Geology Notes
Essay by danielsc • January 20, 2016 • Course Note • 904 Words (4 Pages) • 936 Views
Page 1 of 4
Atmosphere/Climate Change
Atmosphere
- The envelope of gasses surrounding the earth or another planet
- Made mostly of nitrogen and oxygen
- Energy exchanges between the sun and the lithosphere takes place
- 1 of 4 spheres of the earth
- Lithosphere: rock & soil
- Atmosphere: air
- Hydrosphere: water and ice
- Biosphere: life
Air
- Is always moving to try to equalize pressure and temperature
Greenhouse Effect
- Keeps earth at habitable temperatures
- Greenhouse gasses absorb energy from the sun and heat radiated from the ground
- Earths temperature without the GHE would be -19 C
Photochemical Smog
- Sunlight breaks up NO2 and then NO to make Ozone
- Ozone peaks mid day
- Ozone is a strong and unhealthy oxidant
Radon
- Odorless, invisible, tasteless gas
- Occurs naturally
- Not a health problem, but creates Polonium which is
Polonium
- Decays quickly and releases an energetic alpha particle which can break down DNA
- Radioactive decay radon makes polonium
Radon Exposure
- 4 picocuries is the EPA threshold for remediation
- at 4, with constant exposure your whole life, .2% get cancer after 70 years
Ozone
- stratospheric ozone absorbs ultraviolet wavelengths
- UVC makes the ozone
- UVB destroys the ozone
- CFC emit atomic chlorine and destroy ozone
- 1% decrease in Ozone leads to 2% increase in UVB, causing 2% more skin cancer
Climate
- The long term averages conditions for a given locality or region
What Effects Climate
- Amount of sunlight received
- Ocean Circulation
- Winds drive surface currents
- Oceanic gyres:
- Surface current loops in basins
- Caused by trade winds and westerlies, acted on by the Coriolis effect
- Transfer heat from equator to polar regions
- Marine upwelling along some coasts
- Thermohaline Circulation
- Reflectivity of Surface (albedo)
- Snow albedo effect
- Positive feedback
- Snow cover increases reflectivity, which makes it even colder
- Cloud albedo effect
- Negative (and positive) feedback
- Warmer temp results in more moistures/clouds – which blocks incoming solar radiation (and traps more reflected radiation)
- Topography
Variation in Climate Over Time
- Short term variations
Effects of Pinatubo
- Major volcanic eruptions block some incoming sunlight and thus cool the lower atmosphere for a few years, until the finest ash and aerosols settle out of the atmosphere
- Volcanic ash and haze in the atmosphere cools for a few years
Sun Spot Cycles
- Hot
- Plentiful during medieval warm period
- Scarce during little ice age
- Cannot explain variation since then
Variation in Climate During the Earths History
Glaciers
- Give clues about more recent climate change
- Can be used to correlate temperature with date
- Includes air bubbles→ measure greenhouse effect
Human Induced Climate Change
- Carbon Dioxide concentrations have increased from the burning of fossil fuels
- Clearing of Forests and grasslands
IPCC
- Intergovernmental panel on climate change
- Assess scientific, technical, and socio economic info relevant for the understanding of climate change
- Not a research organization
- Government org that collects and evaluates info available to make projections based on peer reviewed published literature
- Always years behind
VA geology
Physiography – west to east
Geology – by province
- Coastal plain→ unconsolidated sediments
- Piedmont→ crystalline metamorphic & igneous rocks
- Blue ridge→ crystalline metamorphic & igneous rocks
- Valley & ridge → Sedimentary rocks
- Appalachian plateau→ Sedimentary rocks
VA physiography is controlled by geology
Appalachian Plateau
- Mostly clastic sedimentary rocks
- Mostly terrestrial (above sea level) deposits
- Gently dipping and broadly folded
- Fossiliferous, may contain coal beds
Valley & Ridge
- Carbonate and clastic sedimentary rocks
- Rare igneous rocks
- Mostly marine (below sea level) deposits
- Steeply dipping, tightly folded, and faulted
- Focciliferous
- Rare coal in youngest part of section
Mesozoic Basins
- Clastic sedimentary rocks
- Igneous rocks
- Rocks are commonly:
- Terrestrial
- Gently dipping
- Fossiliferous
- Coal beds
Blue Ridge
- Intrusive and extrusive igneous rocks
- Metamorphic rocks
- Clastic sedimentary rocks
- Basement and cover rocks
- Two major metamorphic events
- Ductile faulting in basement rocks
- Brittle faulting and folding in cover rocks
- Separated from valley and ridge and piedmont by faults in most places
- Trace fossils only in youngest rocks
Piedmont
- Intrusive and extrusive igneous rocks
- Metamorphic rocks
- Several distinct terranes
- High to low grade metamorphism
- Younger intrusive rocks
- Ductile faulting and younger brittle faulting
- Complex folding is common
- Fossils are rare
Coastal Plain
- Unconsolidated sediments
- Sand rich and clay rich
- Marine and terrestrial
- Flat or gently dipping seaward
- Developed during several periods of sea level change
- Some deposits are highly fossiliferous
Mineral Resources
What do we use minerals for?
...
...
Only available on Essays24.com