logging in or signing up 24.Uranus 7249 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINT lite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 39 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 09, 2011 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Slide 1: August 25 th , 1989 Voyager 2 encounters with Uranus and Neptune January 24 th , 1986 August 25 th , 1989Slide 2: The English astronomer, William Herschel, discovered Uranus in 1781Slide 3: McDonald Observatory image of Uranus and some of its moonsSlide 4: * * * * * * *Slide 5: Uranus is the only planet whose axis of rotation lies in its orbital plane (tilt of 98°), probably caused by a large impact.Slide 6: Comparison of the densities and compositions of the Jovian planetsSlide 7: Interior Structure of Uranus and Neptune *Slide 8: Approach of Viking 2 on July 15, 1985 of Uranus and 4 of its moons (composite).Slide 9: False color (left) and true color images of Uranus, taken by Viking 2Slide 10: The ring system of UranusSlide 11: Some of the rings of Uranus, discovered by the Viking spacecraftSlide 12: Rings of the planet Uranus, with two shepherd moons which keep the ring particles in place, discovered by the Viking spacecraftSlide 13: Continuous distribution of small particles throughout the ring system of Uranus. Picture taken while the Viking spacecraft was in the shadow of Uranus. These dust lanes were previously unknown. 96 second exposure, hence, background stars form streaks.Slide 14: Epsilon ring of Uranus, and three of the moons discovered by the Viking spacecraftSlide 15: Size comparison of the larger moons of UranusSlide 16: Miranda, ~468 km in diameterSlide 17: 5 km high scarp on Miranda – Miranda may have split apart and reassembledSlide 19: 50 km wide “chevron” on Miranda indicates complex historySlide 20: Ariel – 1,160 km in diameter; shows many tectonic featuresSlide 21: Umbriel - 1,168 km in diameter Resolution of this Viking image is ~ 10 km. Umbriel is highly cratered, particularly on its southern hemisphere (right). It is the darkest moon of Uranus, with an albedo of ~ 16 %, like our moon. It also is the moon with lowest internally-generated geologic activity. The bright spot at the top of the image (near the equator) may be frost.Slide 22: Titania – 1,580 in diameter; heavily cratered but also has long scarpsSlide 23: Oberon – 1,520 km in diameter; bright surface markings, many impact craters You do not have the permission to view this presentation. In order to view it, please contact the author of the presentation.
24.Uranus 7249 Download Post to : URL : Related Presentations : Share Add to Flag Embed Email Send to Blogs and Networks Add to Channel Uploaded from authorPOINT lite Insert YouTube videos in PowerPont slides with aS Desktop Copy embed code: (To copy code, click on the text box) Embed: URL: Thumbnail: WordPress Embed Customize Embed The presentation is successfully added In Your Favorites. Views: 39 Category: Entertainment License: All Rights Reserved Like it (0) Dislike it (0) Added: October 09, 2011 This Presentation is Public Favorites: 0 Presentation Description No description available. Comments Posting comment... Premium member Presentation Transcript Slide 1: August 25 th , 1989 Voyager 2 encounters with Uranus and Neptune January 24 th , 1986 August 25 th , 1989Slide 2: The English astronomer, William Herschel, discovered Uranus in 1781Slide 3: McDonald Observatory image of Uranus and some of its moonsSlide 4: * * * * * * *Slide 5: Uranus is the only planet whose axis of rotation lies in its orbital plane (tilt of 98°), probably caused by a large impact.Slide 6: Comparison of the densities and compositions of the Jovian planetsSlide 7: Interior Structure of Uranus and Neptune *Slide 8: Approach of Viking 2 on July 15, 1985 of Uranus and 4 of its moons (composite).Slide 9: False color (left) and true color images of Uranus, taken by Viking 2Slide 10: The ring system of UranusSlide 11: Some of the rings of Uranus, discovered by the Viking spacecraftSlide 12: Rings of the planet Uranus, with two shepherd moons which keep the ring particles in place, discovered by the Viking spacecraftSlide 13: Continuous distribution of small particles throughout the ring system of Uranus. Picture taken while the Viking spacecraft was in the shadow of Uranus. These dust lanes were previously unknown. 96 second exposure, hence, background stars form streaks.Slide 14: Epsilon ring of Uranus, and three of the moons discovered by the Viking spacecraftSlide 15: Size comparison of the larger moons of UranusSlide 16: Miranda, ~468 km in diameterSlide 17: 5 km high scarp on Miranda – Miranda may have split apart and reassembledSlide 19: 50 km wide “chevron” on Miranda indicates complex historySlide 20: Ariel – 1,160 km in diameter; shows many tectonic featuresSlide 21: Umbriel - 1,168 km in diameter Resolution of this Viking image is ~ 10 km. Umbriel is highly cratered, particularly on its southern hemisphere (right). It is the darkest moon of Uranus, with an albedo of ~ 16 %, like our moon. It also is the moon with lowest internally-generated geologic activity. The bright spot at the top of the image (near the equator) may be frost.Slide 22: Titania – 1,580 in diameter; heavily cratered but also has long scarpsSlide 23: Oberon – 1,520 km in diameter; bright surface markings, many impact craters