3 New Frontiers in Cave and Karst Science I
Thursday, 20 March 2025
8:00 AM - 10:00 AM
Alleghany B/C
HEXAGONAL MAPPING: A NEW AND VISUALLY APPEALING METHOD FOR REPRESENTING CAVE AND KARST FEATURES
Paper number: 3-5
Program: Theme Sessions
Time: 9:00 AM – 9:15 AM
Authors
Abstract
Numerous and different approaches to representing karst terrain, particularly cave density, have been adopted over the years with varying degrees of success. This work introduces a new approach, dividing up a region into a hexagonal grid and representing increasing cave and sinkhole density as increasing color intensity within each hexagon. The hexagonal grid is also oriented to the UTM grid to ease geolocation. A hexagon area of 250 meters (approximately 800 feet) from edge to edge is chosen as a compromise between map detail and cave entrance confidentiality. Cave density is approximated by aggregating total known cave passage length within a single hex. In a similar fashion, sinkhole density is approximated by percent of the hexagon mapped as sinkholes.
Hexagons are an improvement over traditional squares in that the hexagon’s edges are more equidistant from the central point of the polygon than a square’s, making the distance in each polygon more intuitively uniform. By using hexagons as discrete shapes to illustrate karst density, a region is pixelated sufficiently to keep cave entrance data confidential (protecting the subterranean resource) while providing acceptable resolution for end users to make informed decisions on the local and county scale. Finally, the use of hexagons in this fashion is applicable beyond karst to other resources including, but not limited to, flood zones, landslide potential, mine subsidence as well as biological variables such as species distribution.
Geological Society of America Abstracts with Programs. Vol. 57, No. 2
doi: 10.1130/abs/2025SE-407905
© Copyright 2025 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.