1. Physical Geography: Landforms of California

4. Overview Geologic Time Movements of the Continents Earth Materials Tectonic Forces Weathering and Erosion Processes Erosional Agents and Deposition

5. Geologic Time Pretend the age of the earth (4.6+ billion years) is compressed into one calendar year. January 1 - Earth and planets formed Early March - liquid water stands in pools. Late March - earliest life July - oxygen is important part of atmosphere October 25 - multicellular organisms Late November - plants and animals abundant December 15 to 25 - dinosaurs arise and disappear 11:20 pm, December 31 - Humans appear One second before midnight - Automobile invented

6. General trends: temperature, density Horizon composition, behavior The Earth ’ s Interior Distance: 6730 km (3963 miles)

7. Earth Materials Three major rock types –Igneous –Sedimentary –Metamorphic

8. Igneous Rocks Igneous (ignus = fire) Formed from the cooling of molten rock (magma/lava), a process called crystallization. –Slow cooling  larger crystals > dense rock –Rapid cooling  small crystals > lighter rock

9. Two classes of igneous rocks –intrusive: formed inside the Earth –extrusive: formed at Earth ’ s surface

10. Igneous Intrusive Rocks Cools slowly (thousands of years) Visible crystals Examples - granite- diorite- gabbro

11. Igneous Extrusive Rocks Cools rapidly - exposed to surface No visible crystals Examples - rhyolite - andesite -basalt

12. Typical Igneous Intrusions Know: Batholith and Dike

13. Exposed Batholiths Sierra Nevada, CA

14. Sedimentary Rocks

15. Compaction Cementing Sedimentary Rocks Formation Relative Abundance by Type

16. Sandstone (larger grains) Shale (fine grains) Limestone (CaCO 3 )

17. Where do Sedimentary Rocks Form? Terrestrial environments (non-marine)  Rivers and floodplains (fluvial environment)  Lakes  Deserts (aeolian environment) Marine environments  Continental shelf  Continental slope and rise (deep sea fans)  Abyssal plain  Beach and barrier islands

19. Metamorphic Gneiss (broad foliation) Schist (narrow foliation)

20. The Unstable Landscape: California Plate Tectonics

21. Crustal Processes –Destruction (subduction) –Creation (volcanism ) –Alteration / deformation (folding and faulting)

22. Introduction Plate boundaries: main location for Earth ’ s volcanic and earthquake activity. Type of plate boundary determines activity. 3 types –diverging (spreading) –converging (colliding) –transform (sliding past each other)

23. Convergent Plate Boundaries Action: –collision; destructional or constructional Activity: –depends on type of convergence –3 types: ocean-continent, ocean-ocean, cont.-cont.

24. Convergent: Ocean-continent Action: –collision; destructional (subduction of ocean plate) Activity: –shallow to deep earthquakes; volcanism (continental) Features: –ocean trench; volcanic mtns on continental margin

25. Volcanoes: Explosive Composite cones (stratovolcano) –pointed, steep-sided, tall volcanoes –“ Composite ” : layers of pyroclastics and lava (mostly felsic) –Explosive and dangerous; found near subduction zones

26. Volcanoes: Explosive Arenal, Costa Rica Mt. Shasta, CaliforniaMt. Lassen, California

30. Crustal Deformation: Folding, Faulting, and Earthquakes

31. Introduction Crustal Processes –Destruction (subduction) –Creation (volcanism - convergent/divergent) –Alteration / deformation (folding and faulting)

32. Crustal Deformation Outcome / result of “ battle ” : Stress v. strain (force v. resistance) –Stress: force imposed on the rock (tension, compression and shear) –Strain: how the rock responds to the stress (folding / bending or faulting / breaking) Is the rock brittle or ductile?

33. Figure 12-7

34. Faulting Definition: fractures where some type of displacement (movement) has occurred along a break in rock. Three types –normal –reverse/thrust –transform (strike-slip) Carmel Valley Fault, CA

36. Normal Faults Tensional stress Earthquake and displacement along fault plane  fault scarp

37. Landforms - Normal Faulting Owens Valley, CA Sierra Nevada, CA Grand Tetons, WY

38. Basin and Range Horst and graben ( “ hill ” and “ grave ” ) Death Valley/ Panamint Ranges Why saline?

39. Landforms: Normal Faulting Grabens ( “ Graves ” )

40. Basin and Range

41. Transform Plate Boundary Action: –shear (lateral motion) –no loss/gain of plate material

42. San Andreas fault system –How long is it? About 1000 km –Relative motion of the Pacific Plate? @ 2 inches (5 cm) northwest per year. In 10 million years Los Angeles will be off of San Francisco.

43. San Andreas Fault System - Southern California

44. Transform Plate Boundary Activity: –shallow to moderate earthquakes –little to no volcanism http://quake.usgs.gov/recenteqs/ Tremblor Range Dragon ’ s Back Carrizo Plain, CA (view to the east)

46. Transform Plate Boundary Features: –shallow, linear rift valleys –sag ponds San Andreas Lake (Crystal Springs Reservoir) - looking south along fault - San Francisco water supply - geology  vegetation Carrizo Plain, central CA

47. Transform Plate Boundary Features: –offset streams, objects Stream channel offset, Carrizo Plain, central CA 1906 earthquake offset, Point Reyes, CA

48. The Geography of Earthquakes USA: 1977-1997 earthquake events USA: every state except ND, FL

49. The Geography of Earthquakes Globally: primarily at plate boundaries Intraplate earthquakes do occur! Mag 6.5

50. Earthquakes Earthquakes are the shaking or vibration of the ground as a result of rocks suddenly breaking along a fault. Focus (hypocenter) = rupture point Epicenter = point on surface above focus Foreshocks Aftershocks

51. Process: the earthquake cycle (elastic rebound theory) Earthquakes are a ‘ release of energy ’ in the form of a seismic wave (vibrates the crust). Plate movement  strain builds rocks “ locked together ” (frictional bond) Rocks bend  hit limit --> rupture/break Cycle repeats  ” start-stop ” motion along fault

53. Seismic waves Some of the waves that are generated by an earthquake travel within the earth and other travel along the surface, creating surface waves. Waves traveling within the earth are known as body waves.

54. Surface Waves Surface waves cause the most damage to buildings during an earthquake. Surface waves can set up liquefaction in wet alluvium. This is where the most extensive damage to buildings occurs. –Liquefaction: wavelike, almost liquid, rolling of surface –Alluvium: fine material deposited by water over many years.

55. Measuring Earthquakes seismograph: records the vibrations of the crust Richter Scale measures vibration, not damage. seismogram: tracing record

56. Major California Earthquakes Fort Tejon, 1857 - 8.0 magnitude San Francisco, 1906 - 7.9 magnitude 1933 Long Beach - 6.3 magnitude Destroyed Glendale College Buildings! San Fernando, 1971 - 6.6 Northridge, 1994 - 6.7 Hector Mine, 1999 - 7.1

57. Fort Tejon, 1857 TIME: January 9, 1857 LOCATION: 35° 43' N, 120° 19' W about 72 km (45 miles) northeast of San Luis Obispo about 120 km (75 miles) northwest of Bakersfield, as shown on the map (epicenter location uncertain). MAGNITUDE: M w 8.3 (approx.) TYPE OF FAULTING: right-lateral strike-slipright-lateral strike-slip FAULT RUPTURED: San Andreas faultSan Andreas fault LENGTH OF SURFACE RUPTURE: about 360 km (225 miles) MAXIMUM SURFACE OFFSET: about 9 meters (30 feet)

58. San Francisco Aftermath, 1906 Magnitude: 7.9

59. San Francisco, 1906 Magnitude: 7.9