File:Isostatic equilibrium EN.svg
Jump to navigation
Jump to search
Size of this PNG preview of this SVG file: 800 × 421 pixels. Other resolutions: 320 × 168 pixels | 640 × 337 pixels | 1,024 × 539 pixels | 1,280 × 674 pixels | 2,560 × 1,347 pixels | 1,900 × 1,000 pixels.
Original file (SVG file, nominally 1,900 × 1,000 pixels, file size: 87 KB)
Captions
Captions
Add a one-line explanation of what this file represents
Summary[edit]
| Description |
English: Schematic representation of the principle of isostatic equilibrium in geodynamics. The three situations in the figure are 1: a mountain range or plateau; 2: a totally filled basin (surface is at sea level); 3 an underfilled basin (with sea water forming the top part of the column). The formulas to the right give the lithostatic pressure at reference height. Symbols used: ρL = density of the lithosphere; ρA = density of the asthenosphere; ρS = density of the sediments in the basin; ρW = density of sea water. The heights of different sections of the columns are represented by a letter h; while g is the gravitational acceleration.
In the case of isostatic equilibrium, the (lithostatic) pressure should be equal for all three cases at the reference height, in formula: P1 = P2 = P3. |
| Date | |
| Source | Own work |
| Author | Woudloper |
| Other versions |
Dutch language version |
Licensing[edit]
|
I, the copyright holder of this work, release this work into the public domain. This applies worldwide. In some countries this may not be legally possible; if so: I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law. |
File history
Click on a date/time to view the file as it appeared at that time.
| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 21:57, 19 April 2009 | | 1,900 × 1,000 (87 KB) | Woudloper (talk | contribs) | removed errors |
| 17:13, 19 April 2009 |  | 1,900 × 1,000 (87 KB) | Woudloper (talk | contribs) | {{Information |Description={{en|1=Schematic representation of the principle of isostatic equilibrium in geodynamics. The three situations in the figure are 1: a mountain range or plateau; 2: a totally filled basin (surface is at sea level); 3 an underfill |
You cannot overwrite this file.
File usage on Commons
The following 2 pages use this file:
File usage on other wikis
The following other wikis use this file:
- Usage on pl.wikipedia.org
