File:Structure planetes telliuriques.jpg
![File:Structure planetes telliuriques.jpg](http://178.128.105.246/cars-https-upload.wikimedia.org/wikipedia/commons/thumb/6/6b/Structure_planetes_telliuriques.jpg/799px-Structure_planetes_telliuriques.jpg?20060304162630)
Original file (3,373 × 900 pixels, file size: 299 KB, MIME type: image/jpeg)
Captions
Captions
Summary
[edit]DescriptionStructure planetes telliuriques.jpg |
Deutsch: Die innere Struktur der inneren Planeten. English: Mercury has an average density of 5430 kilograms per cubic meter, which is second only to Earth among all the planets. It is estimated that the planet Mercury, like Earth, has a ferrous core with a size equivalent to two-thirds to three-fourths that of the planet's overall radius. The core is believed to be composed of an iron-nickel alloy covered by a mantle and surface crust.
It is believed that the composition of the planet Venus is similar to that of Earth. The planet crust extends to around 10-30 kilometers below the surface, under which the mantle reaches to a depth of some 3000 kilometers. The planet core comprises a liquid iron-nickel alloy. Average planet density is 5240 kilograms per cubic meter. The Earth comprises three separate layers: a crust, a mantle, and a core (in descending order from the surface). The crust thickness averages 30 kilometers for land masses and 5 kilometers for seabeds. The mantle extends from just below the crust to some 2900 kilometers deep. The core below the mantle begins at a depth of around 5100 kilometers, and comprises an outer core (liquid iron-nickel alloy) and inner core (solid iron-nickel alloy). The crust is composed mainly of granite in the case of land masses and basalt in the case of seabeds. The mantle is composed primarily of peridotite and high-pressure minerals. Average planet density is 5520 kilograms per cubic meter. Mars is roughly one-half the diameter of Earth. Due to its small size, it is believed that the martian center has cooled. Geological structure is mainly rock and metal. The mantle below the crust comprises iron-oxide-rich silicate. The core is made up of an iron-nickel alloy and iron sulfide. Average planet density is 3930 kilograms per cubic meter. The structure of Pluto is not very well understood at present. Nevertheless, spectroscopic observation from Earth in the 1970s has revealed that the planet surface is covered with methane ice. Surface temperature is -230?C (-382?F), and the frozen methane exhibits a bright coloration. However, with the exception of the polar caps, the frozen methane surface is seen to change to a dark red when eclipsed by its moon Charon. Average planet density is 2060 kilograms per cubic meter. The low average density requires that the planet must be a mix of ice and rock.Français : Noyaux de la Lune et des planètes telluriques du système solaire. Polski: Budowa wewnętrzna planet typu ziemskiego Ελληνικά: Η δομή των εσωτερικών ή γήινων πλανητών και της Σελήνης |
|||
Source |
|
|||
Author | NASA | |||
Other versions |
[edit]
|
Licensing
[edit]Public domainPublic domainfalsefalse |
![]() |
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/Time | Thumbnail | Dimensions | User | Comment | |
---|---|---|---|---|---|
current | 16:26, 4 March 2006 | ![]() | 3,373 × 900 (299 KB) | Vyskocil~commonswiki (talk | contribs) | '''Source:''' http://sse.jpl.nasa.gov/multimedia/display.cfm?IM_ID=168 |
You cannot overwrite this file.
File usage on Commons
The following 9 pages use this file:
- File:Structure planetes telliuriques.jpg
- File:Terrestial Planets internal de.jpg
- File:Terrestial Planets internal en.jpg
- File:Terrestial Planets internal gr.jpg
- File:Terrestial Planets internal it.png
- File:Terrestial Planets internal pl.jpg
- File:Terrestial Planets internal ru.jpg
- File:Երկրային խմբի մոլորակների ներքին կառուցվածքը.jpg
- Template:Other versions/Terrestial Planets internal
File usage on other wikis
The following other wikis use this file:
- Usage on fr.wikipedia.org
- Usage on fr.wikibooks.org
- Usage on ro.wikipedia.org
Metadata
This file contains additional information such as Exif metadata which may have been added by the digital camera, scanner, or software program used to create or digitize it. If the file has been modified from its original state, some details such as the timestamp may not fully reflect those of the original file. The timestamp is only as accurate as the clock in the camera, and it may be completely wrong.
Orientation | Normal |
---|---|
Horizontal resolution | 300 dpi |
Vertical resolution | 300 dpi |
Software used | Adobe Photoshop CS2 Windows |
File change date and time | 17:11, 4 March 2006 |
Color space | sRGB |