Academic literature on the topic 'Topographic evolution of mountains'
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Journal articles on the topic "Topographic evolution of mountains"
Bao, G., Y. Dou, T. A. Ehlers, P. Li, Y. Wang, and Z. Xu. "Quantifying Tectonic and Geomorphic Interpretations of Thermochronometer Data with Inverse Problem Theory." Communications in Computational Physics 9, no. 1 (January 2011): 129–46. http://dx.doi.org/10.4208/cicp.090110.270410a.
Full textTranel, Lisa, and James Spotila. "Relief History and Coupling of Erosional Processes in the Teton Range, Wyoming." UW National Parks Service Research Station Annual Reports 30 (January 1, 2006): 158–63. http://dx.doi.org/10.13001/uwnpsrc.2006.3683.
Full textWu, Li, Binggeng Xie, Xiao Xiao, Bing Xue, and Jingzhong Li. "Classification Method and Determination of Mountainous Area Types at Township Scales: A Case Study of Yuxi City, Yunnan Province." Complexity 2020 (September 3, 2020): 1–13. http://dx.doi.org/10.1155/2020/3484568.
Full textWilliams, Timothy C., Janet M. Williams, Peter G. Williams, and Paul Stokstad. "Bird Migration Through a Mountain Pass Studied With High Resolution Radar, Ceilometers, and Census." Auk 118, no. 2 (April 1, 2001): 389–403. http://dx.doi.org/10.1093/auk/118.2.389.
Full textBi, Rui, Shu Gan, Xiping Yuan, Raobo Li, Sha Gao, Min Yang, Weidong Luo, and Lin Hu. "Multi-View Analysis of High-Resolution Geomorphic Features in Complex Mountains Based on UAV–LiDAR and SfM–MVS: A Case Study of the Northern Pit Rim Structure of the Mountains of Lufeng, China." Applied Sciences 13, no. 2 (January 4, 2023): 738. http://dx.doi.org/10.3390/app13020738.
Full textGong, Ming-Hao, and Yan-Ling Song. "Topographic habitat features preferred by the Endangered giant panda Ailuropoda melanoleuca: implications for reserve design and management." Oryx 45, no. 2 (April 2011): 252–57. http://dx.doi.org/10.1017/s0030605310001043.
Full textPoole, Kim G., Kari Stuart-Smith, and Irene E. Teske. "Wintering strategies by mountain goats in interior mountains." Canadian Journal of Zoology 87, no. 3 (March 2009): 273–83. http://dx.doi.org/10.1139/z09-009.
Full textFarah, Tahar, Nasr-Eddine Taibi, and Mohamed Chouieb. "Evolution of Land Cover in the Traras MTS. Region Between 1984 and 2020 by Remote Sensing and Gis (Northwest Algeria)." Ekológia (Bratislava) 41, no. 4 (December 1, 2022): 375–85. http://dx.doi.org/10.2478/eko-2022-0038.
Full textBíl, Michal. "Using GIS to detect neotectonics in the Vsetínské vrchy Mountains and in their surroundings." Geografie 108, no. 2 (2003): 101–14. http://dx.doi.org/10.37040/geografie2003108020101.
Full textOllier, C. D., and C. F. Pain. "Neotectonic mountain uplift and geomorphology." Geomorphology RAS, no. 4 (November 8, 2019): 3–26. http://dx.doi.org/10.31857/s0435-4281201943-26.
Full textDissertations / Theses on the topic "Topographic evolution of mountains"
Ramsey, Lucy Ann. "Topographic evolution of emerging mountain belts." Thesis, University of Cambridge, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.614292.
Full textPrince, Philip S. "Evolution of transient topography on passive margins: A study of landscape disequilibrium in the southern Appalachian Mountains." Diss., Virginia Tech, 2011. http://hdl.handle.net/10919/77065.
Full textPh. D.
Brocklehurst, Simon H. (Simon Howard) 1975. "Evolution of topography in glaciated mountain ranges." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/29929.
Full textIncludes bibliographical references.
This thesis examines the response of alpine landscapes to the onset of glaciation. The basic approach is to compare fluvial and glacial landscapes, since it is the change from the former to the latter that accompanies climatic cooling. This allows a detailed evaluation of hypotheses relating climate change to tectonic processes in glaciated mountain belts. Fieldwork was carried out in the eastern Sierra Nevada, California, and the Sangre de Cristo Range, Colorado, alongside digital elevation model analyses in the western US, the Southern Alps of New Zealand, and the Himalaya of northwestern Pakistan. The evidence presented here suggests that the so-called "chicken-and-egg" hypothesis is overstated in its appeal to glacial erosion as a major source of relief production and subsequent peak uplift. Glaciers in the eastern Sierra Nevada and the western Sangre de Cristos have redistributed relief, but have produced only modest relief by enlarging drainage basins at the expense of low-relieftopography. Glaciers have lowered valley floors and ridgelines by similar amounts, limiting the amount of "missing mass" that can be generated, and causing a decrease in drainage basin relief.
(cont.) The principal response of glaciated landscapes to rapid rock uplift is the development of towering cirque headwalls. This represents considerable relief production, but is not caused by glacial erosion alone. Large valley glaciers can maintain their low gradient regardless of uplift rate, which supports the "glacial buzzsaw" hypothesis. However, the inability of glaciers to erode steep hillslopes as rapidly can cause mean elevations to rise. Cosmogenic isotope dating is used to show that (i) where plucking is active, the last major glaciation removed sufficient material to reset the cosmogenic clock; and (ii) former glacial valley floors now stranded near the crest of the Sierra Nevada are at varying stages of abandonment, suggesting a cycle of drainage reorganisation and relief inversion due to glacial erosion similar to that observed in river networks. Glaciated landscapes are quite distinct from their fluvial counterparts in both landforms and processes. Given the scarcity of purely fluvial, active mountain ranges, it is essential that glacial erosion be considered amongst the processes sculpting active orogenic belts.
by Simon H. Brocklehurst.
Ph.D.
Barnes, Jason B. "Variable Denudation in the Evolution of the Bolivian Andes: Controls and Uplift-Climate-Erosion Feedbacks." Thesis, The University of Arizona, 2002. http://hdl.handle.net/10150/240131.
Full textRichardson, Paul William Ph D. Massachusetts Institute of Technology. "Topographic asymmetry and climate controls on landscape evolution." Thesis, Massachusetts Institute of Technology, 2015. http://hdl.handle.net/1721.1/101346.
Full textCataloged from PDF version of thesis.
Includes bibliographical references (pages 145-157).
Landscapes are expected to evolve differently under the influence of different climate conditions. However, the relationship between landscape evolution and climate is not well understood. I investigate the relationship between landscape evolution and climate by using natural experiments in which climate varies with slope aspect (geographic orientation) and causes differences in landscape form, such as steeper equator- or pole-facing slopes. In order to understand which mechanisms are responsible for the development of this topographic asymmetry, I adapted a numerical landscape evolution model to include different asymmetry-forming mechanisms such as aspect-induced variations in soil creep intensity, regolith strength, and runoff, and also lateral channel migration. Numerical experiments reveal topographic signatures associated with each of these mechanisms that can be compared with field sites that exhibit asymmetry. I used these numerical model results, along with estimates of field-saturated hydraulic conductivity, soil strength, evidence of stream capture and channel beheadings, and erosion rates determined from cosmogenic radionuclides to determine which asymmetry forming mechanisms are likely responsible for the topographic asymmetry at Gabilan Mesa, a landscape in the central California Coast Ranges. I find that aspect-dependent differences in runoff are most likely responsible for the bulk of the asymmetry at Gabilan Mesa, but lateral channel migration has contributed to the asymmetry in some locations. To further investigate climate's influence on landscape evolution, I compiled new and previously published estimates of slope-dependent soil transport efficiency across a range of climates. I find that soil transport efficiency increases with mean annual precipitation and the aridity index, a measure that describes water availability for plants. I also find that soil transport efficiency varies with lithology and that different measurement techniques can bias estimates of the soil transport coefficient.
by Paul William Richardson.
Ph. D.
Zimmer, Janek, Armin Raabe, and Gerd Tetzlaff. "Quantification of topographic effects on predicted precipitation in the Erzgebirge." Universitätsbibliothek Leipzig, 2017. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-222025.
Full textOrografisch verstärkter Niederschlag im Bereich des Osterzgebirges spielte eine große Rolle bei der Entstehung des Elbehochwassers im August 2002. Sowohl globale als auch mesoskalige Vorhersagemodelle unterschätzten die lokalen Niederschlagsintensitäten trotz richtiger Positionierung des synoptisch-skaligen Frontenzuges. Zur Untersuchung der Gründe wurde das Lokalmodell des DWD für eine Sensitivitätsstudie bezüglich orografisch beeinflussten Niederschlags im Bereich eines idealisierten Glockenberges verwendet. Die Abhängigkeit des Niederschlags von verschiedenen Kontrollparametern wurde untersucht, mit besonderer Beachtung von Schichtungsstabilität und Horizontalwindstruktur. Bei Verwendung der operationellen Gitterweite von 7 km reproduzieren die Simulationen mit dem LM die bekannten Verteilungen von Vertikalwind und Niederschlag für unterschiedliche Schichtungen mit höhenkonstanten Temperaturgradienten. Die höchsten Niederschlagsraten ergeben sich jedoch für stratiforme Aufgleitprozesse im Fall von abnehmender Stabilität in mittleren und hohen Bereichen der Troposphäre sowie für konvektive Umgebungen, in beiden Fällen mit signifikanter Änderung des Vertikalwindfeldes verglichen mit der zuvor erwähnten Strömung. Der Einfluss des Vertikalprofils des horizontalen Windes auf Stärke und vertikale Abschwächung der Aufwärtsbewegung muss beachtet werden. Schließlich wurden die Sensitivitätsstudien ausgedehnt auf ein vereinfachtes Höhenprofil des Osterzgebirges. Als Ausgangssituation wurden dabei die atmosphärischen Bedingungen verwendet, die mit denen des Hochwasserereignisses vergleichbar sind. Diese numerischen Simulationen wurden mit Werten des einfachen diagnostischen Maximalniederschlagsmodells MAXRR verglichen. Entsprechend der relativ groben Gitterweite des LM können kleinräumige Unterschiede durch verstärkte orografische Hebung nicht wider gegeben werden, wogegen die beobachteten Niederschlagsmengen des Hochwasserereignisses mithilfe des hoch aufgelösten diagnostischen Modells erreicht werden
Steele, Jason Keith. "Influence of elevation on tree species distribution and growth in the southern Appalachian Mountains." Thesis, Virginia Tech, 2007. http://hdl.handle.net/10919/31875.
Full textMaster of Science
Mitchell, Sara Gran. "Late-Cenozoic topographic evolution of the Cascade Range, Washington State, USA /." Thesis, Connect to this title online; UW restricted, 2006. http://hdl.handle.net/1773/6713.
Full textZimmer, Janek, Armin Raabe, and Gerd Tetzlaff. "Quantification of topographic effects on predicted precipitation in the Erzgebirge." Wissenschaftliche Mitteilungen des Leipziger Instituts für Meteorologie ; 37 = Meteorologische Arbeiten aus Leipzig … und Jahresbericht … des Instituts für Meteorologie der Universität Leipzig ; 11 (2006), S. 125-136, 2006. https://ul.qucosa.de/id/qucosa%3A15499.
Full textOrografisch verstärkter Niederschlag im Bereich des Osterzgebirges spielte eine große Rolle bei der Entstehung des Elbehochwassers im August 2002. Sowohl globale als auch mesoskalige Vorhersagemodelle unterschätzten die lokalen Niederschlagsintensitäten trotz richtiger Positionierung des synoptisch-skaligen Frontenzuges. Zur Untersuchung der Gründe wurde das Lokalmodell des DWD für eine Sensitivitätsstudie bezüglich orografisch beeinflussten Niederschlags im Bereich eines idealisierten Glockenberges verwendet. Die Abhängigkeit des Niederschlags von verschiedenen Kontrollparametern wurde untersucht, mit besonderer Beachtung von Schichtungsstabilität und Horizontalwindstruktur. Bei Verwendung der operationellen Gitterweite von 7 km reproduzieren die Simulationen mit dem LM die bekannten Verteilungen von Vertikalwind und Niederschlag für unterschiedliche Schichtungen mit höhenkonstanten Temperaturgradienten. Die höchsten Niederschlagsraten ergeben sich jedoch für stratiforme Aufgleitprozesse im Fall von abnehmender Stabilität in mittleren und hohen Bereichen der Troposphäre sowie für konvektive Umgebungen, in beiden Fällen mit signifikanter Änderung des Vertikalwindfeldes verglichen mit der zuvor erwähnten Strömung. Der Einfluss des Vertikalprofils des horizontalen Windes auf Stärke und vertikale Abschwächung der Aufwärtsbewegung muss beachtet werden. Schließlich wurden die Sensitivitätsstudien ausgedehnt auf ein vereinfachtes Höhenprofil des Osterzgebirges. Als Ausgangssituation wurden dabei die atmosphärischen Bedingungen verwendet, die mit denen des Hochwasserereignisses vergleichbar sind. Diese numerischen Simulationen wurden mit Werten des einfachen diagnostischen Maximalniederschlagsmodells MAXRR verglichen. Entsprechend der relativ groben Gitterweite des LM können kleinräumige Unterschiede durch verstärkte orografische Hebung nicht wider gegeben werden, wogegen die beobachteten Niederschlagsmengen des Hochwasserereignisses mithilfe des hoch aufgelösten diagnostischen Modells erreicht werden.
Yuan, Chao, and 袁超. "Magmatism and tectonic evolution of the West Kunlun Mountains." Thesis, The University of Hong Kong (Pokfulam, Hong Kong), 1999. http://hub.hku.hk/bib/B29815162.
Full textBooks on the topic "Topographic evolution of mountains"
Hurni, Lorenz. Verschiedene Felsdarstellungsarten für Gebirgskarten 1:25,000. Zürich: Institut für Kartographie der Eidg. Technischen Hochschule Zürich, 1989.
Find full textVeress, Márton. Covered karst evolution in the Northern Bakony Mountains, W-Hungary. Budapest: Bakonyi Természettudományi Múzeum, 2000.
Find full textLinol, Bastien, and Maarten J. de Wit, eds. Origin and Evolution of the Cape Mountains and Karoo Basin. Cham: Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-40859-0.
Full textWistuba, Małgorzata. Slope-Channel Coupling as a Factor in the Evolution of Mountains. Cham: Springer International Publishing, 2014. http://dx.doi.org/10.1007/978-3-319-05819-1.
Full textJohn, David A. Evolution of hydrothermal fluids in the Alta stock, central Wasatch Mountains, Utah. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Find full textJohn, David A. Evolution of hydrothermal fluids in the Alta stock, central Wasatch Mountains, Utah. [Reston, Va.?]: U.S. Dept. of the Interior, U.S. Geological Survey, 1991.
Find full textICM 2002 Satellite Conference on nonlinear evolution equations and dynamical systems (2002 Huang Mountains, China). Proceedings of the ICM 2002 Satellite Conference: Nonlinear evolution equations and dynamical systems, Yellow Mountains, China, 15-18 August, 2002. Edited by Cheng Yi and International Congress of Mathematicians. Singapore: World Scientific Pub., 2003.
Find full textSutton, Brian. Glacial landforms and sedimentology: The late pleistocene evolution of the Mourne Mountains : Northern Ireland. [S.l: The Author], 1998.
Find full textSchuller, Volker. Evolution and geodynamic significance of the Upper Cretaceous Gosau basin in the Apuseni Mountains (Romania). Tübingen: IFG, 2004.
Find full textThompson, Robert I. Stratigraphy, tectonic evolution and structural analysis of the Halfway River map area (94 B), Northern Rocky Mountains, British Columbia. [Ottawa]: Energy Mines and Resources Canada, 1989.
Find full textBook chapters on the topic "Topographic evolution of mountains"
Andrews, E. D., Christopher E. Johnston, John C. Schmidt, and Mark Gonzales. "Topographic evolution of sand bars." In The Controlled Flood in Grand Canyon, 117–30. Washington, D. C.: American Geophysical Union, 1999. http://dx.doi.org/10.1029/gm110p0117.
Full textJain, A. K. "Geological Evolution of the Himalayan Mountains." In Geodynamics of the Indian Plate, 363–93. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-15989-4_10.
Full textMcLelland, J. M., and Y. W. Isachsen. "Geological Evolution of the Adirondack Mountains: A Review." In The Deep Proterozoic Crust in the North Atlantic Provinces, 175–215. Dordrecht: Springer Netherlands, 1985. http://dx.doi.org/10.1007/978-94-009-5450-2_12.
Full textLidiak, E. G. "Evolution of Proterozoic Granitoids, Eastern Arbuckle Mountains, Oklahoma." In Proceedings of the International Conferences on Basement Tectonics, 265. Dordrecht: Springer Netherlands, 1998. http://dx.doi.org/10.1007/978-94-011-5098-9_32.
Full textAl-Harthy, M. S., R. G. Coleman, M. W. Hughes-Clarke, and S. S. Hanna. "Tertiary Basaltic Intrusions in the Central Oman Mountains." In Ophiolite Genesis and Evolution of the Oceanic Lithosphere, 675–82. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3358-6_33.
Full textNasritdinov, Emil. "Mountains in the Evolution of Visual Arts in Kyrgyzstan." In Educating in the Arts, 121–33. Dordrecht: Springer Netherlands, 2008. http://dx.doi.org/10.1007/978-1-4020-6387-9_8.
Full textRößler, Ole, and Jörg Löffler. "Analyzing Spatio-Temporal Hydrological Processes and Related Gradients to Improve Hydrological Modeling in High Mountains." In Landform - Structure, Evolution, Process Control, 243–56. Berlin, Heidelberg: Springer Berlin Heidelberg, 2009. http://dx.doi.org/10.1007/978-3-540-75761-0_15.
Full textCalvez, J. Y., and J. L. Lescuyer. "Lead Isotope Geochemistry of Various Sulphide Deposits from the Oman Mountains." In Ophiolite Genesis and Evolution of the Oceanic Lithosphere, 385–97. Dordrecht: Springer Netherlands, 1991. http://dx.doi.org/10.1007/978-94-011-3358-6_19.
Full textPatel, Priyank Pravin, Shantamoy Guha, Debsmita Das, and Madhurima Bose. "Spatial Variability of Topographic Attributes and Channel Morphological Characteristics in the Ladakh Trans-Himalayas and Their Tectonic and Structural Controls." In Himalayan Neotectonics and Channel Evolution, 67–110. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-030-95435-2_3.
Full textIrwin, William P. "Terranes of the Klamath Mountains, California and Oregon." In Tectonic Evolution of Northern California: Sausalito to Yosemite National Park, California, June 28–July 7, 1989, 19–32. Washington, D. C.: American Geophysical Union, 1989. http://dx.doi.org/10.1029/ft108p0019.
Full textConference papers on the topic "Topographic evolution of mountains"
Hausback, Brian, Samuel Grandy, Rebecca J. Dorsey, Michael Darin, and Scott Bennett. "VOLCANIC AND TOPOGRAPHIC EVOLUTION OF THE SIERRA SAN FRANCISCO, BAJA CALIFORNIA SUR, MEXICO." In Joint 118th Annual Cordilleran/72nd Annual Rocky Mountain Section Meeting - 2022. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022cd-373847.
Full textValjarević, Aleksandar, and Bojana Jandziković. "DIGITAL AND CARTOGRAPHIC MODELLING OF VRSAC MOUNTAINS TOPOGRAPHIC EXPOSITIONS." In International Scientific Conference Geobalcanica 2015. Geobalcanica Society, 2015. http://dx.doi.org/10.18509/gbp.2015.02.
Full textLiu, Lijun, Quan Zhou, and Diandian Peng. "CENOZOIC TOPOGRAPHIC EVOLUTION OF WESTERN-CENTRAL US." In GSA Connects 2021 in Portland, Oregon. Geological Society of America, 2021. http://dx.doi.org/10.1130/abs/2021am-366161.
Full textTerhune, Patrick, Jeff A. Benowitz, Paul W. Layer, Jeffrey M. Trop, and Paul B. O'Sullivan. "THERMOCHRONOLOGY OF THE TALKEETNA MOUNTAINS OF SOUTHERN ALASKA: CENOZOIC TOPOGRAPHIC DEVELOPMENT HISTORY." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-303757.
Full textLi, Lin, Majie Fan, and Lu Zhu. "MIDDLE–LATE PALEOGENE TOPOGRAPHIC EVOLUTION IN SOUTHWESTERN MONTANA." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334188.
Full textHumphreys, Eugene. "WALLOWA BATHOLITH ROOT FOUNDERING, REGIONAL CRUSTAL FLOW AND TOPOGRAPHIC EVOLUTION." In GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-380003.
Full textAcosta, Lynn A., and Reed J. Burgette. "Scarp Morphology Along the Alamogordo Fault, Sacramento Mountains From a High-Resolution Aerial Topographic Survey." In 2018 New Mexico Geological Society Annual Spring Meeting. Socorro, NM: New Mexico Geological Society, 2018. http://dx.doi.org/10.56577/sm-2018.758.
Full textAchard, V., and X. Lenot. "Atmospheric and topographic corrections for hyperspectral imagery." In 2009 First Workshop on Hyperspectral Image and Signal Processing: Evolution in Remote Sensing (WHISPERS). IEEE, 2009. http://dx.doi.org/10.1109/whispers.2009.5289098.
Full textClark, S. "Regional Tectonics & Structural Framework of Offshore Aceh's Andaman Sub-Basin, Northern Sumatra, Indonesia." In Indonesian Petroleum Association 44th Annual Convention and Exhibition. Indonesian Petroleum Association, 2021. http://dx.doi.org/10.29118/ipa21-g-30.
Full textFreed, Brian, Donald Maute, Gregory Fischer, and Matthew J. Severs. "FLUID EVOLUTION AT THE EXCELSIOR COPPER SKARN, ORGAN MOUNTAINS, NM." In Joint 52nd Northeastern Annual Section and 51st North-Central Annual GSA Section Meeting - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017ne-291083.
Full textReports on the topic "Topographic evolution of mountains"
Monger, J. W. H. Evolution of Canada's western mountains. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2008. http://dx.doi.org/10.4095/225581.
Full textMonger, J. W. H., and J. M. Journeay. Guide to the geology and tectonic evolution of the southern Coast Mountains. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1994. http://dx.doi.org/10.4095/194829.
Full textFerguson, C. A., and P. S. Simony. Preliminary Report On Structural Evolution and Stratigraphic Correlations, northern Cariboo Mountains, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1991. http://dx.doi.org/10.4095/132503.
Full textNuss, Wendell A., and Douglas K. Miller. Evolution of Low-level Flow Patterns in Littoral Regions When Extratropical Marine Cyclones Encounter Coastal Mountains. Fort Belvoir, VA: Defense Technical Information Center, September 2000. http://dx.doi.org/10.21236/ada610253.
Full textNuss, Wendell A., and Douglas K. Miller. Evolution of Low-level Flow Patterns in Littoral Regions when Extratropical Marine Cyclones Encounter Coastal Mountains. Fort Belvoir, VA: Defense Technical Information Center, September 1999. http://dx.doi.org/10.21236/ada630672.
Full textBrodie, Katherine, Ian Conery, Nicholas Cohn, Nicholas Spore, and Margaret Palmsten. Spatial variability of coastal foredune evolution, part A : timescales of months to years. Engineer Research and Development Center (U.S.), July 2021. http://dx.doi.org/10.21079/11681/41322.
Full textRogers, J. A. Structural evolution of the central Shublik Mountains and Ignek Valley, Arctic National Wildlife Refuge, northeastern Brooks Range, Alaska. Alaska Division of Geological & Geophysical Surveys, 1988. http://dx.doi.org/10.14509/1393.
Full textThompson, R. I. Stratigraphy, tectonic evolution and structural analysis of the Halfway River map area (94B), northern Rocky Mountains, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127002.
Full textMeigs, A. J. Structural evolution of the eastern Sadlerochit Mountains, northeastern Brooks Range, Alaska: A preliminary report on the summer 1986 field season. Alaska Division of Geological & Geophysical Surveys, 1986. http://dx.doi.org/10.14509/1281.
Full textSimandl, G. J., R. J. D'Souza, S. Paradis, and J. Spence. Rare-earth element content of carbonate minerals in sediment-hosted Pb-Zn deposits, southern Canadian Rocky Mountains. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/328001.
Full text