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Tesi sul tema "Landscape evolution"

Autore: Grafiati

Pubblicato: 4 giugno 2021

Ultima modifica: 25 luglio 2025

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1

Martin, Yvonne. "Modelling geomorphology in landscape evolution." Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1998. http://www.collectionscanada.ca/obj/s4/f2/dsk2/tape15/PQDD_0030/NQ27198.pdf.

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2

Hurst, Martin David. "Hillslope morphology as an indicator of landscape evolution in tectonically active landscapes." Thesis, University of Edinburgh, 2013. http://hdl.handle.net/1842/12228.

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Hillslopes comprise the majority of unglaciated upland landscapes; they are the primary source for the production of sediment from bedrock, and the routing system by which sediment is delivered to the channel network. Yet the nature of hillslope response to changes in tectonic, climatic or base-level boundary conditions is poorly understood in terms of the spatial and temporal distribution of hillslope morphology. Here I exploit a previously published framework for exploring hillslope morphology in high relief landscapes (Roering et al., 2007), to address several critical questions: Does high

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3

Jamieson, Stewart S. R. "Modelling landscape evolution under ice sheets." Thesis, University of Edinburgh, 2008. http://hdl.handle.net/1842/29818.

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This thesis details the application of numerical modelling techniques to simulate erosion under ice sheets with the aim of better understanding the interrelationships between glacial erosion, long-term landscape evolution and ice dynamics. A model is developed that predicts patterns of basal erosion in a glaciologically sensible manner and shows that ‘fluvial’ landscapes can become ‘glacial’ systems within 100 kyrs. By simulating ice sheet growth and erosion over synthetic landscapes of varying form, amplitude and wavelength the topographic characteristics that are most critical to the evoluti

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4

Boardman, John. "Landscape evolution over Pleistocene and modern timescales." Thesis, Keele University, 2004. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.400115.

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5

Bosch, Rachel. "Landscape Evolution of the Central Kentucky Karst." University of Cincinnati / OhioLINK, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=ucin1627665906577779.

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6

Odoni, Nicholas Alan. "Exploring equifinality in a landscape evolution model." Thesis, University of Southampton, 2007. https://eprints.soton.ac.uk/153687/.

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Model equifinality is the property by which very similar model outputs can be generated by many different combinations of model inputs. It is known in numerical models used in other disciplines, and is thought to be likely in landscape evolution models (“LEMs”) also, as they incorporate many process parameters of uncertain value. LEM equifinality, if pervasive, would be a serious obstacle to falsifying working hypotheses and would frustrate landscape evolution research, but to date it has not been quantified. This is attempted here, by sampling a LEM’s response in its parameter space. A well k

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7

Nicholson, Uisdean A. M. "Landscape evolution and sediment routing across a strike-slip plate boundary." Thesis, Available from the University of Aberdeen Library and Historic Collections Digital Resources. Restricted: no access until July 20, 2014, 2009. http://digitool.abdn.ac.uk:80/webclient/DeliveryManager?application=DIGITOOL-3&owner=resourcediscovery&custom_att_2=simple_viewer&pid=59100.

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8

Baran, Ramona. "Quantification of landscape evolution on multiple time-scales." Diss., lmu, 2012. http://nbn-resolving.de/urn:nbn:de:bvb:19-148038.

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9

CARBONO, ALONSO JOAQUIN JUVINAO. "COMPUTER SIMULATION OF LANDSCAPE EVOLUTION OF DRAINAGE BASINS." PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO, 2010. http://www.maxwell.vrac.puc-rio.br/Busca_etds.php?strSecao=resultado&nrSeq=21617@1.

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PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO<br>A superfície da terra é formada por processos geológicos que geram as rochas, assim como por processos naturais de degradação e de erosão. A erosão destrói as estruturas que compõem o solo e seu transporte é feito pela ação da água da chuva, do vento, da gravidade e até do gelo. A origem e evolução das bacias sedimentares, dentre outros fenômenos, é estudada pela geologia sedimentar, a qual trata do estudo dos processos físicos, químicos e biológicos atuantes na superfície da terra desde o seu início até os dias atuais. Na atualidade, o uso

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10

Richardson, 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.

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Thesis: Ph. D., Massachusetts Institute of Technology, Department of Earth, Atmospheric, and Planetary Sciences, 2015.<br>Cataloged from PDF version of thesis.<br>Includes bibliographical references (pages 145-157).<br>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

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11

SoÌlyom, PeÌter. "The effect of flow path geometry on landscape evolution." Thesis, University of Oxford, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.422439.

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12

Foster, David. "Landscape Evolution in the Northern Basin and Range, USA." Thesis, University of Manchester, 2009. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.503647.

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13

McLaughlin, Win. "Landscape and Biotic Evolution of the Kochkor Basin, Kyrgyzstan." Thesis, University of Oregon, 2018. http://hdl.handle.net/1794/23810.

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Kyrgyzstan is the single most seismically active country in the world. Accessing the past, and therefore future hazard of faults, necessitates a high-resolution understanding of the timing of different geologic events. With no radiometrically datable rocks from the Neogene of Kyrgyzstan, I herein present the first work formally describing Neogene vertebrate faunas from the Kochkor Basin of Kyrgyzstan. I utilize a combination of biostratigraphy and magnetostratigraphy to constrain the timing of when the vertebrate assemblages were emplaced, and have dated the three bone beds to all fall in the

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14

Spry, Melissa J., and n/a. "The Regolith and landscape evolution of a low relief landscape: Cobar, Central New South Wales, Australia." University of Canberra. Resource, Environmental & Heritage Management, 2003. http://erl.canberra.edu.au./public/adt-AUC20050704.162445.

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Construction of a 1:250,000 scale regolith-landform map of the Cobar area of central New South Wales (NSW) Australia, demonstrates the presence of a wide range of previously undescribed regolith materials, landforms and landscape features in the region. The map covers the east-west extent of the Cobar Basin, extends to the west onto the Darling River Floodplain, and east onto rocks of the Girilambone Group. The mapping area is centred on the Cobar township and covers -14,730 krn2 between 303113 and 446113 E and 6483184 and 6586183 N (AGO 66, MGA Zone 55). 48 regolithlandform units have been id

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15

Sharma, Milap Chand. "Quaternary history and landscape evolution of NW Garhwal, central Himalaya." Thesis, Royal Holloway, University of London, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.242051.

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16

Collins, Daniel B. G. (Daniel Benjamin Gardiner) 1976. "Modeling the effects of vegetation-erosion coupling on landscape evolution." Thesis, Massachusetts Institute of Technology, 2002. http://hdl.handle.net/1721.1/84316.

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17

Baker, Katie. "The chromatin landscape of barley : gene expression, evolution and epigenetics." Thesis, University of Dundee, 2015. https://discovery.dundee.ac.uk/en/studentTheses/13a096cd-f45b-4e34-babd-ccb3ff3607ca.

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Barley (Hordeum vulgare) is an economically important crop species with a large diploid genome. Around a half of the barley genome and a fifth of the genes are constrained within a low-recombining pericentromeric (LR-PC) region. I explored the LR-PC gene component with a genomic investigation of gene expression, diversity and evolution. Chromatin environments were also explored in the LR and high recombining (HR) regions by surveying the genic and genomic distributions of nine histone modifications. Firstly, regions of HR and LR were identified and compared for gene evolution, expression and d

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18

Mo, Fei. "The evolution of the urban landscape of Shanghai (1843-1949)." Thesis, University of Sheffield, 2015. http://etheses.whiterose.ac.uk/11585/.

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The character of a city derives in substantial part from buildings, groups of buildings and their associated open spaces. The nature of this relationship remains poorly understood in many cities. Previous studies have shown that the process of modernisation in Asian cities was significantly influenced by European and American practices and theories, although these often interacted with local traditions. From the 1840s, China came into the modern era, and the first treaty port Shanghai has become the key to understand the evolution of Chinese cities under inextricable modernisation, westernisat

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19

Mackey, Benjamin Hunter. "The contribution of large, slow-moving landslides to landscape evolution." Thesis, University of Oregon, 2009. http://hdl.handle.net/1794/10555.

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xvi, 136 p. : ill. (some col.) A print copy of this thesis is available through the UO Libraries. Search the library catalog for the location and call number.<br>This dissertation discusses the contribution of deep-seated landslides and earthflows to the morphology, erosion, and evolution of mountainous landscapes, focusing on the northern California Coast Ranges. In active landscapes, channel incision is necessary to create relief but also increases stresses in adjacent hillslopes, ultimately leading to slope failure. While conceptually simple, the spatial relationships between channel in

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20

Anders, Matt D. "Quaternary Geology and Landscape Evolution of Eastern Grand Canyon, Arizona." DigitalCommons@USU, 2003. https://digitalcommons.usu.edu/etd/6738.

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Tectonics and drainage evolution are controlling overall landscape incision in eastern Grand Canyon. Superimposed on downcutting are dynamic responses of hillslopes, tributary streams, and the Colorado River to glacial-interglacial climate cycles. Five tributary stream fill terraces have been identified, and luminescence dating indicates aggradation was occurring 50- 34 ka {S3), 12-7 ka (S2), and 5-3.5 ka (S1). Seven Colorado River fill terraces have been identified, and luminescence and U-series dating indicate deposition was occurring 343-322 ka (M5), 151-118 ka (M4), and 71-64 ka (M3). Aggr

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21

Chilton, Kristin Danielle. "Investigating the Effects of Lithology on Landscape Evolution Processes across Scales." Diss., Virginia Tech, 2021. http://hdl.handle.net/10919/104740.

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Geomorphologists have long observed the influence of lithology on landscape form and evolution. However, the specific mechanisms by which this is accomplished are not well characterized. Here, I investigate the role of lithology in landscape evolution processes across spatial and temporal scales and geomorphic domains, to progress our understanding of the basic controls on the processes which shape Earth's surface. These investigations were carried out within the Valley and Ridge province of the Appalachian Mountains, where contrasts in strength of underlying lithologies (juxtaposed by Allegha

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22

Fenwick, Helen. "The Lincolnshire marsh : landscape evolution, settlement development and the salt industry." Thesis, University of Hull, 2007. http://hydra.hull.ac.uk/resources/hull:5669.

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The coastal wetland, known as the Lincolnshire Marsh, is investigated in order to understand the ways in which people in the past exploited coastal zones. This research into a previously neglected area has tested the validity of' Rippon's (2000) three-part model ofcoastal strategies - exploitation, modification and transformation. The Lincolnshire Marsh, as considered in this thesis, covers a region from Cleethorpes in the north to Wainfleet in the south. The study area also encompasses areas of the adjacent dry land, of the Middle Marsh and the Wolds, to the west. A wide range of data are stu

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23

Sinclair, Kevin Michael. "Stream erosion and its relation to drainage networks and landscape evolution." Thesis, University of Cambridge, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.627590.

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24

Bäckman, Emma, and Josefin Ellmarker. "The Evolution of Scania: How the landscape grew with the industrialization." Thesis, Högskolan i Halmstad, Akademin för ekonomi, teknik och naturvetenskap, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:hh:diva-33357.

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It has been a constant fight for Scania between Sweden and Denmark, but in 1658 the landscape finally became Swedish. New technologies and innovations emerged with the industrial revolution and influenced Scania. The society developed and the standard of living was improved. The agriculture sector in Scania has always been strong because of the farmable land. From a geographical point of view, the landscape has a good location since it is connected to the Baltic Sea. This has contributed to good trading and communication possibilities, which is why Scania has been a desirable landscape. The in

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25

Peifer, Bezerra Daniel. "The pattern and style of landscape evolution in post-orogenic settings." Thesis, University of Glasgow, 2018. http://theses.gla.ac.uk/30680/.

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26

Cerovski-Darriau, Corina. "Landslides and Landscape Evolution over Decades to Millennia—Using Tephrochronology, Air Photos, Lidar, and Geophysical Investigations to Reconstruct Past Landscapes." Thesis, University of Oregon, 2016. http://hdl.handle.net/1794/20405.

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Landscapes respond to external perturbations over a variety of timescales, including million-year tectonic forcing, millennial to decadal climate fluctuations, and minutes-long high intensity storms or large magnitude earthquakes. In mountainous regions, understanding the role of landslides in driving the hillslope response to these perturbations is paramount for understanding landscape evolution over geologic timescales and hazards over human timescales. Here I analyze the landslide-driven hillslope response over millennial to decadal timescales using a variety of tools and techniques (e.g. t

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27

Farrant, Andrew Roger. "Long-term Quaternary chronologies from cave deposits." Thesis, University of Bristol, 1995. https://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.294897.

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28

Smith, Martin Lancaster, and martin smith@anu edu au. "Towards a Geochronology for Long-term Landscape Evolution, Northwestern New South Wales." The Australian National University. Research School of Earth Sciences, 2006. http://thesis.anu.edu.au./public/adt-ANU20061026.141414.

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The study area extends from west of the Great Divide to the Broken Hill and Tibooburra regions of far western New South Wales, encompassing several important mining districts that not only include the famous Broken Hill lodes (Pb-Zn-Ag), but also Parkes (Cu-Au), Peak Hill (Au), Cobar (Cu-Au-Zn) and White Cliffs (opal). The area is generally semi-arid to arid undulating to flat terrain covered by sparse vegetation. ¶ During the Cretaceous, an extensive sea retreated across vast plains, with rivers draining from the south and east. After the uplift of the Great Divide associated with opening o

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29

Quigley, Mark Cameron. "Continental tectonics and landscape evolution in south-central Australia and southern Tibet /." Connect to thesis, 2006. http://eprints.unimelb.edu.au/archive/00002963.

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30

Schwanghart, Wolfgang [Verfasser]. "Climate and landscape evolution of the Ugii Nuur basin, Mongolia / Wolfgang Schwanghart." Berlin : Freie Universität Berlin, 2009. http://d-nb.info/1023463741/34.

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31

PINTO, RODRIGO WAGNER PAIXAO. "GEOMORPHOLOGICAL LANDSCAPE EVOLUTION OF THE GRANDE RIVER: DISSECTION DYNAMICS AND DRAINAGE CAPTURE." PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO, 2015. http://www.maxwell.vrac.puc-rio.br/Busca_etds.php?strSecao=resultado&nrSeq=27097@1.

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PONTIFÍCIA UNIVERSIDADE CATÓLICA DO RIO DE JANEIRO<br>COORDENAÇÃO DE APERFEIÇOAMENTO DO PESSOAL DE ENSINO SUPERIOR<br>PROGRAMA DE SUPORTE À PÓS-GRADUAÇÃO DE INSTS. DE ENSINO<br>A análise dos sistemas fluviais são de extrema importância na compreensão da evolução geomorfológica da paisagem, pois possuem características, seja no seu arranjo ou distribuição dos canais, que permitem elaborar os episódios que ocorreram ao longo do tempo. A quebra do continente Gondwana e seus múltiplos eventos até a consolidação do Rift Continental do Sudeste (RCS) implicou em uma mudança significativa no relevo su

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32

Gasparini, Nicole M. (Nicole Marie) 1972. "Erosion and deposition of multiple grain sizes in a landscape evolution model." Thesis, Massachusetts Institute of Technology, 1998. http://hdl.handle.net/1721.1/51560.

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33

Deal, Eric. "A Probabilistic Approach to Understanding the Influence of Rainfall on Landscape Evolution." Thesis, Université Grenoble Alpes (ComUE), 2017. http://www.theses.fr/2017GREAU012/document.

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Dans cette thèse je travaille sur la relation entre la pluviosité et l’érosion fluviatile en utilisant une approche probabiliste. Je développe une méthodologie indépendante de la moyenne pour caractériser la variabilité de la pluviosité journalière.L’indépendance vis-à-vis de la moyenne permet une comparaison simpleetobjectivedelavariabilitédelapluviosité sous différents régimes climatiques. Elle semontre également utile pour intégrer le concept de variabilité de la pluviosité dans lathéorie que je développe ensuite. J’applique cette approche à la chaine de montagnesHimalayenne en utilisant de

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34

Jackson, Eric Alan. "Towards a Prediction of Landscape Evolution from Chemical Weathering and Soil Production." Wright State University / OhioLINK, 2017. http://rave.ohiolink.edu/etdc/view?acc_num=wright1516116071724445.

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35

Ebert, Karin. "Cenozoic landscape evolution in northern Sweden : geomorphological interpretation within a GIS-framework /." Stockholm : Department of Physical Geography and Quaternary Geology, Stockholm University, 2009. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-30711.

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Diss. (sammanfattning) Stockholm : Stockholms universitet, 2009.<br>At the time of the doctoral defence, the following papers were unpublished and had a status as follows: Paper 2: In press. Paper 3: Manuscript. Paper 4: Manuscript. Härtill 4 uppsatser.

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36

Marshall, Jill. "Lithologic, Climatic, and Biotic vs. Abiotic Controls on Erosion and Landscape Evolution." Thesis, University of Oregon, 2015. http://hdl.handle.net/1794/19291.

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The triumvirate of tectonics, lithology, and climate control landscape evolution. This study quantifies how lithologic variation and climate-mediated changes in ecosystems perturb steady state processes in the unglaciated, soil-mantled Oregon Coast Range (OCR). I first demonstrate that minor grain-scale differences in rock properties in a seemingly uniform sandstone control differences in rock strength, biotic bedrock-to-soil production efficacy, and erosion rates and influence relief at the watershed scale. I then build on sedimentology, paleoecology, and isotopic-derived paleoerosion data I

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37

Mauch, James P. "Quaternary Incision, Salt Tectonism, and Landscape Evolution of Moab-Spanish Valley, Utah." DigitalCommons@USU, 2018. https://digitalcommons.usu.edu/etd/7068.

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To study the history of processes that shape the Earth’s surface, geologists look for markers in the landscape that they can date and use to measure change. Rivers leave such markers in their deposits and terrace landforms and in the overall shape of their elevation profile from head to toe. This thesis uses luminescence and cosmogenic methods to date the sediment in terraces to determine when the river deposited it. Field mapping and global positioning system (GPS) surveying are also used to measure the distance between terrace levels to quantify how much change has occurred. This study seeks

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38

Smith, Martin Lancaster. "Towards a geochronology for long-term landscape evolution, Northwestern New South Wales /." View thesis entry in Australian Digital Theses Program, 2006. http://thesis.anu.edu.au/public/adt-ANU20061026.141414/index.html.

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39

Hevia, Cruz Francisco. "Climatic and landscape evolution of the Azores over the past million years." Electronic Thesis or Diss., université Paris-Saclay, 2023. http://www.theses.fr/2023UPASJ035.

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L'évolution des îles volcaniques résulte d'interactions complexes entre croissance des volcans et processus de destruction (éruptions explosives, glissements de terrain, érosion fluviale, altération). Les changements climatiques peuvent influencer ces processus sur des échelles variées. A l’échelle événementielle, des précipitations intenses peuvent engendrer des épisodes érosifs extrêmes. Sur le long-terme, des variations des taux d'altération, sensibles aux précipitations et à la température, peuvent impacter la fertilité des sols et le cycle global du carbone.Les îles volcaniques des Açores

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40

Lopes, Ana Muller. "Transformações na paisagem rural do norte de Portugal." Master's thesis, ISA/UTL, 2011. http://hdl.handle.net/10400.5/4132.

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Mestrado em Arquitectura Paisagista - Instituto Superior de Agronomia<br>The Landscape is a fluid and dynamic system that reflects the interaction between its ecological com-ponent and human activity. To speak about Landscape is therefore to speak about nature and human culture. The importance of the evolution of the agricultural and pastoral activities in the shaping of the Landscape, specifically in the North of Portugal, together with the structural role played by the me-thods of appropriation of agricultural territory, are the subject of this thesis. Having recognized the contribution of

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Pina, Carolina do Vale e. "Projectos de arquitectura paisagista no âmbito de planos de gestão de paisagens culturais. Caso de estudo: o acesso da Tapada da Ajuda ao Pólo Universitário da Ajuda." Master's thesis, ISA/UTL, 2011. http://hdl.handle.net/10400.5/4178.

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Mestrado em Arquitectura Paisagista - Instituto Superior de Agronomia<br>The present work is a study about the Tapada da Ajuda and the importance of management plans on landscapes of cultural and patrimonial value like this one. There is also made a proposal of landscape intervention on the acess of the Tapada to the Pólo Universitário da Ajuda. The first chapter is an analysis of the international legal instruments that protects the patrimony, including the landscape heritage. Concerning the national legislation, there are legal means and institutions that protect the landscape heritage in P

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42

Prosser, Lee. "The Keynsham Hundred : a study of the evolution of a North Somerset estate, 350-1550." Thesis, University of Bristol, 1995. http://hdl.handle.net/1983/379582ef-cf43-41d6-94a8-36261070fdf9.

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43

Burg, Joel G. "Exploring the Role of the Artifact: An Evolution of Form, Function and Memory in the Urban Landscape." Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/23255.

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The urban landscape is a diverse environment that is constantly evolving. Such change does not remove and replace all of the remnants of the city\'s past, however, and the remaining artifacts become key pieces of local identity as a result of their persistence. Even so, artifacts are also complex entities and their definition and value can be drastically different given the context in which they exist. Nonetheless, artifacts can be broadly understood as interactive elements in the urban landscape that become enmeshed in their surrounding community, and serve a vital role as a result. This enqu

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44

Morrison, Erin Seidler, and Erin Seidler Morrison. "Exploring the Deterministic Landscape of Evolution: An Example with Carotenoid Diversification in Birds." Diss., The University of Arizona, 2017. http://hdl.handle.net/10150/624290.

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Establishing metrics of diversification can calibrate the observed scope of diversity within a lineage and the potential for further phenotypic diversification. There are two potential ways to calibrate differences between phenotypes. The first metric is based on the structure of the network of direct and indirect connections between elements, such as the genes, proteins, enzymes and metabolites that underlie a phenotype. The second metric characterizes the dynamic properties that determine the strength of the interactions among elements, and influence which elements are the most likely to int

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45

Jansson, Anna. "Stratigraphy, Landscape Evolution, and Past Environments at the Billy Big Spring Site, Montana." Thesis, The University of Arizona, 2018. http://pqdtopen.proquest.com/#viewpdf?dispub=10643050.

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<p> This thesis reconstructs the landscape evolution of the Billy Big Spring site (24GL304, Glacier County, north-central Montana) from the last glacial maximum to present through the analysis of sediment and soil samples collected from a transect of auger tests that bisected the site and surrounding landforms. Interpretations were drawn from stratigraphy, pedologic data, sedimentologic analysis and radiocarbon dating. The site landscape came into being in the late-Pleistocene, after Wisconsin-age glaciers retreated. Glacial retreat left a meltdown depression on the land that filled with water

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Jansson, Anna Maria, and Anna Maria Jansson. "Stratigraphy, Landscape Evolution, and Past Environments at the Billy Big Spring Site, Montana." Thesis, The University of Arizona, 2017. http://hdl.handle.net/10150/626384.

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Abstract (sommario):

This thesis reconstructs the landscape evolution of the Billy Big Spring site (24GL304, Glacier County, north-central Montana) from the last glacial maximum to present through the analysis of sediment and soil samples collected from a transect of auger tests that bisected the site and surrounding landforms. Interpretations were drawn from stratigraphy, pedologic data, sedimentologic analysis and radiocarbon dating. The site landscape came into being in the late-Pleistocene, after Wisconsin-age glaciers retreated. Glacial retreat left a meltdown depression on the land that filled with water to

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47

Falade, J. B. "Nigeria's urban open spaces : an inquiry into their evolution, planning and landscape qualities." Thesis, University of Edinburgh, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.304191.

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48

Schaefer, Carlos Ernesto Reynaud. "Soils and paleosols from northeastern Roraima, north Amazonia : geomorphology, genesis and landscape evolution." Thesis, University of Reading, 1994. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.239746.

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49

Flores, Cervantes Javier Homero 1977. "Headcut retreat resulting from plunge pool erosion in a 3D landscape evolution model." Thesis, Massachusetts Institute of Technology, 2004. http://hdl.handle.net/1721.1/28361.

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Thesis (S.M.)--Massachusetts Institute of Technology, Dept. of Civil and Environmental Engineering, 2004.<br>Includes bibliographical references (p. 139-143).<br>Headcut retreat produced by plunge pools is represented using existing concepts about this type of erosion. The model estimates retreat rates, given flow, height of the headcut, upstream slope and Manning's roughness, and the relevant soil parameters (erodibility and critical shear stress). The model was analyzed to study its behavior as its input parameters changed, and its output was compared to experimental observations. Next, the

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Bradley, J. G. "Thermochronology, landscape evolution and hydrogeology of the Katonga Valley in south west Uganda." Thesis, University College London (University of London), 2012. http://discovery.ucl.ac.uk/1343834/.

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The reversed river systems of south west Uganda attracted geoscientists to study the geomorphology of the region in the mid 20th century. During the succeeding fifty years the population and GDP per capita have both risen between five and six fold with a consequent increase in water demand. This thesis aims to apply modern quantitative techniques and theoretical developments to improve our understanding of the landscape evolution of the Katonga Valley and contribute to the groundwater resource assessment of associated alluvial deposits. Karoo-age glaciogenic strata were discovered filling the

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