ENVIRONMENTAL GEOLOGY (GEOL. 106)
COASTAL ENVIRONMENTS
Tu. 10/28/96
1- Discussion section project (debate)
2- Review of conference in Colorado
3- Coastal Environmental Geology
Topic for This Week's Discussion
WASTE DISPOSAL AND LANDFILLS
Use campus, web, local resources to get familiar with various aspects
of land fills (constuction, contents, regulations, contaminants,
rectification and remediation)
COMMENTS ON CONFERENCE ATTENDED LAST WEEK
Mineralogical Society of America Short Course - Denver
Reactive Transport in Porous Media
Relavance to Environmental Geology
- Groundwater, soil, fractured and porous rock interaction are the "venues"
of fluid transport
- Mineral-water interaction controls the
chemical changes in fluids
- Transport prediction (movement of fluids)
- Driven by various types of environmental problems
- Supported by federal, state agencies or consulting
firms working with various companies and govermental units.
- Knowledge of the chemical and physical processes is important for prediction
of the movement and reactions of groundwaters and soil waters.
- Mathematical modeling and field verification of models are an important
activity of environmental geologists. Course work includes: differential
calculus, differential equations, chemistry, geochemistry, mineralogy,
physics, fluid dynamics, and hydrogeology.
LECTURE: COASTAL ENVIRONMENTS
- Coastal Hazards
- The Geologic and Environmental Setting
- Coastal Dynamics on many time scales
- Shore Processes
Major Hazards Divided into Three Major Categories
- Water Level Changes
- Material Transport (including mass wasting)
- Water and Pollutants
Water Level Changes
- Short and Long Term change
- Tides (twice daily)
- Seasons (storm frequency and intensity)
- Storms
- Tsunamis (earthquakes and submarine landslides)
- Land Subsidence (tectonic)
- Long-Term Sea Level (climate change)
- Effects
- Flooding
- Landslides
- Sand Transport
- Sand and Rock Erosion
Material Transport
- Erosion (headlands)
- Storm Surges sweep salty water over fresh
water environment
- Longshore transport of sediment (see
below)
- Seawater contamination of fresh water
Pollution and water effects in coastal environments
- Seawater Intrusion from wells
- Organic Matter Production in estuaries and Vulnerability
to Pollution
- Sewage treatment outfalls into ocean
- Industrial outfalls
- Oil Spills
- Ships tend to wreck in shallow waters
- Shorelines are living habitats for many types
of wild life (including humans)
Coastal Processes
- TIDES
- Sun and Moon control tidal cycle
- Monthly variation in tides (Spring and Neap tides)
- Variation over the world
- WAVES
- Wavelength and Amplitude of Waves
- Orbital motion of water particles in a wave
- Wave motion extends to depths abou 1/2 the lentgh of the wave
- Coastal zones shallow and when water depth shallows to about 1/2 the
wave length the wave will "feel" the bottom
- Causes steepening of the shoreward front of the wave and collapse of
the wave (Surf)
- The shore is, thus, a location of expenditure of energy from waves
that causes damage and moves sediment
- LONGSHORE CURRENTS
- Waves rarely come directly toward shore; instead strike the shore at
an oblique angle
- The uprush of a wave (and suspended sand grains) in the direction that
the wave strikes the shore
- The downrush of a wave is directly down the shore slope at right angles
to the shore
- The alternate oblique uprush and right angle downrush leads to the
zig zag movement of the grains ALONG the shore.
- Sediment is, thus, transferred PARALLEL to the shore; the so-called
RIVER OF SAND
RETURN TO SYLLABUS