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Relevant bibliographies by topics / Glacial landforms – New Hampshire

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Academic literature on the topic 'Glacial landforms – New Hampshire'

Author: Grafiati

Published: 4 June 2021

Last updated: 1 February 2022

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Journal articles on the topic "Glacial landforms – New Hampshire"

1

Lesemann, Jerome-Etienne, Jan A. Piotrowski, and Wojciech Wysota. "“Glacial curvilineations”: New glacial landforms produced by longitudinal vortices in subglacial meltwater flows." Geomorphology 120, no. 3-4 (2010): 153–61. http://dx.doi.org/10.1016/j.geomorph.2010.03.020.

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Stojilković, Borut. "The traces of the last pleistocene glacial maximum in the eastern Kamnik-Savinja Alps." Dela, no. 1 (December 30, 2017): 127–41. http://dx.doi.org/10.4312/dela.47.1.127-141.

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The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacial Maximum (LGM). The glacial landforms mentioned by the previous researchers and other landforms in the area were examined, gemorphologically mapped, morphographically and morphometrically analysed and a new map of the extent of the LGM was produced. The research revealed several glaciers in the area and that their sizes differed, primarily depending on the slope inclination direction.

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Stojilković, Borut. "The traces of the last pleistocene glacial maximum in the eastern Kamnik-Savinja Alps." Dela, no. 47 (December 30, 2017): 127–41. http://dx.doi.org/10.4312/dela.47.127-141.

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The area of the eastern Kamnik-Savinja Alps was glaciated in the time of the Last Pleistocene Glacial Maximum (LGM). The glacial landforms mentioned by the previous researchers and other landforms in the area were examined, gemorphologically mapped, morphographically and morphometrically analysed and a new map of the extent of the LGM was produced. The research revealed several glaciers in the area and that their sizes differed, primarily depending on the slope inclination direction.

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4

Rosa, Eduardo Luiz Menozzo da, Fernando Farias Vesely, and Almério Barros França. "A review on late Paleozoic ice-related erosional landforms in the Paraná Basin: origin and paleogeographical implications." Brazilian Journal of Geology 46, no. 2 (2016): 147–66. http://dx.doi.org/10.1590/2317-4889201620160050.

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ABSTRACT: The Late Paleozoic Ice Age is recorded in the Paraná Basin as glacial deposits, deformational features and ice-related erosional landforms of the Itararé Group. Erosional landforms are often employed to build paleogeographic models that depict the location of ice masses and paleo ice-flow directions. This paper provides a review of the literature and new data on micro- to meso-scale ice-related, erosional landforms of the Paraná Basin. Examined landforms can be placed into four broad categories based on their mode of origin. Subglacial landforms on rigid substrates occur on the Preca

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5

Anderson, Roger Y., Bruce D. Allen, and Kirsten M. Menking. "Geomorphic Expression of Abrupt Climate Change in Southwestern North America at the Glacial Termination." Quaternary Research 57, no. 3 (2002): 371–81. http://dx.doi.org/10.1006/qres.2002.2323.

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AbstractEolian and subaqueous landforms composed of gypsum sand provide geomorphic evidence for a wet episode at the termination of glacial climate in southwestern North America. Drying of pluvial Lake Estancia, central New Mexico, occurred after ca. 12,000 14C yr B.P. Thereafter, eolian landforms on the old lake floor, constructed of gypsum sand, were overridden by rising lake water, modified by subaqueous processes, and organized into beach ridges along the lake's eastern shore. Preservation of preexisting eolian landforms in the shallow lake suggests abupt changes in lake level and climate.

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Jamšek Rupnik, Petra, Manja Žebre, and Giovanni Monegato. "Late Quaternary evolution of the sedimentary environment in Modrejce near Most na Soči (Soča Valley, Julian Alps)." Geologija 63, no. 2 (2020): 295–309. http://dx.doi.org/10.5474/geologija.2020.022.

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Geomorphological and geological mapping have long been used to study the glacial history of the Slovenian Alps, but many uncertainties remain regarding the time and extent of Pleistocene glaciations there. Glacial landforms and undisturbed glacial deposits are rare in the areas of the former glacier terminus, especially in the Soča Valley, where large discrepancies in the interpretation of the extent of the former Soča Glacier have been reported. Early studies proved inconclusive as to whether one or two glaciations extended into the Soča Valley as far as Most na Soči. In order to answer this

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O'Regan, Matt, Jan Backman, Natalia Barrientos, et al. "The De Long Trough: a newly discovered glacial trough on the East Siberian continental margin." Climate of the Past 13, no. 9 (2017): 1269–84. http://dx.doi.org/10.5194/cp-13-1269-2017.

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Abstract. Ice sheets extending over parts of the East Siberian continental shelf have been proposed for the last glacial period and during the larger Pleistocene glaciations. The sparse data available over this sector of the Arctic Ocean have left the timing, extent and even existence of these ice sheets largely unresolved. Here we present new geophysical mapping and sediment coring data from the East Siberian shelf and slope collected during the 2014 SWERUS-C3 expedition (SWERUS-C3: Swedish – Russian – US Arctic Ocean Investigation of Climate-Cryosphere-Carbon Interactions). The multibeam bat

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8

HALL, Adrian M., Jon W. MERRITT, E. Rodger CONNELL, and Alun HUBBARD. "Early and Middle Pleistocene environments, landforms and sediments in Scotland." Earth and Environmental Science Transactions of the Royal Society of Edinburgh 110, no. 1-2 (2018): 5–37. http://dx.doi.org/10.1017/s1755691018000713.

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ABSTRACTThis paper reviews the changing environments, developing landforms and terrestrial stratigraphy during the Early and Middle Pleistocene stages in Scotland. Cold stages after 2.7 Ma brought mountain ice caps and lowland permafrost, but larger ice sheets were short-lived. The late Early and Middle Pleistocene sedimentary record found offshore indicates more than 10 advances of ice sheets from Scotland into the North Sea but only 4–5 advances have been identified from the terrestrial stratigraphy. Two primary modes of glaciation, mountain ice cap and full ice sheet modes, can be recognise

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9

Miller, Norton G., and Ray W. Spear. "Late-Quaternary history of the alpine flora of the New Hampshire White Mountains." Géographie physique et Quaternaire 53, no. 1 (2002): 137–57. http://dx.doi.org/10.7202/004854ar.

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Abstract A distinctive flora of 73 species of vascular plants and numerous bryophytes occurs in the ca. 20 km 2 of alpine tundra in the White Mountains, New Hampshire. The late- Quaternary distribution of these plants, many of which are disjuncts, was investigated by studies of pollen and plant macrofossils from lower Lakes of the Clouds (1 542 m) in the alpine zone of Mount Washington. Results were compared with pollen and macrofossils from lowland late-glacial deposits in western New England. Lowland paleofloras contained fossils of 43 species of vascular plants, 13 of which occur in the con

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Thompson, Woodrow B. "History of research on glaciation in the White Mountains, New Hampshire (U.S.A.)." Géographie physique et Quaternaire 53, no. 1 (2002): 7–24. http://dx.doi.org/10.7202/004879ar.

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Abstract The glacial geology of the White Mountains in New Hampshire has been the subject of many investigations since the 1840's. A series of controversies evolved during this period. First was the question of what geologic processes were responsible for eroding the bedrock and depositing the cover of surficial sediments. By the 1860's, the concept of glaciation replaced earlier theories invoking floods and icebergs. Research in the late 1800's concerned the relative impact of continental versus local glaciation. Some workers believed that surficial deposits in northern New Hampshire were the

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Dissertations / Theses on the topic "Glacial landforms – New Hampshire"

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LeNoir, James. "Post-Glacial Sedimentation in Ossipee Lake, New Hampshire:." Thesis, Boston College, 2019. http://hdl.handle.net/2345/bc-ir:108650.

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Thesis advisor: Noah P. Snyder<br>Land cover and climate changes, attributed to natural and anthropogenic forcings, cause deviations in geomorphic processes that act to deliver sediment from watersheds to lakes. In New England, contradictory evidence exists as to the influence of deforestation associated with EuroAmerican settlement and major flood events on watershed erosion rates over the past ~250 years. Through combining sediment core analysis from Ossipee Lake, New Hampshire with geomorphic analysis of the Ossipee Lake watershed, this study quantifies Holocene through Anthropocene watersh

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2

Hyatt, Olivia Marie. "Insights into New Zealand glacial processes from studies of glacial geomorphology and sedimentology in Rakaia and other South Island valleys : a thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Geology, University of Canterbury /." 2009. http://hdl.handle.net/10092/3699.

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Pugh, J. M. "The late Quaternary environmental history of the Lake Heron Basin, Mid Canterbury, New Zealand : a thesis submitted in partial fulfilment of the requirements for the degree of Master of Science in Geology in the University of Canterbury /." 2008. http://hdl.handle.net/10092/1766.

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Allen, Simon K. "Geomorphic hazards associated with glacial change, Aoraki/Mount Cook region, Southern Alps, New Zealand : a thesis submitted in partial fulfilment of the requirements for the degree of Doctor of Philosophy in Geography in the University of Canterbury /." 2009. http://hdl.handle.net/10092/3087.

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Evans, M. D. "A geomorphological and sedimentological investigation into the glacial deposits of the Lake Clearwater basin, Mid Canterbury, New Zealand : a thesis submitted in partial fulfilment of the requirements for the degree of Master of Science in Geology in the University of Canterbury /." 2008. http://hdl.handle.net/10092/1531.

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Books on the topic "Glacial landforms – New Hampshire"

1

Sperduto, Daniel D. The nature of New Hampshire: Natural communities of the granite state. University of New Hampshire Press, 2011.

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2

Harte, Philip T. Geohydrology of, and simulation of ground-water flow in, the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire. U.S. Dept. of the Interior, U.S. Geological Survey, 1992.

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3

Harte, Philip T. Effects of historical withdrawals on advective transport of contaminated ground waters in a glacial-drift aquifer, Milford, New Hampshire. U.S. Geological Survey, 1997.

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4

Tiedeman, Claire R. Numerical simulation of ground-water flow through glacial deposits and crystalline bedrock in the Mirror Lake area, Grafton County, New Hampshire. U.S. G.P.O., 1997.

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5

Johnson, Carole D. Ground-water quality data for the Saco River Valley glacial aquifer from Bartlett, New Hampshire to Fryeburg, Maine: July 1984 through November 1985. U.S. Dept. of the Interior, Geological Survey, 1986.

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6

Johnson, Carole D. Ground-water quality data for the Saco River Valley glacial aquifer from Bartlett, New Hampshire to Fryeburg, Maine: July 1984 through November 1985. U.S. Dept. of the Interior, Geological Survey, 1986.

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7

Johnson, Carole D. Ground-water quality data for the Saco River Valley glacial aquifer from Bartlett, New Hampshire to Fryeburg, Maine: July 1984 through November 1985. U.S. Dept. of the Interior, Geological Survey, 1986.

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8

Harte, Philip T. Construction and calibration of numerical ground-water-flow models of the western half of the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire. U.S. Dept. of the Interior, U.S. Geological Survey, 1999.

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9

Johnson, Carole D. Ground-water quality data for the Saco River Valley glacial aquifer from Bartlett, New Hampshire to Fryeburg, Maine: July 1984 through November 1985. U.S. Dept. of the Interior, Geological Survey, 1986.

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10

Johnson, Carole D. Ground-water quality data for the Saco River Valley glacial aquifer from Bartlett, New Hampshire to Fryeburg, Maine: July 1984 through November 1985. U.S. Dept. of the Interior, Geological Survey, 1986.

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Book chapters on the topic "Glacial landforms – New Hampshire"

1

Evans, David J. A. "9. Glaciers, humans, and enduring ice." In Glaciation: A Very Short Introduction. Oxford University Press, 2018. http://dx.doi.org/10.1093/actrade/9780198745853.003.0009.

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A knowledge of glaciation is important because it provides us with an understanding of glaciers as Earth surface systems face climate change and of the glacial materials beneath the surface. Crucial are glacier-related hazards impacting directly on human society and glacial landforms and sediments lying at the surface of some of the most densely populated parts of our planet. ‘Glaciers, humans, and enduring ice’ considers glacial hazards, such as glacial lake outburst floods, and important engineering considerations, including sediment failure and seepage. It discusses the valuable legacy of past glaciations and asks if Earth is entering a new phase of ice-free conditions, the like of which it has not endured for more than 35 million years.

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2

Peterson, Jim A., S. Chandra, and Christian Lundberg. "Landforms from the Quaternary glaciation of Papua New Guinea: an overview of ice extent during the Last Glacial Maximum." In Developments in Quaternary Sciences. Elsevier, 2004. http://dx.doi.org/10.1016/s1571-0866(04)80136-2.

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Dunbar, James S. "Early Paleoindian Potentials on the Continental Shelf in the Southeastern United States." In New Directions in the Search for the First Floridians. University Press of Florida, 2019. http://dx.doi.org/10.5744/florida/9781683400738.003.0007.

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As two researchers with significant credibility in the study of early Florida, James S. Dunbar and David K. Thulman evaluate the potential for Paleoindian research on the Southeastern Continental Shelf (SECS) of the U.S. In this chapter, they discuss ways to explore Clovis and pre-Clovis landscapes (or, as they collectively call them, early Paleoindian sites) in the SECS and how researchers might narrow their search and increase their chances of finding Clovis and pre-Clovis sites offshore. In doing so, they complement Halligan’s chapter in this volume (chapter 3) on exploring Florida’s inland waters for submerged sites. They evaluate the strategies available: thoughtful searching for both analogous natural and manmade landforms and serendipity. Of the two, the second approach has arguably produced the most sites so far. Dunbar and Thulman explore the “thermal enclave hypothesis” of Russell et al (2009) and follow David Webb’s earlier work on his idea for a climatically propitious region that could support animals and plants through the Last Glacial Maximum (LGM). Dunbar and Thulman further suggest the possibility of a shellfish/marine adaptation by early-Paleoindian-period colonists. They posit that finding such sites would open new windows into the study on the behaviors of the early Floridians.

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4

Battiau-Queney, Yvonne. "French Alps and Alpine Forelands." In The Physical Geography of Western Europe. Oxford University Press, 2005. http://dx.doi.org/10.1093/oso/9780199277759.003.0024.

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The French Alps are the western part of the 1,200-km-long Alpine range extending eastward to the Vienna basin. They have the highest summits of the range, in the Mont-Blanc massif (4,807 m a.s.l.). In France, the chain has an arcuate form, convex to the north and west. It lies between Lake Geneva (46° 25′ N) and the Mediterranean coast (approximately 43° 35′ N). The Rhône valley forms a clear geological and morphological western limit. To the north (towards the Jura range) and the south-west (towards the ridges of Provence) the boundary is not so well defined. The French Alps and Alpine forelands have been thoroughly studied for over a century by many researchers from the Universities of Grenoble, Lyons, Aix-en-Provence, Nice, and Chambéry. First, it is necessary to outline the great diversity of landforms in relationship to the complex geological history, tectonics, and lithology. The importance of the Alpine karst landforms and caves must be emphasized; studies of these forms have been extended substantially in the last twenty years and they give many new insights into the Plio-Pleistocene tectonics and climates of this region. The past and present role of glaciers is another important topic in this chapter. From recent studies, we now have a much better knowledge of the transition from the last glacial period to the Holocene. It was impossible to write a chapter on the Alps and ignore the fact that the inhabitants of the Alps have to cope with many permanent natural hazards. The chapter ends with a short synthesis of the main morphogenic systems, which characterize the French Alps and forelands. In the north, the climate is oceanic and precipitation is evenly distributed throughout the year. A high relief, with landforms oriented transverse to the general western atmospheric circulation, results in a great variety of regional climates: from west to east, the continental effect is marked by a decreasing precipitation at the same altitude. Exposure and altitude combine to create contrasting local climates. Temperature inversion is frequent, especially when cold air is trapped in deep valleys.

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Conference papers on the topic "Glacial landforms – New Hampshire"

1

LeNoir, James, Noah P. Snyder, and Timothy L. Cook. "POST-GLACIAL SEDIMENTATION IN OSSIPEE LAKE, NEW HAMPSHIRE." In 54th Annual GSA Northeastern Section Meeting - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019ne-328669.

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2

Thompson, Woodrow, and Gregory Barker. "Glacial Deposits and Late-Glacial to PostGlacial Alluvial Fans in the Northwestern White Mountians, New Hampshire." In New England Intercollegiate Geological Conference. Bates College, 2017. http://dx.doi.org/10.26780/2017.001.0009.

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3

Smith, Chelsea, and Lindley S. Hanson. "LATE PLEISTOCENE GLACIAL STRATIGRAPHY OF THE COLD RIVER VALLEY, SOUTH ACWORTH, NEW HAMPSHIRE." 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-289904.

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Allen, Rachel M., and J. Bradford Hubeny. "GEOPHYSICAL ANALYSIS OF A POORLY DRAINED GLACIAL DELTA PLAIN IN ACWORTH, NEW HAMPSHIRE." 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-291384.

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LeNoir, James, Timothy L. Cook, and Noah P. Snyder. "PRELIMINARY EXAMINATION OF POST-GLACIAL SEDIMENTATION IN OSSIPEE LAKE, NEW HAMPSHIRE: LAND-USE VERSUS CLIMATE CHANGE." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310982.

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6

D. Ayotte, Joseph. "Use Of Ground-Penetrating Radar To Determine The Depositional Environment Of Glacial Deposits In Southern New Hampshire." In 7th EEGS Symposium on the Application of Geophysics to Engineering and Environmental Problems. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.208.1994_040.

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Ayotte, Joseph D. "Use of Ground‐Penetrating Radar to Determine the Depositional Environment of Glacial Deposits in Southern New Hampshire." In Symposium on the Application of Geophysics to Engineering and Environmental Problems 1994. Environment and Engineering Geophysical Society, 1994. http://dx.doi.org/10.4133/1.2922094.

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Dix, Monica, Josh W. Borella, Katherine Pedley, and Stefan Winkler. "GEOMORPHIC MAPPING AND ANALYSIS OF GLACIAL LANDFORMS TO UNDERSTAND THE DEVELOPMENT AND DEFINING CHARACTERISTICS OF ‘GLACIAL’ LAKE SPEIGHT IN THE MIDDLE WAIMAKARIRI RIVER OF THE SOUTHERN ALPS, NEW ZEALAND." In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-341292.

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9

Davis, P. Thompson, Jeremy D. Shakun, Paul R. Bierman, Allie Jo Koester, Lee B. Corbett, and Christopher T. Halsted. "BOISE ROCK, NOT THE GLACIAL ERRATIC THAT WE THOUGHT, BUT RATHER PART OF THE LANDSLIDE HISTORY OF FRANCONIA NOTCH, NEW HAMPSHIRE." In 53rd Annual GSA Northeastern Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018ne-310785.

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Reports on the topic "Glacial landforms – New Hampshire"

1

Geohydrology of, and simulation of ground-water flow in, the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire. US Geological Survey, 1992. http://dx.doi.org/10.3133/wri914177.

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2

Hydrogeology, water quality, and effects of increased municipal pumpage of the Saco River Valley glacial aquifer; Bartlett, New Hampshire to Fryeburg, Maine. US Geological Survey, 1990. http://dx.doi.org/10.3133/wri884179.

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