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In planetary geology, a ray system comprises radial streaks of fine ejecta thrown out during the formation of an impact crater, looking somewhat like many thin spokes coming from the hub of a wheel. The rays may extend for lengths up to several times the diameter of their originating crater, and are often accompanied by small secondary craters formed by…
Lunar rays & Overview
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rays albedo ejecta moon ray craters impact crater material surface lunar infrared system thermal also systems moons planets mars micrometeorites
| Subject | Predicate | Object | Confidence | Src |
|---|---|---|---|---|
| the Moon | instance of | On non-atmosphered bodies | 0.80 | text |
| space weathering from exposure to cosmic rays | instance of | On non-atmosphered bodies | 0.80 | text |
| micrometeorites causes a steady reduction of the differential between the ejecta's albedo | instance of | On non-atmosphered bodies | 0.80 | text |
| that of the underlying material | instance of | On non-atmosphered bodies | 0.80 | text |
| Ray system | related to Lunar rays | The | 0.60 | section |
| Ray system | related to Lunar rays | Early | 0.60 | section |
| Ray system | related to Lunar rays | Later | 0.60 | section |
| Ray system | related to Lunar rays | After | 0.60 | section |
| Ray system | related to Lunar rays | Eugene Shoemaker | 0.60 | section |
| Ray system | related to Lunar rays | Recent | 0.60 | section |
| Ray system | related to Lunar rays | Instead | 0.60 | section |
| Ray system | related to Lunar rays | FeO | 0.60 | section |
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