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Related Concept Videos

Global Climate Change01:50

Global Climate Change

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.
The Carbon Cycle01:14

The Carbon Cycle

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.
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
Temperature Dependence on Reaction Rate02:55

Temperature Dependence on Reaction Rate

The Collision Theory
Atoms, molecules, or ions must collide before they can react with each other. Atoms must be close together to form chemical bonds. This premise is the basis for a theory that explains many observations regarding chemical kinetics, including factors affecting reaction rates.
The collision theory is based on the postulates that (i) the reaction rate is proportional to the rate of reactant collisions, (ii) the reacting species collide in an orientation allowing contact between...
Threats to Biodiversity01:50

Threats to Biodiversity

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...

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Related Experiment Video

Updated: Jul 11, 2026

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
07:58

Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

Published on: August 7, 2017

Can rapid climatic change cause volcanic eruptions?

M R Rampino, S Self, R W Fairbridge

    Science (New York, N.Y.)
    |November 16, 1979
    PubMed
    Summary

    Major volcanic eruptions may be triggered by climate change. Climate variations can alter Earth's crust, potentially increasing volcanic and seismic activity over longer timescales.

    Area of Science:

    • Earth Science
    • Climate Science
    • Volcanology

    Background:

    • Major volcanic eruptions often follow decadal or longer cooling trends.
    • Volcanic dust veils cause short-term global cooling but are unlikely to initiate glaciations or longer climate shifts.
    • Climate variations can induce crustal stress changes.

    Purpose of the Study:

    • To investigate the relationship between climate change and volcanic activity.
    • To explore the mechanisms by which climate variations might influence Earth's crust and augment volcanic potential.

    Main Methods:

    • Analysis of historical climate data and volcanic eruption records.
    • Modeling of crustal stress changes due to climate-driven ice and water mass variations.
    • Examination of Earth's axial and spin-rate changes in relation to geological events.

    More Related Videos

    Rapid PCR Thermocycling using Microscale Thermal Convection
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    Rapid PCR Thermocycling using Microscale Thermal Convection

    Published on: March 5, 2011

    Atom Probe Tomography Analysis of Exsolved Mineral Phases
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

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    Last Updated: Jul 11, 2026

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt
    07:58

    Data Processing Methods for 3D Seismic Imaging of Subsurface Volcanoes: Applications to the Tarim Flood Basalt

    Published on: August 7, 2017

    Rapid PCR Thermocycling using Microscale Thermal Convection
    09:02

    Rapid PCR Thermocycling using Microscale Thermal Convection

    Published on: March 5, 2011

    Atom Probe Tomography Analysis of Exsolved Mineral Phases
    08:14

    Atom Probe Tomography Analysis of Exsolved Mineral Phases

    Published on: October 25, 2019

    Main Results:

    • Climate-induced crustal stress changes, such as ice/water loading/unloading, may influence volcanic and seismic potential.
    • Long-term climate cooling trends precede major volcanic eruptions.
    • Dust veils have a limited impact on long-term climate stability.

    Conclusions:

    • Climate variations, rather than volcanic dust, may play a significant role in triggering major volcanic eruptions.
    • Earth's climate system and geological activity are interconnected.
    • Further research is needed to fully understand the feedback mechanisms between climate and volcanism.