Mongolia/Baikal Rift Volcanic Province

Khoid Naiman Nuur

Pyroclastic cone · 2,532m · Mongolia

Elevation
2,532m
Eruptions
0
Max VEI
Last Eruption
Unknown
All Volcanoes
Overview

About Khoid Naiman Nuur

Khoid Naiman Nuur is a pyroclastic cone rising to 2,532 meters (8,307 feet) in Mongolia's Eastern Asia Volcanic Regions. No historical eruptions have been recorded, though the volcano is classified based on geological evidence of past activity.

Geography & Climate

Khoid Naiman Nuur is located in Mongolia, within the Baikal Rift Volcanic Province of the broader Eastern Asia Volcanic Regions. Situated at 46.65° N, 101.80° E in the Northern Hemisphere, the volcano lies within a temperate climate zone. At 2,532 meters above sea level, Khoid Naiman Nuur rises above the surrounding terrain into montane or subalpine conditions. The elevation creates distinct ecological zones along its flanks, from forested lower slopes to exposed rocky terrain near the summit. The volcanic landform is characterized as a minor (basaltic), which describes the physical shape and structure of the volcanic edifice as observed from the surface.

Geological Context

Khoid Naiman Nuur is an intraplate volcano, meaning it formed away from any plate boundary. These volcanoes are often powered by hotspots — plumes of abnormally hot mantle material rising from deep within the Earth. Hotspot volcanoes like Khoid Naiman Nuur tend to produce effusive eruptions with lava flows that can be relatively predictable, giving nearby communities in Mongolia more time to prepare. However, they can also produce explosive phases, particularly when magma interacts with groundwater.

GVP Reference Summary

A cone, designated here as Khoid Naiman Nuur ("North Eight Lakes"), is located in the upper reaches of a river valley ~25 km SW from the Orkhan (or Tsutgalan) waterfall, just N of the Khuisiin Naiman Nuur ("Eight Lakes of the Navel") area. Lava flows extend from the cone ~3.5 km S towards the lakes and ~15 km NW then NE down the valley towards the waterfall. Ivanov et al. (2015) noted that the cone and flows were probably Holocene based on their field observations.

— Smithsonian Institution, Global Volcanism Program
Type
Pyroclastic cone
Tectonic Setting
Intraplate / Continental crust (> 25 km)
Dominant Rock
Coordinates
46.646°, 101.798°
Activity Evidence
Evidence Uncertain
Geologic Epoch
Holocene

Eruption History

0 Recorded Eruptions

No eruption records available for Khoid Naiman Nuur.


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Common Questions

Frequently Asked Questions About Khoid Naiman Nuur

Is Khoid Naiman Nuur an active volcano?+

Khoid Naiman Nuur is not currently classified as active. Its activity evidence is listed as "Evidence Uncertain." No recorded eruptions have been documented. However, no volcano is ever considered permanently extinct.

How high is Khoid Naiman Nuur?+

Khoid Naiman Nuur has a summit elevation of 2,532 meters (8,307 feet) above sea level. At 2,532 meters, it is comparable in height to many significant mountain peaks and stands well above the tree line.

What type of volcano is Khoid Naiman Nuur?+

Khoid Naiman Nuur is classified as a Pyroclastic cone. Pyroclastic cone volcanoes have distinct geological characteristics that set them apart from other volcanic types.

Where is Khoid Naiman Nuur located?+

Khoid Naiman Nuur is located in Mongolia, in the Eastern Asia Volcanic Regions. More specifically, it lies within the Baikal Rift Volcanic Province. Its exact coordinates are 46.646° latitude, 101.798° longitude.

Is it safe to visit Khoid Naiman Nuur?+

Khoid Naiman Nuur can generally be visited, but as with any volcano, visitors should check local conditions and any advisory notices before traveling. Mongolia may have specific regulations for accessing volcanic areas. Guided tours are often the safest and most informative way to experience a volcano.