|2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)|
|Paper No. 96-29|
|Presentation Time: 9:00 AM-6:00 PM|
DEVELOPING TERRESTRIAL-LIDAR MODELS OF PERIGLACIAL BOULDER-FIELD FABRIC
CARISIO, Sebastian1, CONLON, Alexander1, O'NEAL, Michael2, and HANSON, Brain1, (1) Geography, University of Delaware, 125 Academy Street, Newark, DE 19716, email@example.com, (2) Geography Department, University of Delaware, Newark, DE 19716|
Boulder colluvium mantles with areas of unvegetated boulder fields can be found throughout the Late-Pleistocene periglacial fringe of the Mid-Atlantic, USA. The genesis of these boulder fields has been attributed to different processes that include fluvial, glaciofluvial, and freeze-thaw coupled with down-slope gelifluction. The latter has gained preference as the most appropriate model for boulder field genesis in recent years; however, the exact process by which these areas form remains unclear. Data to support the movement of boulders by gelifluction has typically relied on intense field surveys that require direct measurements of boulder aspect and slope. In this study, we develop laboratory terrain models consisting of small blocks of known geometry and orientation, and create DEMs of these physical models from terrestrial LIDAR. Analyses of the DEMs successfully characterize the known biases and trends in slope and orientation of the blocks. Our results suggest that a DEM created from terrestrial LIDAR provides an effective method for characterizing boulder field fabric without direct boulder measurement. The continuation of this project will involve analyses of a Pennsylvania boulder field using the same methods.
2011 GSA Annual Meeting in Minneapolis (9–12 October 2011)
General Information for this Meeting
|Session No. 96--Booth# 49|
Minneapolis Convention Center: Hall C
9:00 AM-6:00 PM, Monday, 10 October 2011
Geological Society of America Abstracts with Programs, Vol. 43, No. 5, p. 252
© Copyright 2011 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.