Mare Crisium , Mare Undarum , are close enough to the visible Moon to always be observed in the first half of lunation, except the first days, when detailed visual observation is impossible.
Optics: Celestron C8"-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105 at 7x optical zoom
Total magnification: 700x
Filter: No
Date: 12/05/2011
Location: Baia Mare, Romania
Editing: Video stabilized in Sony Vegas 10
Monday, October 22, 2012
Saturday, October 6, 2012
Craters formed when meteorites, small pieces of rock and metal, roam the Solar System,and fall on the surface of a planet.The resulting impact is called crater.
Optics: Celestron C8"-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105
Total magnification: 100x
Filter: No
Date: 12/05/2011
Location: Baia Mare, Romania
Editing: Video stabilized in Sony Vegas 10
http://astrofotografieluna.blogspot.com
http://lupuvictor.blogspot.com/
Wednesday, December 7, 2011
Video: Victor Lupu
Optics: Celestron C8-Newtonian reflector telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Camera: Sony HDR CX105
Filter: no
Date: 09/02/2011
Location: Baia Mare, Romania
Processing: Sony Vegas 10, Registax
Posidonius Moon crater
The rim of Posidonius is shallow and obscured, especially on the western edge, and the interior has been overlain by a lava flow in the past. The crater ramparts can still be observed to the south and east of the crater rim, and to a lesser degree to the north. (Source: Wikipedia)
Monday, December 5, 2011
Video: Victor Lupu
Optics: Celestron C8-Newtonian reflector telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Camera: Sony HDR CX105
Filter: no
Date: 09/02/2011
Location: Baia Mare, Romania
Processing: Sony Vegas 10, Registax
Mare Crisium through telescope.
Mare Crisium (the "Sea of Crises") is a lunar mare located in the Moon's Crisium basin, just northeast of Mare Tranquillitatis. This basin is of the Pre-Imbrian period, 4.55 to 3.85 billion years ago. This mare is 555 km (345 mi) in diameter,[1] and 176,000 km2 in area. It has a very flat floor, with a ring of wrinkled ridges toward its outer boundaries. Ghost craters, craters that have largely been buried under deposits of other material, are located to the south. (Source: Wikipedia)