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Showing posts sorted by relevance for query Boguslawsky. Sort by date Show all posts
Showing posts sorted by relevance for query Boguslawsky. Sort by date Show all posts

Monday, 23 May 2011

Nearch Jacobi and Boguslawsky-South Moon craters

A
B
C

Photographer: Victor Lupu
Optics: Celestron C8-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105
Filter: No
Date: 10/02/2011
Location: Baia Mare, Romania
Processing: Sony Vegas 10, video captures

In photo A: craters Hommel, Vlaq, Pitiscus, Rosenberger, Nearch (76 km) and Hagecius (76 km).

         Nearch (76 km) is an impact crater, situated on the south-east region of the Moon, south-east of the crater Hommel. North of Nearch is Vlacq, and north-east lies Rosenberger. Nearch is 76 kilometers in diameter and 2.9 km deep and dates from pre-nectarian era, now 4.55 - 3.92 billion years ago.
The outer edge of the crater has been affected by small craters, which overlap along the eastern edge. The most important of these is Nearch A (43 km) on south-east edge. Small craters are found on the north and west. The rest of the interior walls are relatively intact, and retains its circular shape.


          Hagecius (76 km), this crater forms a triangle with crater Rosenberger on north-west and Nearch on west-north-west. Like other craters, Hagecius was undergone further erosion of the impacts. South-eastern edge is overlaped by three smaller craters called Hagecius C (24 km), B (34 km) and G (30 km).


In photo C: crater Mutus, Manzinus, Jacobi (68 km), Boguslawsky (97 km), Tannerus (29 km), Kinau (42 km) and Sempilius (70 km).

      Jacobi (68 km), has a margin of several overlapping craters along the southern edge, including Jacobi J (19 km), and a pair on the north side. The result is that the outer edges are flat along the north and south sides. On the north side, Jacobi A, forms a member of a chain of craters, forming a line on the floor inside, from north-east to south-west.

        Boguslawsky (97 km) is located near the southern edge of the Moon. It lies northwest of the crater Demonax, and south-west of Boussingault (131 km). Due to its location Boguslawsky appears elongated.
 Crater floor is flooded and with no many features. The edge is low. Crater Boguslawsky D is on the east side.
The name comes from the Palm (or Palon) Heinrich Ludwig (Pruß) von Boguslawski (7 September 1789-5 Iun 1851) who was a German professor of astronomy.

         Tannerus (29 km). The edge of this crater is almost circular, with only a slight inward bulge along the northern edge where it is joined with Tannerus P (20 km). Edge is clear and well defined, although there are small craters along the border in the west and south. Crater floor is without marks or features.
Crater name is given from Adam Tanner (in Latin, Tannerus) (14 April 1572 - May 25, 1632) which was an Austrian Jesuit professor of mathematics and philosophy.

         Kinau (42 km), is a mile deep. Kinau may date from the pre-nectarian era, 4.55 - 3.85 billion years ago. North-western edge of the crater walls was strongly affected by the impacts, and is overlaid by a pair of small craters, bowl-shaped. The remaining edge is distorted into a hexagonal shape, with the small craters along its rim. The interior walls are relatively low and the interior floor is with almost no characteristics. There is a small rise near the middle of the crater.
The crater is named after 19th century German priest, teacher and amateur astronomer Adolph Gottfried Kinau.

          Sempilius (70 km).  The crater may also date back to pre-nectariana, 4.55 - 3.85 billion years ago.Sempilius was affected by impacts and is relatively circular.The crater is named after Hugh Sempill (or Semple ) (Latin Sempilius) (between 1589 or 1596, and 1654) which was a Scottish Jesuit mathematician and linguist.

To locate craters above, I've described crater names in the picture below, taken on 14/11/2010.

Thursday, 26 May 2011

Pentland Scott and Demonax-Moon craters




Photographer: Victor Lupu
Optics: Celestron C8-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105
Filter: No
Date: 10/02/2011
Location: Baia Mare, Romania
Processing: 10 Sony Vegas, video captures


In both top and bottom photos are craters Boguslawsky, Manzinus and Mutus, in the first photo are Pentland (56 km), Sempilius A, Scott (108 km) and Demonax (114 km) ,Schomberger (85 km) and Boussingault (131 km) .

Pentland (56 km), is a Moon impact crater on the south regions, and it appears distorted when viewed from Earth. Sempilius A is neighbor to the south, and Manzinus at east. On the rim of this crater is a depression along the southern edge,on which is attached a small crater on the outside. The inner wall keeps some untouched structures. The interior shows an elongated central increase in the midpoint. The floor is almost with no features, except for some small craters.
Crater name comes from Joseph Barclay Pentland (1797 - 12th July 1873) which was an Irish geographer and natural scientist. Born in Ireland, was educated at Pentland. He also studied in Paris and worked with Georges Cuvier.

Scott (108 km) is a crater near the south pole of the Moon. The northern side of the crater is in continuous darkness, and has not been mapped in detail. Scott is between similar-sized crater Amundsen  in the southeast and Schomberger northwest . In the northeast is Demonax.The placement of Scott and Amundsen crater on the south pole , refers to two antarctic explorers, Roald Amundsen and Robert Falcon Scott, in their race to be the first people to reach the south pole of the Earth.

Demonax (114 km) is in a difficult location to be watched.Demonax crater lies north of Scott. To the northwest is the crater Boguslawsky.The floor was renewed, leaving it flat. However, there is a group of central peaks near the middle.
The name comes from Demonax (Greek: Δημώναξ, Dēmōnax, 70-170) who was a philosopher born in Cyprus. He moved to Athens, known for his wisdom and talent for resolving disputes.This brought him the admiration of the citizens.

Schomberger (85 km) is located near the southern edge of the Moon. The younger satellite Schomberger A (31 km) is attached to the southern rim and Schomberger C (43 km), much older, just outside western edge. Crater is a relatively well defined, with sharp features and was not significantly affected by impacts. Edge is approximately circular with an inner wall complex marked by increased peaks and several terraces. Interior floor is relatively flat. At the midpoint of the interior is a complex of central peaks.
Boussingault (131 km). The most notable aspect of this crater is the large crater that is entirely within its outer walls, so that it resembles a double-wall formation. Outer edge is affected by other impacts and Boussingault K (29 km), is located in north-western edge. To the northwest there is also a formation of craters superposed: Boussingault E (98 km), B (54 km) and C (24 km).
Crater name comes from Jean-Baptiste Joseph Dieudonné Boussingault (February 2 1802- 11 May, 1887) which was a french chemist who has made a significant contribution to the science of agriculture, oil and metallurgical science.

Wednesday, 4 July 2012

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Saturday, 10 December 2011

Demonax crater. Pictures of Moon through the telescope

Photographer: Victor Lupu
Optics: Celestron C8-Newtonian telescope, plossl 20mm, 2x Barlow
Mount: CG5 (EQ5)
Device: Sony CX105 to 8x optical zoom
Total Magnification: 800x
Filter: no
Date: 08/16/2011
Location: Baia Mare, Romania
Processing: video captures, FastStone Image Viewer

 
Demonax (114 km), is a large crater with a depth of 3.9 km, located near the lunar South Pole, and has a relatively comparable size with the nearby crater Boussingault (131 km), which is partially visible in the images above.
 In the photos in this article, the floor of Demonax crater is not visible because the Moon inclination in 16 August did not allow this. This is also because the Sun was on a small angle.
 
We need to know that the Moon does not have its own fixed axis, but is leaning forward and backward within a month, making craters in some periods to not always be seen the same.This phenomenon is called wobble.
 
 For example, these craters are on the south of the Moon, and we can not see the floor of Demonax (as in the old photo below of 10 February), this means that the northern Moon craters are more visible, even more craters on Moon's North terminal. This means that in August 16th, the Moon was inclined forward.
 
Other craters of these photos are Boguslawsky and Manzinus.
 
                      Picture of the craters on the Moon's south pole, made on 10 February 2011.

 
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