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dc.contributor.authorRoningen, Jeanne Marieen_US
dc.date.accessioned2014-03-14T20:34:22Z
dc.date.available2014-03-14T20:34:22Z
dc.date.issued2011-04-22en_US
dc.identifier.otheretd-04262011-154246en_US
dc.identifier.urihttp://hdl.handle.net/10919/31950
dc.description.abstractMountain Lake in Giles County, Virginia, has a documented history of severe natural lake-level changes involving groundwater seepage [Jansons, 2004] that extend over the past 4200 years [Cawley, 1999], and as of December 2010 the lake was about 2% full by volume. Situated in the Valley and Ridge physiographic province on the axis of a plunging anticline and straddling contacts between three upper Ordovician and lower Silurian formations, the lake is one of two natural lakes in Virginia.

A daily water balance, geophysical surveying with dipole-dipole electrical resistivity, and chemical sampling have shed light on the nature of flow to and from the lake, including: 1) the steady nature of net groundwater outflow, 2) the seasonal response to precipitation of a forested first-order drainage system in fractured rock, 3) the influence of a fault not previously discussed in literature regarding the lake, and 4) the possibility of flow pathways through karst features.

Results from a water balance indicate steady lake drainage and significant recharge when vegetation is dormant, particularly during rain-on-snow melt events. The resistivity profiles display a highly heterogeneous subsurface and reveal low-resistivity areas that suggest flow pathways to and from the lake. Well logs, satellite images, and outcrop observations appear to confirm the presence of a fault to the east of the lake. Chemical evidence suggests that karst features may be present in the upper Reedsville-Trenton formation underlying the lakebed.

en_US
dc.publisherVirginia Techen_US
dc.relation.haspartRoningen_JM_T_2011_Copyright.pdfen_US
dc.relation.haspartRoningen_JM_T_2011.pdfen_US
dc.rightsI hereby certify that, if appropriate, I have obtained and attached hereto a written permission statement from the owner(s) of each third party copyrighted matter to be included in my thesis, dissertation, or project report, allowing distribution as specified below. I certify that the version I submitted is the same as that approved by my advisory committee. I hereby grant to Virginia Tech or its agents the non-exclusive license to archive and make accessible, under the conditions specified below, my thesis, dissertation, or project report in whole or in part in all forms of media, now or hereafter known. I retain all other ownership rights to the copyright of the thesis, dissertation or project report. I also retain the right to use in future works (such as articles or books) all or part of this thesis, dissertation, or project report.en_US
dc.subjectelectrical resistivityen_US
dc.subjectkarsten_US
dc.subjecthydrogeologyen_US
dc.subjectbaseflowen_US
dc.subjectevapotranspirationen_US
dc.titleHydrogeologic Controls on Lake Level at Mountain Lake, Virginiaen_US
dc.typeThesisen_US
dc.contributor.departmentGeosciencesen_US
thesis.degree.nameMaster of Scienceen_US
thesis.degree.levelmastersen_US
thesis.degree.grantorVirginia Polytechnic Institute and State Universityen_US
dc.contributor.committeechairBurbey, Thomas J.en_US
dc.contributor.committeememberHenika, William S.en_US
dc.contributor.committeememberMauldon, Matthewen_US
dc.contributor.committeememberParker, Bruce C.en_US
dc.identifier.sourceurlhttp://scholar.lib.vt.edu/theses/available/etd-04262011-154246/en_US
dc.date.sdate2011-04-26en_US
dc.date.rdate2012-08-07
dc.date.adate2011-05-09en_US


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