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Lava flow volume estimates are currently based on field mapping, photogrammetry and InSAR analysis (Peltier et al. 2016).
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Evaluation was based on field assessment during mapping of a well-exposed coastal section of deformed Carboniferous and Permian rocks at N. Tynemouth in NE England.
Based on field investigations, topographic maps, and digital elevation model, the local geomorphological aspects will be discussed from south to north in the following: Open image in new window Fig. 2 The main landforms in the northwestern coast (includes the four studied basins) Open image in new window Fig. 3 Digital elevation model of the studied basins, created from topographic maps 1 25,000.
First, a regional geomorphological map based on field surveys, remote sensing and previous environmental studies was developed.
This registerial map is thus based on field and tenor rather than on field and mode.
The maps should be based on field studies, supplemented by desk studies and remote sensing data interpretation.
By definition they captured all of the map-based CPs as these were also calculated based on field edge distance, only using smaller distances of separation.
Semi-detailed maps like SSURGO, are based on field measurements, aerial photography and visual inspection of landscape features.
Figure 24 Registerial map of medical discourse based on field of activity and mode (turn and medium).
A Kenya-wide 1973 survey of tsetse distribution by species based on field reports and other sampling [2] is considered among the best maps of fly distribution (hereafter, "1973 data"), but that map is now over 30 years old.
Based on field reporting by Javier Marroquin and Amita Kulkarni.
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