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Books on the topic 'Glacial environments'

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

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1

Glacial environments. Vancouver: UBC Press, 1994.

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2

Glacial environments. London: UCL Press, 1994.

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3

John, Shaw, Smith Norman D, and Society of Economic Paleontologists and Mineralogists., eds. Glacial sedimentary environments. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1985.

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4

Andrew, Goudie, Goudie Andrew, and Parker Adrian 1969-, eds. Global environments through the Quaternary: Exploring environmental change. Oxford: Oxford University Press, 2007.

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5

Midwest Friends of the Pleistocene. Field Conference, ed. Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: The Altonian revised. Champaign Ill: Illinois Dept. of Energy and Natural Resources, State Geological Survey Division, 1985.

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6

Midwest Friends of the Pleistocene. Field Conference. Illinoian and Wisconsinan stratigraphy and environments in northern Illinois: The Altonian revised. Champaign Ill: Illinois Dept. of Energy and Natural Resources, State Geological Survey Division, 1985.

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7

Dredge, L. A. Glacial and environmental geology of northeastern Manitoba. Ottawa, Canada: Geological Survey of Canada, 1992.

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8

Chang Jiang San Xia di qu xin gou zao di zhi zai hai he di si ji bing chuan zuo yong yu San xia xing cheng tu ji: An atlas of neotectonics geological hazards and quaternary glacial geomorphy in the Yangtze three georges area. Huhan Shi: Hubei ke xue ji shu chu ban she, 2001.

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9

Knight, Peter G., ed. Glacier Science and Environmental Change. Malden, MA, USA: Blackwell Publishing, 2006. http://dx.doi.org/10.1002/9780470750636.

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10

The periglacial environment. 2nd ed. Harlow, Essex: Longman, 1996.

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11

Environmental change. 3rd ed. Oxford [England]: Clarendon Press, 1992.

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12

Ukraintseva, Valentina V. Vegetation cover and environment of the "mammoth epoch" in Siberia. [Hot Springs, S.D.?: Mammoth Site of Hot Springs?, 1992.

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13

Menzies, John. Glacial Environments. Butterworth-Heinemann Ltd, 1995.

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14

Menzies, John, and Jaap van der Meer. Past Glacial Environments. Elsevier Science & Technology Books, 2017.

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15

M, Ashley Gail, Shaw John, Smith Norman D, and Society of Economic Paleontologists and Mineralogists., eds. Glacial sedimentary environments. Tulsa, Okla: Society of Economic Paleontologists and Mineralogists, 1985.

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16

Past Glacial Environments. Elsevier, 2018. http://dx.doi.org/10.1016/c2014-0-04002-6.

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17

Menzies, John. Past Glacial Environments: Sediments, Forms and Techniques: Glacial Environments Volume Two (Glacial Environments ; V. 2). Butterworth-Heinemann, 1996.

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18

Menzies, John. Modern Glacial Environments: Processes, Dynamics and Sediments (Glacial Environments ; V. 1). Butterworth-Heinemann, 1995.

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19

John, Menzies, ed. Modern and past glacial environments. Oxford: Butterworth-Heinemann, 2002.

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20

Modern and Past Glacial Environments. Elsevier, 2002. http://dx.doi.org/10.1016/b978-0-7506-4226-2.x5000-4.

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21

Glacimarine environments. London: Geological Society, 1990.

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22

Menzies, J. Glacial Environments: Processes, Sediments and Landforms. Elsevier Science, 1993.

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23

John, Menzies, ed. Modern glacial environments: Processes, dynamics, and sediments. Boston: Butterworth-Heinemann, 1995.

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24

Menzies, John. Modern Glacial Environments: Processes, Dynamics, and Sediments. Pergamon, 1995.

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25

John, Menzies, ed. Modern glacial environments: Processes, dynamics, and sediments. Kidlington, England: Pergamon, 1994.

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26

Menzies, John. Modern Glacial Environments Processes, Dynamics and Sediments. Butterworth-Heinemann, 1995.

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27

Past glacial environments: Sediments, forms, and techniques. Boston: Butterworth-Heinemann, 1995.

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28

), Menzies John (Ed, ed. Modern Glacial Environments: Processes, Dynamics and Sediments. Butterworth-Heinemann, 1996.

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29

John, Menzies, ed. Past glacial environments: Sediments, forms, and techniques. Oxford: Butterworth-Heinemann, 1996.

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30

Manuel, Vilaplana Joan, and Gray James, eds. Glacial and periglacial geomorphology in mountain environments. Berlin: Gebrüder Borntraeger, 2007.

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31

Glacial and Periglacial Environments (Access to Geography). Hodder Murray, 2004.

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32

Menzies, John. Modern Glacial Environments: Processes, Dynamics, and Sediments. Pergamon, 1995.

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33

Menzies. Glacial Environments Processes Sediments and Land Forms. Pergamon Pr, 1995.

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34

Microbiology and biogeochemistry of glacial and permafrost environments. Cambridge, UK: International Glaciological Society, 2010.

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35

Menzies, John. Modern and Past Glacial Environments Revised Student Edition. Butterworth-Heinemann, 2002.

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36

Cold Environments: Processes and Outcomes (Epics). Nelson Thornes, 2002.

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37

A, Dowdeswell J., and Scourse James D, eds. Glacimarine environments: Processes and sediments. London: Geological Society, 1990.

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38

Glacial Sedimentary Environments (Sepm Short Course Notes, No 16). Sepm Society for Sedimentary, 1985.

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39

I, Mead Jim, Meltzer David J, Society for American Archaeology, and University of Maine at Orono. Center for the Study of Early Man., eds. Environments and extinctions: Man in late glacial North America. Orono, Me: Center for the Study of Early Man, University of Maine at Orono, 1985.

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40

Vuorinen, Ilppo. Post-Glacial Baltic Sea Ecosystems. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.675.

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Post-glacial aquatic ecosystems in Eurasia and North America, such as the Baltic Sea, evolved in the freshwater, brackish, and marine environments that fringed the melting glaciers. Warming of the climate initiated sea level and land rise and subsequent changes in aquatic ecosystems. Seminal ideas on ancient developing ecosystems were based on findings in Swedish large lakes of species that had arrived there from adjacent glacial freshwater or marine environments and established populations which have survived up to the present day. An ecosystem of the first freshwater stage, the Baltic Ice Lake initially consisted of ice-associated biota. Subsequent aquatic environments, the Yoldia Sea, the Ancylus Lake, the Litorina Sea, and the Mya Sea, are all named after mollusc trace fossils. These often convey information on the geologic period in question and indicate some physical and chemical characteristics of their environment. The ecosystems of various Baltic Sea stages are regulated primarily by temperature and freshwater runoff (which affects directly and indirectly both salinity and nutrient concentrations). Key ecological environmental factors, such as temperature, salinity, and nutrient levels, not only change seasonally but are also subject to long-term changes (due to astronomical factors) and shorter disturbances, for example, a warm period that essentially formed the Yoldia Sea, and more recently the “Little Ice Age” (which terminated the Viking settlement in Iceland).There is no direct way to study the post-Holocene Baltic Sea stages, but findings in geological samples of ecological keystone species (which may form a physical environment for other species to dwell in and/or largely determine the function of an ecosystem) can indicate ancient large-scale ecosystem features and changes. Such changes have included, for example, development of an initially turbid glacial meltwater to clearer water with increasing primary production (enhanced also by warmer temperatures), eventually leading to self-shading and other consequences of anthropogenic eutrophication (nutrient-rich conditions). Furthermore, the development in the last century from oligotrophic (nutrient-poor) to eutrophic conditions also included shifts between the grazing chain (which include large predators, e.g., piscivorous fish, mammals, and birds at the top of the food chain) and the microbial loop (filtering top predators such as jellyfish). Another large-scale change has been a succession from low (freshwater glacier lake) biodiversity to increased (brackish and marine) biodiversity. The present-day Baltic Sea ecosystem is a direct descendant of the more marine Litorina Sea, which marks the beginning of the transition from a primeval ecosystem to one regulated by humans. The recent Baltic Sea is characterized by high concentrations of pollutants and nutrients, a shift from perennial to annual macrophytes (and more rapid nutrient cycling), and an increasing rate of invasion by non-native species. Thus, an increasing pace of anthropogenic ecological change has been a prominent trend in the Baltic Sea ecosystem since the Ancylus Lake.Future development is in the first place dependent on regional factors, such as salinity, which is regulated by sea and land level changes and the climate, and runoff, which controls both salinity and the leaching of nutrients to the sea. However, uncertainties abound, for example the future development of the Gulf Stream and its associated westerly winds, which support the sub-boreal ecosystems, both terrestrial and aquatic, in the Baltic Sea area. Thus, extensive sophisticated, cross-disciplinary modeling is needed to foresee whether the Baltic Sea will develop toward a freshwater or marine ecosystem, set in a sub-boreal, boreal, or arctic climate.
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41

Dowdeswell, J. A. Glacimarine Environments: Processes and Sediments (Geological Society Special Publication). Amer Assn of Petroleum Geologists, 1990.

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42

Hewitt, Kenneth. Glaciers of the Karakoram Himalaya: Glacial Environments, Processes, Hazards and Resources. Springer, 2016.

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43

Glaciers Of The Karakoram Himalaya Glacial Environments Processes Hazards And Resources. Springer, 2013.

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44

Global Environments Through the Quaternary: Exploring Evironmental Change. Oxford University Press, 2013.

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45

Depositional environments and correlation problems of the Wedron Formation (Wisconsinan) in northeastern Illinois. Champaign, Ill. (615 E. Peabody Dr., Champaign 61820): Illinois State Geological Survey, 1985.

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46

(Editor), Robson Bonnichsen, and Karen L. Turnmire (Editor), eds. Ice Age Peoples Of North America: Environments, Origins, and Adaptations. Texas A&M University Press, 2005.

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47

Mead, Jim I., and David J. Meltzer. Environments and Extinctions: Man in Late Glacial North America (Symposium Series, Peopling of the Americas). Center for the Study of the First, 1986.

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48

Oregon State University Center for the S (Corporate Author), Robson Bonnichsen (Editor), and Karen L. Turnmire (Editor), eds. Ice Age Peoples of North America: Environments, Origins, and Adaptations. Oregon State University Press, 1999.

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49

Marine geology of Hudson Strait and Ungava Bay, eastern Arctic Canada: Late Quaternary sediments, depositional environments, and late glacial-deglacial history derived from marine and terrestrial studies. Ottawa, Ont: Geological Survey of Canada, 2001.

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50

Jacobsen, Dean, and Olivier Dangles. Living conditions in high altitude waters. Oxford University Press, 2017. http://dx.doi.org/10.1093/oso/9780198736868.003.0003.

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Chapter 3 deals with the abiotic environment in high altitude lakes and streams worldwide. It searches for general patterns in relation to altitude, without overlooking the enormous variability, both temporally as well as at small and large spatial scales. Overall, environmental conditions in high altitude waters may be regarded as harsh. Indeed, certain features such as low temperature, low oxygen pressure, and high ultraviolet radiation (all a direct result of high altitude) as well as transparent and ion-poor waters with low nutrient concentrations are typical of high altitude aquatic systems. However, streams and lakes turbid from inflow of glacial meltwater loaded with glacial mineral flour and peatbogs with deep brown water from a high concentration of coloured dissolved organic matter are equally prominent. So, evidently, environmental conditions in aquatic systems are probably just as variable at high as at low altitudes.
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