THE GREAT TYCHO ZOOM 2-4

THE GREAT TYCHO ZOOM 2-4

THE GREAT TYCHO ZOOM 2-4

Photo Credit: NASA Lunar Reconnaissance Orbiter (LRO): CLICK for larger photo and look below for links and information.

2-4: Zooming in one step to the uplift/rebound region or as its known, the “central peak”. This is the 6562 ft. high mountain at the center of Tycho Crater captured at an oblique angle by LRO. It’s not hard to imagine climbing this mountain and local terrain. As its set into the crater, its peak still below the rim of the crater itself as you stood on top of this mountain you would only see a 360 degree wall of material stretching up above you another 8,858 ft. Perhaps you could, at times see Earth or LRO (which took this photo) flying overhead. I’d love to stand at the peak of this mountain or in the shadow of a mountain, during sunrise on the Moon. If you look closely near the peak of the mountain there’s a saddle and in that saddle is an extremely large boulder. I think we will visit that next…..

Tycho Crater is a paraboloid shaped, complex impact crater on the Moon which bears the name of the great Danish astronomer Tycho Brahe. The name was given by Giovanni Riccioli whose 1651 lunar nomenclature system is todays standard. It was formed on the approximately 110 million years ago which is very young in astronomical terms. It’s approximately 51 mi (82 km) in diameter with a depth of 2.9 mi (4.8 km). When viewed through binocular or telescope the albedo alerts you to its young age as its interior and ejecta “spokes” or “rays” appear to overlay the surrounding environment as they stretch as long as 932 mi (1500 km), especially when in sunlight.
One of the most incredible features is the uplift or rebound area at the crater’s center known as the central peak. It stretches about 9.3 mi (15 km) and rises off the crater floor to a height of 6562 ft. while the crater floor itself lies 15,420 ft. (4700 m) below the rim.
The rigidity and sharpness to the structure also lends itself to a young crater as it hasn’t yet been worn away by micrometeorites as it will through the years (to see what this crater may look like in a billion years check out Bhabha crater). It’s believed but not proven that this crater was created from the Baptistina family of asteroids, caused by the breakup and multiple impacts of asteroid 298 Baptistina. That is the asteroid which is believed to have also created the 110 mi (180 km) wide Chicxulub Crater in the Yucatan Peninsula on Earth which ended the era of the dinosaurs. Note that it’s believed to be the same material, this doesn’t imply that it happened at the same time as it’s estimated that the Chicxulub Crater was formed approximately 65-66 million years ago.
To locate Tycho Crater, Northern Hemisphere sky watchers will want to look near the very bottom of the Moon while my upside down friends in the Southern Hemisphere will need to search near the top of the Moon. In both cases it will be the brightest most prominent crater in that region. Its selenographic coordinates are 43.37°S, 348.68°E.

NASA LRO page for this crater: http://lroc.sese.asu.edu/news/?archives/411-Tycho-Central-Peak-Spectacular!.html

Incredible NASA LRO Tycho peak interactive zoom: http://wms.lroc.asu.edu/lroc_browse/view/M162350671

Tycho polygonal fractures: http://lroc.sese.asu.edu/news/index.php?/archives/403-Polygonal-fractures-on-Tycho-ejecta-deposits.html#extended

Tycho floor ejecta: http://lroc.sese.asu.edu/news/index.php?/archives/318-Ejecta-in-Tycho-crater.html#extended

Chaotic Tycho floor: http://lroc.sese.asu.edu/news/index.php?/archives/404-Chaotic-crater-floor-in-Tycho.html#extended

Impact melt on Tycho floor: http://lroc.sese.asu.edu/news/index.php?/archives/319-Impact-melt-features-in-Tycho-craters-floor.html#extended

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