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

Ronkonkoma Moraine

From Wikipedia, the free encyclopedia

A map showing Long Island's topography and the generalized locations of the glacial moraines.

The Ronkonkoma Moraine, in the geography of Long Island, forms the southern of two ridges along Long Island's "backbone."[1]

Description

The Ronkonkoma Moraine, a terminal moraine, predates the Harbor Hill Moraine (which reached Long Island during the Wisconsin Glacial Episode); the Harbor Hill Moraine cut through the Ronkonkoma Moraine's western portions.[2]

The Ronkonkoma Moraine and the Harbor Hill Moraine intersect at Lake Success in western Nassau County.[2] Today, the moraine is most prominent in Suffolk County, where it traverses the center of Long Island and forms the South Fork.[3]

Notable summits

See also

References

  1. ^ Geological Survey: Quaternary History of the New York Bight: retrieved 2013-08-23.
  2. ^ a b Garvies Point Museum and Reserve: the Geology of Long Island.
  3. ^ Ph.D, Kathleen M. Fallon (2021-09-24). "Long Island's Dynamic History". ArcGIS StoryMaps. Retrieved 2021-12-20.
  4. ^ "Holtsville Site The Better One". Suffolk County News. March 7, 1913.("The Bald Hills near Holtsville are the highest land in Suffolk County")
  5. ^ "Sixty-Seven Fires Reported Last Year From The Selden Observation Tower". The Mid-Island Mail. August 15, 1935.

This page was last edited on 5 January 2022, at 18:18
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.