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

Werribee Plain

From Wikipedia, the free encyclopedia

The Werribee Plain is an expansive low-lying flat land located between the northwestern shore of Port Phillip Bay and the Grampians Central Highlands of Victoria, Australia, shared between Melbourne and Geelong. Named after the Werribee River, the plains are notable for their extensive, flat and rather featureless spans, interspersed by the occasional vertical feature, such as the You Yangs, a series of granite ridges and several small extinct volcanoes.

The Werribee Plain forms the eastern bayside portion of the vast Western Volcanic Plains between the Grampians and the Otway Ranges, which extend from the western suburbs of Melbourne to the South Australian border.[1]

YouTube Encyclopedic

  • 1/2
    Views:
    519
    3 765
  • FLINDERS PEAK & CIRCUIT - Hiking Trail - Yangs Regional Park - Victoria
  • The rainbow bee eater Merops ornatus - You Yangs Australia

Transcription

Geology

Volcanoes began erupting lava flows about 4.5 million years ago, and the youngest eruptions are only about 10,000 years old. There are over 400 mapped craters and vents on the plains. While all these individual volcanoes are extinct, the volcanic field itself is only dormant, so new eruptions are possible at any time.

The granite that forms the You Yangs was originally a mass of magma that worked its way up into the surrounding sedimentary rocks during a period of geological time known as the Devonian. The magma crystallised before it reached the surface, so it did not produce any volcanic activity. Instead, a very slow cooling rate allowed many large white crystals of feldspar to form. These can be seen in many of the granite outcrops throughout the ranges.

The nearest volcanoes to the You Yangs are the Anakies, which appear as three low hills on the western horizon. These all have summit craters and provided lava flows for the plains south of the You Yangs. There were also flows from the low volcanoes of Bald Hill and Spring Hill to the north of the You Yangs. When these volcanoes were active, probably between 2 and 3 million years ago, the You Yangs would have been granite islands in a sea of lava.

References

  1. ^ "Archived copy" (PDF). Archived from the original (PDF) on 2016-04-01. Retrieved 2016-09-05.{{cite web}}: CS1 maint: archived copy as title (link)

This page was last edited on 7 May 2023, at 18:55
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.