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Contig maps were verified by comparing restriction digest patterns from laboratory produced gels to those generated in silico from the consensus sequences.
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Excellent prediction capability of the maps was verified at temperatures of 573 673 K.
Presumably, all credible maps are verified against a more reliable source to estimate overall error, but the spatial distribution of errors may not be the same for different maps.
The areas identified based on integrated mapping of various features with intensive geological and geomorphological mapping were verified by field observation of groundwater level data which proved to be comparable.
As noted in the methods section, the study findings (narrative and stakeholder mapping) were verified with more than half of respondents.
Accuracy of the infestation map was verified by ground sampling.
The delineated map was verified using the GIS Digital Elevation Model (DEM).
The resulting synthesis map was verified using three different data layers.
The level of accuracy of the landslide susceptibility map was verified by overlaying with the landslide data for validation.
Then, landslide-susceptibility map was drawn using the frequency ration and finally, the map was verified by comparing with existing landslide locations.
The seismic landslide zone map was verified by comparison with the findings of a geological engineering survey conducted in the study area.
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CEO of Professional Science Editing for Scientists @ prosciediting.com