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Mapping Surficial Geology in Three Dimensions

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TGI: Targeted Geoscience Initiative - South-central Cape Breton Island

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Click on dots to visit type sections of surficial deposits

Study 1 Big Brook Quarry Sugar Camp Quarry River Inhabitants Section Mapping Mapping Yard Site Northwest Ice Flow

Why map surficial geology in Cape Breton?

  • Evaluate the resource potential of south-central Cape Breton, especially such industrial minerals as clay, silica sand and aggregates.
  • Provide 3-D geological maps and databases for this developing region.

Surficial deposits are defined as the mantle of loose sediment derived from underlying solid rock by wind, water or glacial erosion and chemical weathering.


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Surficial sediments are vital to human existence. Without loose sediment, we would have to eke out an existence on solid rock, much like lichens. Geological mapping of the mantle of weathered rock on the Earth's surface is the fundamental activity of this part of the TGI project. Geological maps and comprehensive data on the Earth's resources are a vital part of the sustainable development of the region. Water resources, agriculture, forestry, construction design and materials, coastal erosion, contamination of land and water, and ecosystem change are all issues that rely on surficial earth science data. Geological maps can help unlock the mineral potential of this region. The TGI project will provide this region with high quality surficial geological maps, reports and databases that will be an invaluable resource.


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Field Mapping

How do we map surficial deposits?

  • Rock Surface mapping and air photograph interpretation
  • Rock Compilation of previous stratigraphic data, including water well logs, diamond-drill holes and geotechnical drilling, and integration of these data into a Geographic Information System.
  • Rock High resolution seismic surveys.
  • Rock New diamond-drilling and wire-line coring in areas of thick unconsolidated deposits. Results of a previous survey in central Nova Scotia will be used as a model for the work in Cape Breton.

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Results
Browse some of the initial results of the survey.

  • Rock Test seismic surveys done in the summer of 2000.
  • Rock Ceramic and structural clay deposits.

Quaternary type stratigraphic sections and new radiocarbon-dated localities (see location map above)

  • Rock Big Brook Section (RS-28/00)
  • Rock Sugar Camp Section (RS-75/00)
  • Rock River Inhabitants Section (RS-30/00)
  • Rock Judique South Section (RS-117/00)
  • Rock Creignish Hills striation site (RS-109/00)

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Go to the virtual field trip of Nova Scotia landscapes to learn about the surficial geology of the rest of Nova Scotia.