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Intro- The Ice Age in Utah The Ice Age in Utah The landscape and life in Utah during the most recent Ice Age in Utah 10,000 to 30,000 years ago. Lake  Bonneville glaciers Salt Lake City 18,000 years ago  .  in Utah
Ice Ages Throughout Geologic Time Average Global Temperature ( 0 C) Figure modified after C.R. Scotese PALEOMAP Project (www.scotese.com) Quaternary 12° 22° 17° Ice Age Ice Age Ice Age Ice Age
Last Glacial Maximum 18,000 years ago ,[object Object]
Milankovitch Cycles   Eccentricity 90,000 to 100,000 years Precession 19,000 to 23,000 years Obliquity (Axial Tilt)  41,000 years Figures modified after Matt Beedle, Montana Sate University. ~5% ~0%
Lake Bonneville and Ice Coverage in Utah During the Late Pleistocene ~18,000 years ago Lake Bonneville Uinta Mountains Wasatch Range
Lake Bonneville ~18,000 years ago Utah Salt Lake Delta
The Rise and Fall of Lake Bonneville Bonneville Level 18,000 years ago Gilbert Level 12,000 years ago Provo Level 17,000 years ago Stansbury Level 24,000 years ago Hydrograph of Lake Bonneville Great Salt Lake today
Stansbury Shoreline Red Rock Pass ~24,000 years ago Stansbury Island Ogden Delta Nephi Provo Salt Lake UT ID NV
Bonneville Shoreline ~18,000 years ago Point of the Mountain Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
Provo Shoreline ~17,000 years ago Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
Gilbert Shoreline ~12,000 years ago Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
Great Salt Lake Today Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
Shorelines of Lake Bonneville at Antelope Island Provo Stansbury Gilbert Bonneville Unnamed shoreline Unnamed shoreline
Bonneville Shoreline at Point of the Mountain Paragliders
Bonneville Shoreline at Point of the Mountain Bonneville Shoreline at the “U”
Stockton Bar, Utah Modern Barrier Bar and Spit Lake Bonneville Barrier Bar and Spit Kiawah Island, South Carolina
Lake Bonneville Spits Older spit Younger spit Contact surface
Lake Bonneville Deep-Water Sediments Laminations
Tufa on the Provo Shoreline Tufa on Quartzite
Lake Bonneville Delta Sediment Transport Direction
Provo Shoreline Wave-Cut Platform Wave Direction
Bonneville Salt Flats Provo Shoreline Bonneville Shoreline Salt
Modern Glaciers Alaska Devil’s Desk Glacier Halo Glacier, Cook Inlet
Holgate Glacier, Alaska
Glacial Cirques Uinta Mountains Convict Lake, Sierra Nevada Mountains Glacial Cirque Glacial Cirque
U-shaped Glacial Canyons Little Cottonwood Canyon Yosemite Valley Glacier National Park
Mill Creek Canyon “V-shaped”  Stream-  eroded canyon Little Cottonwood Canyon “U-shaped”  Glacier-  eroded canyon
Glacial Scenery at Alta, Utah U-shaped Valley Arêtes
Moraines   Chugach Mountains,   Alaska Image by Michael Collier Medial Moraine Image by Bruce Molnia, Terra Photographics
Glacial Features at Little Cottonwood Canyon Fault Scarps Trimline Moraines U-Shaped Valley
Bells Canyon, Utah Lateral Moraine Fault Scarp
Glacial Erratics Voyageurs National Park, Minnesota Denali National Park, Alaska Person
Little Cottonwood Canyon Glacial Erratics
Glacial Polish and Grooves Grooves and polish on bedrock Glacier National Park, Montana Striations
Life in Utah During the Ice Age
Life in Utah at the end of the Ice Age
Assorted Lake Bonneville Mollusks
Hunting for Gastropods (Snails)
Bonneville Cutthroat Trout Known Distribution Today are isolated in streams that once drained into Lake Bonneville.
Utah’s Giant Ice Age Birds Teratornis- “ giant condor” Teratornis  skeleton Endangered California Condor Teratornis  skull
Ice Age Land Bridges and Mammal Migrations
Ice Age Elephants Mammoth  Mastodon Detail from Joseph S. Venus mural, College of Eastern Utah (CEU) Prehistoric Museum, Price, Utah The Huntington Mammoth   ( Mammathus columbi ) skeleton at the CEU Prehistoric Museum
Mammoth & Elephants vs. Mastodons Columbian Mammoth ( M. columbi ) American Mastodon ( Mammut americanum ) Elephants and mammoths have high skulls, while mastodons have low skulls. Elephants and mammoths have low, highly enfolded teeth for grazing, while mastodons have high crested teeth for browsing leaves . Elephants and mammoths are tall, while mastodons are shorter with more massive bodies .
Saber-toothed Cat Skeletal reconstruction and detail from Joseph S. Venus mural, CEU Prehistoric Museum, Price, Utah Smilodon   fatalis
Giant Ground Sloth Skeletal reconstruction and detail from Joseph S. Venus mural, CEU Prehistoric Museum, Price, Utah
Other Extinct Ice Age Mammals Extinct Musk Ox Extinct Long-Horned Bison Camels, together with native horses, went extinct in North America at the end of the Ice Age
Mountain mammals that lived in Ice Age Lowlands The   American pika,  Ochotona princeps ,  The wolverine,  Gulo gulo
Power Point Presentation  (list of slides) ,[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object],[object Object]

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The Iceage in Utah

  • 1. Intro- The Ice Age in Utah The Ice Age in Utah The landscape and life in Utah during the most recent Ice Age in Utah 10,000 to 30,000 years ago. Lake Bonneville glaciers Salt Lake City 18,000 years ago . in Utah
  • 2. Ice Ages Throughout Geologic Time Average Global Temperature ( 0 C) Figure modified after C.R. Scotese PALEOMAP Project (www.scotese.com) Quaternary 12° 22° 17° Ice Age Ice Age Ice Age Ice Age
  • 3.
  • 4. Milankovitch Cycles Eccentricity 90,000 to 100,000 years Precession 19,000 to 23,000 years Obliquity (Axial Tilt) 41,000 years Figures modified after Matt Beedle, Montana Sate University. ~5% ~0%
  • 5. Lake Bonneville and Ice Coverage in Utah During the Late Pleistocene ~18,000 years ago Lake Bonneville Uinta Mountains Wasatch Range
  • 6. Lake Bonneville ~18,000 years ago Utah Salt Lake Delta
  • 7. The Rise and Fall of Lake Bonneville Bonneville Level 18,000 years ago Gilbert Level 12,000 years ago Provo Level 17,000 years ago Stansbury Level 24,000 years ago Hydrograph of Lake Bonneville Great Salt Lake today
  • 8. Stansbury Shoreline Red Rock Pass ~24,000 years ago Stansbury Island Ogden Delta Nephi Provo Salt Lake UT ID NV
  • 9. Bonneville Shoreline ~18,000 years ago Point of the Mountain Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
  • 10. Provo Shoreline ~17,000 years ago Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
  • 11. Gilbert Shoreline ~12,000 years ago Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
  • 12. Great Salt Lake Today Ogden Delta Nephi Provo Salt Lake UT ID NV Red Rock Pass
  • 13. Shorelines of Lake Bonneville at Antelope Island Provo Stansbury Gilbert Bonneville Unnamed shoreline Unnamed shoreline
  • 14. Bonneville Shoreline at Point of the Mountain Paragliders
  • 15. Bonneville Shoreline at Point of the Mountain Bonneville Shoreline at the “U”
  • 16. Stockton Bar, Utah Modern Barrier Bar and Spit Lake Bonneville Barrier Bar and Spit Kiawah Island, South Carolina
  • 17. Lake Bonneville Spits Older spit Younger spit Contact surface
  • 18. Lake Bonneville Deep-Water Sediments Laminations
  • 19. Tufa on the Provo Shoreline Tufa on Quartzite
  • 20. Lake Bonneville Delta Sediment Transport Direction
  • 21. Provo Shoreline Wave-Cut Platform Wave Direction
  • 22. Bonneville Salt Flats Provo Shoreline Bonneville Shoreline Salt
  • 23. Modern Glaciers Alaska Devil’s Desk Glacier Halo Glacier, Cook Inlet
  • 25. Glacial Cirques Uinta Mountains Convict Lake, Sierra Nevada Mountains Glacial Cirque Glacial Cirque
  • 26. U-shaped Glacial Canyons Little Cottonwood Canyon Yosemite Valley Glacier National Park
  • 27. Mill Creek Canyon “V-shaped” Stream- eroded canyon Little Cottonwood Canyon “U-shaped” Glacier- eroded canyon
  • 28. Glacial Scenery at Alta, Utah U-shaped Valley Arêtes
  • 29. Moraines Chugach Mountains, Alaska Image by Michael Collier Medial Moraine Image by Bruce Molnia, Terra Photographics
  • 30. Glacial Features at Little Cottonwood Canyon Fault Scarps Trimline Moraines U-Shaped Valley
  • 31. Bells Canyon, Utah Lateral Moraine Fault Scarp
  • 32. Glacial Erratics Voyageurs National Park, Minnesota Denali National Park, Alaska Person
  • 33. Little Cottonwood Canyon Glacial Erratics
  • 34. Glacial Polish and Grooves Grooves and polish on bedrock Glacier National Park, Montana Striations
  • 35. Life in Utah During the Ice Age
  • 36. Life in Utah at the end of the Ice Age
  • 39. Bonneville Cutthroat Trout Known Distribution Today are isolated in streams that once drained into Lake Bonneville.
  • 40. Utah’s Giant Ice Age Birds Teratornis- “ giant condor” Teratornis skeleton Endangered California Condor Teratornis skull
  • 41. Ice Age Land Bridges and Mammal Migrations
  • 42. Ice Age Elephants Mammoth Mastodon Detail from Joseph S. Venus mural, College of Eastern Utah (CEU) Prehistoric Museum, Price, Utah The Huntington Mammoth ( Mammathus columbi ) skeleton at the CEU Prehistoric Museum
  • 43. Mammoth & Elephants vs. Mastodons Columbian Mammoth ( M. columbi ) American Mastodon ( Mammut americanum ) Elephants and mammoths have high skulls, while mastodons have low skulls. Elephants and mammoths have low, highly enfolded teeth for grazing, while mastodons have high crested teeth for browsing leaves . Elephants and mammoths are tall, while mastodons are shorter with more massive bodies .
  • 44. Saber-toothed Cat Skeletal reconstruction and detail from Joseph S. Venus mural, CEU Prehistoric Museum, Price, Utah Smilodon fatalis
  • 45. Giant Ground Sloth Skeletal reconstruction and detail from Joseph S. Venus mural, CEU Prehistoric Museum, Price, Utah
  • 46. Other Extinct Ice Age Mammals Extinct Musk Ox Extinct Long-Horned Bison Camels, together with native horses, went extinct in North America at the end of the Ice Age
  • 47. Mountain mammals that lived in Ice Age Lowlands The American pika, Ochotona princeps , The wolverine, Gulo gulo
  • 48.

Editor's Notes

  1. During the most recent Ice Age in Utah, glaciers blanketed the mountains and Lake Bonneville covered most of Utah’s western valleys. Habitats suitable for mammoths, mastodons, camels, horses, muskoxen, long-horned bison, and saber-toothed cats, were restricted to the margins of Lake Bonneville and the periphery of mountain glaciers. Climate effects during the Ice Age became drastic by the end of the Pleistocene. There was a net loss of plant and animal diversity and ultimately mastodons, mammoths, camels, horses, ground sloths, and many other species became extinct. The extinction of these Pleistocene animals is not well understood. Two main theories are the “Pleistocene Overkill Theory”, which states that large animals were killed off by early humans, and the “Climate Theory” which holds that large animals failed to adjust to rapid climate changes.