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Related Concept Videos

Gravity between Spherical Bodies01:27

Gravity between Spherical Bodies

Newton's law of gravitation describes the gravitational force between any two point masses. However, for extended spherical objects like the Earth, the Moon, and other planets, the law holds with an assumption that masses of spherical objects are concentrated at their respective centers.
This assumption can be proved easily by showing that the expression for gravitational potential energy between a hollow sphere of mass (M) and a point mass (m) is the same as it would be for a pair of extended...
Gravimetry: Overview01:05

Gravimetry: Overview

Gravimetric analysis is a quantitative method where the analyte is isolated and weighed directly or after conversion into a substance of known composition. Gravimetric analysis can be classified as precipitation, electrogravimetry, volatilization, and particulate gravimetry, based on the method used to isolate the analyte.
In precipitation gravimetry, the analyte is converted into a precipitate and weighed. For example, the silver content in a sample can be estimated by precipitating and...
Acceleration due to Gravity on Other Planets01:24

Acceleration due to Gravity on Other Planets

The gravitational acceleration of an object near the Earth's surface is called the acceleration due to gravity. It can be measured by conducting simple experiments on Earth. However, such an experiment is impossible to conduct on the surface of other planets.
Astronomical observations are thus used to measure the acceleration due to gravity on other planets. This can be determined by observing the effect of a planet's gravity on objects close to it. The crucial factor that helps in this...
Measuring Acceleration Due to Gravity01:12

Measuring Acceleration Due to Gravity

Consider a coffee mug hanging on a hook in a pantry. If the mug gets knocked, it oscillates back and forth like a pendulum until the oscillations die out.
A simple pendulum can be described as a point mass and a string. Meanwhile, a physical pendulum is any object whose oscillations are similar to a simple pendulum, but cannot be modeled as a point mass on a string because its mass is distributed over a larger area. The behavior of a physical pendulum can be modeled using the principles of...
Acceleration due to Gravity on Earth00:55

Acceleration due to Gravity on Earth

Newton's second law is closely related to his first law of motion. It mathematically gives the cause-and-effect relationship between force and changes in motion. Newton's second law is quantitative and is used extensively to calculate what happens in situations involving a force. All external forces acting on a system add together to produce a net force Fnet. A larger net external force produces a larger acceleration. This acceleration is directly proportional to, and in the same direction as,...
Acceleration due to Gravity on Earth01:21

Acceleration due to Gravity on Earth

According to Newton's law of gravitation, the gravitational force on a body is proportional to its mass. According to Newton's second law of motion, the acceleration produced by an external force is inversely proportional to the force. Hence, the acceleration of an object under an external force of gravitation is independent of its mass.
The acceleration of an object close to the Earth, because of the Earth's gravitational pull, is called the acceleration due to gravity. It is always directed...

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Related Experiment Video

Updated: Jul 12, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Mars gravity: high-resolution results from viking orbiter 2.

W L Sjogren

    Science (New York, N.Y.)
    |March 9, 1979
    PubMed
    Summary

    Detailed Martian gravity mapping reveals significant anomalies, including a large one near Olympus Mons. This research provides new insights into Mars

    Area of Science:

    • Planetary Science
    • Geophysics

    Background:

    • Understanding Mars' gravity field is crucial for deciphering its geological history and internal structure.
    • Previous gravity maps had limited resolution and spatial coverage.

    Purpose of the Study:

    • To create a high-resolution gravity map of Mars.
    • To identify and characterize gravitational anomalies and their correlation with geological features.

    Main Methods:

    • Utilized Doppler radio-tracking data from spacecraft.
    • Generated a gravity map covering 30°S to 65°N latitude and 360° longitude.
    • Achieved a feature resolution of approximately 500 kilometers.

    Main Results:

    • Revealed a significant gravity anomaly associated with Olympus Mons.

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  • Identified a mascon (mass concentration) in Isidis Planitia.
  • Correlated other anomalies with known volcanic structures.
  • Conclusions:

    • The new gravity map provides unprecedented detail of Martian gravitational variations.
    • The identified anomalies, particularly near Olympus Mons, offer insights into the planet's crustal and mantle processes.
    • The modeling of Olympus Mons suggests a substantial subsurface mass concentration.