An investigation of two periglacial landforms on ignimbrite blockslopes in Kluane National Park and Reserve, Yukon Territory

dc.contributor.advisorHugenholtz, Christopher
dc.contributor.authorBoulding, Adam David
dc.contributor.committeememberMoorman, Brian
dc.contributor.committeememberDutchak, Alex
dc.date.accessioned2024-05-21T16:02:11Z
dc.date.available2024-05-21T16:02:11Z
dc.date.issued2024-05-14
dc.description.abstractAn expedition to the subarctic mountain of Campsite Peak, Yukon Territory, within the Kluane National Park and Reserve (KNPR), was conducted during the summer of 2019 to investigate two undocumented periglacial forms identified in satellite imagery. The overall goal of this MSc research is to present and measure these two features spatially, morphologically, and sedimentologically, placing them within the periglacial literature and hypothesizing plausible formative processes. The first study documents a feature similar to stone-banked solifluction terraces, termed blockslope terraces (BSTs) within this research, and are found in large numbers on low- to mid-slopes of Campsite Peak above the treeline, mantling a blocky open matrix of ignimbrite cobble-to-boulder material. BSTs differ from expected solifluction characteristics by showing apparent periodicity, large sample sizes, oblique orientations relative to their slope, and material too coarse to support the formation of ice needed for active solifluction. In-field morphological measurements combined with spatial and remote sediment sieving using photography and structure from motion modelling provided the exploratory measurements needed to place BSTs within the literature. It is the hypothesis of this research that BSTs are either a relict gelifluction feature from deglaciation, or nivation features of uncommon size and occurrence. The second study documents a feature, termed banded lichen formations (BLFs) within this research, found on the upper slopes of Campsite Peak. BLFs exhibit an alternating dark-and-light pattern caused by the presence and absence of lichens on the lighter felsic tuff material of Campsite Peak. It is hypothesized that BLFs are attributed to periglacial processes such as solifluction and frost heave, the form and relief of which are influenced by slope gradient and availability of fine-grained sediment in the system, leading to diverse spatial patterns, even across the same slopes. This research introduces two novel forms of periglacial landforms, both occurring on ignimbrite material, and both occurring on other mountains in KNPR of the same geologic unit. Further, the results of these studies underline the knowledge gaps in the solifluction and nivation literature surrounding landforms occurring on coarse, blocky material.
dc.identifier.citationBoulding, A. D. (2024). An investigation of two periglacial landforms on blockslopes in Kluane National Park and Reserve, Yukon Territory (Master's thesis, University of Calgary, Calgary, Canada). Retrieved from https://prism.ucalgary.ca.
dc.identifier.urihttps://hdl.handle.net/1880/118795
dc.identifier.urihttps://doi.org/10.11575/PRISM/46392
dc.language.isoen
dc.publisher.facultyGraduate Studies
dc.publisher.institutionUniversity of Calgary
dc.rightsUniversity of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
dc.subjectgeomorphology
dc.subjectlandform
dc.subjectperiglacial
dc.subjectsolifluction
dc.subjectpatterned ground
dc.subjectterrace
dc.subjectblockslope
dc.subjectblockfield
dc.subject.classificationPhysical Geography
dc.titleAn investigation of two periglacial landforms on ignimbrite blockslopes in Kluane National Park and Reserve, Yukon Territory
dc.typemaster thesis
thesis.degree.disciplineGeography
thesis.degree.grantorUniversity of Calgary
thesis.degree.nameMaster of Science (MSc)
ucalgary.thesis.accesssetbystudentI do not require a thesis withhold – my thesis will have open access and can be viewed and downloaded publicly as soon as possible.
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