T372 Remote Sensing Applications in Hydrology and Geology (Posters)
Wednesday, 25 October 2017
9:00 AM - 6:30 PM
Halls 4EF
APPLICATION OF ELECTROMAGNETIC INDUCTION AT THE UPPER CAMP BIRD III ROCK GLACIER IN THE SAN JUAN MOUNTAINS, COLORADO
Paper number: T372-15
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Raquel Granados-AguilarTexas A&M University, College Station, TX
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John R. GiardinoTexas A&M University, College Station, TX
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Mark E. EverettTexas A&M University, College Station, TX
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Dennis MmasaTexas A&M University, College Station, TX
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Maximilian WitekTexas A&M University, College Station, TX
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Rodrigo RodriguezUniversity of Guanajuato, Guanajuato
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Potpreecha PondthaiTexas A&M University, College Station, TX
Abstract
In order to interpret hydrogeological characteristics, as well as to quantify their potential for freshwater resources, it is integral to understand the internal structure of these periglacial landforms. To obtain a detailed representation of the internal structure and determine the boundaries between resistive (rocks, sediment, and ice) and conductive materials (water and ore deposits) of the rock glacier, time-domain and frequency-domain methods along with detailed geological and geomorphological mapping will be used.
Many studies have been conducted using several geophysical methods, such as seismic refraction, gravimetry, resistivity, radio-echo surveys, GPR, and EM profilers to study the internal structure of rock glaciers. However, to date, no published research using the novel G-TEM system by Geonics has been found.
The G-TEM by Geonics Ltd. is an innovative controlled-source time-domain electromagnetic induction system. Using the G-TEM, the distribution of electrical conductivity in the subsurface can be mapped in order to characterize the internal structure of the rock glacier from 5-10 m depth and below. The EM Profiler is a frequency-domain electromagnetic induction system that will be used for the investigation of the uppermost layers of the rock glacier. For the proposed research, the use of two different systems will provide continuity across the data sets and will help validate the measurements recorded with the new equipment. The proposed research will validate the use of unique equipment in combination with traditional methods to characterize the internal structure and quantify the untapped water resource stored within the Upper Camp Bird III rock glacier located in the Camp Bird mine area in Ouray, CO, with potential application to the study of rock glaciers all over the world.
Geological Society of America Abstracts with Programs. Vol. 49, No. 6
doi: 10.1130/abs/2017AM-307832
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