HR: 1340h
AN: V53B-1568    [Abstracts]
TI: Integrating laser-range finding, electronic compass measurements and GPS to rapidly map vertical changes in volcanic stratigraphy and constrain unit thicknesses and volumes: two examples from the northern Cordilleran volcanic province
AU: * Nogier, M
EM: nogierm@dickinson.edu
AF: Department of Geology Dickinson College, P.O.Box 1773, Carlisle, PA 17013 United States
AU: Edwards, B R
EM: edwardsb@dickinson.edu
AF: Department of Geology Dickinson College, P.O.Box 1773, Carlisle, PA 17013 United States
AU: Wetherell, K
EM: wetherek@dickinson.edu
AF: Department of Geology Dickinson College, P.O.Box 1773, Carlisle, PA 17013 United States
AB: We present preliminary results of laser-range finding-GPS surveys from two separate locations in northern British Columbia, in the south-central northern Cordilleran volcanic province: Hoodoo Mountain volcano and Craven Lake cone. This technique, described in detail below, is appropriate for rapidly measuring changes in vertical thicknesses of units that either would be difficult or impossible to measure by most other techniques. The ability to accurately measure thicknesses of geologic units in otherwise difficult-to-access locations will aide in generating better quantitative estimates of deposit geometries and eruption volumes. Such data is particularly important for constraining quantitative models of magma production and eruption dynamics. The deposits of interest in this study comprised at least partly inaccessible, largely pyroclastic units, although the technique could be used to map any vertical surfaces. The first field location was the northern side of Hoodoo Mountain volcano (56deg47'23.72'N/131deg17'36.97'W/1208m-asl), where a sequence of welded to unwelded, trachytic-phonolitic tephra was deposited in a paleovalley. This deposit is informally referred to as the Pointer Ridge deposit, and it comprises at least 7 distinct subunits. The horizontal limit of the exposures is approximately 1.5km, and the vertical limit is approximately 250m. Three different GPS base stations were used to map the lateral and vertical variations in the deposit. The second field location is north of Craven Lake (56deg54'44.55'N/129deg21'42.17'W/1453m-asl), along Craven Creek, where a sequence of basaltic tephra is overlain by pillow lava and glacial diamicton. This exposure is 200m long and approximately 30m high, much smaller than the area mapped at Hoodoo Mountain. The basaltic tephra appears to comprise 4 distinct sequences (measured thicknesses vary from 3-4m) not including the overlying pillow lava (measured thickness varies from 2 to 10m), and measurements of the sequences give average thicknesses of 5-10m. The laser-range finding-GPS setup used in these studies comprises an IMPULSE LR laser-range finder, a MapStar Module II electronic compass, and a Trimble ProXL global positioning (GPS) unit attached to a tripod specially designed to hold all three pieces of equipment. The three units communicate via a variety of cables. The maximum distance over which the laser can used is 500m (this distance varies for different lasers); the tripod was set at a relatively short distance from the exposure of interest at Craven Lake (95-115m), but further away at Hoodoo Mountain (up to 450m). The range finder was used to 'shoot' bottom and top contacts of each unit within the vertical faces. The distance and relative bearing were automatically transferred into compass and then to the GPS unit, producing in a map of the vertical face with horizontal and vertical coordinates. Analysis of the data provides detailed estimates of unit thicknesses across the vertical faces. The data collected can be imported into ArcGIS as a SHAPE file and overlain on DEM models for the areas of interest. ArcGIS extensions such as Spatial Analyst and 3D Analyst can be used to estimate surface areas and volumes for units mapped within the laser-GPS setup.
DE: 8428 Explosive volcanism
DE: 8429 Lava rheology and morphology
DE: 8486 Field relationships (1090, 3690)
DE: 8494 Instruments and techniques
SC: Volcanology, Geochemistry, Petrology [V]
MN: Fall Meeting 2005