1. Class 2a: Landforms or What goes up must come down

2. Today’s class "The summit of Mt. Everest is marine limestone." Tectonic forces –Earthquakes, volcanoes –Diastrophism Gradational processes –Weathering, mass wasting –Erosion/deposition: water, waves, wind Examples from CA, SW Asia, Oceania

3. Rock cycle Your responsibility! Differences between igneous, sedimentary, metamorphic Examples of each

4. Plate tectonics Theorized in 1912; proven after WWII 12 large plates (lithosphere) float on liquid rock (asthenosphere) 200 million years ago, all one continent (Pangaea)

7. Plate tectonics Divergent boundaries –Generally mid-ocean –Underwater volcanoes, few quakes Convergent boundaries –Usually near continental edges –Violent volcanoes near ocean, strong quakes Transform boundaries –No volcanoes, mild to strong quakes

10. Earthquakes Stress relief via crust movement 500,000 per year; 800 felt Seismic waves of energy –P-waves or primary waves (Slinky) –S-waves or secondary waves (up and down) Earthquakes don't kill people, buildings (and gas mains) do

11. Bam, Iran 12/26/2003

12. Diastrophism Your responsibility! Folding vs. faulting Escarpment, rift valley, fault- block mountain (Sierra Nevada)

13. Volcanism Pressure on molten rock Composite volcanoes –Violent and explosive –Along subduction zones –Relatively hard to predict Shield volcanoes –More calm and constant –Along divergent boundaries or at hot spots –Relatively less dangerous

14. Mt. St. Helens 5/18/1980

17. Krakatoa, Indonesia 8/26/1883

19. Gradational processes Weathering –Chemical vs. physical Mass movement Erosion/deposition –Water (rivers, oceans) –Ice (glaciers) –Wind

20. Weathering Most mountains are going down faster than they’re going up Mechanical weathering breaks rocks into smaller pieces –Frost action –Salt crystals –Roots –Exfoliation Rock chemistry does not change

21. Frost action

23. Weathering Chemical weathering changes the chemistry of rocks –Oxidation (exposure to oxygen) –Hydrolysis (exposure to water) –Carbonation (exposure to carbon dioxide) Warmth and water encourage chemical reactions Weathering loosens rock particles, creates soil

24. Oxidation

25. Carbonation

26. Carbonation: Karst

27. Carbonation: Sinkholes

29. Erosion and deposition Erosion carries particles away Deposition deposits them Running water –Constant water, floods –Most important landform agent in deserts –Floodplains, levees, and deltas –Arroyos and alluvial fans

30. Floodplain Delta Levee

31. IL MO

32. Alluvial fan

33. Arroyo (TX) Wadi (Oman)

34. Glaciers Rivers of ice Carve out landforms from mountains –Glacial troughs –Fjords –Cirques And deposit material when they leave –Outwash plain –Moraines

35. Glacial landforms Tajikistan Kyrgyzstan

36. Glacial landforms: California

37. Glacial landforms: Iowa

38. Waves and coastlines Waves transfer energy, don’t move water Energy moves particles down the coast (longshore current) Newer coastline=erosion Older coastline=deposition Barrier reef: only organically formed landform

39. Longshore current Pacific Palisades

40. Erosion vs. deposition Acapulco Cancún

41. Great Barrier Reef