The past few decades have seen rapid improvement in technologies related to remote sensing, specifically in digital photogrammetry and the use of unmanned aerial vehicles (UAVs). This has presented new opportunities to collect imagery at both a high temporal and spatial resolution to create detailed digital elevation models (DEMs) and investigate small-scale geomorphological features and their development over time. The high-resolution capacity of this methodology is well-suited to the study of a variety of terrains in which many critical geomorphological features are low relief and difficult or impossible to delineate using traditional remote sensing datasets. This study utilizes UAV-based imagery collection and data analysis, in conjunction with sedimentological analysis, of two study sites in Iceland and southern Ontario. The primary objective of this work is to explore the utility of integrating high-resolution spatial surveys with more traditional field techniques to identify geomorphological features, interpret their depositional origin, and quantify temporal changes in their form. The first study was completed on the forefields of Öldufellsjökull and western Sléttjökull, two surge-type outlet glaciers of the Mýrdalsjökull Ice Cap in southeast Iceland. Glacial deposits are important sources of paleoclimatic information but not all deposits are formed by processes that reflect the overall climatic conditions of a region; surge-type (fast-flowing) glaciers undergo periodic episodes of rapid ice movement, often unrelated to ambient climatic conditions. Remotely sensed data and field investigations were combined to complete a landsystem analysis of the forefields at each of Öldufellsjökull and western Sléttjökull, and an unmanned aerial vehicle (UAV) was used to collect high-resolution imagery of areas of particular interest. The forefields of Öldufellsjökull and western Sléttjökull, lack many of the characteristics typical of surge-type landsystems and instead are more similar to the active temperate landsystem common in Iceland. The identification of landforms considered to be diagnostic of surge-type glacier behaviour was only possible through a targeted high-resolution UAV survey suggesting that small-scale diagnostic landforms may be overlooked in many investigations. The second study area focused on the Niagara Escarpment in Hamilton, Ontario, a major landform resulting from extensive glacial and fluvial erosion of Paleozoic sedimentary rocks during the late Quaternary. In Hamilton, the Niagara Escarpment is a steep faced cuesta composed of Ordovician and Silurian sedimentary rocks. Recent rockfalls onto roads crossing the escarpment have raised serious concerns about its stability. To address these concerns, and to provide more information on erosional processes active along the escarpment in Hamilton, a comprehensive study of the Niagara Escarpment was completed including the collection of multi-temporal photogrammetric surveys of select rock faces, and detailed sedimentological and fracture analysis. A comprehensive lithological investigation was completed of all accessible rock outcrops in Hamilton to identify areas most likely to experience erosion based on site characteristics. A second component of this investigation was to evaluate the utility of using high-resolution imagery combined with Structure from Motion (SfM) software to detect temporal changes on the escarpment face. A staged erosion study was conducted in which lithological blocks of a known size were removed from the escarpment face at a selected site, to determine the lower limits of detection of erosion using this methodology. The study found that the location of block removal (erosion) was consistently identified, but the calculated volume of blocks removed was less accurately determined, differing by an average of 175% from the known volume of the block. A further study using this same methodology tested its ability to identify areas of natural loss (erosion) from the escarpment face. Based on multiple surveys taken 14 months apart at a selected study site, approximately one third of the area of interest experienced either loss (erosion) or gain (deposition) of material. There appear to be clear connections between lithology, density of fracturing, and the location of material loss (erosion); areas of the outcrop characterised by interbedded shales, and those areas exposing densely fractured sandstone or dolostone, were most likely to erode. The lithological characteristics of the Niagara Escarpment, including the strength of individual stratigraphic units, their vertical arrangement, and their density of fracturing, as well as climatic and hydrological factors (e.g., groundwater flow, location of surficial water features, mean annual temperature, mean annual precipitation etc.), all contribute to the amount and types of erosion active on the exposed rock face. The studies reported in this thesis have integrated high-resolution, close-range imagery with traditional field techniques to explore the characteristics and development of geomorphological forms in different terrain types. In each of the studies, the importance of collecting high-resolution imagery (<10 cm) to map geomorphological features of various scales is highlighted. / Dissertation / Doctor of Science (PhD)

Submitted by Leandro de Godoi Pinton null (lgpgeo@yahoo.com.br) on 2016-07-28T12:06:59Z No. of bitstreams: 1 LeandroGPinton.Texto.Completo.pdf: 92573539 bytes, checksum: 396e33f24ed85b443feec9a43b8689b2 (MD5) / Approved for entry into archive by Ana Paula Grisoto (grisotoana@reitoria.unesp.br) on 2016-08-01T14:19:35Z (GMT) No. of bitstreams: 1 pinton_lg_dr_rcla.pdf: 92573539 bytes, checksum: 396e33f24ed85b443feec9a43b8689b2 (MD5) / Made available in DSpace on 2016-08-01T14:19:35Z (GMT). No. of bitstreams: 1 pinton_lg_dr_rcla.pdf: 92573539 bytes, checksum: 396e33f24ed85b443feec9a43b8689b2 (MD5) Previous issue date: 2016-06-10 / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / A presente pesquisa teve como objetivo geral avaliar a dinâmica dos processos morfogenéticos do relevo cuestiforme no Quaternário Tardio (Pleistoceno Superior-Holoceno Superior) e no período antrópico recente. Com base nessa avaliação, propôs-se reconstituir a sequência denudativa numa escala de tempo geológico, assim como verificar as implicações da constituição de morfologias antropogênicas na evolução desse compartimento numa escala histórica de tempo. A fim de atender tal objetivo, foram realizadas datações de episódios deposicionais por Luminescência Opticamente Estimulada (LOE) e pelo método do chumbo-210 (210Pb). Ademais, foram elaborados mapeamentos específicos para a obtenção de dados morfoestruturais, geomorfológicos e de uso e cobertura da terra. A bacia hidrográfica do Córrego do Cavalheiro – Analândia (SP) – foi selecionada como área de estudo em virtude de sua disposição natural, na transição entre as Cuestas Areníticas-Basálticas e a Depressão Periférica Paulista, associada, ainda, à evolução do uso da terra essencialmente rural. A análise sistêmica entre as idades LOE do material coluvionar com as flutuações paleoclimáticas regionais e o arranjo de feições morfoestruturais e antropogênicas possibilitou a proposição de um modelo evolutivo do relevo cuestiforme, caracterizado pela seguinte sequência denudativa: 1) Primeira fase seca de 30.770 ± 4.930 a 8.000 ± 1.000 anos A.P. (transição do Pleistoceno Superior com o Holoceno Inferior, estendendo-se até o início do Holoceno Médio); 2) Primeira fase úmida de 7.420 ± 980 a 4.500 ± 750 anos A.P. (Holoceno Médio-Superior); 3) Segunda fase seca de 3.940 ± 665 a 2.215 ± 250 anos A.P. (Holoceno Superior) e; 4) Fase antropogênica de 1962 a 2013 (série histórica de 51 anos). A datação dos sedimentos fluviais pelo método do 210Pb foi ineficaz como recurso complementar para o detalhamento da fase antropogênica nas cuestas em razão do predomínio de coberturas sedimentares na composição litopedológica desse compartimento. Todavia, a quantificação das mudanças morfológicas mediante a sistematização de geoindicadores corrobora a ação antropogênica condicionando a esculturação do relevo cuestiforme. A reconstituição paleomorfogenética das cuestas demonstrou que os processos denudativos no Quaternário Tardio (Pleistoceno Superior-Holoceno Superior) e no período antrópico recente se configuram de forma complexa, sendo a sua dinâmica cíclica e poligênica. / The present research aimed to evaluate the dynamics of the morphogenetic processes of the cuesta relief in the Late Quaternary (Upper Pleistocene-Upper Holocene) and in the current anthropic periods. Based on this evaluation, the denudative sequence was reconstituted in a geological time scale, and the implications of the anthropogenic morphology constitution in the evolution of this compartment in a historical time scale were verified as well. In order to achieve this objective, depositional dating were performed through Optically Stimulated Luminescence (OSL) and the Pb-210 method (210Pb). In addition, specific morphostructural, geomorphological and land-use/land-cover mapping were performed. The Cavalheiro Stream basin – Analândia (SP) – was chosen as the study area due to its natural distribution, in the transition of the sandstone-basaltic Cuestas and the Paulista Peripheral Depression and the essentially rural land-use evolution as well. The systemic analysis comparing the colluvium material ages (OSL) with the regional paleoclimatic fluctuations and the morphostructural/anthropogenic features arrangement provided an evolutionary model of the cuestas relief, characterized by the following denudative sequence: 1) First dry phase from 30,770 ± 4,930 to 8,000 ± 1,000 years BP (transition between the Upper Pleistocene and the Lower Holocene, extended until the beginning of the Middle Holocene); 2) First wet phase from 7,420 ± 980 to 4,500 ± 750 years BP (Middle-Upper Holocene); 3) Second dry phase from 3,940 ± 665 to 2,215 ± 250 years BP (Upper Holocene); and 4) Anthropogenic phase, from 1962 to 2013 (historical series of 51 years). Fluvial sediments dating through the 210Pb method was inefficient as a complementary resource to detail the anthropogenic phase in the cuestas due to the predominance of sedimentary covers in the lithopedologic composition of this compartment. However, the quantification of the morphological changes in relation with the systematization of the geoindicators corroborates the anthropogenic action on the cuestas relief formation. The cuestas paleomorphogenetic reconstitution demonstrated that the denudative processes in the Late Quaternary (Upper Pleistocene-Upper Holocene) and in the recent anthropic period display a complex configuration, with a cyclic and polygenic dynamics. / FAPESP: 2012/20513-0

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