Vitello (crater)

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Vitello
Vitello crater 4136 h3.jpg
Coordinates 30°25′S37°33′W / 30.42°S 37.55°W / -30.42; -37.55
Diameter 42.51 km (26.41 mi)
Depth 1.7 km (1.1 mi)
Colongitude 37° at sunrise
Eponym Vitello
Altered Rectified Proiection (ARP) Selenochromatic Image (Si) of the Mare Humorum area with some selenochromatic landmarks Humorum Lum Si ARP- Ferruggia-Zetta.jpg
Altered Rectified Proiection (ARP) Selenochromatic Image (Si) of the Mare Humorum area with some selenochromatic landmarks
Lunar Orbiter 5 closeup of an area west of the central peak, showing large boulders on the surface. Vitello boulders 5168 h2.jpg
Lunar Orbiter 5 closeup of an area west of the central peak, showing large boulders on the surface.
    LRO image of the pattern of dark deposits at the crest of the central peak of Vitello Vitello M135433752L.png
    LRO image of the pattern of dark deposits at the crest of the central peak of Vitello

    Vitello is a lunar impact crater that lies along the southern edge of the small Mare Humorum, in the southwest part of the Moon's near side. It was named after 13th century Polish theologian and physicist Vitello. [1] It lies just to the east of the lava-flooded crater Lee. To the northeast along the edge of the lunar mare is the Rupes Kelvin, an irregular fault line.

    Contents

    Description

    This crater has a low, roughly circular rim with a sharp edge. The interior floor is irregular, rugged and hilly, with a ring of deep fractures [2] surrounding the central peak. A low ridge projects out from the northwest rim into the mare.

    Vitello was once believed to be a caldera rather than an impact crater. In To A Rocky Moon, lunar geologist Don Wilhelms summarized: It "is a Saari-Shorthill infrared hotspot, [3] is fractured, and is blanketed and surrounded by a dark deposit. If there is a caldera on the moon, this ought to be it." However, Lunar Orbiter 5 acquired high-resolution images of the interior and geologists noted that the fractures were filled with boulders which caused the infrared anomaly, and so volcanic heat was not escaping from Vitello. Wilhelms concluded "...if it is a caldera, its activity expired long ago." [4]

    Satellite craters

    By convention these features are identified on lunar maps by placing the letter on the side of the crater midpoint that is closest to Vitello.

    VitelloLatitudeLongitudeDiameter
    A34.1° S41.9° W21 km
    B31.1° S35.4° W11 km
    C32.4° S42.5° W14 km
    D33.2° S41.0° W18 km
    E29.2° S35.8° W7 km
    G32.3° S37.6° W10 km
    H32.8° S43.0° W12 km
    K31.9° S37.6° W13 km
    L31.6° S35.3° W7 km
    M32.4° S36.0° W7 km
    N32.1° S36.1° W5 km
    P31.2° S38.4° W9 km
    R33.0° S37.0° W3 km
    S30.8° S35.2° W6 km
    T33.8° S39.6° W9 km
    X32.2° S40.6° W8 km

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    References

    1. "Vitello (crater)". Gazetteer of Planetary Nomenclature. USGS Astrogeology Research Program.
    2. The geologic history of the Moon, 1987, Wilhelms, Don E.; with sections by McCauley, John F.; Trask, Newell J. USGS Professional Paper: 1348. (online)
    3. Shorthill, R. W., and Saari, J. M. 1966, Recent discovery of hot spots on the lunar surface - a brief report of infrared measurements on the eclipsed Moon. in Hess, W. N., Menzel, D. H., and O'Keefe, J. A., eds. The nature of the lunar surface - Proceedings of the 1965 IAU-NASA symposium: Baltimore, Johns Hopkins Press p. 215-228
    4. To a Rocky Moon: A Geologist's History of Lunar Exploration. Don E. Wilhelms, University of Arizona Press (1993). ISBN   978-0816510658