Gravitational anomalies (or gravity anomalies) are local deviations in the strength of Earth's gravitational field from the expected theoretical value.

Short explanation (in English):

They occur when the measured gravity at a specific location on Earth differs from what a standard model predicts (based on a smooth reference ellipsoid). These differences are usually tiny — up to about ±0.002 m/s² (0.02% of normal gravity).

Main causes:

• Uneven mass distribution underground (e.g., denser rocks, mountains, or ocean trenches).

• Variations in crustal thickness (isostasy).

• Density contrasts between Earth's crust and mantle.

Positive anomalies mean stronger gravity (more mass pulling), negative ones mean weaker gravity (less mass or lower density).

Examples:

• Mountain ranges or dense mineral deposits often show positive anomalies.

• Ocean trenches or areas with lighter crust show negative anomalies.

• Famous large-scale one: the "gravity hole" in the Indian Ocean, where sea level is about 100 meters lower due to weaker gravity.

In geophysics, scientists measure these anomalies with gravimeters or satellites (like GRACE) to map underground structures, find oil/minerals, or study Earth's interior.

(Note: This is the scientific/geophysical meaning. In physics theory, "gravitational anomaly" can also refer to quantum effects breaking symmetry, but the common usage — especially with the German term — is about Earth's gravity variations.)

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