1. Landforms Geography Glaciers

2. Development of a Glacier Glacier – slowly moving mass of dense ice formed by gradual thickening, compaction, and refreezing of snow & water over time After summer melt, some snow left over With weight and partial melting, snow turns to Firn, crunchy transition from snow to ice Further compaction, ice crystals align, become dense glacial ice which flows slowly downslope At least 40-m thick to become glacier

3. Glacial Mass Budget Glacial input : Snow Glacial output : ice, meltwater or water vapor Zone of Accumulation – top of glacier where temps are cooler - input > output Zone of Ablation – lower part of glacier where temps are higher – output > input Equilibrium line – point on glacier where input = output

4. Glacial Formation

5. Glacial Mass Budget

7. Glacial Movement Glaciers move through internal deformation Interior of glacier like malleable plastic

8. Glacial Movement

9. Glacier Types Mountain Glaciers –Ice Cap – Continuous sheet of ice covering entire landscape –Ice Field – Buries all but tallest mountains – can be very thick –Alpine Glacier – Flows down valleys away from high country –Cirque - Bowl-shaped depression on mountain flank due to glacial erosion – snow source

11. Alaskan Glaciers Hubbard Glacier

12. Continental Glaciers Huge ice masses covering a large part of a continent or large island – also called ice sheets More than 3000 m deep in places Covers most of Antarctica and Greenland Weight of ice presses lithosphere down into asthenosphere, called isostatic depression

13. Continental Glaciers

14. Glacial Landforms Rock & debris picked up by glaciers, transported in direction of movement & deposited Glacial erosion: –Glacial Abrasion – scratch and gouge bedrock –Glacial Striations – caused by glacial abrasion –Glacial Grooves – deep striations –Glacial Plucking – boulders ripped from ground by glacier – deposited by retreating glacier, called Glacial Erratics

15. Glacial Erosional Landforms Roche Moutonnée – rounded hill, gradual on side toward direction from which glacier comes Glacial Striations Glacial Erratic

16. Alpine Erosional Landforms Glacial Erosion: –Cirque – bowl-like feature on mountain flanks –Tarn – small lake in bottom of cirque –Arête – narrow, steep ridges between cirques –Horn – mountain with 3 or more arêtes at summit –Glacial Trough – u-shape valley eroded by glacier –Hanging Valley – side trough above main trough – possible waterfall

17. Alpine Erosional Landforms Cirque Horn “Matterhorn” Glacial Trough

18. Glacial Depositional Landforms (Till) Glacial Till – sediment directly deposited by glacier – many particle sizes Moraine – winding ridge formed by till at the front or side of glacier – Moraine types: –Lateral – along former edges of glacier –Terminal – along front of former glacier –Recessional – formed as glacier recedes –Medial – between 2 glaciers –Ground – irregular deposition as glacier recedes

19. Glacial Depositional Landforms (Till)

20. Glacial Depositional Landforms (outwash) Glacial Outwash – sediments deposited by water out & under a glacier as it melts – forms Outwash Plain, flat feature in front of former glacier Kame – large mound deposited near glacier front Esker – winding ridge from water flowing in tunnel through ice under glacier Kettle Lake – big ice block fallen off glacier front is buried by outwash, melts later forming lake

21. Glacial Depositional Landforms

23. Physical Geography Arid Landscapes and Eolian Processes

24. Arid Landscapes & Eolian Processes Arid Landscapes Eolian Erosion & Transportation Eolian Deposition & Landforms Human Interactions with Eolian Processes

25. Arid Landscapes 3 factors influence arid climates: –Subtropical high pressure –Rainshadow –Distance from large bodies of water

26. Desert Geomorphology Water important to landforms in arid regions – little vegetation to slow intermittent erosion Arroyo – steep-sided gully cut into alluvium In undisturbed, horiz. rock layers more resistant sandstone or limestone forms flat caprock above easily eroded shale Result is landforms flat on top w/steep sides: -Plateau-Canyon -Butte-Mesa -Pinnacle-Playa

27. Arroyo

28. Desert Landforms Note: Tops of most landforms once part of same surface, since partially eroded away

29. Playa

30. Eolian Erosion and Transport Wind-based processes important in deserts b/c: –Strong winds common in desert –Large supply of sand & silt to be blown –Vegetation minimal – wind free to erode

31. Fluid Behavior of Wind Wind acts like a fluid, like water, but less dense Faster wind can move larger particles Threshold Velocity for wind to carry different sized particles

32. Particle Transport Silts and Clays carried in suspension Sand bounces along – saltation, or Sand rolls slowly along – creep

33. Eolian Erosional Landforms 2 types of wind erosion: –Deflation – wind blows loose soil away: leaves coarser pebbles & cobbles, called Desert Pavement when deflation causes basin to form, called Deflation Hollow

34. Eolian Erosional Landforms Abrasion – wind blows sand along a surface to polish & abrade it Ventifacts – rocks shaped by abrasion: pitted, grooved, polished Yardangs – elongated, wind-sculpted ridges caused by abrasion

35. Eolian Erosional Landforms Deflation/Desert Pavement

36. Eolian Erosional Landforms Abrasion VentifactsYardangs

37. Loess Fine-grained, wind-blown silt – high in calcium – usually from alluvial deposits or glacial till Can be transported farther than sand

38. Loess Deposits around the World Loess Deposits Arid Landscapes and Eolian Processes

39. Loess Terraces

40. Human Impact/Desertification Desertification – transforming a vegetated landscape to one that is barren & susceptible to wind erosion Population pressure has forced more people to clear marginal, semi-arid-to-arid land for agriculture & firewood In wind, cleared land loses topsoil and nutrients Vegetation unlikely to reestablish

41. Regions Prone to Desertification

42. Desertification in African Sahel Semi-arid region in transition region from Sahara Desert in north to rainforest in south Traditionally nomadic herders & small, sedentary farmers – north-south migrations to follow rain Into 20 th century, European borders & resource exploitation made people more sedentary – over- cultivation of soil, overgrazing, and tree removal Add in extended drought since late 1960s, & you have desertification

43. The Sahel

44. Desertification in Great Plains Great Plains lie east of Rocky Mts in semi-arid climate with short grass as dominant natural vegetation Dust Bowl Region

45. Early 1900s Americans moved to region to farm, plowing and clearing native grasses – unusually wet period 1930s – terrible drought hits – topsoil blows into dust storms – called “Dust Bowl” Many migrated to California & elsewhere Those who stayed have employed irrigation & soil conservation, including windbreaks, and conservation tillage Desertification in Great Plains