O konieczności wykonania drugiej edycji Szczegółowej Mapy Geologicznej Sudetów w skali 1 : 25 000 – przykłady rewizji budowy geologicznej z wykorzystaniem podkładu lidarowego numerycznego modelu powierzchni terenu
Abstract
About the need to develop the second edition of the detailed geological map of the Sudetes at the scale of
1 : 25,000 – examples of a revision of the geological pattern using the LIDAR Digital Elevation Models.
A b s t r a c t. The currently available map sheets issued under the edition of the Detailed Geological Map of the Sudetes at the scale of 1 : 25,000 (SMGS25), and especially those compiled in the 1950s and 1960s, does not meet the requirement of uniformity and accuracy of mapping, and they do not contain some key information that has been acquired as a result of multidisciplinary geological studies in the Sudetes over the last half-century. New research tools, such as LIDAR models of the land surface (DEM), allow for partial migration of data and (or) the implementation of recent research results, however, it should be verified by experienced geologists in the field. This is documented by two examples of their use to different areas in the Sudetes, which are composed primarily of sedimentary rocks.
1 : 25,000 – examples of a revision of the geological pattern using the LIDAR Digital Elevation Models.
A b s t r a c t. The currently available map sheets issued under the edition of the Detailed Geological Map of the Sudetes at the scale of 1 : 25,000 (SMGS25), and especially those compiled in the 1950s and 1960s, does not meet the requirement of uniformity and accuracy of mapping, and they do not contain some key information that has been acquired as a result of multidisciplinary geological studies in the Sudetes over the last half-century. New research tools, such as LIDAR models of the land surface (DEM), allow for partial migration of data and (or) the implementation of recent research results, however, it should be verified by experienced geologists in the field. This is documented by two examples of their use to different areas in the Sudetes, which are composed primarily of sedimentary rocks.