Related Experiment Video
Updated: Sep 9, 2025

07:58
Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
Published on: August 7, 2017
9.5K
Volcanoes stunt nearby glaciers
Tryggvi Unnsteinsson1, Matteo Spagnolo2, Brice R Rea3
1School of Geosciences, University of Aberdeen, Aberdeen, Scotland, UK. t.unnsteinsson.23@abdn.ac.uk.
Nature Communications
|August 29, 2025
Summary
Volcanic activity negatively impacts nearby glacier mass balance, confining glaciers to higher elevations. This effect is most pronounced within 5 km of volcanoes, crucial for hazard monitoring.
Area of Science:
- Glaciology
- Volcanology
- Earth Science
Background:
- Glacierised volcanoes present significant societal hazards.
- Monitoring volcanic activity is challenging due to glacier cover and remoteness.
- Traditional geophysical and geochemical methods are often hindered in these environments.
Purpose of the Study:
- To assess the global impact of 307 active volcanoes on glacier mass balance within a 40 km radius.
- To quantify the influence of volcanic activity on glacier elevation and mass balance.
- To establish a baseline for future monitoring of volcanic-glacial interactions.
Main Methods:
- Analysis of relative median elevations for 40,667 glaciers worldwide.
- Comparison of glacier elevations near active volcanoes versus those further away.
- Assessment of volcanic influence within a 40 km radius, with a focus on the 5 km footprint.
Main Results:
- Glaciers near volcanoes are progressively confined to higher elevations.
- Volcanic processes demonstrate a negative impact on nearby glacier mass balance.
- The primary influence of volcanic activity on glacier mass balance is within a 5 km radius.
Conclusions:
- Volcanic activity significantly affects glacier mass balance globally.
- The findings provide a critical baseline for monitoring volcanic impacts on glaciers.
- Understanding these interactions is essential for hazard assessment and mitigation strategies.
Related Concept Videos
Global Climate Change
24.7K
Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
24.7K
The Carbon Cycle
39.7K
Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
39.7K
Threats to Biodiversity
22.9K
There have been five major extinction events throughout geological history, resulting in the elimination of biodiversity, followed by a rebound of species that adapted to the new conditions. In the current geological epoch, the Holocene, there is a sixth extinction event in progress. This mass extinction has been attributed to human activities and is thus provisionally called the Anthropocene. In 2019 the human population reached 7.7 billion people and is projected to comprise 10 billion by...
22.9K
Viruses of Archaea
75
Archaeal viruses play a crucial role in the ecosystems of extremophilic archaea, particularly those belonging to the phyla Euryarchaeota and Crenarchaeota. By shaping host evolution and facilitating gene transfer, these viruses influence microbial communities and contribute to genetic diversity in extreme environments. The archaea they infect thrive in acidic hot springs and hydrothermal vents characterized by high temperatures and low pH. Archaeal viruses exhibit remarkable structural...
75
Impact
196
Impact occurs when two bodies collide, leading to the application of impulsive forces between them. Analyzing impact mechanics involves considering two colliding particles moving along a line known as the line of impact, which passes through their centers and is perpendicular to the contact plane.
When particles with different initial velocities collide, they induce deformation by applying equal and opposite impulses. At the point of maximum deformation, the particles move together with...
When particles with different initial velocities collide, they induce deformation by applying equal and opposite impulses. At the point of maximum deformation, the particles move together with...
196
Impact: Problem Solving
258
In an experiment conducted during a Mars mission, a rover propels a projectile with an initial velocity, and the projectile rebounds after colliding with the Martian surface. To ascertain the maximum height attained by the projectile after this collision, the known restitution coefficient and acceleration due to gravity are employed.
By designating the launch point as the origin and utilizing kinematic equations, the vertical component of the projectile's velocity at the point of impact is...
By designating the launch point as the origin and utilizing kinematic equations, the vertical component of the projectile's velocity at the point of impact is...
258

