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This 3D "Surficial Geology Map" represents the 4 main geologic units in the Connecticut River Valley near Springfield, MA. The map was created by overlaying SHP files on a 3D surface. The 3D surface was created from open-source Lidar data downloaded from The National Map. Geologic units were downloaded from the MassGIS (https://www.mass.gov/info-details/massgis-data-usgs-124000-surficial-geology). The airports lay on deltas formed from glacial outwash flows into historical Glacial Lake Hitchcock. You can read Steve’s article on his map here: https://www.linkedin.com/pulse/whats-better-old-school-new-stephen-boynton/?trackingId=wWetnzsfR%2Fq6n0gMKb6eSw%3D%3D"View Larger Image
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NOAA's Pacific Marine Environmental Lab estimated the aragonite and calcite saturation state, excess alkalinity and carbonate dissolution in the water column. This plot displays the location of aragonite and calcite saturation state and allowed them to determine the amount of calcium carbonate added by particle dissolution in the Pacific Ocean, north of 40°S, to be 157 Pg C as calcium carbonate. This amounts to an average dissolution rate of ~0.31 Pg C per year, which is approximately 74% of the export production of calcium carbonate estimated for the Pacific Ocean. Image courtesy of Dana Greeley, Physical Scientist, NOAA's Pacific Marine Environmental Lab. Feely, R.A., C.L. Sabine, K. Lee, F.J. Millero, M.F. Lamb, D. Greeley, J.L. Bullister, R.M. Key, T.-H. Peng, A. Kozyr, T. Ono, and C.S. Wong, "In situ calcium carbonate dissolution in the Pacific Ocean", Global Biogeochemical Cycles, AGU, December 2002 (https://www.pmel.noaa.gov/public/pmel/publications-search/search_abstract.php?fmContributionNum=2438)View Larger Image
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An interesting "collapse structure" close to the Elysium Mons volcano complex on Mars. It may be possible that this feature is linked to both volcanic activity and/or melting of sub-surface ice to generate a "void" into which the surface rocks have collapsed but is difficult to prove conclusively. Ring faults are well defined and a localised ejecta margin. An explosive volcanic event followed by collapse is also a possibility given the proximity to the Elysium complex. Image courtesy of Lester AndersonView Larger Image
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Cross section plotted in Strater visualize the lithology of the layers and Gamma Ray logs. The map in the cross section view was mapped in Surfer. Image courtesy of http://www.strike-dip.comLearn More
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Thickness maps of two target formations mapped in Surfer. The cross section was plotted in Strater. Image courtesy of http://www.strike-dip.comLearn More
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Well section plotted in Strater shows detailed lithological description and the micropaleonthological data of the well. Image courtesy of http://www.strike-dip.comLearn More
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Surfaces mapped in Surfer visualized in Voxler with well paths to better visualize the data. Image courtesy of http://www.strike-dip.comLearn More
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Illustrative cross section of multiple layers plotted in Surfer. Image courtesy of http://www.strike-dip.comLearn More
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The primary data for this model originated from a 3D seismic interpretation along with data from five wells within the area. Surfer was used to interpolate the geological layers and calculate the depths of every layer. Strater cross sections display well logs, lithology, and surfaces of the laters between the wells. Voxler was used for the final visualization. Only the top and bottom surfaces are visible for improved visualization. Image courtesy of http://www.strike-dip.comLearn More
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LiDAR data for the Crater Lake area of Oregon with a full resolution of 3m for areas within the Cascades.View Larger Image
Image courtesy of Lester Anderson B.Sc. M.Sc. D.I.C, Structural geologist and cartographer
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