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. 2018 Nov 5;18(11):3777. doi: 10.3390/s18113777

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© 2018 by the authors.

Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (http://creativecommons.org/licenses/by/4.0/).

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Landslide susceptibility mapping prepared by the ADTree model and its ensemble: (a) ADTree, sample size 60/40 & Resolution: 10 m; (b) RS-ADT, sample size 60/40 & Resolution: 10 m; (c) ADTree, sample size 70/30 & Resolution: 10 m; (d) RS-ADTree, sample size 70/30 & Resolution: 10 m; (e) ADTree, sample size 80/20 & Resolution: 20 m; (f) MB-ADTree, sample size 80/20 & Resolution: 20 m; (g) ADTree, sample size 90/10 & Resolution: 20 m; (h) MB-ADTree, sample size 90/10 & Resolution: 20 m.

Landslide susceptibility mapping prepared by the ADTree model and its ensemble: (a) ADTree, sample size 60/40 & Resolution: 10 m; (b) RS-ADT, sample size 60/40 & Resolution: 10 m; (c) ADTree, sample size 70/30 & Resolution: 10 m; (d) RS-ADTree, sample size 70/30 & Resolution: 10 m; (e) ADTree, sample size 80/20 & Resolution: 20 m; (f) MB-ADTree, sample size 80/20 & Resolution: 20 m; (g) ADTree, sample size 90/10 & Resolution: 20 m; (h) MB-ADTree, sample size 90/10 & Resolution: 20 m.