Tuesday, April 30, 2013
Wednesday, April 24, 2013
Buffalo River karst studies
Geosciences and Environmental Change Science Center
Geologic Mapping Studies at Buffalo National River, Northern Arkansas
Figure 1. Location map.
Detailed geologic mapping is being conducted by the USGS in and adjacent to the Buffalo National River (figs. 1, 2), a park administered by the National Park Service, to better understand and characterize the natural resources and associated ecosystems of this area within the Ozark Plateau region. General-purpose geologic maps (fig. 3) are created to provide a framework for a host of natural resource, natural history, and public education uses. The mapping activities focus on understanding development of karst features (fig. 4) and ground water flow paths through extensive karst aquifers within Ordovician through Pennsylvanian rock strata that underlie the Buffalo River watershed.
The geologic maps provide background to understand major cave resources in the park, geologic controls on major spring locations, and recharge areas for springs, including recharge basins that extend beyond the surface watershed boundaries of the Buffalo River.
Figure 2. Photograph of Buffalo River from river trail overlook near Steel Creek.
Figure 3. Geologic map of the Jasper Quadrangle - example of products.
Figure 4. Examples of karst features within the Buffalo National River Park. Karst is a type of topography that is formed over limestone, dolomite, or gypsum by dissolving or solution, and that is characterized by closed depressions or sinkholes, caves, and underground drainage (American Geological Institute Dictionary of Geologic Terms).
Project Activities
- Conduct geologic mapping at 1:24,000 scale of quadrangles in and adjacent to the Buffalo River watershed (fig. 5). As part of geologic mapping for each quadrangle, summarize the stratigraphic succession, document structural features, and develop a structure contour map for the major aquifer unit.
Figure 5. Status of Geologic Mapping in Western Part of Buffalo National River
- Construct and compile Geographic Information System (GIS) databases of the geologic data.
- Integrate geology with National Park Service karst and spring inventories and dye tracer results to investigate geologic controls on karst hydrology.
- Buffalo River incision history through OSL (Optically Stimulated Luminescence) dating of river terraces.
- Conduct three-dimensional modeling of geologic framework (fig. 6).
Figure 6. Three-dimensional geology model of the western part of the Buffalo River area. View is toward the north and colors show different rock formations that are distributed across the area.
Results
The geologic mapping helps place inventories of springs and caves within the park in proper stratigraphic context. Caves and springs are present in a variety of geologic formations ranging in age from Ordovician to Pennsylvanian, but they are concentrated within the 120-m-thick, Mississippian-aged limestone of the Boone Formation. Springs (fig. 7) in the western part of the park are most frequent near the unconformable contact between the basal St. Joe Member of the Boone Formation and underlying sandstone-rich Ordovician Everton Formation. These features indicate that the Boone Formation, comprising the karstic Springfield aquifer, is the principal path for ground-water flow into the western Buffalo River watershed. New mapping documents that major springs and cave systems are localized in structural lows (fig. 8) of the Boone Formation where ground water discharges at lowest elevations within the perched Springfield aquifer. Dye-tracer studies indicated that some springs localized in structural lows have captured recharge from beyond topographic watershed boundaries (fig. 9). This interbasin flow of ground water becomes a land management concern if agricultural land use of adjacent watersheds results in transfer of nutrient-enriched ground water in the Buffalo River.
Figure 7. Springs localized in basal St. Joe Limestone Member of Boone Formation, the principal karst aquifer of the western Buffalo River region.
Figure 8. Three-dimensional model of geology showing major springs localized at base of structural low in Boone Formation.
Figure 9. Dye tracer study of Dogpatch Springs interbasin recharge area. Discharge springs are localized at corner of structural low formed by intersection of two faults.
New geologic mapping in the middle part of the Buffalo River documents a transition from the Springfield Plateau aquifer to lower karstic Ordovician formations of the Ozark aquifer. The largest spring in the park, Mitch Hill Spring (fig. 10), discharges from a stratigraphic level in the lowest part of the Ordovician Everton Formation above impervious argillaceous dolostone of the Powell Dolomite that is brought to the surface along the Buffalo River in a structural high. Dye tracer studies integrated with the geologic mapping are investigating probable pathways for ground water between the two aquifers.
Figure 10. Mitch Hill Spring. (Click on image for a larger view.)
New geologic mapping has recognized many new faults and folds in the region and has added information on the age and character of new and previously recognized faults. These data are revealing new insights into the ancient history of deformation in the area that was probably related to past interactions among tectonic plates in late Paleozoic time.
Results of these mapping efforts were presented to fieldtrip participants at the Geological Society of America North Central/South Central section combined meeting in April 2010. Mark Hudson and Kenzie Turner of the USGS and Chuck Bitting of the National Park Service led the field trip to emphasize geologic controls on karst development in the Buffalo National River area (fig. 11).
Figure 11. Field trip leaders describe the geologic controls on the formation of the large sinkhole in the Batesville Sandstone.
Funding Sources
- Internal
- Karst Applied Research Studies through Geologic Mapping Project, USGS National Cooperative Geologic Mapping Program
- Department of the Interior Ozark Landscapes Project
- External
- National Park Service Water Resources and Geologic Divisions
Staff
- Mark R. Hudson, geologic mapping, geohydrology applications, tectonics
- Kenzie J. Turner, geologic mapping, GIS applications, 3D geologic modelling
Key Collaborators
- Chuck Bitting, Geologist and Karst Specialist, Buffalo National River, Harrison, Arkansas
- Doy Zachry, University of Arkansas, Fayetteville, Arkansas
- Van Brahana, University of Arkansas, Fayetteville, Arkansas
- Angela Chandler, Arkansas Geological Survey, Little Rock, Arkansas
- Scott Ausbrooks, Arkansas Geological Survey, Little Rock, Arkansas
- Richard Hutto, Arkansas Geological Survey, Little Rock, Arkansas
- Shannon Mahan, USGS, Denver, Colorado
- James Kaufmann, USGS, Rolla, Missouri
- Timothy Kresse, USGS, Little Rock, Arkansas
Related Links
- Water resources of Arkansas
- Arkansas Geological Survey
- National Park Service, Buffalo National River
Publications (by date; most recent first)
Hudson, M.R., Turner, K.J. and Bitting, C., 2011, Geology and karst landscapes of the Buffalo National River area, northern Arkansas: in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011: U.S. Geological Survey Scientific Investigations Report 2011-5031, p. 191-212.
Hudson, M.R., Turner, K.J., Bitting, C., Kaufmann, J.E., Kresse, T.M., and Mott, D.N., 2011, Geologic controls on karst landscapes in the Buffalo National River Area of northern Arkansas: Insights gained from comparison of geologic mapping, topography, dye tracers, and karst inventories,in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011: U.S. Geological Survey Scientific Investigations Report 2011-5031, p. 86.
Turner, K.J., and Hudson, M.R., 2010, Geologic map of the Maumee Quadrangle, Searcy and Marion counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 3134, 1:24,000 scale.
Turner, K.J., and Hudson, M.R., 2010, Geologic features of the Maumee Quadrangle, Marion and Searcy counties, Arkansas: Geological Society of America Abstracts with Programs, v. 41, n. 2, p. 71.
Hudson, M.R., Turner, K.J., and Trexler, C.C., 2010, Geometry, relative ages, and tectonic implications of joints from regional assessment of the Buffalo National River area, northern Arkansas: Geological Society of America Abstracts with Programs, v. 41, n. 2, p. 71.
Hudson, M.R., Turner, K.J., and Trexler, C.C., 2009, Regional joint analysis for the Buffalo National River area of northern Arkansas: Implications for tectonic history and landscape influence: Geological Society of America Abstracts with Programs, v. 41, n. 7, p. 367.
Hudson, M.R., and Turner, K.J., 2009, Geologic map of the St. Joe Quadrangle, Searcy and Marion counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 3074, 1:24,000 scale.
Hudson, M.R., and Turner, K.J., 2008, Geologic framework of the Boxley Quadrangle on the southern flank of the Ozark Dome, northern Arkansas: Geological Society of America Abstracts with Programs, v. 40, n. 3, p 33.
Turner, K.J., and Hudson, M.R., 2008, Improved understanding of a karst aquifer system through utilization of a 3D geologic model, Buffalo National River, Arkansas: Geological Society of America Abstracts with Programs, v. 40, n. 3, p. 36.
Hudson, M.R., and Turner, K.J., 2007, Geologic map of the Boxley Quadrangle, Newton and Madison Counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 2991, 1:24,000 scale.
Turner, K.J., Hudson, M.R., Murray, K.E., and Mott, D.N., 2007, Three-dimensional geologic framework model for a karst aquifer system, Hasty and Western Grove quadrangles, northern Arkansas: U.S. Geological Survey Scientific Investigations Report 2007-5095, 12 p. and CD digital archive.
Hudson, M.R., Turner, K.J., and Repetski, J.E., 2006, Geologic map of the Western Grove Quadrangle, Northwestern Arkansas: U.S. Geological Survey Scientific Investigations Map 2921, 1:24,000 scale.
Hudson, M.R., and Turner, K.J., 2006, Three-phase late Paleozoic deformation on the southern flank of the Ozark dome, northern Arkansas: Geological Society of American Abstracts with Programs, v. 38, n. 6, p. 12.
Hudson, M. R., Mott, D.N., Turner, K.J., and Murray, K.E., 2005, Geologic controls on a transition between karst aquifers at Buffalo National River, northern Arkansas, in Knuiansky, E.L., editor, U.S. Geological Survey Scientific Investigations Report 5160, p. 143.
Hudson, M.R., and Murray, K.E., 2004, Geologic map of the Hasty Quadrangle, Boone, and Newton Counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 2847, 1:24,000 scale.
Hudson, M.R., and Murray, K.E., 2003, Geologic map of the Ponca Quadrangle, Newton, Boone, and Carroll Counties, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 2412, 1:24,000 scale.
Hudson, M.R., 2003, The Indian Creek fault zone: a late Paleozoic oblique rift in northern Arkansas: Geological Society of America Abstract with Programs, v. 35, n. 1, p. 71.
Hudson, M.R., and Cox, R.T., 2003, Late Paleozoic tectonics of the southern Ozark dome, in Cox, R.T., compiler, Field trip guidebook for Joint South-Central and Southeastern Sections, Geological Society of America, Tennessee Division of Geology Report of Investigations 51, p. 15-32.
Hudson, M.R., Mott, D.N., Murray, K.E., and Bitting, C.J., 2002, Geologic framework of karst development and groundwater flow, Buffalo National River, northern Arkansas, in Proceedings of National Park Service Water Professionals Meeting, Fort Collins, Colorado, p. 22.
Murray, K.E., and Hudson, M.R., 2002, Three-dimensional geologic framework modeling in the Buffalo National River, Arkansas: Geological Society of America Abstract with Programs, v. 34, n. 6, p. 120.
Hudson, M.R., 2002, Three-phase late Paleozoic deformation of the southern Ozark dome, western Buffalo River region, northern Arkansas: Geological Society of America Abstract with Programs, v. 34, n. 6, p. 79.
Murray, K.E., and Hudson, M.R., 2002, Three-dimensional geologic framework modeling for a karst region in the Buffalo National River, Arkansas:in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Water-Resources Investigations Report 02-4174, p. 51-58.
Hudson, M.R., Murray, K.E., and Pezzutti, D., 2001, Geologic map of the Jasper Quadrangle, Newton and Boone Counties, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 2356, 1:24,000 scale.
Hudson, M.R., Mott, D.N., and Bitting, C.J., 2001, Geologic framework of karst features in western Buffalo National River, northern Arkansas, in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, U.S. Geological Survey Water-Resources Investigations Report 01-4011, p. 16-17.
Mott, D.N., Hudson, M.R., and Aley, T., 2000, Hydrologic investigations reveal interbasin recharge contributes significantly to detrimental nutrient loads at Buffalo National River, Arkansas: Proceedings of Arkansas Water Resources Center Annual Conference MSC-284, Fayetteville, Ark., p. 13-20.
Hudson, M.R., 2000, Coordinated strike-slip and normal faulting in the southern Ozark dome of northern Arkansas: Deformation in a late Paleozoic foreland: Geology, v. 28, p. 511-514.
Mott, D.N., Hudson, M.R., and Aley, T., 2000, Hydrogeologic investigations reveal interbasin recharge contributes significantly to nutrient loads at Buffalo National River, Arkansas: Geological Society of America Abstracts with Programs, v. 32, n. 3, p. 36-37.
Hudson, M.R., 2000, Multiphase late Paleozoic deformation in the western Buffalo River region of northern Arkansas: A foreland record of an evolving Ouachita orogeny: Geological Society of America Abstracts with Programs, v. 32, n. 3, p. 15.
Mott, D.N., Hudson, M.R., and Aley, T., 1999, Nutrient loads traced to interbasin groundwater transport at Buffalo National River, Arkansas, in Harmon, D., ed., Proceedings of the 10th Conference on Research and Resource Management in Parks and on Public Lands, George Wright Society, Hancock, Michigan, p. 114-121.
Mott, D.N., Hudson, M.R., and Aley, T., 1998, Water resources, geologic mapping, and dye-tracings employed to develop a model of interbasin recharge, Buffalo National River: Proceedings of the Friends of Karst/International Geologic Correlation Program Conference, Western Kentucky University, Bowling Green, Kentucky, p 26.
Hudson, M.R., and Mott, D.N., 1998, Structural influence on springs and interbasin recharge in a karst aquifer, Buffalo National River, northwestern Arkansas, USA: Proceedings of American Institute of Hydrology/International Association of Hydrologists "Gambling with Groundwater" Conference, p. 36-37.
Hudson, M.R., 1998, Geologic map of parts of the Jasper, Hasty, Ponca, Gaither, and Harrison quadrangles in and adjacent to Buffalo National River, northwestern Arkansas: U.S. Geological Survey Open-File Report 98-116, 1:24,000 scale with 20 p. text.
Hudson, M.R., and Mott, D.N., 1997, Faulting and coincident interbasin ground water flow in a karst aquifer, Buffalo National River region, northwestern Arkansas: Geological Society of America Abstracts with Programs, v. 29, n. 6, p. 181-182.
U.S. Department of the Interior | U.S. Geological SurveyURL: http://esp.cr.usgs.gov/projects/buffaloriver/
Page Contact Information: Website Manager
Page Last Modified: Wednesday, 09-Jan-2013 13:12:34 Mountain Standard Time
Geosciences and Environmental Change Science Center
Geologic Mapping Studies at Buffalo National River, Northern Arkansas
Figure 1. Location map.
Detailed geologic mapping is being conducted by the USGS in and adjacent to the Buffalo National River (figs. 1, 2), a park administered by the National Park Service, to better understand and characterize the natural resources and associated ecosystems of this area within the Ozark Plateau region. General-purpose geologic maps (fig. 3) are created to provide a framework for a host of natural resource, natural history, and public education uses. The mapping activities focus on understanding development of karst features (fig. 4) and ground water flow paths through extensive karst aquifers within Ordovician through Pennsylvanian rock strata that underlie the Buffalo River watershed.
The geologic maps provide background to understand major cave resources in the park, geologic controls on major spring locations, and recharge areas for springs, including recharge basins that extend beyond the surface watershed boundaries of the Buffalo River.
Figure 2. Photograph of Buffalo River from river trail overlook near Steel Creek.Figure 3. Geologic map of the Jasper Quadrangle - example of products.Figure 4. Examples of karst features within the Buffalo National River Park. Karst is a type of topography that is formed over limestone, dolomite, or gypsum by dissolving or solution, and that is characterized by closed depressions or sinkholes, caves, and underground drainage (American Geological Institute Dictionary of Geologic Terms).
Project Activities
- Conduct geologic mapping at 1:24,000 scale of quadrangles in and adjacent to the Buffalo River watershed (fig. 5). As part of geologic mapping for each quadrangle, summarize the stratigraphic succession, document structural features, and develop a structure contour map for the major aquifer unit.
Figure 5. Status of Geologic Mapping in Western Part of Buffalo National River
- Construct and compile Geographic Information System (GIS) databases of the geologic data.
- Integrate geology with National Park Service karst and spring inventories and dye tracer results to investigate geologic controls on karst hydrology.
- Buffalo River incision history through OSL (Optically Stimulated Luminescence) dating of river terraces.
- Conduct three-dimensional modeling of geologic framework (fig. 6).
Figure 6. Three-dimensional geology model of the western part of the Buffalo River area. View is toward the north and colors show different rock formations that are distributed across the area.
Results
The geologic mapping helps place inventories of springs and caves within the park in proper stratigraphic context. Caves and springs are present in a variety of geologic formations ranging in age from Ordovician to Pennsylvanian, but they are concentrated within the 120-m-thick, Mississippian-aged limestone of the Boone Formation. Springs (fig. 7) in the western part of the park are most frequent near the unconformable contact between the basal St. Joe Member of the Boone Formation and underlying sandstone-rich Ordovician Everton Formation. These features indicate that the Boone Formation, comprising the karstic Springfield aquifer, is the principal path for ground-water flow into the western Buffalo River watershed. New mapping documents that major springs and cave systems are localized in structural lows (fig. 8) of the Boone Formation where ground water discharges at lowest elevations within the perched Springfield aquifer. Dye-tracer studies indicated that some springs localized in structural lows have captured recharge from beyond topographic watershed boundaries (fig. 9). This interbasin flow of ground water becomes a land management concern if agricultural land use of adjacent watersheds results in transfer of nutrient-enriched ground water in the Buffalo River.
Figure 7. Springs localized in basal St. Joe Limestone Member of Boone Formation, the principal karst aquifer of the western Buffalo River region.Figure 8. Three-dimensional model of geology showing major springs localized at base of structural low in Boone Formation.Figure 9. Dye tracer study of Dogpatch Springs interbasin recharge area. Discharge springs are localized at corner of structural low formed by intersection of two faults.
New geologic mapping in the middle part of the Buffalo River documents a transition from the Springfield Plateau aquifer to lower karstic Ordovician formations of the Ozark aquifer. The largest spring in the park, Mitch Hill Spring (fig. 10), discharges from a stratigraphic level in the lowest part of the Ordovician Everton Formation above impervious argillaceous dolostone of the Powell Dolomite that is brought to the surface along the Buffalo River in a structural high. Dye tracer studies integrated with the geologic mapping are investigating probable pathways for ground water between the two aquifers.
Figure 10. Mitch Hill Spring. (Click on image for a larger view.)
New geologic mapping has recognized many new faults and folds in the region and has added information on the age and character of new and previously recognized faults. These data are revealing new insights into the ancient history of deformation in the area that was probably related to past interactions among tectonic plates in late Paleozoic time.
Results of these mapping efforts were presented to fieldtrip participants at the Geological Society of America North Central/South Central section combined meeting in April 2010. Mark Hudson and Kenzie Turner of the USGS and Chuck Bitting of the National Park Service led the field trip to emphasize geologic controls on karst development in the Buffalo National River area (fig. 11).
Figure 11. Field trip leaders describe the geologic controls on the formation of the large sinkhole in the Batesville Sandstone.
Funding Sources
- Internal
- Karst Applied Research Studies through Geologic Mapping Project, USGS National Cooperative Geologic Mapping Program
- Department of the Interior Ozark Landscapes Project
- External
- National Park Service Water Resources and Geologic Divisions
Staff
- Mark R. Hudson, geologic mapping, geohydrology applications, tectonics
- Kenzie J. Turner, geologic mapping, GIS applications, 3D geologic modelling
Key Collaborators
- Chuck Bitting, Geologist and Karst Specialist, Buffalo National River, Harrison, Arkansas
- Doy Zachry, University of Arkansas, Fayetteville, Arkansas
- Van Brahana, University of Arkansas, Fayetteville, Arkansas
- Angela Chandler, Arkansas Geological Survey, Little Rock, Arkansas
- Scott Ausbrooks, Arkansas Geological Survey, Little Rock, Arkansas
- Richard Hutto, Arkansas Geological Survey, Little Rock, Arkansas
- Shannon Mahan, USGS, Denver, Colorado
- James Kaufmann, USGS, Rolla, Missouri
- Timothy Kresse, USGS, Little Rock, Arkansas
Related Links
- Water resources of Arkansas
- Arkansas Geological Survey
- National Park Service, Buffalo National River
Publications (by date; most recent first)
Hudson, M.R., Turner, K.J. and Bitting, C., 2011, Geology and karst landscapes of the Buffalo National River area, northern Arkansas: in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011: U.S. Geological Survey Scientific Investigations Report 2011-5031, p. 191-212.
Hudson, M.R., Turner, K.J., Bitting, C., Kaufmann, J.E., Kresse, T.M., and Mott, D.N., 2011, Geologic controls on karst landscapes in the Buffalo National River Area of northern Arkansas: Insights gained from comparison of geologic mapping, topography, dye tracers, and karst inventories,in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Fayetteville, Arkansas, April 26-29, 2011: U.S. Geological Survey Scientific Investigations Report 2011-5031, p. 86.
Turner, K.J., and Hudson, M.R., 2010, Geologic map of the Maumee Quadrangle, Searcy and Marion counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 3134, 1:24,000 scale.
Turner, K.J., and Hudson, M.R., 2010, Geologic features of the Maumee Quadrangle, Marion and Searcy counties, Arkansas: Geological Society of America Abstracts with Programs, v. 41, n. 2, p. 71.
Hudson, M.R., Turner, K.J., and Trexler, C.C., 2010, Geometry, relative ages, and tectonic implications of joints from regional assessment of the Buffalo National River area, northern Arkansas: Geological Society of America Abstracts with Programs, v. 41, n. 2, p. 71.
Hudson, M.R., Turner, K.J., and Trexler, C.C., 2009, Regional joint analysis for the Buffalo National River area of northern Arkansas: Implications for tectonic history and landscape influence: Geological Society of America Abstracts with Programs, v. 41, n. 7, p. 367.
Hudson, M.R., and Turner, K.J., 2009, Geologic map of the St. Joe Quadrangle, Searcy and Marion counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 3074, 1:24,000 scale.
Hudson, M.R., and Turner, K.J., 2008, Geologic framework of the Boxley Quadrangle on the southern flank of the Ozark Dome, northern Arkansas: Geological Society of America Abstracts with Programs, v. 40, n. 3, p 33.
Turner, K.J., and Hudson, M.R., 2008, Improved understanding of a karst aquifer system through utilization of a 3D geologic model, Buffalo National River, Arkansas: Geological Society of America Abstracts with Programs, v. 40, n. 3, p. 36.
Hudson, M.R., and Turner, K.J., 2007, Geologic map of the Boxley Quadrangle, Newton and Madison Counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 2991, 1:24,000 scale.
Turner, K.J., Hudson, M.R., Murray, K.E., and Mott, D.N., 2007, Three-dimensional geologic framework model for a karst aquifer system, Hasty and Western Grove quadrangles, northern Arkansas: U.S. Geological Survey Scientific Investigations Report 2007-5095, 12 p. and CD digital archive.
Hudson, M.R., Turner, K.J., and Repetski, J.E., 2006, Geologic map of the Western Grove Quadrangle, Northwestern Arkansas: U.S. Geological Survey Scientific Investigations Map 2921, 1:24,000 scale.
Hudson, M.R., and Turner, K.J., 2006, Three-phase late Paleozoic deformation on the southern flank of the Ozark dome, northern Arkansas: Geological Society of American Abstracts with Programs, v. 38, n. 6, p. 12.
Hudson, M. R., Mott, D.N., Turner, K.J., and Murray, K.E., 2005, Geologic controls on a transition between karst aquifers at Buffalo National River, northern Arkansas, in Knuiansky, E.L., editor, U.S. Geological Survey Scientific Investigations Report 5160, p. 143.
Hudson, M.R., and Murray, K.E., 2004, Geologic map of the Hasty Quadrangle, Boone, and Newton Counties, Arkansas: U.S. Geological Survey Scientific Investigations Map 2847, 1:24,000 scale.
Hudson, M.R., and Murray, K.E., 2003, Geologic map of the Ponca Quadrangle, Newton, Boone, and Carroll Counties, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 2412, 1:24,000 scale.
Hudson, M.R., 2003, The Indian Creek fault zone: a late Paleozoic oblique rift in northern Arkansas: Geological Society of America Abstract with Programs, v. 35, n. 1, p. 71.
Hudson, M.R., and Cox, R.T., 2003, Late Paleozoic tectonics of the southern Ozark dome, in Cox, R.T., compiler, Field trip guidebook for Joint South-Central and Southeastern Sections, Geological Society of America, Tennessee Division of Geology Report of Investigations 51, p. 15-32.
Hudson, M.R., Mott, D.N., Murray, K.E., and Bitting, C.J., 2002, Geologic framework of karst development and groundwater flow, Buffalo National River, northern Arkansas, in Proceedings of National Park Service Water Professionals Meeting, Fort Collins, Colorado, p. 22.
Murray, K.E., and Hudson, M.R., 2002, Three-dimensional geologic framework modeling in the Buffalo National River, Arkansas: Geological Society of America Abstract with Programs, v. 34, n. 6, p. 120.
Hudson, M.R., 2002, Three-phase late Paleozoic deformation of the southern Ozark dome, western Buffalo River region, northern Arkansas: Geological Society of America Abstract with Programs, v. 34, n. 6, p. 79.
Murray, K.E., and Hudson, M.R., 2002, Three-dimensional geologic framework modeling for a karst region in the Buffalo National River, Arkansas:in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, Water-Resources Investigations Report 02-4174, p. 51-58.
Hudson, M.R., Murray, K.E., and Pezzutti, D., 2001, Geologic map of the Jasper Quadrangle, Newton and Boone Counties, Arkansas: U.S. Geological Survey Miscellaneous Field Studies Map 2356, 1:24,000 scale.
Hudson, M.R., Mott, D.N., and Bitting, C.J., 2001, Geologic framework of karst features in western Buffalo National River, northern Arkansas, in Kuniansky, E.L., ed., U.S. Geological Survey Karst Interest Group Proceedings, U.S. Geological Survey Water-Resources Investigations Report 01-4011, p. 16-17.
Mott, D.N., Hudson, M.R., and Aley, T., 2000, Hydrologic investigations reveal interbasin recharge contributes significantly to detrimental nutrient loads at Buffalo National River, Arkansas: Proceedings of Arkansas Water Resources Center Annual Conference MSC-284, Fayetteville, Ark., p. 13-20.
Hudson, M.R., 2000, Coordinated strike-slip and normal faulting in the southern Ozark dome of northern Arkansas: Deformation in a late Paleozoic foreland: Geology, v. 28, p. 511-514.
Mott, D.N., Hudson, M.R., and Aley, T., 2000, Hydrogeologic investigations reveal interbasin recharge contributes significantly to nutrient loads at Buffalo National River, Arkansas: Geological Society of America Abstracts with Programs, v. 32, n. 3, p. 36-37.
Hudson, M.R., 2000, Multiphase late Paleozoic deformation in the western Buffalo River region of northern Arkansas: A foreland record of an evolving Ouachita orogeny: Geological Society of America Abstracts with Programs, v. 32, n. 3, p. 15.
Mott, D.N., Hudson, M.R., and Aley, T., 1999, Nutrient loads traced to interbasin groundwater transport at Buffalo National River, Arkansas, in Harmon, D., ed., Proceedings of the 10th Conference on Research and Resource Management in Parks and on Public Lands, George Wright Society, Hancock, Michigan, p. 114-121.
Mott, D.N., Hudson, M.R., and Aley, T., 1998, Water resources, geologic mapping, and dye-tracings employed to develop a model of interbasin recharge, Buffalo National River: Proceedings of the Friends of Karst/International Geologic Correlation Program Conference, Western Kentucky University, Bowling Green, Kentucky, p 26.
Hudson, M.R., and Mott, D.N., 1998, Structural influence on springs and interbasin recharge in a karst aquifer, Buffalo National River, northwestern Arkansas, USA: Proceedings of American Institute of Hydrology/International Association of Hydrologists "Gambling with Groundwater" Conference, p. 36-37.
Hudson, M.R., 1998, Geologic map of parts of the Jasper, Hasty, Ponca, Gaither, and Harrison quadrangles in and adjacent to Buffalo National River, northwestern Arkansas: U.S. Geological Survey Open-File Report 98-116, 1:24,000 scale with 20 p. text.
Hudson, M.R., and Mott, D.N., 1997, Faulting and coincident interbasin ground water flow in a karst aquifer, Buffalo National River region, northwestern Arkansas: Geological Society of America Abstracts with Programs, v. 29, n. 6, p. 181-182.
U.S. Department of the Interior | U.S. Geological SurveyURL: http://esp.cr.usgs.gov/projects/buffaloriver/
Page Contact Information: Website Manager
Page Last Modified: Wednesday, 09-Jan-2013 13:12:34 Mountain Standard Time
Thursday, April 18, 2013
Wednesday, April 17, 2013
Earth Day events April 20 and 21, 2013: Both free to everyone
Please click on images to ENLARGE for easy reading.
John Rule looking across Frog Bayou where it runs through his property in Crawford County
Earth Day poster with Western Wall Flower on WPWP
Mayor's Town Hall meeting recorded April 1, 2013, at Fayetteville Boys and Girls Club
Mayor Lioneld Jordan's Town Hall meeting video from April 1, 2013
Friday, April 5, 2013
Facts about Keystone XL Pipeline
Keystone XL Pipeline forum recorded in Oklahoma by Quinn Montana and Luke Simons. Edited at Fayetteville Public Television station by David Druding for OMNI Center for Peace, Justice and Ecology.
Monday, April 1, 2013
Ouachita River pollution continues to dismay of Ouachita Riverkeeper
Koch Industries accused of polluting waterway
Public Employees for Environmental responsibility
by Chris Zawistowski, CBS News investigates intern
A Koch Industries paper mill is violating the Clean Water Act by pumping out massive amounts of pollution into an Arkansas waterway, according to an EPA enforcement complaint to be filed tomorrow by Public Employees for Environmental Responsibility (PEER) and the Ouachita Riverkeeper.
The complaint alleges that a Georgia-Pacific paper mill on the Coffee Creek in Arkansas - owned by the billionaire Koch Brothers -emits 45 million gallons of paper mill waste including hazardous materials like ammonia, chloride, and mercury each day
Coffee Creek then flows into Louisiana's Ouachita River where the pollutants have left the formerly pristine water speckled with odorous foam, slime and black pockets of water, said Jerry Johnson, who has been visiting the Ouachita River for 35 years.
"People used to swim in it," said Johnson, who now lives along the river. "In the summertime, it was the place to go."
But Johnson said the number of visitors has dwindled as the river conditions continued to grow worse, preventing the area from reaching its full economic potential as a vacation destination. The pollution is so bad it has kept Johnson from fishing in the river.
"If I did fish out of it, I don't know if I would eat it," Johnson said.
Barry Sulkin, a field office director for PEER, said Georgia-Pacific is blatantly breaking a provision of the Arkansas state permit that prohibits the discharge of "distinctly visible solids, scum or foam of a persistent nature."
Though the pollution problem with Coffee Creek started years ago, the issue was compounded by the state's refusal to correct water quality standards in 2010, said Sulkin, a former chief of environmental enforcement for the Tennessee Division of Water Pollution Control.
Environmental groups lobbied for stronger environmental standards but in September, the state issued the Georgia-Pacific mill a permit.
"It's obvious to me that the state is allowing this to continue for apparent economic reasons," Sulkin said.
Georgia-Pacific said in a statement that the water has been repeatedly analyzed by the EPA and the Arkansas and Louisiana regulatory agencies.
"We are in compliance with all water permits issued by these agencies, most recently, our updated water discharge permit, which was issued in 2010," Georgia-Pacific said in the statement.
"For decades, Georgia-Pacific has been a very active environmental steward in Ashley County and surrounding areas in Arkansas and Louisiana," the statement added. "Our employees live in this community and we are committed to operating a facility that is environmentally sound. We have a long-term interest in the Ouachita River's quality and habitat."
An EPA spokesperson for the South Central Regional Office said he could not comment on this specific complaint but said "we will review them and respond as appropriate."
Regardless of the outcome with the EPA, Cheryl Slavant, the designated Riverkeeper for the Ouachita River, said she knows the damage to the waterway can still be easily repaired.
"All the corporation has to do is spend some money-a lot of money-but they can clean this up," she said.
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