Chapter 2 Flashcards
Rock Cycle
relationship between rock types and their formation processes demonstrates constant change in the crust and at surface over time, aka tectonic cycle.
Rock cycle changes can lead to major temperature changes (Ex: volcanic eruption).
Rock Types
Igneous, sedimentary, metamorphic
Formation of igneous rock
Magma cools and crystallizes to form igneous rock
Formation of Sedimentary rocks
can be weathered, eroded, deposited and lithified to form sedimentary rock
Formation of Metamorphic rock
buried and subjected to greater pressure and temperature, recrystallizing the rock into a metamorphic rock
Physical Weathering
(the actual break-down of materials) wedging (frost/ice; root; salt); abrasion, remove confining stress.
Can occur within the Earth (ex: beneath volcano), or at the surface (ex: crystallization).
Chemical Weathering
dissolution, oxidation, hydrolysis. Gases can be a component to the weathering of rocks.
Effect of Rock cycle and weathering
rock cycle and weather cycles can both have detrimental effects on society, humans, and Earth. Human intervention can worsen it, or relieve the negative effects of the cycles.
Water Cycle
- The Water Cycle describes the movement of water through different environments across the planet.
- liquid, solid, gas (water vapor) are the three states of water.
- Energy exchanges as changing states. Usually, heat energy is involved with transferring energy when water changes states. Oceans (97.2%) and ice caps/glaciers (2.15%) consist of the greatest % of Earth’s water supply, as compared to other water supply sources (ex: the least amount is held in rivers/streams).
Carbon Cycle
- sugar and oxygen are released into atmosphere by plants (autotrophs) through the process of photosynthesis. Plants absorb carbon dioxide, or carbon, and water.
- the accumulation of (CO2) gas (greenhouse) emissions lead to excess heat energy.
- The sedimentary rock limestone is an important reservoir of the carbon cycle, incorporating carbonate molecules during deposition and storing them for long periods of time.
Fast Carbon cycle
Years to centuries
Slow Carbon Cycle
operates through rock/tectonic systems. Millions of years. Emissions of CO2 (and other emissions) which form sedimentary rocks.
Nitrogoen Cycle
atmosphere has Nitrogen,
makes its way into the soil,
interacts/bonds with bacteria in the soil,
good for growing plants and useful to animals.
Phosphorus Cycle
phosphate mining and uplifting of phosphate sediment (concentrated amounts for mining in Idaho/Wyoming) (fertilizers have nitrogen and phosphorous).
Weathering/erosion breaks apart minerals (phosphate (appetite/turquoise)) within rocks.
Phosphorous nourishes soil, and plants, and makes its way back into the soil, or water (marine environment; ex: ocean, lake, etc.) and helps marine life/organisms.
Sulfur Cycle
consists of the mineral sulfur (sulfate minerals, like pyrite).
This cycle often occurs near volcanos (mountain ranges), where sulfur is released into the environment (ocean, rivers), soil (sulfate), and atmosphere/fossil fuels (gas form, sulfide).
sulfur reacts with water vapor in the atmosphere. Forms H2SO4. Not an issue with a natural sulfur contribution. The average global surface ocean pH is 8 (neutral, but more basic than acidic).
The water cycle can carry sulfur throughout the environment. Sulfur can be manually added to soil to help fertilize plants. Gypsum and pyrite can be found in coal deposits due to this process. Human interaction (extraction/burning of fossil fuels) is partly responsible for the sulfur cycle.