Relevant bibliographies by topics / Geology – Montana – Glacier National Park

Academic literature on the topic 'Geology – Montana – Glacier National Park'

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Published: 10 December 2022
Last updated: 28 January 2023

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Journal articles on the topic "Geology – Montana – Glacier National Park"

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Wilkerson, Forrest D., and Ginger L. Schmid. "Distribution of debris flows in Glacier National Park, Montana, U.S.A." Journal of Mountain Science 5, no. 4 (November 28, 2008): 318–26. http://dx.doi.org/10.1007/s11629-008-0232-7.

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Lambert, Callie B., Lynn M. Resler, Yang Shao, and David R. Butler. "Vegetation change as related to terrain factors at two glacier forefronts, Glacier National Park, Montana, U.S.A." Journal of Mountain Science 17, no. 1 (January 2020): 1–15. http://dx.doi.org/10.1007/s11629-019-5603-8.

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Yin, An, and Thomas K. Kelty. "Development of normal faults during emplacement of a thrust sheet: an example from the Lewis allochthon, Glacier National Park, Montana (U.S.A.)." Journal of Structural Geology 13, no. 1 (January 1991): 37–47. http://dx.doi.org/10.1016/0191-8141(91)90099-5.

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DeBolt, Ann, and Bruce McCune. "Lichens of Glacier National Park, Montana." Bryologist 96, no. 2 (1993): 192. http://dx.doi.org/10.2307/3243801.

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Nielsen, Lewis T. "The Mosquitoes Of Glacier National Park, Montana." Journal of the American Mosquito Control Association 25, no. 3 (September 2009): 246–47. http://dx.doi.org/10.2987/09-5753.1.

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Butler, David R. "GLACIAL HAZARDS IN GLACIER NATIONAL PARK, MONTANA." Physical Geography 10, no. 1 (January 1989): 53–71. http://dx.doi.org/10.1080/02723646.1989.10642367.

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Waller, John S. "Status of Fishers in Glacier National Park, Montana." Northwestern Naturalist 99, no. 1 (March 2018): 1–8. http://dx.doi.org/10.1898/nwn17-07.1.

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Kendall, Katherine C., Jeffrey B. Stetz, David A. Roon, Lisette P. Waits, John B. Boulanger, and David Paetkau. "Grizzly Bear Density in Glacier National Park, Montana." Journal of Wildlife Management 72, no. 8 (November 2008): 1693–705. http://dx.doi.org/10.2193/2008-007.

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Stetz, Jeff B., Katherine C. Kendall, and Amy C. Macleod. "Black bear density in Glacier National Park, Montana." Wildlife Society Bulletin 38, no. 1 (November 8, 2013): 60–70. http://dx.doi.org/10.1002/wsb.356.

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Butler, David R., Jack G. Oelfke, and Lori A. Oelfke. "Historic Rockfall Avalanches, Northeastern Glacier National Park, Montana, U.S.A." Mountain Research and Development 6, no. 3 (August 1986): 261. http://dx.doi.org/10.2307/3673396.

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Dissertations / Theses on the topic "Geology – Montana – Glacier National Park"

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Brett, Melissa Carrie. "Glacier Inventories and Change in Glacier National Park." PDXScholar, 2018. https://pdxscholar.library.pdx.edu/open_access_etds/4348.

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Glacier National Park, in northwestern Montana, is a unique and awe-inspiring national treasure that is often used by the media and public-at-large as a window into the effects of climate change. An updated inventory of glaciers and perennial snowfields (G&PS) in the Park, along with an assessment of their change over time, is essential to understanding the role that glaciers are playing in the environment of this Park. Nine inventories between 1966 and 2015 were compiled to assess area changes of G&PS. Over that 49-year period, total area changed by nearly -34 ± 11% between 1966 and 2015. Volume change, determined from changes in surface topography for nine glaciers, totaling 8.61 km² in area, was +0.142 ± 0.02 km³, a specific volume loss of -16.3 ± 2.5m. Extrapolating to all G&PS in the Park in 1966 yields a park-wide loss of -0.660 ± 0.099 km³. G&PS have been receding in the Park due to warming air temperatures rather than changes in precipitation, which has not changed significantly. Since 1900, air temperatures in Glacier National Park have warmed by +1.3 C°, compared to +0.9 C° globally. Spatially, G&PS at lower elevations and on steeper slopes lost relatively more area than other G&PS.
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Urion, Celeste Josephine. "Construction of wilderness in the formation of Glacier National Park, Montana." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp01/MQ40018.pdf.

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Williams, Thomas James. "Estimating organic carbon on avalanche paths in Glacier National Park, Montana." Thesis, University of Iowa, 2014. https://ir.uiowa.edu/etd/4795.

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Avalanche paths are unique ecosystems that represent a significant portion of the landscape in the northern Rocky Mountains. Frequent avalanche disturbance results in vegetative cover that is unlike the adjacent coniferous forest. These high relief environments have the potential to remove carbon from the atmosphere at rates differing from those of the surrounding forest, and to regulate matter and/or energy fluxes to downslope ecosystems. This thesis attempts to estimate organic carbon on south-facing avalanche paths in the southern portion of Glacier National Park, Montana. I am specifically interested in total organic carbon density, compartmental carbon density, and change in organic carbon over time as a function of shrub and tree diameter. Using an integrated sampling method, estimates of total organic carbon on avalanche paths appear to be different than those of the adjacent forest and similar to those of other shrub formation types in the area. However, the potentially moveable litter compartment is consistently larger. Organic carbon from shrub and trees growing on paths appears to be increasing at a continuous rate leading up to disturbance, while a typical individual's rate of increase appears to be slowing. The organic material temporarily stored on avalanche paths could serve as an important outside carbon source for near and distant aquatic ecosystems.
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Lambert, Callie Brooke. "Spatio-Temporal Vegetation Change as related to terrain factors at two Glacier Forefronts, Glacier National Park, Montana." Thesis, Virginia Tech, 2019. http://hdl.handle.net/10919/87411.

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Glacier retreat is considered a clear sign of global climate change. Although a rich body of work has documented glacial response to climate warming trends, comparatively little research has assessed vegetation change in recently deglaciated areas. In this study, we assess vegetation change at two glacier forefronts in Glacier National Park, Montana, through remote sensing analysis, fieldwork validation, and statistical modelling. The research objectives were to: 1) quantify the spatial and temporal patterns of landcover change of five classes"ice, rock, tree, shrub, and herbaceous at the two glacier forefronts in Glacier National Park, and 2) determine the role of selected biophysical terrain factors (elevation, slope, aspect, solar radiation, flow accumulation, TWI, and geology) on vegetation change at the deglaciated areas. Landsat imagery of the study locations in 1991, 2003, and 2015 were classified and validated using ground truth points and visual interpretation for accuracy. Overall accuracies were above 75% for all classified images. To identify biophysical correlates of change, we used generalized linear mixed models with non-vegetated surfaces to vegetation (code=1) or stable non-vegetation class (code=0) as a binary response variable. Results revealed elevation, slope, TWI, geology, and aspect to be associated with increased vegetation over time at Jackson Glacier forefront, whereas elevation, slope, solar radiation, and geology were significant at Grinnell Glacier forefront. New case studies on vegetation change in recently deglaciated regions can deepen our knowledge about how glacier retreat at local scales results in recharged ecosystem dynamics.
Master of Science
Glacier retreat is considered a clear sign of global climate change. Although glaciers are retreating globally, comparatively little research has assessed how vegetation changes in recently deglaciated areas. The research objectives were to: 1) quantify patterns of landcover change of five classes—ice, rock, tree, shrub, and herbaceous at two glacier forefronts in Glacier National Park, and 2) determine the environmental and terrain factors that affect vegetation change at the deglaciated areas. Landsat imagery of the study locations in 1991, 2003, and 2015 were classified and validated using ground truth points and visual interpretation for accuracy. To identify terrain and environmental factors that influence change, we modeled change from nonvegetated surfaces to vegetation (code=1) and the stable non-vegetation class (code=0). Results revealed elevation, slope, topographic moisture, geology, and aspect to be associated with increased vegetation over time at Jackson Glacier forefront. Elevation, slope, solar radiation, and geology were significant at Grinnell Glacier forefront, indicating some geographic differences in important factors. New case studies on vegetation change in recently deglaciated regions can deepen our knowledge about how glacier retreat at local scales results in recharged ecosystem dynamics. This study provides further insight on the future of alpine ecosystems as they respond to global climate change and a compelling new perspective on the future of the Park. Additionally, we demonstrate the benefits of using remote sensing applications to study land cover change as a proxy for vegetation colonization, especially in remote mountainous environments.
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Pederson, Gregory Thomas. "Long-term perspectives on Northern Rockies climatic variability from tree rings in Glacier National Park, Montana." Thesis, Montana State University, 2004. http://etd.lib.montana.edu/etd/2004/pederson/PedersonG04.pdf.

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Instrumental climate records reveal fluctuations in summer moisture anomalies and winter snowpack in Glacier National Park, Montana, on decadal and multidecadal timescales. However, because climate records for the region are limited to the 20th century, studies on the impacts of long-duration variations in climate on physical and ecosystem processes were limited. Therefore, a reconstruction of summer moisture variability (June - August) spanning A.D. 1540-2000 was created from a multi-species network of tree-ring chronologies sampled in Glacier National Park. The reconstruction shows decadal-scale shifts between drought and pluvial events with a pronounced cool/wet period spanning the end of the Little Ice Age (A.D. 1770-1840). The single most exceptional drought event occurred over the 20th century (A.D. 1917-1941) and was associated with the most spatially consistent drought regime throughout the northern Rockies and Pacific Northwest over the past ~500 yrs. Among a wider spatial network of hydroclimatic reconstructions arrayed along a north-south Rocky Mountain transect, trends at Glacier National Park were found to be most similar to those in the Canadian Rockies and the Pacific Northwest. Also, many decadal-scale drought/pluvial events were consistent among all sites along the north-south transect - although magnitude, intensity, and time of onset varied. To investigate climatic drivers related to the Little Ice Age glacial maximum and rapid 20th-century retreat, I explored the impact of north Pacific Basin sea-surface temperature anomalies on low-frequency variations in winter snowpack for the park. Temperature anomalies in the north Pacific basin exhibit tight linkages to variations in snowpack; therefore, I used a tree-ring based reconstruction of north Pacific temperature variability and summer drought as proxies for winter glacial accumulation and summer ablation, respectively, over the past three centuries (A.D. 1700-2000). These records show that the 1850's glacial maximum was likely produced by ~70 yrs of cool/wet summers coupled with high snowpack. Glacial retreat coincided with an extended period (>50 yr) of summer drought and low snowpack culminating in the exceptional events of 1917-1941 when retreat rates exceeded 100 m/yr. This research highlights the difficulty in detecting regional expression of global climate change when 'natural' decadal-scale variations in climate are regionally common.
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Schoenenberger, Katherine R. "LITTLE ICE AGE CHRONOLOGY FOR CLASSEN AND GODLEY GLACIERS, MOUNT COOK NATIONAL PARK, NEW ZEALAND." University of Cincinnati / OhioLINK, 2001. http://rave.ohiolink.edu/etdc/view?acc_num=ucin990634749.

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Damm, Christian. "A phytosociological study of Glacier National Park, Montana, U.S.A., with notes on the syntaxonomy of alpine vegetation in Western North America." Doctoral thesis, [S.l.] : [s.n.], 2001. http://deposit.ddb.de/cgi-bin/dokserv?idn=963101552.

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Michaels, Amanda Paige. "Land Use and Land Cover Change in the Crown of the Continent Ecosystem, Montana, USA from 1992-2011." Thesis, Virginia Tech, 2016. http://hdl.handle.net/10919/72842.

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In recent decades land use and land cover change (LULCC) has occurred throughout the Intermountain West. The Crown of the Continent Ecosystem (CCE) extends along the Rocky Mountains adjacent to the Canada-U.S. International border. In the U.S. portion of the CCE, located in northwestern Montana, development has increased since the 1990s, largely because of urban to rural migration. The CCE has become an amenity-based destination, which in turn is likely to threaten its terrestrial and aquatic ecological diversity (Quinn and Broberg 2007). Specifically, development pressures on private lands surrounding federally protected lands, are intensifying and thus threatening core habitat of native species and connectivity of forested areas. By characterizing the spatial and temporal patterns of LULCC, we can better understand landscape-scale changes influenced by human-environment interactions. Using National Land Cover Database (NLCD) products, I identified areas that have experienced land cover change for three time periods: 1992-2001, 2001-2006, and 2006-2011. Additionally, I used case studies to further investigate LULCC in the study area. The findings suggest that the highest rates of development in proximity to Glacier National Park were dependent on existing urban land cover, meaning existing roadway infrastructure and established urban areas saw the greatest urban development. Additionally, communities adjacent to Glacier National Park were hotspots for urban development. Based on the results, areas in proximity to federally protected lands are likely to experience continued urban intensification over the next few decades.
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Syverson, Kent Maurice. "Glacial geology of the southeastern Burroughs Glacier, Glacier Bay National Park and Preserve, Alaska." 1992. http://catalog.hathitrust.org/api/volumes/oclc/27399422.html.

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Damm, Christian [Verfasser]. "A phytosociological study of Glacier National Park, Montana, U.S.A., with notes on the syntaxonomy of alpine vegetation in Western North America / vorgelegt von Christian Damm." 2001. http://d-nb.info/963101552/34.

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Books on the topic "Geology – Montana – Glacier National Park"

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Carrara, Paul E. Late Quaternary glacial and vegetative history of the Glacier National Park region, Montana. Washington, D.C: U.S. G.P.O., 1989.

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Whipple, James W. Stratigraphy and lithocorrelation of the Snowslip Formation (Middle Proterozoic Belt Supergroup), Glacier National Park, Montana. [Washington, D.C.]: U.S. G.P.O., 1988.

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Mulvaney, Tom. Glacier National Park. Charleston, SC: Arcadia Pub., 2010.

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Gildart, Robert C. Glacier National Park. Guilford, Conn: FalconGuides, Globe Pequot Press, 2008.

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Transportation plan: Glacier National Park, Montana. [Washington, D.C.?]: U.S. Dept. of the Interior, National Park Service, 1990.

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McRae, W. C. Montana handbook: Including Glacier National Park. 4th ed. Chico, Calif: Moon Publications, 1999.

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Lomax, Becky. Glacier National Park. 2nd ed. Berkeley, Calif: Avalon Travel, 2009.

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Leftridge, Alan. The Best of Glacier National Park. Helena, MT: Farcountry Press, 2013.

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Fire lookouts of Glacier National Park. Charleston, South Carolina: Arcadia Publishing, 2014.

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The trail guide to Glacier National Park. Helena, MT: Falcon Press, 1992.

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Book chapters on the topic "Geology – Montana – Glacier National Park"

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Horodyski, Robert J. "Stromatolites of the Belt Supergroup, Glacier National Park, Montana." In Middle Proterozoic Belt Supergroup, Western Montana: Great Falls, Montana to Spokane, Washington, July 20–28, 1989, 27–42. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft334p0027.

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Butler, David R., George P. Malanson, Forrest D. Wilkerson, and Ginger L. Schmid. "Late Holocene Sturzstroms in Glacier National Park, Montana, U.S.A." In The GeoJournal Library, 149–66. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5228-0_9.

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Debinski, Diane M., and Peter F. Brussard. "Biological Diversity Assessment in Glacier National Park, Montana: I. Sampling Design." In Ecological Indicators, 393–407. Boston, MA: Springer US, 1992. http://dx.doi.org/10.1007/978-1-4615-4659-7_24.

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Wilkerson, Forrest, and Ginger Schmid. "Dendrogeomorphic Applications to Debris Flows in Glacier National Park, Montana USA." In Advances in Global Change Research, 207–9. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-8736-2_19.

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Butler, David R., Carol F. Sawyer, and Jacob A. Maas. "Tree-Ring Dating of Snow Avalanches in Glacier National Park, Montana, USA." In Advances in Global Change Research, 35–46. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-8736-2_3.

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Apple, Martha E., Macy K. Ricketts, Alice C. Martin, and Dennis J. Moritz. "Distance from Retreating Snowfields Influences Alpine Plant Functional Traits at Glacier National Park, Montana." In Mountain Landscapes in Transition, 331–48. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-70238-0_12.

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Butler, David R., and Lisa M. DeChano. "Landslide Risk Perception, Knowledge and Associated Risk Management: Case Studies and General Lessons from Glacier National Park, Montana, USA." In Landslide Hazard and Risk, 199–218. Chichester, West Sussex, England: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9780470012659.ch6.

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Horodyski, R. J. "Stromatolites of the Middle Proterozoic Belt Supergroup, Glacier National Park, Montana: a Summary and a Comment on the Relationship Between Their Morphology and Paleoenvironment." In Paleoalgology, 34–39. Berlin, Heidelberg: Springer Berlin Heidelberg, 1985. http://dx.doi.org/10.1007/978-3-642-70355-3_4.

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"Transect across the northeastern margin of the Mesoproterozoic Belt Basin and Lewis thrust, Glacier National Park, Montana." In Unfolding the Geology of the West, 231–45. Geological Society of America, 2016. http://dx.doi.org/10.1130/2016.0044(10).

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Newell, Robert L., R. W. Baumann, and J. A. Stanford. "Stoneflies of Glacier National Park and Flathead River Basin, Montana." In International Advances in the Ecology, Zoogeography, and Systematics of Mayflies and Stoneflies, 173–86. University of California Press, 2008. http://dx.doi.org/10.1525/california/9780520098688.003.0013.

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Conference papers on the topic "Geology – Montana – Glacier National Park"

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MacGregor, Kelly, and Amy Myrbo. "LANDSCAPE AND ENVIRONMENTAL CHANGE IN GLACIER NATIONAL PARK, MONTANA, U.S.A." In Keck Proceedings. Keck Geology Consortium, 2019. http://dx.doi.org/10.18277/akrsg.2019.32.01.

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Principato, Sarah M., Dori L. Gorczyca, and Salma B. Monani. "CLIMATE CHANGE COMMUNICATION USING VIRTUAL PLACE ATTACHMENT AT GLACIER NATIONAL PARK, MONTANA, USA." In GSA Annual Meeting in Denver, Colorado, USA - 2016. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016am-276974.

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MacGregor, Kelly, Amy Myrbo, Diala Abboud, Elizaveta Atalig, Etienne Chenevert, Elizabeth Moore, Bonnie Page, Anna Pearson, Joshua Stephenson, and Jacob Watts. "Sediment Transport and Deposition in Fishercap Lake and the Swiftcurrent Valley, Glacier National Park, Montana, USA." In Keck Proceedings. Keck Geology Consortium, 2018. http://dx.doi.org/10.18277/akrsg.2019.32.02.

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MacGregor, Kelly, Amy Myrbo, Diala Abboud, Elizaveta Atalig, Etienne Chenevert, Elizabeth Moore, Bonnie Page, Anna Pearson, Joshua Stephenson, and Jacob Watts. "SEDIMENT TRANSPORT AND DEPOSITION IN FISHERCAP LAKE AND THE SWIFTCURRENT VALLEY, GLACIER NATIONAL PARK, MONTANA, USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321580.

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Myrbo, Amy, Kelly MacGregor, Diala Abboud, Elizaveta Atalig, Etienne Chenevert, Elizabeth Moore, Bonnie Page, Anna Pearson, Joshua Stephenson, and Jacob Watts. "Using Lake Cores to Analyze Sediment Transport and Environmental Change in Swiftcurrent Lake, Glacier National Park, Montana." In Keck Proceedings. Keck Geology Consortium, 2018. http://dx.doi.org/10.18277/akrsg.2019.32.03.

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Benson, David. "Move, Adapt, or Die: Lagopus leucura Changes in Distribution, Habitat and Number at Glacier National Park, Montana." In Gyrfalcons and Ptarmigan in a Changing World. The Peregrine Fund, 2011. http://dx.doi.org/10.4080/gpcw.2011.0121.

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MacGregor, Kelly, Joshua Bruns, Allison Hidalgo, Louis Miller, Evelyn Solis Cabrera, Reydaliz Torres Lopez, and Amy Myrbo. "SEDIMENT TRANSPORT AND DEPOSITION IN REDROCK AND FISHERCAP LAKES IN SWIFTCURRENT VALLEY, GLACIER NATIONAL PARK, MONTANA, USA." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-377951.

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MacGregor, Kelly, Amy Myrbo, Diala Abboud, Elizaveta Atalig, Etienne Chenevert, Elizabeth Moore, Bonnie Page, Anna Pearson, Joshua Stephenson, and Jacob Watts. "USING LAKE CORES TO ANALYZE SEDIMENT TRANSPORT AND ENVIRONMENTAL CHANGE IN SWIFTCURRENT LAKE, GLACIER NATIONAL PARK, MONTANA, USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-321678.

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MacGregor, Kelly. "GLACIAL EROSION, SEDIMENT TRANSPORT, AND ENVIRONMENTAL CHANGE IN THE GRINNELL AND SWIFTCURRENT VALLEYS, GLACIER NATIONAL PARK, MONTANA, USA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-323010.

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Miller, Louis, Kelly MacGregor, Maximillian Van Wyk de Vries, Emi Ito, Mark D. Shapley, Guido Brignone, and Matias Romero. "USING CESIUM-137 TO DETERMINE SEDIMENTATION PATTERNS IN TWO PROGLACIAL LAKES - LAGO ARGENTINO, SOUTHERN PATAGONIAN ICEFIELD, ARGENTINA, AND LAKE JOSEPHINE, GLACIER NATIONAL PARK, MONTANA, USA." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-377913.

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Reports on the topic "Geology – Montana – Glacier National Park"

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Geologic map of Glacier National Park, Montana. US Geological Survey, 1992. http://dx.doi.org/10.3133/i1508f.

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Surficial geologic map of Glacier National Park, Montana. US Geological Survey, 1990. http://dx.doi.org/10.3133/i1508d.

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Geologic maps, cross section, and photographs of the central part of Glacier National Park, Montana. US Geological Survey, 1989. http://dx.doi.org/10.3133/i1508b.

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Bedrock geologic map of part of the disturbed belt south and east of Glacier National Park, Montana. US Geological Survey, 1991. http://dx.doi.org/10.3133/i2130.

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Geologic map and cross section across Belt terrane from Chewlah, Washington, to Glacier National Park, Montana. US Geological Survey, 1998. http://dx.doi.org/10.3133/i2594.

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Late quaternary glacial and vegetative history of the Glacier National Park region, Montana. US Geological Survey, 1989. http://dx.doi.org/10.3133/b1902.

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Stratigraphy and lithocorrelation of the Snowslip Formation (Middle Proterozoic Belt Supergroup), Glacier National Park, Montana. US Geological Survey, 1988. http://dx.doi.org/10.3133/b1833.

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Map showing distribution of moraines and extent of glaciers from the mid-19th century to 1979 in the Mount Jackson area, Glacier National Park, Montana. US Geological Survey, 1988. http://dx.doi.org/10.3133/i1508c.

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