Week 1: Your place on planet Earth Flashcards
Antarctica annual ice loss
125km^3
125 gigatons
The earth systems interconnected subsystems
Atmosphere
Geosphere
Hydrosphere
Biosphere
Processes in the earth system act on length scales of
Microns to thousands of kilometres
Processes in the earth system act on time scales of
Milliseconds to millions of years
The external source powering the earth system
The sun
The internal sources powering the earth system
Radioactive decay and gravitational energy
Constant movement of material or energy between reservoirs produces
Cycles
Earth system science studies:
- The whole planet as a system of innumerable interacting parts
- Focuses on the changes within and among those parts
The four interconnected spheres house the earth system’s:
Reservoirs
We learn about the earth system by measuring how what passes between earths reservoirs
Mass/volume of material and exchange of energy
Hydrosphere
Oceans, lakes, rivers and groundwater
Atmosphere
Troposphere, stratosphere, clouds which hold gases, water vapor and aerosols
Geosphere
Continents, seafloor, sediments, lava, soils
Biosphere
Animals, plants, bacteria both terrestrial and marine
The constant exchange of energy and matter between earths reservoirs is called
Flux
Reservoirs that donate energy or matter are called
Sources
Reservoirs that receive energy or matter are called
Sinks
Natural cycles exist in a state of
Dynamic equilibrium
When a system is in dynamic equilibrium
- All parts of the system are in continuous motion
- But they move in opposing directions at equal rates so that the system as a whole does not change
Uniformitarianism
The theory that changes in the earths crust during geological history have resulted from continuous and uniform processes
The geologic record
The memory bank of earths history
Classification of rocks
Sedimentary, Igneous, Metamorphic
Making a sedimentary rock
- Weathering of existing rocks
- Transportation of weathered products via air, water or ice
- Sedimentary deposition
4a. Settling 4b. Chemical precipitation
5a. Detrital sediments 5b. Chemical sediments - Lithification
7a. Detrital sedimentary rocks 7b. Chemical sedimentary rocks
Making an igneous rock
- Magma (molten rock derived from crust or mantle)
2a. Surface effusion as lava or pyroclastics
2b. Cool and solidify as intrusions or plutons at depth
3a. Volcanic or extrusive (fast cooling, fine-grained)
3b. Plutonic or intrusive (slow cooking, coarse-grained) - Igneous rocks
Making a metamorphic rock
- Apply pressure from deep burial
- Apply heat from plutons or normal geothermal gradient
- Deform old rock from directed stresses and redistribute fluid to transform material
Lithification
The process in which sediments compact under pressure and gradually become solid rock
Relationships between rock units
- Superposition
- Original horizontality
- Faults (reverse, normal)
- Unconformities
- Inclusion