Geologic Tours Of Northern Utah
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Geology of Millard County, Utah
Author | : Lehi F. Hintze |
Publisher | : Utah Geological Survey |
Total Pages | : 324 |
Release | : 2003 |
Genre | : Science |
ISBN | : 1557916926 |
This bulletin serves not only to introduce the non-geologist to the rich geology of Millard County, but also to provide professional geologists with technical information on the stratigraphy, paleontology, and structural geology of the county. Millard County is unique among Utah’s counties in that it contains an exceptionally complete billion-year geologic record. This happened because until about 200 million years ago the area of present-day Millard County lay near sea level and was awash in shallow marine waters on a continental shelf upon which a stack of fossil-bearing strata more than 6 miles (10 km) thick slowly accumulated. This bulletin summarizes what is known about these strata, as well as younger rocks and surficial deposits in the county, and provides references to scientific papers that describe them in greater detail. Mountains North 30 x 60 (1:100,000-scale) quadrangles. These companion maps and this bulletin portray the geology of Millard County more completely and accurately than any previously published work.
Windows into the Earth
Author | : Robert B. Smith |
Publisher | : Oxford University Press |
Total Pages | : 255 |
Release | : 2000-05-25 |
Genre | : Science |
ISBN | : 0195355601 |
Millions of years ago, the North American continent was dragged over the world's largest continental hotspot, a huge column of hot and molten rock rising from the Earth's interior that traced a 50-mile wide, 500-mile-long path northeastward across Idaho. Generating cataclysmic volcanic eruptions and large earthquakes, the hotspot helped lift the Yellowstone Plateau to more than 7,000 feet and pushed the northern Rockies to new heights, forming unusually large glaciers to carve the landscape. It also created the jewel of the U.S. national park system: Yellowstone. Meanwhile, forces stretching apart the western U.S. created the mountainous glory of Grand Teton National Park. These two parks, with their majestic mountains, dazzling geysers, and picturesque hot springs, are windows into the Earth's interior, revealing the violent power of the dynamic processes within. Smith and Siegel offer expert guidance through this awe-inspiring terrain, bringing to life the grandeur of these geologic phenomena as they reveal the forces that have shaped--and continue to shape--the greater Yellowstone-Teton region. Over seventy illustrations--including fifty-two in full color--illuminate the breathtaking beauty of the landscape, while two final chapters provide driving tours of the parks to help visitors enjoy and understand the regions wonders. Fascinating and informative, this book affords us a striking new perspective on Earth's creative forces.
Geologic Field-trip Guide to the Volcanic and Hydrothermal Landscape of the Yellowstone Plateau
Author | : Lisa A. Morgan |
Publisher | : Government Printing Office |
Total Pages | : 116 |
Release | : 2017 |
Genre | : Calderas |
ISBN | : 9781411342040 |
Vertebrate Paleontology in Utah
Author | : David D. Gillette |
Publisher | : Utah Geological Survey |
Total Pages | : 568 |
Release | : 1999 |
Genre | : Nature |
ISBN | : 1557916349 |
The 52 papers in this vary in content from summaries or state-of-knowledge treatments, to detailed contributions that describe new species. Although the distinction is subtle, the title (Vertebrate Paleontology in Utah) indicates the science of paleontology in the state of Utah, rather than the even more ambitious intent if it were given the title “Vertebrate Paleontology of Utah” which would promise an encyclopedic treatment of the subject. The science of vertebrate paleontology in Utah is robust and intense. It has grown prodigiously in the past decade, and promises to continue to grow indefinitely. This research benefits everyone in the state, through Utah’s muse ums and educational institutions, which are the direct beneficiaries.
Rainbow of Rocks
Author | : Marjorie A. Chan |
Publisher | : Utah Geological Survey |
Total Pages | : 20 |
Release | : 2002-10 |
Genre | : Science |
ISBN | : 1557916810 |
Sunrise illuminates Colorado Plateau’s canyon country. In the early morning light, cliffs radiate a rich red glow, and a sculptured panorama of sandstone is revealed in a rich palette of crimson, vermilion, orange, salmon, peach, pink, gold, yellow, and white. Nearby are black, spherical rock marbles (iron concretions) collecting in small depressions, like puddles of ball bearings. These natural spherical balls have been called various names such as iron nodules, iron sandstone balls, or moki marbles. However, we use the name “iron concretion” to describe both the composition (iron oxide that is the dark mineral which cements the sandstone grains) and the formed shape (concretion). What paints the sandstone such rich colors? Why is red a dominant color? Where do the black marbles come from? How did the black marbles form? Is there a relationship between sandstone colors and the marbles? This booklet explores the answers to these questions and poses other questions yet unanswered.
SP026: Traveling America's loneliest road: A geologic and natural history tour through Nevada along U.S. Highway 50, with GPS coordinates
Author | : Kris Ann Pizarro |
Publisher | : NV Bureau of Mines & Geology |
Total Pages | : 137 |
Release | : 2010 |
Genre | : Geology |
ISBN | : 1888035145 |
Neotectonics of Bear Lake Valley, Utah and Idaho
Author | : James McCalpin |
Publisher | : Utah Geological Survey |
Total Pages | : 49 |
Release | : 2003-01-20 |
Genre | : Science |
ISBN | : 1557916942 |
This report presents the results of a preliminary evaluation of the East Bear Lake (EBF) and West Bear Lake (WBF) fault zones, which bound the east and west sides, respectively, of the Bear Lake Valley. The Bear Lake Valley straddles the Utah/Idaho border northeast of Logan, Utah. The results of this study show that both the EBF and the WBF have experienced surface-faulting earthquakes in the recent geologic past and therefore represent an ongoing seismic hazard to northeastern Utah and southeastern Idaho.