Triangles: 1.7M
Vertices: 866.9k
More model informationSouthern termination of the Pakuashan anticline, in the Western Foothills of Taiwan. This anticline is an active fault-bend fold, i.e. it is caused by reverse slip along a blind fault located below it at several km depth. The Chelungpu fault, which has a surface trace and produced the 1999 ChiChi Earthquake, is just east of it.
Vertical exaggeration 1.5x
- Generator: DEM Net Elevation API
- Digital Elevation Model: Laurence Hawker, Jeffrey Neal (2021): FABDEM
- Imagery: MapTiler Cloud Satellite
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Sep 17th 2023
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