1. The document discusses the landscape and life in Utah during the last Ice Age between 10,000 to 30,000 years ago when large glaciers and Lake Bonneville covered much of the state.
2. Lake Bonneville was a prehistoric lake that existed in the Great Basin during the last ice age. At its largest extent, it covered much of northern and central Utah and small parts of Nevada and Idaho.
3. The landscape was shaped by glacial features such as cirques, moraines, and U-shaped valleys carved by the large glaciers. Glacial erratics and polish on rock surfaces provide evidence of past glacial activity.
THE OBSTACLES THAT IMPEDE THE DEVELOPMENT OF BRAZIL IN THE CONTEMPORARY ERA A...
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
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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
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
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
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Editor's Notes
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.