China/Central East Asia Volcanic Province

Honggeertu

Volcanic field · 1,605m · China

Elevation
1,605m
Eruptions
0
Max VEI
Last Eruption
Unknown
All Volcanoes
Overview

About Honggeertu

Honggeertu is a volcanic field rising to 1,605 meters (5,266 feet) in China'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

Honggeertu is located in China, within the Central East Asia Volcanic Province of the broader Eastern Asia Volcanic Regions. Situated at 41.59° N, 113.11° E in the Northern Hemisphere, the volcano lies within a temperate climate zone. With a summit elevation of 1,605 meters above sea level, Honggeertu is a moderately sized peak that remains accessible to hikers and researchers for much of the year. The volcanic landform is characterized as a cluster, which describes the physical shape and structure of the volcanic edifice as observed from the surface.

Geological Context

Honggeertu 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 Honggeertu tend to produce effusive eruptions with lava flows that can be relatively predictable, giving nearby communities in China more time to prepare. However, they can also produce explosive phases, particularly when magma interacts with groundwater. The dominant rock type is basalt / picro-basalt, a dark, fine-grained volcanic rock that forms from rapidly cooling, low-viscosity lava. Basaltic eruptions tend to be less explosive and produce fluid lava flows that can travel long distances. While less immediately dangerous than explosive eruptions, basaltic lava flows can destroy structures and infrastructure in their path, and volcanic gases released during these eruptions can affect air quality over a wide area.

GVP Reference Summary

The Honggeertu volcanic field is located in Nei Mongol Province, NW of Beijing. The basaltic volcanic field consists of a group of six cinder cones extending along an arc for about 10 km that were considered to be of Holocene age by IAVCEI (1973). Liu (1998, p.c.), however, considered the existence of Holocene volcanism at this location to be uncertain.

— Smithsonian Institution, Global Volcanism Program
Type
Volcanic field
Tectonic Setting
Intraplate / Continental crust (> 25 km)
Dominant Rock
Basalt / Picro-Basalt
Coordinates
41.590°, 113.111°
Activity Evidence
Evidence Uncertain
Geologic Epoch
Holocene

Eruption History

0 Recorded Eruptions

No eruption records available for Honggeertu.


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Common Questions

Frequently Asked Questions About Honggeertu

Is Honggeertu an active volcano?+

Honggeertu 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 Honggeertu?+

Honggeertu has a summit elevation of 1,605 meters (5,266 feet) above sea level. At 1,605 meters, it is a moderately sized volcanic peak, roughly comparable to Mount Vesuvius (1,281m).

What type of volcano is Honggeertu?+

Honggeertu is classified as a Volcanic field. Volcanic fields consist of clusters of small volcanic vents and cinder cones spread across a region. Rather than a single central vent, eruptions can occur at many points across the field.

Where is Honggeertu located?+

Honggeertu is located in China, in the Eastern Asia Volcanic Regions. More specifically, it lies within the Central East Asia Volcanic Province. Its exact coordinates are 41.590° latitude, 113.111° longitude.

Is it safe to visit Honggeertu?+

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