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			<titleStmt><title level='a'>Erosion of a young volcanic cone: a case study at Ahmanilix, Okmok Volcano, Alaska</title></titleStmt>
			<publicationStmt>
				<publisher>American Geophysical Union</publisher>
				<date>12/11/2024</date>
			</publicationStmt>
			<sourceDesc>
				<bibl> 
					<idno type="par_id">10572310</idno>
					<idno type="doi"></idno>
					
					<author>Daniel Orejuela</author><author>Jasper Baur</author><author>Einat Lev</author><author>Frank Oliver Nitsche</author><author>Terry A Plank</author><author>Conor Bacon</author>
				</bibl>
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			<abstract><ab><![CDATA[Cinder cones are a common feature at many volcanic eruptions. Their shapes and volumescan reveal information about eruption conditions, and their geomorphological evolution shapesthem and their surrounding environment. It is thus important to quantify the rate and patternsof erosion of young cinder cones. In this study, we examine the Ahmanilix cone, which formedduring the 2008 eruption of Okmok volcano in the Aleutian islands region of Alaska.Ahmanilix, located on the eastern side of Okmok’s large caldera, is >250 meters tall andcharacterized by dramatic gullies formed by the harsh wind, snow and rain conditions typical ofthe Aleutians. We usd photogrammetry to create 3D models of Ahmanilix using aerialphotographic surveys taken from a helicopter in 2021, 2022, 2023 and 2024. We utilize AgisoftMetashape to build point clouds, Cloud Compare to align the point clouds and build rasterDigital Elevation Models (DEMs), and QGIS and Python to visualize and analyze theseproducts. By subtracting DEM rasters we quantify year-to-year erosion. We compare ourresults with erosion rates estimated from satellite observations (Dai et al., 2020), identifyregions dominated by erosion or deposition and correlate them with slopes and cinderlithology. Our observations can be extended to other cinder cones and help predict theirgeomorphological evolution.]]></ab></abstract>
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