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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...
Influence of Earth's Curvature and Atmospheric Refraction on Leveling01:26

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During leveling, the Earth's curvature and atmospheric refraction introduce deviations in the line of sight from a true horizontal reference. When the line of sight is leveled, it remains perpendicular to the plumb line only at a single point. Beyond this, it deviates due to the Earth’s curvature, represented by the correction C. For a sight distance D, the deviation can be derived using the relationship:This relationship shows that the deviation increases quadratically with distance. Over a...
Meridians01:28

Meridians

In surveying, meridians are vital reference lines to measure directions and establish accurate land orientations. Meridians run from the north to the south poles, providing a stable framework for angular measurements and mapping. Meridians are fundamental in survey design, with the primary types being astronomic, magnetic, and assumed meridians. Each type offers distinct benefits and limitations, selected based on the project's scale and precision needs.The astronomic meridian is aligned with...
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Midpoint Rule

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Updated: Jun 22, 2026

Scattering And Absorption of Light in Planetary Regoliths
11:34

Scattering And Absorption of Light in Planetary Regoliths

Published on: July 1, 2019

Lunar transient phenomena: topographical distribution.

B M Middlehurst, P A Moore

    Science (New York, N.Y.)
    |January 27, 1967
    PubMed
    Summary

    Transient lunar phenomena (TLP) sites are classified into three main types: maria-peripheral, ray craters, and dark-floored ring plains. These TLP locations are not found in the rugged southeastern lunar highlands.

    Area of Science:

    • Lunar science
    • Astronomy
    • Geology

    Background:

    • Lunar transient phenomena (TLP) are brief, unexplained visual events observed on the Moon.
    • Understanding TLP sites is crucial for lunar geology and observational astronomy.
    • Previous classifications of TLP sites have been limited.

    Purpose of the Study:

    • To classify the known sites of lunar transient phenomena (TLP).
    • To analyze the geographical distribution of TLP occurrences.
    • To compare visual TLP records with permanent observational data.

    Main Methods:

    • Analysis of nearly 400 reports detailing TLP occurrences.
    • Categorization of TLP sites into distinct classes based on lunar geography.
    • Comparison of visual TLP site data with available permanent records.

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    Main Results:

    • TLP sites fall into three primary categories: peripheral to maria, ray craters, and ring plains with dark floors.
    • No TLP sites are reported in the rugged highland areas of the southeastern lunar quadrant.
    • Existing permanent records of TLP sites align with visual observations.

    Conclusions:

    • The geographical distribution of TLP sites suggests specific lunar surface conditions may favor these events.
    • Further research into the characteristics of these three TLP site classes is warranted.
    • Consistency between visual and permanent records supports the validity of TLP site classifications.