2013
DOI: 10.1016/j.jglr.2013.01.003
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Using LiDAR to reconstruct the history of a coastal environment influenced by legacy mining

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Cited by 12 publications
(30 citation statements)
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“…No local water-clarity information is available in the study area during the time of data acquisition, but in general, Lake Superior is an optically complex, oligotrophic case 2 water body [54]. Dominant coastal substrates in the region include high-reflectance white quartz sand derived from Jacobsville sandstone, lower-reflectance gray stamp sands, a product of the region's historic copper mining, and localized cobble fields [55][56][57].…”
Section: Mabel Datamentioning
confidence: 99%
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“…No local water-clarity information is available in the study area during the time of data acquisition, but in general, Lake Superior is an optically complex, oligotrophic case 2 water body [54]. Dominant coastal substrates in the region include high-reflectance white quartz sand derived from Jacobsville sandstone, lower-reflectance gray stamp sands, a product of the region's historic copper mining, and localized cobble fields [55][56][57].…”
Section: Mabel Datamentioning
confidence: 99%
“…A change in actual bathymetry over the intervening two years is also a likely factor, as the project area is characterized by dynamic bedform features, including nearshore sand bars and troughs and offshore shoals likely influenced by migrating sand [72]. The sedimentary regime of Keweenaw Bay has not been fully described, but a key regional sedimentary process occurring along the northern reaches of the Bay is the southwestward long-shore movement and deposition of stamp sands, which eventually migrate laterally to coalesce with deeper, larger bars [55,56]. Keweenaw Bay's exposure to an approximately 230-km northeasterly fetch could also play a significant role in the sediment dynamics of the project area [57].…”
Section: Bathymetry Accuracy Assessmentmentioning
confidence: 99%
“…The advantage of multiple-year overflights is that the mosaicked images will allow for estimates of underwater stamp sand bar volume, mass and movement (via difference calculations between different dates; see [31] for a preliminary example). For a check on the accuracy of bathymetric measurements, the LiDAR-derived depths are cross-compared with each other and with georegistered NWRI (National Water Resources Institute) SONAR-derived depths and sediment classification maps [32].…”
Section: Charts Overflights and Mass Calculationsmentioning
confidence: 99%
“…Using CHARTS LiDAR data along with eight aerial photos from 1938 to 2010, we reconstructed the 1938 Gay stamp sand pile volume and, with some reasonable assumptions, calculated the shoreline erosion rate of the pile between 1938 and 2010 ( Figure 7; [3,31]). To measure the erosion of the tailing pile and the mass of sands washed into Lake Superior, three estimates were needed: (1) the area and volume of the pile above water level (available from the 2008 LiDAR); (2) the below-water volume, i.e., calculating the true depth of the stamp sand pile above lake bottom bedrock; and (3) the area of the pile lost through time (erosion at the shoreline face, estimated from aerial photos, essentially treated as vertical slices across the pile.…”
Section: Charts Overflights and Mass Calculationsmentioning
confidence: 99%
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