Test 2 (lecture Recording 1) Flashcards
Rock Cycle
-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.
Formation of Rocks
-Cooling and crystallization for igneous rocks.
-Weathering, erosion, and sediment transport for sedimentary rocks.
-Metamorphism for metamorphic rocks.
Lithification and Diagenesis
Explanation of the processes involved in forming sedimentary rocks.
Tectonic Environments
-Different tectonic settings where igneous rocks can form.
-Brief overview of large igneous provinces.
Ways Rocks Melt to Form Magma
1-Decompression melting
2-Heat transfer melting
3-Flux melting
Decompression melting:
decrease in pressure leading to melting.
Flux melting:
addition of volatiles like water and CO2.
Heat transfer melting
transfer of heat from hotter magma to cooler rocks.
Igneous Rocks:
Rocks formed from the cooling and solidification of magma.
Sediments:
Small pieces of rocks, minerals, and organic materials that are transported and deposited.
Sedimentary Rocks:
Rocks formed from the lithification of sediments through compaction and cementation.
Metamorphic Rocks:
Rocks formed from the alteration of existing rocks due to changes in temperature and pressure.
Lithification:
The process of compacting and cementing sediments to form sedimentary rocks.
Diagenesis:
Another term for the process of lithification.
Metamorphism:
The process through which existing rocks undergo changes in temperature and pressure to form metamorphic rocks.
Subduction Zones:
Areas where one tectonic plate moves under another.
Divergent Boundaries:
Areas where tectonic plates move away from each other.
Hotspots:
Areas where magma from the mantle rises to the Earth’s surface.
Magma Formation:
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.
Magma Processes:
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.
Igneous Rocks Formation:
Tectonic environments like subduction zones or divergent boundaries lead to magma formation.
Sedimentary Rocks Formation:
Deposition of sediments in areas such as oceans or lakes.
Metamorphic Rocks Formation:
High pressure and temperature conditions in regions of tectonic activity.
Protolith:
Initial rock before metamorphism.
Metamorphism:
Process where rocks undergo changes in pressure and temperature, resulting in the formation of new rocks.
Metamorphic Rocks:
Resulting rocks from metamorphism, such as marble from limestone and quartzite from sandstone.
Migmatites:
Rocks formed from partial melting during metamorphism.
Lava vs. Magma:
Lava is found on the surface, while magma is beneath the Earth’s surface.
Extrusive vs. Intrusive Igneous Rocks:
Extrusive rocks form on the surface, while intrusive rocks form beneath the surface.
Volcanic vs. Plutonic Rocks:
Volcanic rocks erupt to the surface, while plutonic rocks remain beneath the Earth’s surface.
Tectonic Environments for Igneous Activity:
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.
Ways to Melt the Earth’s Mantle:
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.
Understanding Igneous Processes:
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.