Controls on Fluvial Geomorphology in the Canadian Rocky Mountains
The Canadian Rocky Mountains record a dynamic history of erosion. Presently, bedrock rivers interact with the lithology and structural architecture of a large fold-and-thrust belt. Because the alpine landscape has been modified by Pleistocene and Holocene glaciation, rivers are also influenced by re...
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University of North Carolina at Chapel Hill Graduate School
2014
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ftcarolinadr:cdr.lib.unc.edu:dn39x1977 2023-10-09T21:49:44+02:00 Controls on Fluvial Geomorphology in the Canadian Rocky Mountains Quinlan, Kevin College of Arts and Sciences, Department of Geological Sciences Pavelsky, Tamlin Stewart, Kevin Willis, Michael 2014-08 https://doi.org/10.17615/q1ab-9j95 https://cdr.lib.unc.edu/downloads/j96020977?file=thumbnail https://cdr.lib.unc.edu/downloads/j96020977 English eng University of North Carolina at Chapel Hill Graduate School https://doi.org/10.17615/q1ab-9j95 https://cdr.lib.unc.edu/downloads/j96020977?file=thumbnail https://cdr.lib.unc.edu/downloads/j96020977 http://rightsstatements.org/vocab/InC/1.0/ Geomorphology Geology Geographic information systems Geodesy Schmidt Hammer Canadian Rocky Mountains GIS Fluvial Processes Erosion Masters Thesis 2014 ftcarolinadr https://doi.org/10.17615/q1ab-9j95 2023-09-09T22:31:29Z The Canadian Rocky Mountains record a dynamic history of erosion. Presently, bedrock rivers interact with the lithology and structural architecture of a large fold-and-thrust belt. Because the alpine landscape has been modified by Pleistocene and Holocene glaciation, rivers are also influenced by relict glacial landscape features. Here, we use topographic analysis and rock erodibility data to test the impact of lithology and glacial influence on fluvial form and incision potential in the headwaters of the Athabasca River Watershed. For 30 streams, we identify spikes in normalized channel steepness (ksn) where fluvial incision is focused. Results show that proximity to major lithologic contacts is not a predictor of knickzone location. Instead, bedrock channels are most perturbed from equilibrium where they flow over convexities at the intersection between hanging valleys and mainstem valley walls. These results suggest that glacial imprinting--mediated by variations in bedrock geology--controls Holocene erosion in this region. Master of Science Master Thesis Athabasca River Carolina Digital Repository (UNC - University of North Carolina) Athabasca River |
institution |
Open Polar |
collection |
Carolina Digital Repository (UNC - University of North Carolina) |
op_collection_id |
ftcarolinadr |
language |
English |
topic |
Geomorphology Geology Geographic information systems Geodesy Schmidt Hammer Canadian Rocky Mountains GIS Fluvial Processes Erosion |
spellingShingle |
Geomorphology Geology Geographic information systems Geodesy Schmidt Hammer Canadian Rocky Mountains GIS Fluvial Processes Erosion Quinlan, Kevin Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
topic_facet |
Geomorphology Geology Geographic information systems Geodesy Schmidt Hammer Canadian Rocky Mountains GIS Fluvial Processes Erosion |
description |
The Canadian Rocky Mountains record a dynamic history of erosion. Presently, bedrock rivers interact with the lithology and structural architecture of a large fold-and-thrust belt. Because the alpine landscape has been modified by Pleistocene and Holocene glaciation, rivers are also influenced by relict glacial landscape features. Here, we use topographic analysis and rock erodibility data to test the impact of lithology and glacial influence on fluvial form and incision potential in the headwaters of the Athabasca River Watershed. For 30 streams, we identify spikes in normalized channel steepness (ksn) where fluvial incision is focused. Results show that proximity to major lithologic contacts is not a predictor of knickzone location. Instead, bedrock channels are most perturbed from equilibrium where they flow over convexities at the intersection between hanging valleys and mainstem valley walls. These results suggest that glacial imprinting--mediated by variations in bedrock geology--controls Holocene erosion in this region. Master of Science |
author2 |
College of Arts and Sciences, Department of Geological Sciences Pavelsky, Tamlin Stewart, Kevin Willis, Michael |
format |
Master Thesis |
author |
Quinlan, Kevin |
author_facet |
Quinlan, Kevin |
author_sort |
Quinlan, Kevin |
title |
Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
title_short |
Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
title_full |
Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
title_fullStr |
Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
title_full_unstemmed |
Controls on Fluvial Geomorphology in the Canadian Rocky Mountains |
title_sort |
controls on fluvial geomorphology in the canadian rocky mountains |
publisher |
University of North Carolina at Chapel Hill Graduate School |
publishDate |
2014 |
url |
https://doi.org/10.17615/q1ab-9j95 https://cdr.lib.unc.edu/downloads/j96020977?file=thumbnail https://cdr.lib.unc.edu/downloads/j96020977 |
geographic |
Athabasca River |
geographic_facet |
Athabasca River |
genre |
Athabasca River |
genre_facet |
Athabasca River |
op_relation |
https://doi.org/10.17615/q1ab-9j95 https://cdr.lib.unc.edu/downloads/j96020977?file=thumbnail https://cdr.lib.unc.edu/downloads/j96020977 |
op_rights |
http://rightsstatements.org/vocab/InC/1.0/ |
op_doi |
https://doi.org/10.17615/q1ab-9j95 |
_version_ |
1779312769966800896 |