2. ORIGIN OF MOUNTAINS Orogeny = process of mountain building, takes tens of millions of years; usually produces long linear structures, known as orogenic belts Two main processes: –Deformation: continental collisions, resulting in folding and thrust-faulting –Volcanic Activity Other processes: –Metamorphism, intrusions: batholiths, etc.

3. Mountain orogeny Geog 1011 Landscape and water, fall 2005

4. Clues for mountain formation

5. …more clues: marine fossils on top of Everest N side, view from Rongbuk Monastery, Tibet Granite core sedimentary rock layer Limestone (top) Material composition clue for plate tectonics

6. Three types of plate boundary

7. TYPES OF MOUNTAINS (according to their origin) Fault-block: tension, normal faulting Folded: compression, reverse faulting Volcanic: Shield and composite Complex: mixture of most of the above

8. HANGING WALL 1. Fault-block mountains large areas widely broken up by faults Force: TENSION Footwall moves up relative to hanging wall Normal fault

9. Tilted fault-block range: Sierra Nevada from east, Steep side of block fault; Ansel Adams photo

10. Tilted Fault-block Sierra Nevada from west Side, low angle Yosemite valley the result Of glaciation on low-angle relief Central cores consists of intrusive igneous rocks (granite). Half Dome is a core (batholit) that was exposed by erosion, Batholith

11. Wasatch Range From Salt Lake City Typically fault- Block system

12. Grand Tetons: another fault-block system

13. Alternating normal faults lead to a characteristic pattern called a “horst and graben” system. An area under tension will often have multiple mountain ranges as a result. Horst and graben

14. Horst and Graben Landscapes Figure 12.14

15. tilted fault-block mountains in Nevada result of a horst and graben system Nevada is under tension because of rising magma which is unzipping the system, all the way from Baja California Sierra Nevada and Wasatch Ranges part of this system Basin and Range province :

16. Reverse fault Force: COMPRESSION Hanging wall moves up relative to footwall Two types: -low angle -high angle Individual layers can move 100’s of kilometers Alps are a great example

17. Flatirons Classic example of high-angle reverse faults -> Form “Sawtooth Mtns” due to differential erosion Seal rock

18. Thrust faults main cause of folded mountains 3. Folded mountains “nappe” (fr.) = table cloth Where rock does not fault it folds, either symmetrically or asymmetrically. upfolds:anticlines downfolds: synclines

19. Classic folded terrain: well-developed anticline

20. Appalachian Mountains of the US

21. Atlas Mountains, Northern Africa

22. Zagros Crush Zone Alternating Anticlines and Synclines

23. White Cloud peak SAWTOOTH RANGE, IDAHO Alice Lake

24. 3. Volcanic mountains 2 types of volcanoes: Shield volcanoes: – gentle-sloping –basaltic lava flows –associated with hot spots Composite volcanoes: –steep –andesitic composition –explosive –occur at subduction zones

25. Shield volcanoes -Compressive forces -Basaltic composition At hot spots

26. Mauna Kea Shield volcano Hot Spot Basalt Mauna Loa in Background Kilaeua is Behind Mauna Loa

27. Composite volcanoes -andesitic composition -steep cones, explosive at subduction zones

28. Mt Rainier: example of composite volcano

29. Guagua Pichincha, Ecuador Quito in foreground Composite volcanoes explosive

30. Why do shield and composite volcanoes differ in composition? Basaltic magmas rise along fractures through the basaltic layer. Due to the absence of granitic crustal layer, magmas are not changed in composition and they form basaltic volcanoes. Mountainous belts have thick roots of granite rock. Magmas rise slowly or intermittently along fractures in the crust; during passage through the granite layer, magmas are commonly modified or changed in composition and erupt on the surface to form volcanoes constructed of nonbasaltic (andesitic) rocks.

31. continental-continental collision tend to have a little of everything: volcanoes,folds, thrust faults, normal faults 4. Complex Mountains

32. ALPS HIMALAYAS View of Everest and Khumbu ice fall from Kala Patar, Nepal Himalayas

33. ANDES: classic example of orogenic belt “cordillera” NASA satellite image View from Nev. Pisco, Cordillera Blanca

34. ANDES: CLASSIC EXAMPLE OF GENERIC MTNS

35. A)Compression causes expansion B)Layered rock formed C)Thrust-faulting D)Igneous intrusions: Plutons E)Underplating F)Regional metamorphism Nazca Plate South American Plate

36. ANATOMY OF AN OROGENIC BELT

37. Summary Orogeny = mountain building Plate tectonics used to explain mountain building Plate collisions: oceanic-oceanic, oceanic-continental, continental-continental Forces: tension, compression, shear Mountain types: faulted, folded, volcanic, complex Examples of each