text web site | main class page | Gonzaga home | Power Point presentation with photographs
I. Plate tectonics
A. Structure of the earth’s interior fig. 16-2
B. Convection cells within the earth’s mantle drive plate movement (fig. 16-2 and 16-3)
- the movement of the continents and other evidence
- animation of the earth's plates and how they fit
C. Divergent boundaries (fig. 16-5)
1. in ocean - mid-Atlantic ridge (more)
2. on land - rift valleys (Iceland (take a virtual field trip) and east Africa)
Lake Baikal in Russia is located on a rift (more) a new ocean is forming in the rift valley of Africa 1. subduction zone
2. trenches and island/volcano (fig. 16-5) arcs in the ocean
- the Marianas trench is the deepest spot in the ocean
3. mountain building on land
4. ring of fire (fig. 16-4)
- volcanoes
- Volcano under the city - explore volcano "anatomy"
- Tsunamis are caused by the subduction zone along the N.A. west coast (pictures and explanation)
- more on tsunamis
- one of the largest tsanamis on record struck Lituya Bay, Alaska in 1958
- Krakatoa - one of the most significant eruptions in recent history
- Mt. St. Helens and volcano cam | before and after satellite photos
- Crater Lake in Oregon formed as a result of a large eruption 1000 years ago.
- Explore National Park system volcanoes
- Smithsonian Volcano page (links to a Google Earth interactive of worldwide volcanoes!!)
- Google-earth earthquake monitor
1. boundary between sections of divergent plates (fig. 16-5)
2. earthquakes (fig. 16-6 and 16-7)
Plate Tectonics links
- The PaleoMap - an excellent overview
- USGS plate tectonics overview (excellent site with graphics)
- Hell's Crust: Our ever-changing planet: background and animations of plate tectonics, earthquakes, volcanoes, and tsunamis
- diagram of Pangea -- the supercontinent
- this animation shows the breakup of Gondwana (the supercontinent) and the formation of the island Seychelles
- another animation - overview of plate tectonics interactions
- This shockwave animation allows you to move around plates and see the effects
- See how "atolls" are built - it's not tectonics, but an interesting geological process
- Separation of the Seychelles island chain from Asia
- Natural hazards page has lots of info on earthquakes, tsunamis, and volcanoes
- Basic overview of tsunamis and earthquakes
- NOAA tsunami research program
- Lots of animations - plate tectonics, tides, hurricanes, etc
- Schoolyard Geology - looking at urban features as a way to understand geology
- The Earthscope project explores plate movement in the US
- Tour of National Park System geological features and Park Service Geologic Wonders
- Plates on the move
- Geology of New Zealand has lots of good stuff
- Science Bulletins - interactives and videos from the American Museum of Natural History - includes features on volcanoes, Yellowstone, and other geology topics
- Geology of the Colorado Plateau
- Geology of the National Parks - 3-D views | another site
II. Non-tectonic processes produce most surface features
A. glaciation
- Mystery of the Megaflood - explore geological evidence of post-glacial flooding in North America
- Quiz yourself - identify geological origin of landscapes
- power point presentation on glacial effects
- Explore glacial features in the National Parks
- 3-D images of glaciers and other features in national parks (USGS)
- Forest Service National Avalanche Center
B. mechanical weathering/erosion by wind and water
- Explore cave and karst features in the National Parks
- Explore coastal geology in the National Parks
C. chemical weathering
D. The geologic history of the mid-Atlantic
Geology of Virginia (JMU)
Geology of Virginia (William and Mary)
Sierra Club: Atlantic Coast | Central Appalachians
National Park Service Nature and Science overviews: Shenandoah | George Washington Parkway
III. The rock cycle (another link) (fig. 16-9)
A. igneous rock is formed beneath the earth’s surface in a molten state
B. sedimentary rock forms from sediments weathered off existing rock/soil and deposited in water
C. metamorphic rock is produced when existing rock is heated enough to change its form
IV. Soils
A. layers – fig. 4-25
1. Surface layer (O horizon) surface litter
2. A horizon topsoil mostly organic (varies with soil type)
3. B horizon subsoil
4. C horizon parent material lies on the bedrock
- in desert and near-desert regions, the soil crust is very thin and fragile. Check out the basics (soil 101) and some pictures
B. soil organisms create soil (fig. 4-26) and add nutrients to it
C. soil profiles vary in different biomes and are a determining factor for biome types (fig. 4-27, and more later in chap 6)
D. soil types (more on soil classification) (more here - info on the 12 soil "orders", range maps, etc) (technical info)
1. clay
2. sand
3. silt
4. soils are a mixture of the three types, which results in a complex assortment of soil texture
5. soils with roughly-equal mixtures are called loams
6. differing properties result from varying combinations of the three types
E. erosion
1. three types – p. 279
2. historical examples - dust bowl (p. 281)
3. seriousness of erosion worldwide – fig. 14-7
4. desertification is a related problem (fig. 14-9)
- both of these problems are related to water over-use and over-grazing by livestock
- the Aral Sea provides a frightening example of the worst-case scenario (check out satellite images)
- we will discuss this further with regard to resource use and food production
5. solutions to soil erosion problems
- farming adjustments - p. 284-286
- animal and artificial fertilizers can present a host of problems more on this when we discuss water pollution
- Natural Resource Conservation Service (a program of the USDA) addresses erosion in the US