Relevant bibliographies by topics / Petroglyphs – South Central Idaho

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  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Petroglyphs – South Central Idaho'

Author: Grafiati
Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Petroglyphs – South Central Idaho"

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Lewis, Reed S., and Thor H. Kiilsgaard. "Eocene plutonic rocks in south central Idaho." Journal of Geophysical Research: Solid Earth 96, B8 (1991): 13295–311. http://dx.doi.org/10.1029/91jb00601.

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Pfister, James A., Daniel Cook, and Dale R. Gardner. "Cattle Grazing Toxic Delphinium andersonii in South-Central Idaho." Rangeland Ecology & Management 64, no. 6 (2011): 664–68. http://dx.doi.org/10.2111/rem-d-11-00001.1.

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Kudinova, Maria A. "An Overview of Rock Art Sites in Gansu Province, China." Oriental Studies 20, no. 4 (2021): 23–36. http://dx.doi.org/10.25205/1818-7919-2021-20-4-23-36.

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The paper presents a brief overview of rock art sites known to date on the territory of Gansu Province in north-western China. Petroglyphs have been discovered in all parts of the province, most of them concentrate in the north-western and central parts of the region. Over the past decades, a significant number of rock art sites has been found in the eastern and south-eastern parts of Gansu, but many materials from this territory have not yet been published or were published in hard-to-get local periodicals, quite often without any illustrations. The purpose of this article is to fill the lacu
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Bayarsaikhan, J. "Fish depictions in the deer stones." Turkic Studies Journal 3, no. 2 (2021): 44–53. http://dx.doi.org/10.32523/2664-5157-2021-2-44-53.

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The autochthonous community of Central Asia, including Mongolia, is based on a nomadic culture, the origins of which go back to the paleoculture, the Bronze Age. The article is devoted to the topic of Central Asia - study drawings, petroglyphs in the Late Bronze Age. On the deer stones, petroglyphs, logograms depicting heavenly bodies (sun, moon), hunting and labor tools, wild and domestic animals, fish, as well as the so-called «pair fish» of which were found during archaeological work in Mongolia, South Siberia, Central Asia. The article notes that in the depicted figures, logos reflected th
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Dungan, Robert S., Daniel D. Snow, and David L. Bjorneberg. "Occurrence of Antibiotics in an Agricultural Watershed in South-Central Idaho." Journal of Environmental Quality 46, no. 6 (2017): 1455–61. http://dx.doi.org/10.2134/jeq2017.06.0229.

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Rickart, Eric A., Obedh E. Ornelas, Douglas J. Merkler, and Lois F. Alexander. "Small Mammal Activity in South-Central Idaho during the 2017 Solar Eclipse." Western North American Naturalist 80, no. 1 (2020): 76. http://dx.doi.org/10.3398/064.080.0109.

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Cluer, Brian L. "Storage Basin Volume and Drainage Basin Dynamics: Camas Prairie, South-Central Idaho." Ground Water 27, no. 3 (1989): 323–32. http://dx.doi.org/10.1111/j.1745-6584.1989.tb00456.x.

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Clark, G. M., and D. S. Ott. "SPRINGFLOW EFFECTS ON CHEMICAL LOADS IN THE SNAKE RWER, SOUTH-CENTRAL IDAHO." Journal of the American Water Resources Association 32, no. 3 (1996): 553–63. http://dx.doi.org/10.1111/j.1752-1688.1996.tb04053.x.

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Constantopoulos, James. "Fluid inclusions and rare earth element geochemistry of fluorite from south-central Idaho." Economic Geology 83, no. 3 (1988): 626–36. http://dx.doi.org/10.2113/gsecongeo.83.3.626.

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Hasselblad, Kristin, and Marc Bechard. "Male Northern Goshawk Home Ranges in the Great Basin of South-central Idaho." Journal of Raptor Research 41, no. 2 (2007): 150–55. http://dx.doi.org/10.3356/0892-1016(2007)41[150:mnghri]2.0.co;2.

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Dissertations / Theses on the topic "Petroglyphs – South Central Idaho"

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Hambelton, Karla Lucille. "Scratched Petroglyphs in the Bennett Hills, Idaho." PDXScholar, 2011. https://pdxscholar.library.pdx.edu/open_access_etds/329.

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This study examines rock art sites containing scratched petroglyphs in the Bennett Hills, Idaho. Despite their research potential, scratched petroglyphs have received little attention in rock art research or literature. This study contributes valuable data to scratched rock art research and the corpus of rock art research in general. Two samples of ten scratched petroglyph sites were examined and recorded for a total of twenty petroglyph sites. Using formal and contextual research methods, multiple attributes of scratched petroglyphs are identified and analyzed. The formal qualities of scratch
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Silverberg, David Scott. "The tectonic evolution of the pioneer metamorphic core complex, south-central Idaho." Thesis, Massachusetts Institute of Technology, 1990. http://hdl.handle.net/1721.1/17274.

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Staley, Joshua. "A business plan for a 600-acre farm & 300-head commercial cow herd in south central Idaho." Thesis, Kansas State University, 2010. http://hdl.handle.net/2097/7033.

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Master of Agribusiness<br>Department of Agricultural Economics<br>Michael R. Langemeier<br>This thesis was written for the purpose of looking at the feasibility of operating a prospective business; a farm and ranch in southern Idaho. For practical reasons, I looked at a specific farm consisting of 600 irrigated acres, which are irrigated via 5 center pivots. Attached to the farm is an additional 400 acres of pasture ground seeded to crested wheat. In conjunction with operating the farm, I examined the feasibility of leasing a 300 head commercial cow herd from a separate owner than the land
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Knott, Thomas Ryan. "Mid-Miocene explosive super-eruptions from the Yellowstone hotspot track : the rhyolitic ignimbrite record in south central Snake River Plain, Idaho, USA." Thesis, University of Leicester, 2014. http://hdl.handle.net/2381/37920.

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Explosive super-eruptions (≥450 km³) are amongst the most catastrophic events at the Earth's surface, with immediate and devastating regional environmental consequences. Recent catastrophic super-eruptions at Yellowstone are well-known, but the previous (Miocene) history of large explosive eruptions from the Yellowstone hotspot is less-well understood, even though some in the central Snake River Plain (cSRP) may have been similar in size, or larger. To test this, local successions of rhyolitic welded ignimbrites in the southern cSRP have been studied to distinguish and characterise individual
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Books on the topic "Petroglyphs – South Central Idaho"

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Wallace, Henry D. Petroglyphs of the Picacho Mountains, South Central, Arizona. Institute for American Research, 1986.

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2

Young, H. W. Hydrology of the Oakley Fan area, South-Central Idaho. Dept. of the Interior, U.S. Geological Survey, 1989.

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Ruth, Gruhn. New excavations at Wilson Butte Cave, South-Central Idaho. Idaho Museum of Natural History, 2006.

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Young, H. W. Hydrology of the Oakley Fan area, South-Central Idaho. Dept. of the Interior, U.S. Geological Survey, 1989.

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Young, H. W. Hydrology of the Oakley Fan area, South-Central Idaho. Dept. of the Interior, U.S. Geological Survey, 1989.

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6

Maley, Terry S. Rocks and potholes of the Big Wood River, south-central Idaho. Idaho Geological Survey, University of Idaho, 1994.

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Hurlow, Hugh A. Geology and ground-water chemistry, Curlew Valley, Northwestern Utah and South-Central Idaho, implications for hydrogeology. Utah Geological Survey, 2008.

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Arkush, Brooke S. The archaeology of Trapper Cliff Shelter: A late Holocene residential site in Cassia County, South Central Idaho. United States Department of Agriculture, Forest Service, Intermountain Region, Sawtooth National Forest, 2013.

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Imágenes a través del tiempo: Arte rupestre y construcción social del paisaje en la meseta central de Santa Cruz. Sociedad Argentina de Antropología, 2009.

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Maria, Olivieri Luca, Bruneau Laurianne, Ferrandi Marco, Fondation Carlo Leone et Mariena Montandon, and Istituto italiano per l'Africa e l'Oriente, eds. Pictures in transformation: Rock art research between central Asia and the subcontinent : thematic symposium (special sessions) XIX International Conference on South Asian Archaeology, Ravenna, 6 July 2007. Archaeopress, 2010.

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Book chapters on the topic "Petroglyphs – South Central Idaho"

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Link, Paul K., and Mary K. V. Hodges. "The Neogene drainage history of south-central Idaho." In Geologic Field Trips to the Basin and Range, Rocky Mountains, Snake River Plain, and Terranes of the U.S. Cordillera. Geological Society of America, 2011. http://dx.doi.org/10.1130/2011.0021(05).

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Alexander, Earl B., Roger G. Coleman, Todd Keeler-Wolfe, and Susan P. Harrison. "Blue Mountains, Domain 6." In Serpentine Geoecology of Western North America. Oxford University Press, 2007. http://dx.doi.org/10.1093/oso/9780195165081.003.0024.

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The Blue Mountains domain is mostly in northeastern Oregon. It is the name that we and others (Orr and Orr 1996) have adopted for the Central Highlands subprovince of the Columbia Intermountain province (Freeman et al. 1945). Small areas of Blue Mountains ultramafic rocks are exposed in an arcuate trend from central Oregon through northeastern Oregon into western Idaho. They are in the Baker and Wallowa terranes (Vallier and Brooks 1995). These terranes with the ultramafic rocks are covered or surrounded by Tertiary volcanic flows, largely Columbia River basalt. The ultramafic rocks are exposed in the Canyon Mountain and Sparta complexes and in smaller areas from the edge of the Idaho Batholith near Riggins in Idaho south–southwest across northeastern Oregon to the Aldrich Mountains south of Dayville. The Snake River has cut a deep gorge through the Blue Mountains domain. At Hells Canyon it is &gt;2000 m deep. Strawberry Mountain southeast of John Day rises to 2755 m. Ultramafic rocks are exposed from about 975 m at the foot of the Strawberry Range, near Canyon City, to 2243 m on Baldy Mountain in the Strawberry Range and a bit higher on Vinegar Hill, which is about 45 km northeast of the Strawberry Range, although the summit of Vinegar Hill (2478 m above sea level) is not composed of ultramafic rocks. Summers are hot and dry and winters are cold, with snow that persists through winters at the higher elevations. Mean annual temperatures are mostly in the 3°C–9oC range, and mean annual precipitation ranges from 25 to 100 cm. The frost-free period is about 150 days at lower elevations and &lt;60 days at higher elevations. The ultramafic rocks were exposed by late Tertiary uplift and erosion of the overlying volcanic sequence. The older rocks are composed of a volcanic island arc complex that contains marine sediments interlayered with mafic volcanic flows. Deep erosion of this area has exposed the roots of the volcanic arc. The roots contain gabbro and peridotite–serpentine at their lowest levels. Seven-thousand-year-old volcanic ash from Mt.
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"Cutthroat Trout: Evolutionary Biology and Taxonomy." In Cutthroat Trout: Evolutionary Biology and Taxonomy, edited by Paul K. Link and Ernest R. Keeley. American Fisheries Society, 2018. http://dx.doi.org/10.47886/9781934874509.ch3.

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&lt;em&gt;Abstract&lt;/em&gt;.—In the past 17 million years (myr), the topography and drainage systems of the northwestern United States were drastically modified by the Yellowstone–Snake River Plain (YSRP) hotspot and associated east–west extension of the Basin and Range Province. These geologic changes influenced distribution and diversification of Cutthroat Trout &lt;em&gt;Oncorhynchus clarkii&lt;/em&gt; and allowed connections between Snake River, Colorado River, and Great Basin fish populations beginning in the late Miocene. Studies of detrital zircon grains in Miocene to Holocene fluvial sands of the Snake River document the eastward migration of the regional drainage divide from central Idaho to northwestern Wyoming. This migration was concomitant with the southwest migration of the North American tectonic plate over the YSRP hotspot. In the late Miocene and Pliocene, since 10 million years before present (Ma), the Chalk Hills and Glenns Ferry lake systems formed on the western Snake River Plain and were hosts to diverse fish fauna. The modern Snake River formed after 3 Ma with the cutting of Hells Canyon and integration of the Snake and Columbia River drainage. In the Great Basin south of the Snake River watershed, Lake Lahontan has a history that goes back to the Miocene. Connections between the western Snake River Plain and the Great Basin were recurrent over the past 10 myr. In southeastern Idaho, the Bear River has had a complex drainage interaction with the Snake River and Bonneville watersheds. Lake Bonneville, in northern Utah, grew during Pleistocene glacial climate regimes. The modern Bear River connection to Lake Bonneville was initiated about 50,000 years before the present. The integration of the Green River with the Colorado River occurred in the late Miocene, developing after breaking of Eocene connections between the Green River and streams draining to the Atlantic Ocean. In sum, geological constraints are compatible with patterns of fish fossils and genetic linkages and identify mechanisms of colonization and isolation of fish populations that have resulted in regional diversification of Cutthroat Trout.
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Fernández, James D. "Between Empires: Spanish Immigrants in the United States (1868–1945)." In Transatlantic Studies. Liverpool University Press, 2019. http://dx.doi.org/10.3828/liverpool/9781789620252.003.0020.

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In the late nineteenth and early twentieth centuries, tens of thousands of Spanish peasants, seamen, and workers emigrated to the United States, and settled in an archipelago of tight-knit enclaves that dotted the entire country from Barre, Vermont to Monterey, California, and from Boise, Idaho, to Tampa, Florida. Neither friars nor conquistadors, those tens of thousands of immigrants from Spain who ended up in the United States represent just a tiny percentage of the millions of Spaniards who, in those same years, crossed the Atlantic, most with the goal of settling in various points of the Spanish-speaking Americas. Herein lies one of the best-kept demographic secrets of the American hemisphere: the massive presence of Spaniards in the Americas –South, Central and North– is largely a post-imperial phenomenon. For every Spanish friar or explorer from Spain’s Age of Empire who is commemorated by a statue or a street name in the United States, there would arrive, during the Age of Immigration, thousands of Spanish seamen, nannies, cigar-makers, canners, miners, shopkeepers, sheepherders and steelworkers. But because their stories do not easily fit into any conventional national narrative in either country, these working-class Spaniards are, for the most part, absent from standard historical accounts of both Spanish emigration and US immigration. They are, as it were, invisible immigrants.
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Smith, Robert B., and Lee J. Siegel. "Cataclysm!: The Hotspot Reaches Yellowstone." In Windows into the Earth. Oxford University Press, 2000. http://dx.doi.org/10.1093/oso/9780195105964.003.0007.

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Epicenters from numerous earthquakes fall approximately along two parallel lines that stretch from southeast to northwest through Yellowstone National Park. During the past 630,000 years, lava flowed from eruptive vents located roughly along the same lines. The alignment of earthquakes and small volcanoes suggests that zones of weakness are deep beneath them within the Earth. Those zones may be the still-active roots of faults that once ran along the base of towering mountains. Such mountains would have made ancient Yellowstone resemble today’s Grand Teton National Park. Indeed, a few million years ago these mountains may have stretched northward through Yellowstone and hooked up with the Gallatin Range, which now extends from Montana south into Yellowstone’s northwest corner. So why is today’s Yellowstone Plateau relatively flat? What happened to the mountains that once may have rose thousands of feet skyward like the Tetons do today? The answer, quite simply, is that they were destroyed 2 million years ago during a caldera eruption, which is the largest, most catastrophic kind of volcanic outburst—an explosion so cataclysmic that it dwarfs any eruption in historic time. North America had continued its southwestward slide over the Yellowstone hotspot. After blasting and repaving the Snake River Plain, the hotspot was finally beneath the place for which it later was named. The power of its rising heat and hot rock began to shape Yellowstone into what it is today. The first eruptive blast at Yellowstone 2 million years ago left a gigantic hole in the ground—a hole larger than the state of Rhode Island. The huge crater, known as a caldera, measured about 5o miles long, 40 miles wide, and hundreds of yards deep. It extended from Island Park in Idaho to the central part of Yellowstone in Wyoming. During the volcanic cataclysm, hot ash and rock blew into the heavens over Yellowstone, then rained like hell from the sky. As heavier pumice and ash particles debris piled up on the ground, their heat welded the debris together to form a layer of solid rock called ash-flow tuff or welded tuff.
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Conference papers on the topic "Petroglyphs – South Central Idaho"

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Clason, Hayden D., Esther C. Badon, Keeanah M. Jones, Scott Vetter, and John Shervais. "ORIGIN AND EVOLUTION OF LATE MIOCENE-PLEISTOCENE BASALT: CENTRAL MOUNT BENNETT HILLS, CENTRAL SNAKE RIVER PLAIN, IDAHO." In 54th Annual GSA South-Central Section Meeting 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020sc-343518.

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Smith, Connor J., Thomas E. Lachmar, John W. Shervais, James P. Evans, and Dennis L. Newell. "EVALUATION OF THE GEOTHERMAL POTENTIAL OF THE CAMAS PRAIRIE, SOUTH-CENTRAL IDAHO." In 72nd Annual GSA Rocky Mountain Section Meeting - 2020. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020rm-346772.

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Galletly, Aaron, Alison Graettinger, and Alex Bearden. "BILLOWED STRUCTURES OF BASALTIC INTRUSIONS: A COMPARISON OF BIG BEND NATIONAL PARK, TEXAS AND 71 GULCH, IDAHO." In Joint 55th Annual North-Central / 55th Annual South-Central Section Meeting - 2021. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021nc-362762.

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LeBlanc, Catherine G., Mitchell S. Tarantolo, Scott Vetter, and John Shervais. "ORIGIN AND EVOLUTION OF QUATERNARY BASALTS: CAMAS PRAIRIE RIFT BASIN, CENTRAL SNAKE RIVER PLAIN, IDAHO." In Joint 53rd Annual South-Central/53rd North-Central/71st Rocky Mtn GSA Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019sc-326710.

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Bullock, Murray S. "Sugar beet yield increases following oil radish green manure nematode trap crops in South Central Idaho." In 33rd Biennial Meeting of American Society of Sugarbeet Technologist. ASSBT, 2005. http://dx.doi.org/10.5274/assbt.2005.21.

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Mario E de Haro Marti, Ronald E Sheffield, and Mireille Chahine. "Emissions from a Dairy Wastewater Storage Pond, Manure Processing Area, and Composting Yard in south-central Idaho." In International Symposium on Air Quality and Waste Management for Agriculture, 16-19 September 2007, Broomfield, Colorado. American Society of Agricultural and Biological Engineers, 2007. http://dx.doi.org/10.13031/2013.23852.

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Burton, Bradford R., and Paul Karl Link. "GEOLOGIC MAPPING OF A POLYPHASE TECTONIC-MAGMATIC COMPLEX IN THE ROCK ROLL CANYON 7.5’ QUADRANGLE, SOUTH-CENTRAL IDAHO." In Joint 70th Annual Rocky Mountain GSA Section / 114th Annual Cordilleran GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018rm-314244.

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Temple, Dan, Daniel Murdock, Bruce Sandoval, and Ron Bishop. "Case History: Large Diameter High Volume Water Resource Development and Conservation Project at USBR’s Minidoka North, South Central Idaho, Located A&B Irrigation District Incorporating “Sustainable Design Principles”." In Pipelines 2017. American Society of Civil Engineers, 2017. http://dx.doi.org/10.1061/9780784480878.003.

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Reports on the topic "Petroglyphs – South Central Idaho"

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Hostetler, Steven, Cathy Whitlock, Bryan Shuman, David Liefert, Charles Wolf Drimal, and Scott Bischke. Greater Yellowstone climate assessment: past, present, and future climate change in greater Yellowstone watersheds. Montana State University, 2021. http://dx.doi.org/10.15788/gyca2021.

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The Greater Yellowstone Area (GYA) is one of the last remaining large and nearly intact temperate ecosystems on Earth (Reese 1984; NPSa undated). GYA was originally defined in the 1970s as the Greater Yellowstone Ecosystem, which encompassed the minimum range of the grizzly bear (Schullery 1992). The boundary was enlarged through time and now includes about 22 million acres (8.9 million ha) in northwestern Wyoming, south central Montana, and eastern Idaho. Two national parks, five national forests, three wildlife refuges, 20 counties, and state and private lands lie within the GYA boundary. GY
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Hydrology of the Oakley Fan Area, south-central Idaho. US Geological Survey, 1989. http://dx.doi.org/10.3133/wri884065.

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Geology and stratigraphy of the Challis Volcanic Group and related rocks, Little Wood River area, south-central Idaho. US Geological Survey, 2005. http://dx.doi.org/10.3133/b2064ii.

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Probability of detecting elevated concentrations of nitrate in ground water in a six-county area of south-central Idaho. US Geological Survey, 2003. http://dx.doi.org/10.3133/wri034143.

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Map showing geologic terranes of the Hailey 1 degree x 2 degrees quadrangle and the western part of the Idaho Falls 1 degree x 2 degrees quadrangle, south-central Idaho. US Geological Survey, 1995. http://dx.doi.org/10.3133/b2064a.

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Map showing distribution, composition, and age of early and middle Cenozoic volcanic centers in Idaho, Montana, west-central South Dakota, and Wyoming. US Geological Survey, 1994. http://dx.doi.org/10.3133/i2291c.

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Geologic map of the Craters of the Moon, Kings Bowl, and Wapi Lava Fields, and the Great Rift Volcanic Rift Zone, south-central Idaho. US Geological Survey, 1988. http://dx.doi.org/10.3133/i1632.

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Geologic map of outcrop areas of sedimentary units in the eastern part of the Hailey 1 degree x 2 degrees quadrangle and part of the southern part of the Challis 1 degree x 2 degrees quadrangle, south-central Idaho. US Geological Survey, 1995. http://dx.doi.org/10.3133/b2064c.

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