Cunitz (krater wenusjański)

Cunitz
Ilustracja
Obszar Eistla Regio z widocznym kraterem uderzeniowym Cunitz. Na horyzoncie Gula Mons.
Ciało niebieskieWenus
Średnica krateru48,6 km
Źródło nazwyMaria Cunitz
Położenie na mapie Wenus
Mapa konturowa Wenus, w centrum znajduje się punkt z opisem „Cunitz”
Wenus14,50°N 350,90°E/14,500000 350,900000

Cunitzkrater uderzeniowy na planecie Wenus, o średnicy 48,6 km, położony na współrzędnych 14,5° szerokości północnej i 350,9° długości wschodniej[1], w okolicach Gula Mons.

Nazwany nazwiskiem Marii Cunitz[1], śląskiej astronom, która w swoich badaniach zajmowała się ruchem i fazami Wenus.

Zobacz też

Przypisy

  1. a b Cunitz (ang.). W: Gazetteer of Planetary Nomenclature [on-line]. IAU, USGS, NASA, 2010-05-15. [dostęp 2015-03-24].

Media użyte na tej stronie

Symbol venus blue.svg
Autor: , Licencja: CC-BY-SA-3.0
Venus/female symbol, rеcolour by Vade Parvis
Venus map NASA JPL Magellan-Venera-Pioneer.jpg
Stitched from Magellan RADAR imagery. Gaps filled in with Pioneer Venus Orbiter and Venera 13/14 images. Resolution 4 pixels per degree
Steel pog.svg
Shiny LightSteelBlue button/marker widget. Used to mark the location of something such as a tourist attraction.
PIA00233- Venus - 3D Perspective View of Eistla Regio.jpg

Original Caption Released with Image:

A portion of western Eistla Regio is displayed in this three-dimensional perspective view of the surface of Venus. The viewpoint is located 1,310 kilometers (812 miles) southwest of Gula Mons at an elevation of 0.78 kilometer (0.48 mile). The view is to the northeast with Gula Mons appearing on the horizon. Gula Mons, a 3 kilometer (1.86 mile) high volcano, is located at approximately 22 degrees north latitude, 359 degrees east longitude. The impact crater Cunitz, named for the astronomer and mathematician Maria Cunitz, is visible in the center of the image. The crater is 48.5 kilometers (30 miles) in diameter and is 215 kilometers (133 miles) from the viewer's position. Magellan synthetic aperture radar data is combined with radar altimetry to develop a three-dimensional map of the surface. Rays cast in a computer intersect the surface to create a three-dimensional perspective view. Simulated color and a digital elevation map developed by the U.S. Geological Survey, are used to enhance small-scale structure. The simulated hues are based on color images recorded by the Soviet Venera 13 and 14 spacecraft. The image was produced at the JPL Multimission Image Processing Laboratory and is a single frame from a video released at the March 5, 1991, JPL news conference.