File:PIA00210 Venus - Golubkina Crater.jpg

Page contents not supported in other languages.
This is a file from the Wikimedia Commons
From Wikipedia, the free encyclopedia

Original file(1,024 × 1,250 pixels, file size: 200 KB, MIME type: image/jpeg)

Summary

Description
English: This image of the Venusian crater Golubkina, a 340 kilometer (20.4 miles) diameter impact crater located at about 60.5 degrees north latitude, 287.2 degrees east longitude, contains Magellan data mosaiced with a Soviet Venera 15/16 radar image of the same feature. The Magellan part of the image (right) reveals details of the geology of the crater such as the central peak, the inner terraced walls, and the extremely smooth floor of the crater. The smoothness of the floor may be due to pounding of volcanic lava flows in the crater floor. The rough, blocky morphology of the crater ejecta and the sharp terraced crater wall suggest that this feature is relatively young. The Soviet data have a resolution of 102 km (0.601.2 miles); the Magellan data have a resolution of about 120 meters (400 feet).
Date
Source https://photojournal.jpl.nasa.gov/catalog/PIA00210
Author NASA/JPL

Licensing

Public domain This file is in the public domain in the United States because it was solely created by NASA. NASA copyright policy states that "NASA material is not protected by copyright unless noted". (See Template:PD-USGov, NASA copyright policy page or JPL Image Use Policy.)
Warnings:

File history

Click on a date/time to view the file as it appeared at that time.

Date/TimeThumbnailDimensionsUserComment
current10:20, 5 May 2024Thumbnail for version as of 10:20, 5 May 20241,024 × 1,250 (200 KB)PlanetUser{{Information |Description={{en|This image of the Venusian crater Golubkina, a 340 kilometer (20.4 miles) diameter impact crater located at about 60.5 degrees north latitude, 287.2 degrees east longitude, contains Magellan data mosaiced with a Soviet Venera 15/16 radar image of the same feature. The Magellan part of the image (right) reveals details of the geology of the crater such as the central peak, the inner terraced walls, and the extremely smooth floor of the crater. The smoothness of...
The following pages on the English Wikipedia use this file (pages on other projects are not listed):