THE GEOHERITAGE AND GEO-CULTURAL IMPORTANCE OF MONGOLIA’S NORTHEAST GOBI ALTAI REGION
The region under consideration encompasses the southern slopes of the Hangay Dome, the easternmost Valley of Lakes and the basins and ranges of the northeastern Gobi Altai. The area is arid to semi-arid throughout with excellent rock exposures of a wide variety of igneous, metamorphic and sedimentary strata. The geology and landscape record a complex Precambrian-Quaternary geological evolution. The region is also tectonically active as expressed by Holocene fault scarps, co-seismic landslides, youthful mountain ranges flanked by aggrading alluvial fan systems, and internally drained fault-bound basins.
Within a rectangular area of approximately 30,000 km2, there is a remarkable concentration and variety of world-class geological and geomorphological features in the NE Gobi Altai region that are related to: 1) active tectonics, 2) Neogene volcanism, 3) arid-land sedimentary systems, 4) dinosaur and mammal paleontology, 5) mass wasting, and 6) bedrock geology. In this presentation, I describe and show individual features in each of these categories. In addition, throughout the region, there are important geological influences on the distribution of human settlements and endangered wildlife that merit description and recognition. Mining, hydrocarbon exploration and increasing numbers of international tourists pose a growing threat to the region’s unique geoheritage, spectacular natural scenery, biodiversity and traditional nomadic culture.