“We are both small agile companies and do things a little differently than large companies” said Smith. When Ross approached Teknologic with an offer to sell there was no hesitation Smith said. Ross and Teknologic both concentrate on underwater acoustics and have worked together over the years. employees Duane Moloney Steve Reynolds and Dean Graddon will also continue with the company. Jim Ross former owner and president of Ross Laboratories is staying with the company in an advisory capacity with the title of manager of sales and technical support. Smith and Bill Beatty senior program manager will be the primary contacts for Ross Labs LLC. Brent Smith is CEO and Terry Stodeller is CFO of Teknologic. The new Ross Labs LLC joins Teknologic LLC as an entity of the corporation.
of Edmonds Washington completed the asset purchase of Ross Laboratories Inc. Shore parallel lines were spaced at ~ 300 m, and shore perpendicular tie lines were spaced at ~ 2 km to provide adequate cross-shelf control within the seismic reflection data set.Teknologic Engineering Services Inc.
#HYPACK SWEEP SOFTWARE#
Boomer data were acquired using TEI Delph Seismic acquisition software and recorded in SEG-Y standard format. CHIRP data were extracted and converted to single-channel SEG-Y standard format (Barry and others, 1975) using a USGS C program (QMIPSTOSEGY). CHIRP data acquired with the SIS-1000 system were logged in the QMIPS format using Triton Elics International (TEI) ISIS acquisition software. During the MGNM00014 cruise, CHIRP data were acquired at a 0.27-s fire interval, a 263-ms sweep length, and a 0.274-ms sampling interval, and boomer data were acquired at a 0.5-s sampling rate, a 250-ms sweep, and a 0.2-ms sampling interval. During the ATSV99044 cruise, CHIRP data were acquired at a 0.27-s fire interval, a 274-ms sweep length, and a 0.263-ms sampling interval, and boomer data were acquired at a 0.5-s sampling rate, a 180-ms sweep length, and a 0.083-ms sampling interval.
Boomer and CHIRP seismic data were acquired digitally during both offshore cruises.
#HYPACK SWEEP SERIES#
Submetrix 2000 Series interferometric sonar system (234 kHz). Analysis of these data will be incorporated into this mapping in a subsequent report.Īcquisition systems for the 19 offshore cruises (ATSV99044 and MGNM00014) included a Datasonics SIS-1000 sidescan-sonar (100-120 kHz swept FM) and CHIRP sub-bottom profiler (2-7 kHz swept FM), a Huntec 300-3000 Hz boomer, and an SEA Ltd. Data from a fifth offshore cruise, conducted in June 2002 aboard the R/V Atlantic Surveyor ( USGS cruise ATSV02014), extend southward between North Inlet and the mouth of Winyah Bay. High-resolution sidescan-sonar, seismic reflection and interferometric sonar bathymetry were acquired during four USGS cruises: October-November 1999 aboard the R/V Atlantic Surveyor ( USGS cruise ATSV99044, Hill and others, 2000a Hill and others, 2000b Roberts and others, 2002), March 2000 aboard the R/V Megan Miller ( USGS cruise MGNM00014, Dadisman et al, 2001a Dadisman and others, 2001b Denny and Schwab, In Prep.), and May 20 aboard the R/V Coastal II ( USGS cruises COAS01008 and COAS02011). The study area covers nearly 700 km 2 of the lower shoreface and inner-continental shelf of Long Bay, from just seaward of the breaking waves (> 1 km) to ~ 10 km offshore ( Figure 2). Geophysical Data - Acquisition - Maps Showing the Stratigraphic Framework of South Carolina's Long Bay from Little River to Winyah BayĬoastal & Marine Geology Program > South Carolina Coastal Erosion Study > Open File Report 2004-1013 Maps Showing the Stratigraphic Framework of South Carolina's Long Bay from Little River to Winyah Bay USGS Open File Report 2004-1013 by: Wayne E.
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