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Dissertations / Theses on the topic 'Landforms'

Author: Grafiati

Published: 4 June 2021

Last updated: 25 July 2025

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1

Grecchi, Rosana Cristina. "Zoneamento geoambiental da região de Piracicaba - SP, com auxílio de geoprocessamento." Universidade de São Paulo, 1998. http://www.teses.usp.br/teses/disponiveis/18/18132/tde-06102017-110122/.

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O trabalho consiste na realização de um zoneamento geoambiental para a região de Piracicaba-SP, com base na análise de variáveis ambientais, principalmente de atributos do meio físico, tais como: geologia, solos, hidrologia, etc. A área estudada localiza-se na bacia hidrográfica do Rio Piracicaba, uma das mais importantes do estado de São Paulo e que vem apresentando intenso desenvolvimento econômico e consequentemente problemas de degradação ambiental. Este estudo foi realizado seguindo-se os pressupostos da cartografia geoambiental, mas utilizando-se também os procedimentos da cartografia ge

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2

Dilts, Thomas E. "Morphometric characterization of artificial post-mining landforms and natural landforms using a Geographic Information System." abstract and full text PDF (free order & download UNR users only), 2007. http://0-gateway.proquest.com.innopac.library.unr.edu/openurl?url_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:dissertation&res_dat=xri:pqdiss&rft_dat=xri:pqdiss:1447595.

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3

Lauder, Glen A. "Coastal landforms and sediments of the Marlborough Sounds." Thesis, University of Canterbury. Geography, 1987. http://hdl.handle.net/10092/4518.

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This thesis examines coastal form and sediments of the Marlborough Sounds, New Zealand. An important aspect of coastal behaviour in this landscape stems from linkages between catchment and coast. Focus is therefore placed on the manner in which sediment delivered from catchment sources is redistributed within the shore and offshore domains. Coastal response is shown to depend on two factors: the form of the receiving sites and the mobility of sediments within them. Investigation of coastal landforms at a range of scales identifies the framework within which sedimentation takes place. Considera

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4

Hassan, Wael. "Comparing Geomorphometric Pattern Recognition Methods for Semi-Automated Landform Mapping." Ohio University / OhioLINK, 2020. http://rave.ohiolink.edu/etdc/view?acc_num=ohiou160690391009081.

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5

George, Chinotu Franklin. "Geometries of surface and subsurface landforms and deposits in the Niger Delta." Thesis, University of Aberdeen, 2014. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?pid=211213.

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This research is focused on mapping the geometries of surface and subsurface landforms and their relationship in the Niger Delta. Landforms on the surface are studied to improve our understanding of the spatial distribution of buried landforms. GIS techniques are applied to high resolution Landsat and SPOT imagery to map surface landforms, a necessary step in order to improve and better constraint subsurface modelling. Also, attributes from three dimensional seismic data are used to map buried landforms. Both techniques are focused on mapping the spatial distribution of landforms and analysis

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6

Vere, D. M. "Depositional characteristics of ice-marginal landforms, Jotunheimen, Southern Norway." Thesis, Coventry University, 1986. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.374681.

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7

Nelson, Timothy L. "Hydrodynamic Controls on the Morphodynamic Evolution of Subaqueous Landforms." ScholarWorks@UNO, 2017. https://scholarworks.uno.edu/td/2425.

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The southern Chandeleur Islands are an ideal setting to study shoal evolution given their history of submergence and re-emergence. Here, numerical models shed light on the attendant processes contributing to shoal recovery/reemergence following a destructive storm event. Simulations of a synthetic winter storm along a cross-shore profile using Xbeach shows that convergence of wave-induced sediment transport associated with repeated passage of cold-fronts initiates aggradation, but does not lead to reemergence. A Delft3d model of the entire island chain shows that as these landforms aggrade alo

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8

Peterson, Gustaf. "The development and relative chronology of landforms at Kongsfjordhallet, Spitsbergen." Thesis, Stockholm University, Department of Physical Geography and Quaternary Geology, 2008. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-37061.

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<p>Kongsfjordhallet is situated at 79° N on the North coast of Kongsfjorden, Spitsbergen.The landscape shows a large diversity of landforms and sediments and the aim of thisstudy has been to investigate the spatial distribution and temporal differences betweenthese landforms.The most prominent landform is interpreted as a lateral moraine dividing the area fromsoutheast to northwest. This is probably a sign of a standstill during the deglaciation ofan ice-sheet glacier tongue filling the fjord. The valley-glaciers at Kongsfjordhallet haveadvanced after this event and left end moraines on top of

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9

Anderson, Dustin Carl. "How landforms and geology affect the structure of riparian areas." Thesis, Montana State University, 2012. http://etd.lib.montana.edu/etd/2012/anderson/AndersonD0812.pdf.

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Current riparian zone assessments focus on the morphological features of the stream channel and ocular vegetation measurements. This procedure fails to address the hydraulic features responsible for the floristic structure and composition of the riparian zone. We looked at how the geology and landforms function as drivers of groundwater and surface-water exchange. These can mitigate watershed processes via groundwater availability to shape riparian processes; e.g. discharge, seasonality. We hypothesized that groundwater surface-water exchange is a first order process and that it dictates ripar

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10

Sharpe, David Robert. "Glacial sediments and landforms, southern Victoria Island, Northwest Territories, Canada." Thesis, University of Ottawa (Canada), 1992. http://hdl.handle.net/10393/7846.

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Wollaston Peninsula and most of southern Victoria Island comprise Palaeozoic carbonate lowlands, scarps, and tableland situated between rises and arches of underlying Precambrian sedimentary and igneous rocks. Quaternary sediments are hummocky, thick and ice-cored near escarpments where ice flow resistance, thrusting and meltwater concentrated glacial debris; thinner, streamlined drift occurs in lowlands. Quaternary sediments are mainly Late Wisconsinan in age. Glacial sediments predominate but surficial raised marine and periglacial sediments are noted. Fluvial modification of the landscape i

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11

Sefton-Nash, Elliot. "Water-altered mineralogy and landforms in equatorial regions of Mars." Thesis, University of Bristol, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.541616.

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12

James, H. C. L. "Late Quaternary coastal landforms and associated sediments of west Cornwall." Thesis, University of Reading, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239536.

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13

Al-Garni, Abdullah Mohammed. "Image interpretation for landforms using expert systems and terrain analysis /." The Ohio State University, 1992. http://rave.ohiolink.edu/etdc/view?acc_num=osu1487777170407991.

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14

Phillips, Zachary Rockford. "Holocene Postglacial Fluvial Processes and Landforms in Low Relief Landscapes." Diss., North Dakota State University, 2020. https://hdl.handle.net/10365/32036.

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Postglacial rivers are part of the relatively young low-relief landscape system left behind by glaciers. Over time, postglacial rivers are susceptible to both minor and major channel planform changes as the Earth and its newly exposed rivers adjust to new isostatic and geomorphic equilibriums. Those planform changes result in topographic features that are well preserved among the largely unaltered landscape and offer opportunities to learn about the processes that create them. This work focuses on those minor and major planform changes and the resulting landforms, with a focus on processes eff

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15

Fontes, Silvana Brandão. "Mapeamento geotécnico com ênfase em erosões no município de Ouro Preto - MG, escala 1:5.000." Universidade de São Paulo, 1999. http://www.teses.usp.br/teses/disponiveis/18/18132/tde-23082018-145637/.

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Este trabalho consiste no estudo sistemático dos fenômenos erosivos em áreas urbanas, tendo como objetivo a avaliação e identificação das causas destes fenômenos no município de Ouro Preto - MG. Como ferramenta principal utilizou-se o mapeamento geotécnico, na escala de detalhe 1:5.000 em uma área de aproximadamente 6 Km2, com o objetivo de fazer uma caracterização geotécnica das feições erosivas existentes na área. Buscou-se também fazer um levantamento de dados geológicos, geomorfológicos e de influência antrópica. Os resultados obtidos através deste mapeamento possibilitaram a elaboração do

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16

Chandra, Shobhit. "Fluvial landforms and sediments in the north-central Gangetic Plain, India." Thesis, University of Cambridge, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.309855.

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17

Channon, Heather. "Multiscale analysis of the landforms and sediments of palaeo-ice streams." Thesis, Queen Mary, University of London, 2013. http://qmro.qmul.ac.uk/xmlui/handle/123456789/8398.

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Ice streams play a fundamental role in the stability and dynamics of ice sheets. They are defined by their rapid flow and this is enabled by conditions and processes at the icebed interface. A significant limitation to our understanding of this environment is that most studies, of both contemporary and palaeo-ice streams, have focussed on only one or two, discrete spatial scales of analysis and so integration between scales is restricted. This thesis investigates palaeo-ice streams at multiple scales in order to examine their subglacial processes and characteristics, and to assess the links be

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18

Hughes, Anna L. C. "The last British Ice Sheet : a reconstruction based on glacial landforms." Thesis, University of Sheffield, 2008. http://etheses.whiterose.ac.uk/16363/.

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The last British Ice Sheet has been a focus of research for over a century, and yet we have only a generalised picture of its extent and internal geometry. This is a remarkable situation compared to knowledge of the larger former ice sheets of North America and Fennoscandia. The central tenet of this thesis is that the glacial landform record has been neglected as a source of spatial information, hindering our attempts to reconstruct the characteristics of the ice sheet. This motivated systematic mapping of glacial landforms (subglacial bedforms, moraines, eskers, and meltwater channels) for t

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19

von, Holdt Johanna R. C. "Aeolian dust emission dynamics across spatial scales: landforms, controls and characteristics." Doctoral thesis, University of Cape Town, 2018. http://hdl.handle.net/11427/28364.

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Variable erodibility (surface characteristics) and erosivity factors (meteorological conditions) result in dust emission dynamics being complex in both space and time. Accounting for localscale surface variability is critical to our understanding of dust emitting processes. This study identifies mineral dust using remote sensing, establishes emission thresholds through field measurements and identifies particle chemistry for major dust sources in the Central Namib Desert. Examining over 2000 Landsat images over a period from 1972 to 2016, identified 40 days of visually detectable dust, origina

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20

Arnold, Billie J. "A Comparitive Analysis of Glacial Landforms: Skeidararsandur Iceland and Northwestern Pennsylvania." Kent State University / OhioLINK, 2014. http://rave.ohiolink.edu/etdc/view?acc_num=kent1389103411.

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21

Faivre, Sanja. "Landforms and tectonics of the Velebit mountain rance (Outer Dinarides, Croatia)." Clermont-Ferrand 2, 2000. http://www.theses.fr/2000CLF20005.

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Cette étude s'inscrit dans le cadre de la géomorphologie structurale. Le but en est d'apporter une explication à la répartition des formes du relief par rapport aux nouvelles conceptions tectoniques. Pour examiner ce lien, les déformations et les contraintes ont été calculées à partir des dolines des crêtes. L'intérêt de la montagne de Velebit tient à sa grande densité en formes karstiques et à sa dynamique tectonique récente. Ce travail a permis de dégager une nouvelle méthodologie en la matière. 2 méthodes géologiques, la méthode de centre et celle de projection, ont été adaptées aux conditi

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22

Cannon, Charles Matthew. "Landforms along the Lower Columbia River and the Influence of Humans." PDXScholar, 2015. https://pdxscholar.library.pdx.edu/open_access_etds/2231.

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River systems, such as the Columbia River in the Pacific Northwest, USA have been influenced by human activities, resulting in changes to the physical processes that drive landform evolution. This work describes an inventory of landforms along the Columbia River estuary between the Pacific Ocean and Bonneville Dam in Oregon and Washington. Groupings of landforms are assigned to formative process regimes that are used to assess historical changes to floodplain features. The estuary was historically a complex system of channels with a floodplain dominated by extensive tidal wetlands in the lower

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23

Lo, Edward Limin. "FLUVIAL-LACUSTRINE PROCESSES SHAPING THE LANDFORMS OF THE DISTAL PARAGUAY FLUVIAL MEGAFAN." UKnowledge, 2017. http://uknowledge.uky.edu/ees_etds/54.

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Tropical wetlands such as the Pantanal help regulate global biogeochemical cycles, but climate change is modifying these environments. Controls on environmental changes can potentially be assessed from ancient, well-dated lacustrine sedimentary records. An integrated field and laboratory approach was undertaken to study the limnogeology of Lake Uberaba in the northern Pantanal, and test whether the lake has preserved a reliable record of environmental change in its strata. This study was designed to understand how the basin accumulates sediment and to assess its sensitivity to hydroclimatic va

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24

Scott, David Alan. "On active layer processes and landforms in western Dronning Maud Land, Antarctica." Thesis, Rhodes University, 2015. http://hdl.handle.net/10962/d1019757.

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Permafrost is a variable in Antarctic terrestrial ecosystems, and the role it plays in the cryosphere is not well understood. There is much still to be learnt about the thermal state, physical properties, thickness and age of permafrost in Western Dronning Maud Land (WDML). Active layer dynamics and observed change over time have the potential to improve our knowledge of climate change. Understanding the effects of a warming climate on permafrost can also be of benefit to infrastructure, especially in areas with a large amount of frozen ground such as Scandinavia, Canada and Russia. Active lay

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25

Voelker, Martin [Verfasser]. "Glacial and Fluvial Evolution of Landforms in Hellas Planitia, Mars / Martin Voelker." Berlin : Freie Universität Berlin, 2018. http://d-nb.info/1170877036/34.

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26

Magri, Rômulo Amaral Faustino. "Análise da suscetibilidade à erosão da região do Médio Rio Grande (MG)." Universidade de São Paulo, 2013. http://www.teses.usp.br/teses/disponiveis/18/18132/tde-28082013-091459/.

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Este trabalho objetivou analisar a suscetibilidade à erosão linear da região do Médio Rio Grande (MG), que abrange uma área de 9794,12 km², através de documentos cartográficos interpretativos. Utilizando técnicas de geoprocessamento e sensoriamento remoto associadas a levantamentos de campo e ensaios de laboratório, foram produzidos os seguintes documentos cartográficos: Carta de Declividade, Mapa de Landforms, Mapa de Materiais Inconsolidados e Inventário de Feições Erosivas. O produto final do trabalho, a Carta de Suscetibilidade à Erosão em escala 1:100.000, foi elaborada utilizando informa

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27

White, Shawn K. "Validating Missouri landtype associations using tree species composition, forest structure, and productivity." Diss., Columbia, Mo. : University of Missouri-Columbia, 2005. http://hdl.handle.net/10355/4296.

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Thesis (M.S.)--University of Missouri-Columbia, 2005.<br>The entire dissertation/thesis text is included in the research.pdf file; the official abstract appears in the short.pdf file (which also appears in the research.pdf); a non-technical general description, or public abstract, appears in the public.pdf file. Title from title screen of research.pdf file viewed on (January 10, 2007) Vita. Includes bibliographical references.

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28

Hartley, Kelley A. "Stratigraphic anaylsis [sic] of areal discontinuities of late Wisconsinan till sheets near Conneaut Lake, northwestern Pennsylvania." Akron, OH : University of Akron, 2009. http://rave.ohiolink.edu/etdc/view?acc%5Fnum=akron1248371875.

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Thesis (M.S.)--University of Akron, Dept. of Geology, 2009.<br>"August, 2009." Title from electronic thesis title page (viewed 10/21/2009) Advisor, John P. Szabo; Faculty readers, Linda Barrett, LaVerne Friberg; Department Chair, John P. Szabo; Dean of the College, Chand Midha; Dean of the Graduate School, George R. Newkome. Includes bibliographical references.

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29

Gercek, Deniz. "Object-based Classification Of Landforms Based On Their Local Geometry And Geomorphometric Context." Phd thesis, METU, 2010. http://etd.lib.metu.edu.tr/upload/12611780/index.pdf.

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Terrain as a continuum can be categorized into landform units that exhibit common physiological and morphological characteristics which might serve as a boundary condition for a wide range of application domains. However, heterogeneous views, definitions and applications on landforms yield inconsistent and incompatible nomenclature that lack interoperability. Yet, there is still room for developing methods for establishing a formal background for general type of classification models to provide different disciplines with a basis of landscape description that is also commonsense to human insigh

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30

VALLE, BARBARA. "PLANT AND ARTHROPOD COMMUNITIES OF ALPINE ICE-RELATED LANDFORMS: ECOLOGICAL AND BIOGEOGRAPHIC IMPORTANCE." Doctoral thesis, Università degli Studi di Milano, 2022. https://hdl.handle.net/2434/947188.

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This PhD thesis is mainly organised as collection of research papers published, submitted, and in preparation. Chapter 1 outlines the state of the art, the main aims of the PhD project and the approaches used for reaching these objectives on peculiar study areas Chapter 2, “Vanishing habitats”, presents, as a first result, a scientific call for studying and monitoring glacial and periglacial habitats – refugia for a cold-adapted and threatened biodiversity - because of the lack of knowledge that still affects these habitats (Gobbi et al. 2021). The study points out the urgency in planning th

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31

Fogwill, Christopher J. "The application of cosmogenic exposure dating to glacial landforms : examples from Antarctica and Patagonia." Thesis, University of Edinburgh, 2003. http://hdl.handle.net/1842/24576.

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Through the measurement of the concentrations of the in situ cosmogenic nuclides 1°Be and 26A1 within rock surfaces, this thesis has attempted to solve previously intractable problems regarding the timing and magnitude of glaciation during the last glacial cycle in the vicinity of the Drake Passage. In southernmost Patagonia we have been able to constrain the timing of two major advances of the formerly expanded Patagonian Ice Sheet during the last glacial interglacial transition. In the past these have been in question due to the paucity of radiocarbon dates, in the extremely and conditions p

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32

Wilmot, Nicola. "Periglacial landforms of the Ahlmannryggen and Jutulsessen areas of western Dronning Maud land, Antarctica." Thesis, Rhodes University, 2018. http://hdl.handle.net/10962/61535.

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Periglacial landforms are a common occurrence in Ahlmannryggen and Jutulsessen areas of western Dronning Maud land (WDML). Classification and formation of these landforms were disputed in literature. In Antarctica information on periglacial landforms is limited or confined to a specific landform. Thus a holistic approach was taken when investigating the periglacial landforms found in WDML. An overview of the existing knowledge base on periglacial landforms in WDML was given which was coupled with the analysis of archival data. The landforms found in this area were patterned ground, openwork bl

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33

Havel, Jaroslav J. "Ecology of the forests of south western Australia in relation to climate and landforms." Murdoch University, 2000. http://wwwlib.murdoch.edu.au/adt/browse/view/adt-MU20060815.114944.

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This thesis sets out to test the hypothesis that the vegetational patterns in the forested region of south western Australia are primarily determined by the interaction of climate and landform. The region is an area of 4.25 million hectares subject to recent agreement between the Commonwealth of '4ustralia and the state of Western Australia regarding long-term protection and management of forest (Regional Forest Agreement). The climate of the South Western forest region is warm temperate and summer dry, matching Koeppen's category Cs, usually described as mediterranean. The dominant geological

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34

Hjort, Jan. "Environmental factors affecting the occurrence of periglacial landforms in Finnish Lapland : a numerical approach /." Aachen : Shaker, 2006. http://bvbr.bib-bvb.de:8991/F?func=service&doc_library=BVB01&doc_number=014835670&line_number=0001&func_code=DB_RECORDS&service_type=MEDIA.

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35

Havel, J. J. "Ecology of the forests of south western Australia in relation to climate and landforms /." Access via Murdoch University Digital Theses Project, 2000. http://wwwlib.murdoch.edu.au/adt/browse/view/adt-MU20060815.114944.

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36

Drake, Nick A. "Mapping and monitoring surficial materials, processes and landforms in southern Tunisia using remote sensing." Thesis, University of Reading, 1992. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.333490.

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37

Sutton, Brian. "Glacial landforms and sedimentology and Late Pleistocene evolution of the Mourne Mountains, Northern Ireland." Thesis, University of Ulster, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.267825.

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38

Van, Dijk Thaienne A. G. P. "Glacier surges as a control on the development of proglacial fluvial landforms and deposits." Thesis, Keele University, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.392176.

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39

Havel, Jaroslav Joseph. "Ecology of the forests of south western Australia in relation to climate and landforms." Thesis, Havel, Jaroslav Joseph (2000) Ecology of the forests of south western Australia in relation to climate and landforms. PhD thesis, Murdoch University, 2000. https://researchrepository.murdoch.edu.au/id/eprint/70/.

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This thesis sets out to test the hypothesis that the vegetational patterns in the forested region of south western Australia are primarily determined by the interaction of climate and landform. The region is an area of 4.25 million hectares subject to recent agreement between the Commonwealth of Australia and the state of Western Australia regarding long-term protection and management of forest (Regional Forest Agreement). The climate of the South Western forest region is warm temperate and summer dry, matching Koeppen's category Cs, usually described as mediterranean. The dominant geologi

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40

Jones, Andrew. "Sedimentological record of the late palaeozoic Gondwanan glaciation in Queensland /." St. Lucia, Qld, 2003. http://www.library.uq.edu.au/pdfserve.php?image=thesisabs/absthe17532.pdf.

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41

D'Urso, Gary John. "Revised glacial margins and Wisconsin meltwater paleoflood hydrology in Slippery Rock Creek Basin, central western Pennsylvania." Morgantown, W. Va. : [West Virginia University Libraries], 2000. http://etd.wvu.edu/templates/showETD.cfm?recnum=1436.

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Thesis (Ph. D.)--West Virginia University, 2000.<br>Title from document title page. Document formatted into pages; contains x, 174 p. : ill. (some col.), maps (some col.) Includes abstract. Includes bibliographical references (p. 171-174).

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42

Stark, Jonathan Michael. "Use of LIDAR in geomorphic mapping and interpretation of coastal, fluvial, glacial and anthropogenic landforms." The Ohio State University, 2006. http://rave.ohiolink.edu/etdc/view?acc_num=osu1409232439.

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Park, Soojin. "Modelling soil-landform continuum on a three-dimensional hillslope." Thesis, University of Oxford, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.670238.

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44

Lopes, Rita Pereira. "A delimitação de unidades de terra. Caso do concelho de Lourinhã." Master's thesis, ISA/UL, 2015. http://hdl.handle.net/10400.5/9212.

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Mestrado em Arquitectura Paisagista - Instituto Superior de Agronomia<br>Land units have become an important mapping tool as they express similar climate, geology, soils, landforms and vegetation characteristics. They summarize all information that facilitate mapping development and can be applied at any scale. Land units are used for many purposes, such as landscape characterization and support for land evaluation processes. Hence it is important to deepen the knowledge and practice of the delimitation procedures in areas where the required information is complex and insufficient. In the

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45

Zhang, Fangli. "A particle-set distributed hydrological model for the dynamic simulation of surface runoff." HKBU Institutional Repository, 2017. https://repository.hkbu.edu.hk/etd_oa/472.

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1.1\xThis study proposed a particle-set distributed hydrological model for the dynamic simulation of rainfall-runoff process. With the supports of remote sensing, GIS, terrain analysis and distributed computing techniques, a representation-simplified and physically-based high-performance watershed framework has been developed. It simplifies the underlying watershed with a flow path network model, and represents the moving surface flow with independent runoff particles.;1.2\xThe original idea was to investigate a real-time modeling system for the space-time dynamics of increasingly frequent ext

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46

Hjort, Jan [Verfasser]. "Environmental factors affecting the occurrence of periglacial landforms in Finnish Lapland: a numerical approach / Jan Hjort." Aachen : Shaker, 2006. http://d-nb.info/1170529194/34.

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47

Peagler, Arriyan L. "Design guidelines for incorporating landforms and sculptural elements into residential treatment centers for at-risk youth." Virtual Press, 2008. http://liblink.bsu.edu/uhtbin/catkey/1397794.

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A wide range of individuals, from counselors to psychiatrists, have recognized the value of residential treatment centers for at-risk youth. Many residential treatment centers foster therapeutic interventions indoors. Typically, however, there have been few initiatives taken to enhance the outdoor landscapes of these facilities. In particular, potential supplements to therapeutic practices such as landforms and sculpture have been overlooked. This creative project explores how outdoor settings can be enhanced with landforms to provide at-risk youth with alternative venues to address aggressive

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48

Osei, Nana Akwasi. "Large wood in fluvial systems : quantity, structure and landforms, sediment retention, and riparian seed bank development." Thesis, Queen Mary, University of London, 2014. http://qmro.qmul.ac.uk/xmlui/handle/123456789/8813.

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This thesis investigates the characteristics and impacts of large wood accumulations within river reaches of different size and style. Four reaches were studied: (i) a wide, braided, headwater reach, characterised by dead wood (Tagliamento River, Italy); (ii) a lower gradient, wide, braided reach, characterised by resprouting wood (Tagliamento River, Italy); (iii) a low gradient, single thread reach with a natural supply of dead wood (Highland Water, UK), and (iv) a low gradient, single thread reach that has been restored by felling trees into the river (River Bure, UK). In each reach, quantit

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Korzeniowska, Karolina [Verfasser], and Oliver [Akademischer Betreuer] Korup. "Object-based image analysis for detecting landforms diagnostic of natural hazards / Karolina Korzeniowska ; Betreuer: Oliver Korup." Potsdam : Universität Potsdam, 2017. http://d-nb.info/1218402792/34.

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Grimm, Günter Albin. "Vegetation succession on glacier forelands in the Jostedalsbreen region and Jotunheimen, south-central Norway." Thesis, University of Oxford, 2000. http://ora.ox.ac.uk/objects/uuid:aedabc31-7022-4666-8121-7379b1bc4998.

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In this study four different aspects of primary successions on glacier forelands in South-Central Norway are investigated. First, general vegetation and environment trends, which have been observed by other scientists, were studied on two forelands. It is shown that the two selected forelands (one low- and one high-altitude foreland, Nigardsbreen and Storbreen, respectively) differ in the speed of vegetation cover change and in the overall species richness developed over the last 250 years since deglaciation. This is attributed to differences in the severity of the environment between the two

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