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Nonconnah Creek

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Line plot of discharge measurements at sites along <b>Nonconnah</b> <b>Creek</b> during 2...
Published: 01 August 2013
Figure 4. Line plot of discharge measurements at sites along Nonconnah Creek during 2004 and early 2005. The discharge at Mt. Moriah is the sum of that from Nonconnah and Johns creeks. Johns Creek is the only major tributary to enter Nonconnah Creek between Winchester Road and Getwell Road
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Line plots of selected water quality measurements in (A) <b>Nonconnah</b> <b>Creek</b> an...
Published: 01 August 2013
Figure 10. Line plots of selected water quality measurements in (A) Nonconnah Creek and (B) well 99s during May 2004 through February 2005.
Journal Article
Published: 01 August 2013
Environmental and Engineering Geoscience (2013) 19 (3): 265–287.
...Figure 4. Line plot of discharge measurements at sites along Nonconnah Creek during 2004 and early 2005. The discharge at Mt. Moriah is the sum of that from Nonconnah and Johns creeks. Johns Creek is the only major tributary to enter Nonconnah Creek between Winchester Road and Getwell Road...
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Water levels (in meters above sea level) measured in the NC cluster and fro...
Published: 01 August 2013
Figure 5. Water levels (in meters above sea level) measured in the NC cluster and from a survey point on the Getwell Road Bridge along Nonconnah Creek during 2004 and early 2005.
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Line plot of time-averaged values (2004 and early 2005) for selected oxidat...
Published: 01 August 2013
Figure 12. Line plot of time-averaged values (2004 and early 2005) for selected oxidation-reduction measurements and constituents with depth at the NC cluster. Plotted depth is the middle of the screened interval for the wells and the water surface for Nonconnah Creek.
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Trilinear major ion (Piper) diagram of water compositions in the Memphis aq...
Published: 01 August 2013
Figure 8. Trilinear major ion (Piper) diagram of water compositions in the Memphis aquifer (2002 data; Ivey et al., 2008 ) and time-averaged data from the shallow aquifer and Nonconnah Creek during 2004 and early 2005.
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Study area in Memphis, Tennessee. (A) Map of southwestern Tennessee showing...
Published: 01 August 2013
are windows through the upper Claiborne confining unit, as mapped by Parks (1990) . (B) Map of the Sheahan well field and nearby reach of Nonconnah Creek. Also shown are production wells in the Sheahan well field as well as shallow aquifer wells and discharge sites along Nonconnah Creek investigated
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Scale diagram of well installation and stilling well at the NC cluster alon...
Published: 01 August 2013
Figure 3. Scale diagram of well installation and stilling well at the NC cluster along Nonconnah Creek. (A) Well NC-3; (B) well NC-2; (C) well NC-1; (D) stilling well box; (E) well head and cover; (F) 10-cm–thick concrete pad; (G) concrete-filled post-holes; (H) aluminum well casing; (I) 5-cm
Journal Article
Published: 01 September 2005
Seismological Research Letters (2005) 76 (5): 598–614.
... deposit that has erosional upper and lower contacts. The Upland Complex is overlain by up to three Pleistocene loess deposits and locally by Late Pleistocene and Holocene alluvium of the Wolf River and Nonconnah Creek in southern Shelby County ( Figure 3 ). Geological and geophysical evidence...
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Journal Article
Published: 01 May 2012
Environmental and Engineering Geoscience (2012) 18 (2): 113–158.
... by the Loosahatchie and Wolf rivers and Nonconnah Creek, all of which flow westerly into the Mississippi River. At Memphis the Mississippi River is bounded on the east by the Chickasaw Bluffs and on the west by a 9.1-m– (30-ft)–high U.S. Army Corps of Engineers (USACE) retention levee. This falls under...
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Journal Article
Published: 01 May 2002
Seismological Research Letters (2002) 73 (3): 380–392.
...-velocity layer may not be present at the surface-wave test site because it has been removed by Nonconnah Creek erosion (Van Arsdale, personal communication). At Mud Island B and Shelby Farms, we also performed passive surface-wave tests to complement the active data. Typical passive sources...
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Journal Article
Published: 01 May 2008
Seismological Research Letters (2008) 79 (3): 416–423.
... liquefaction probability curves for LPI exceeding 5 and 15 for four surface soil types in Memphis: Holocene alluvial flood plain deposits of the Wolf River (Qal), Holocene alluvial flood plain deposits of Nonconnah Creek and tributaries to the Wolf River (Qa), Late Pleistocene loess deposits (Ql...
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Journal Article
Published: 01 February 2003
Earthquake Spectra (2003) 19 (1): 159–189.
... located on large areas of Pleistocene loess deposits and on smaller areas of Pleistocene and Holocene alluvial deposits (Saucier 1974). The alluvium was deposited in the floodplains of the Mississippi, Loosahatchie, and Wolf Rivers, as well as Nonconnah Creek, all of which have dissected the loess...
Journal Article
Published: 03 January 2018
Seismological Research Letters (2018) 89 (2A): 688–701.
... streams (both natural and artificial), some of which are located in downtown Memphis. Liquefaction hazard is low in the loess‐covered uplands, where much of Memphis is built, and in Nonconnah Creek. 2%‐in‐50‐yr probability of exceedance hazard maps (that include all known seismic sources...
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Journal Article
Journal: GSA Bulletin
Published: 01 July 2017
GSA Bulletin (2017) 129 (7-8): 970–996.
... most of central Shelby County ( Figs. 5 , 7 , and 8 ) and contains the major county streams. Nonconnah Creek flows along the southern boundary of the graben, the Wolf River flows near its center, and the Loosahatchie River is within the northern portion of the graben. It is the least well defined...
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