To install click the Add extension button. That's it.

The source code for the WIKI 2 extension is being checked by specialists of the Mozilla Foundation, Google, and Apple. You could also do it yourself at any point in time.

4,5
Kelly Slayton
Congratulations on this excellent venture… what a great idea!
Alexander Grigorievskiy
I use WIKI 2 every day and almost forgot how the original Wikipedia looks like.
Live Statistics
English Articles
Improved in 24 Hours
Added in 24 Hours
What we do. Every page goes through several hundred of perfecting techniques; in live mode. Quite the same Wikipedia. Just better.
.
Leo
Newton
Brights
Milds

From Wikipedia, the free encyclopedia

Vid Flumina
Physical characteristics
MouthLigeia Mare
Length>400 km[1]
Synthetic aperture radar image mosaic of Titan's north polar region

Vid Flumina is a river of liquid methane and ethane on Saturn's moon Titan. It is more than 400 km (249 mi) long and flows into Titan's second largest hydrocarbon sea, Ligeia Mare.[1] The surface of Titan is mostly water ice, so Vid Flumina is a river of methane and ethane flowing across and cutting canyons into ice as though it were bedrock. NASA scientists think that it likely has rapids, whirlpools and falls, just like rivers on Earth.

YouTube Encyclopedic

  • 1/3
    Views:
    127 617
    341 056
    820 692
  • Nasa Astronaut Returns With Chilling Information About Earth
  • Get Plastics Out Of Your Body & The Oceans #TeamSeas
  • How Ripples on Titan's Lakes Shocked NASA Scientists

Transcription

Discovery

Earlier findings

In 2004, NASA's probe, Cassini arrived at Saturn to study it and its moons. The scientists at NASA were expecting to find some evidence for liquid methane because of Titan's surface temperature and its methane-rich atmosphere. However, Cassini's early findings that were focused on Titan's equator revealed no traces of seas or rivers.[2]

The early disappointment changed as the Cassini's orbit shifted and allowed the researchers at NASA to bounce radar off other regions of the moon. The radar signals were then routinely reflected off angled, rough features such as sand dunes and rocks and cliffs, but when the radar reached the polar regions of Titan, the regular signals ceased. These non-reflecting dark spots were actually reminiscent of the lakes, rivers and tributaries on Earth.[2]

Discovery

In December 2012, Jani Radebaugh, a scientist on Cassini's team along with an international team of colleagues, announced that they had discovered a liquid methane river of over 200 miles resembling the Nile from an image taken on 26 September 2012.[2]

Geology

The river flows along a relatively straight course, suggesting that it follows one or more fault lines, similar to other large nearby rivers.[3][4] The river slices through a rough and slanted terrain, which suggests operation of processes similar to tectonic movements on Earth.

Radar studies show that Vid Flumina and its tributaries flow through canyons about one km wide and 0.57 km deep, with slopes of about 40°. Flowing methane was detected in the channels. The elevation of the main channel was found to be within 1 m of that of Ligeia Mare, while tributary channels have higher elevations. The canyons are thought to have formed by erosion stimulated either by uplift of the area or a decline in the level of Ligeia Mare.[5][6]

References

  1. ^ a b "Methane-filled canyons line Titan's surface, study finds". AGU. Retrieved 1 April 2024.
  2. ^ a b c "Cassini Finds a New Nile River on Titan". Discover Magazine. Retrieved 2022-10-25.
  3. ^ "NASA - Cassini Spots Mini Nile River on Saturn Moon".
  4. ^ Yang, Koh Xuan (24 May 2013). "Beyond Earthly Skies: A River on Titan".
  5. ^ "Methane-filled canyons line Titan's surface, study finds". news.AGU.org. American Geophysical Union and Jet Propulsion Laboratory. 2016-08-10. Retrieved 2016-08-11.
  6. ^ Poggiali, V.; Mastrogiuseppe, M.; Hayes, A. G.; Seu, R.; Birch, S. P. D.; Lorenz, R.; Grima, C.; Hofgartner, J. D. (2016-08-09). "Liquid-filled canyons on Titan" (PDF). Geophysical Research Letters. 43 (15): 7887–7894. Bibcode:2016GeoRL..43.7887P. doi:10.1002/2016GL069679. hdl:11573/932488. S2CID 132445293.
This page was last edited on 15 May 2024, at 13:04
Basis of this page is in Wikipedia. Text is available under the CC BY-SA 3.0 Unported License. Non-text media are available under their specified licenses. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc. WIKI 2 is an independent company and has no affiliation with Wikimedia Foundation.