Melting that happens when hotter magma transfers heat to cooler rocks.

20
Q

Magma Processes:

A

1-Cooling and Crystallization:The process through which magma cools and solidifies to form igneous rocks.
2-Weathering:The breaking down of rocks into smaller pieces.
3-Erosion: The transportation of weathered materials.
4-Sediment Transport:The movement of sediments by water, wind, or ice.

21
Q

Igneous Rocks Formation:

A

Tectonic environments like subduction zones or divergent boundaries lead to magma formation.

22
Q

Sedimentary Rocks Formation:

A

Deposition of sediments in areas such as oceans or lakes.

23
Q

Metamorphic Rocks Formation:

A

High pressure and temperature conditions in regions of tectonic activity.

24
Q

Protolith:

A

Initial rock before metamorphism.

25
Q

Metamorphism:

A

Process where rocks undergo changes in pressure and temperature, resulting in the formation of new rocks.

26
Q

Metamorphic Rocks:

A

Resulting rocks from metamorphism, such as marble from limestone and quartzite from sandstone.

27
Q

Migmatites:

A

Rocks formed from partial melting during metamorphism.

28
Q

Lava vs. Magma:

A

Lava is found on the surface, while magma is beneath the Earth’s surface.

29
Q

Extrusive vs. Intrusive Igneous Rocks:

A

Extrusive rocks form on the surface, while intrusive rocks form beneath the surface.

30
Q

Volcanic vs. Plutonic Rocks:

A

Volcanic rocks erupt to the surface, while plutonic rocks remain beneath the Earth’s surface.

31
Q

Tectonic Environments for Igneous Activity:

A

1-Subduction Zones: Occur where plates collide, leading to magma formation.
2-Divergent Boundaries: Plates move apart, allowing magma to rise and create new crust.
3-Hotspots: Deep mantle plumes create magma, forming islands like Hawaii.
4-Continental Rifts: Rifts form as continents split, leading to volcanic activity.
5-Large Igneous Provinces (LIPs): Massive outpourings of igneous rock, potentially related to mantle plumes.

32
Q

Ways to Melt the Earth’s Mantle:

A

1-Decompression Melting: Decreasing pressure allows rocks to melt, occurring at divergent boundaries.
2-Flux Melting: Adding volatiles like water and CO2 lowers the melting temperature of rocks, occurring at subduction zones.
3-Heat Transfer Melting: Hotter magma can transfer heat to cooler rocks, causing them to melt, less common but still significant.

33
Q

Understanding Igneous Processes:

A

1-Partial Melting: Only a portion of the rock melts, leading to the formation of magma.
2-Influence of Volatiles: Water plays a crucial role in melting rocks by lowering their melting temperature.
3-Complex Interactions: Igneous processes involve a combination of factors, including pressure, temperature, and the presence of volatiles.