Jove
Visualize
Contact Us
JoVE
x logofacebook logolinkedin logoyoutube logo
ABOUT JoVE
OverviewLeadershipBlogJoVE Help Center
AUTHORS
Publishing ProcessEditorial BoardScope & PoliciesPeer ReviewFAQSubmit
LIBRARIANS
TestimonialsSubscriptionsAccessResourcesLibrary Advisory BoardFAQ
RESEARCH
JoVE JournalMethods CollectionsJoVE Encyclopedia of ExperimentsArchive
EDUCATION
JoVE CoreJoVE BusinessJoVE Science EducationJoVE Lab ManualFaculty Resource CenterFaculty Site
Terms & Conditions of Use
Privacy Policy
Policies

Related Concept Videos

Threats to Biodiversity01:50

Threats to Biodiversity

22.6K
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...
22.6K
Plotting of Topographic Maps01:29

Plotting of Topographic Maps

83
Topographic maps represent the Earth's surface features using contour lines, which connect points of equal elevation to create a two-dimensional representation of three-dimensional terrain. Creating a topographic map requires a systematic approach.Begin by plotting a scaled grid and marking intersections corresponding to the survey's elevation data points. Assign elevation values at these intersections to build the base map. Next, determine contour levels using a consistent contour interval,...
83
The Fossil Record02:56

The Fossil Record

25.4K
The fossil record documents only a small fraction of all organisms that have ever inhabited Earth. Fossilization is a rare process, and most organisms never become fossils. Moreover, the fossil record only exhibits fossils that have been discovered. Nevertheless, sedimentary rock fossils of long-lived, abundant, hard-bodied organisms dominate the fossil record. These fossils offer valuable information, such as an organism's physical form, behavior, and age. Studying the fossil record helps...
25.4K
The Carbon Cycle01:14

The Carbon Cycle

39.3K
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.
39.3K
Methods of Obtaining Topography01:25

Methods of Obtaining Topography

104
Topography involves measuring and mapping land elevations, natural features, and artificial structures to create accurate representations of the terrain. Topographic surveying relies on traditional and modern methods, each with distinct advantages and limitations.Traditional Surveying Methods:Transit stadia surveys and plane table surveys were widely used traditional surveying methods. These techniques relied on instruments like theodolites and stadia rods for measuring distances and angles,...
104
Viruses of Archaea01:29

Viruses of Archaea

58
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...
58

You might also read

Related Articles

Articles linked to this work by shared authors, journal, and citation graph.

Sort by
Same author

Coordinating science during an eruption: lessons from the 2020-2021 Kīlauea volcanic eruption.

Bulletin of volcanology·2023
Same author

Time scales and temperatures of crystal storage in magma reservoirs: implications for magma reservoir dynamics.

Philosophical transactions. Series A, Mathematical, physical, and engineering sciences·2019
Same author

Response to Comment on "Rapid cooling and cold storage in a silicic magma reservoir recorded in individual crystals".

Science (New York, N.Y.)·2017
Same author

Rapid cooling and cold storage in a silicic magma reservoir recorded in individual crystals.

Science (New York, N.Y.)·2017
Same author

Rapid remobilization of magmatic crystals kept in cold storage.

Nature·2014
Same author

Drilling to gabbro in intact ocean crust.

Science (New York, N.Y.)·2006
Same journal

Erratum for the Research Article "Detecting supramolecular organic nanoparticles during heat wave".

Science (New York, N.Y.)·2026
Same journal

Local signals, systemic decline.

Science (New York, N.Y.)·2026
Same journal

The mechanics of liver regeneration.

Science (New York, N.Y.)·2026
Same journal

Computing in a memory with physics.

Science (New York, N.Y.)·2026
Same journal

Retraction.

Science (New York, N.Y.)·2026
Same journal

Making time.

Science (New York, N.Y.)·2026
See all related articles

Related Experiment Video

Updated: Aug 19, 2025

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

9.4K

What lies beneath Yellowstone?

Kari M Cooper1

  • 1Department of Earth and Planetary Sciences, University of California Davis, Davis, CA, USA.

Science (New York, N.Y.)
|December 1, 2022
PubMed
Summary
This summary is machine-generated.

Volcanic magma reservoirs are larger than previously thought. However, this increased magma volume may not lead to more volcanic eruptions.

More Related Videos

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

8.3K
Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations
10:30

Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations

Published on: September 11, 2016

10.8K

Related Experiment Videos

Last Updated: Aug 19, 2025

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

9.4K
Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling
06:55

Kinematic History of a Salient-recess Junction Explored through a Combined Approach of Field Data and Analog Sandbox Modeling

Published on: August 5, 2016

8.3K
Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations
10:30

Soil Lysimeter Excavation for Coupled Hydrological, Geochemical, and Microbiological Investigations

Published on: September 11, 2016

10.8K

Area of Science:

  • Geology
  • Volcanology
  • Earth Science

Background:

  • Magma accumulation beneath volcanoes is a key factor in eruption forecasting.
  • Previous estimates of magma volume may have underestimated the total amount present.

Purpose of the Study:

  • To reassess the volume of magma present in volcanic systems.
  • To determine the eruptibility of the newly recognized magma volumes.

Main Methods:

  • Geophysical surveys to detect subsurface magma.
  • Petrological analysis of volcanic rocks to understand magma properties.

Main Results:

  • Substantial volumes of magma, exceeding prior estimations, have been identified.
  • The identified magma exhibits characteristics that may inhibit its ascent and eruption.

Conclusions:

  • Volcanic systems may host larger magma reservoirs than currently recognized.
  • Increased magma volume does not automatically equate to a higher probability of eruption due to factors influencing magma mobility and composition.