Wilhelm and Montanari craters flooded by darkness.

This area south of the Moon, east of the crater Tycho (85 km), is almost conquered the darkness. Most "affected" crters are Wilhelm (107 km) and Montanari (77 km). To these, the interiors are in total darkness. At both are observed only the outer edges. Wilhelm D is close to the eastern edge of Wilhelm (pictured on the west side because the images are upside down).

Moon Age: 9.05 days
Phase: 70.5% (0% = New, 100% = Full)
Distance: 399.221 km

Optics: Celestron C8-Newtonian telescope, 20mm Plossl, 2x barlow
Mount: CG5 (EQ5)
Camera: Sony CX130
Filter: no
Date: 10/03/2014
Location: Baia Mare, Romania
Processing: FastStone Image Viewer

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List of south features of the Moon-Southern lunar Hemisphere

Southern hemisphere of the Moon is in rough terrain, heavily cratered and with mountainous areas.
At the poles, the sun is always at small angles, so this is creating a unique environment, but also some difficulties in interpreting the geological region.
The southern hemisphere of the Moon craters are very different in size, appearance and how they were formed by impacts in the past.
Personally, the most interesting craters on south, I find Tycho, a crater with rays showing a very high albedo, rays that are left behind from the initial impact, wich can be seen from Earth with the naked eye or binoculars.
Another great crater is Clavius​​, a large crater with other small craters lying inside it in a decreasing order to form a spiral.
Shiller is another crater, interesting to me because of its elongated shape similar to a caterpillar.
 On the southern hemisphere of the Moon seen from Earth, there is only a sea, Mare Nubium that penetrate down to the crater Pitatus.

There are not mountains on the Moon's southern hemisphere. Maybe were probably destroyed by countless impacts were.

Most notable craters of the Moon southern hemisphere, in alphabetical order, are:

Aliacensis
Apianus
Asclepi
Baco
Ball
Barocius
Biela
Blanchinus
Boguslawsky
Bosching
Boussingault
Brown
Buch
Casatus
Cichus
Clairaut
Clavius
Curtius
Cuvier
Cysatus
Deluc
Demonax
Deslandres
Fabricius
Faraday
Fernelius
Frisius
Gauricus
Gemma
Gruemberger
Hagecius
Heinsius
Hell
Helmholtz
Heraclitus
Hommel
Jacobi
Janssen
Kaiser
Kinau
Klaproth
Lexell
Licetus
Lilius
Longomontanus
Maginus
Manzinus
Maurolycus
Metius
Miller
Montanari
Moretus
Mutus
Neander
Nearch
Neumayer
Newton
Nonius
Orontius
Pentland
Picret
Pitatus
Pitiscus
Playfair
Poisson
Pontanus
Pontecoulant
Proctor
Rabbi Levi
Rheita
Riccius
Rosenberger
Sasserides
Saussure
Sempilius
Short
Scheiner
Schiller
Schomberger
Scott
Steinheil
Stofler
Tannerus
Tycho
Vlaq
Watt
Weiss
Werner
Wilhelm
Wurzelbauer
Zach


Seas:
Mare Nubium

Space missions on the south side of the Moon:
Ranger 9 was launched on March 24, 1965 by United States of America and was intentionally crashed on the lunar surface, on crater Alphonsus.
Ranger 9 was designed to achieve an impact trajectory and to transmit pictures of the lunar surface in high-resolution during the flight until the impact.
  Ranger 9 successfully transmitted 5814 images with a resolution of up to 1.5 m.

LCROSS United States launched the LCROSS (Lunar Crater Observation and Sensing Satellite) which was deliberately crashed into the Moon's south pole on crater Cabeus on October 9, 2009
The mission was designed to search for water ice on the lunar surface and examining the resulting cloud, caused by impact. The mission ended with the discovery of significant amounts of water.

Moon Impact Probe was launched by India, and it was deliberately crashed on 14 November 2008 at the lunar south pole.
 It had 35 kg, and was released from Chandrayaan-1 Lunar Orbiter. It was equipped with a video camera, a radar altimeter and a mass spectrometer.

Video: Victor Lupu
Optics: CelestronC8 "-Newtonian telescope, plossl20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: SonyCX105 at 7x optical zoom
Total Magnification: 700x
Filter: no
Date: 16/08/2011
Location: Baia Mare, Romania
Processing and editing: Sony Vegas 10

To see the photographic map of the south area of the Moon, view: Photographic map of the Moon: South Zone. Lunar Atlas.

For those who like my astro pictures or my articles, it woul be great if you could pay attention on advertising that appear in the blog by a click and maybe one day I could buy a better telescope.

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How do the craters looks through an astronomical telescope. Tycho.

Tycho crater (85 km) is impressive in any light, and is easily distinguished among other craters around, especially because its shape and very long and intense rays that start from it.
 
Here, Tycho is half in darkness, shadow which bypasses the central peak on the floor, being left in the light.

Around it, there are many small holes, which are its satellite craters, and of other craters as of Heinsius (64 km) and Pictet (62 km).
Dark craters left are Longomontanus (145 km) and Montanari (77 km).
Moon Age: 9.05 days
Phase: 70.5% (0% = New, 100% = Full)
Distance: 399.221 km

Optics: Celestron C8-Newtonian telescope, 20mm Plossl, 2x barlow
Mount: CG5 (EQ5)
Camera: Sony CX130
Filter: no
Date: 10/03/2014
Location: Baia Mare, Romania
Processing:  FastStone Image Viewer

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Wilhelm and Pitatus Moon craters

Photographer: Victor Lupu
Optics: Celestron C8-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105
Filter: No
Date: 13/04/2011
Location: Baia Mare, Romania
Processing: Sony Vegas 10 captures video

        Wilhelm (107 km), is a lunar crater in the southern part of the Moon, west of the crater Tycho. Wilhelm has attached to its southern edge, Montanari crater (77 km), while Lagalla (85 km) is attached to the southwest. On the northeast is Heinsius (64 km).
Wilhelm's interior has a rough area to the northeast. The rest is flat and almost wih no features, except for ome small craters.

         Pitatus (97 km) is a crater located at the southern edge of Mare Nubium. It is connected to the northwest edge is Hesiodus (43 km), and the two are joined by a narrow crack. To the south is Wurzelbauer (88 km) and Gauricus (79 km).
Pitatus's walls are worn, and were covered by lava flows. Near the middle is a small central peak which is northwest of the center. This peak rises to a height of 0.5 km. The name is from Pietro Pitati an italian mathematician and asronomer.

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