Presqu'ile (Ontario): Difference between revisions

From Citizendium
Jump to navigation Jump to search
(first draft here)
 
mNo edit summary
 
(4 intermediate revisions by 2 users not shown)
Line 1: Line 1:
'''Presqu'ile''' is a [[tombolo]] on the north shore of [[Lake Ontario]] in [[Northumberland County, Ontario|Northumberland County]].<ref name=friendsofpresquileGeology/>
{{subpages}}
When proglacial [[Glacial Lake Iroquois|Lake Iroquois]] drained, leaving the lower Lake Ontario five limestone islands, the largest of which was [[Presqu'ile Island]] reduced the speed of currents carrying sand and silt, causing the dynamic sand spit to grow.  The spit eventually engulfed Presqu'ile Island, and two small islands.  [[Gull Island (Lake Ontario)|Gull]] and [[High Bluff Island (Lake Ontario)|High Bluff]] islands remain unattached,
[[File:Waterfront (142819807).jpg | thumb]]
'''Presqu'ile''' is a [[tombolo]] on the north shore of [[Lake Ontario]] in Northumberland County near the town of Brighton, [[Ontario]].<ref name=friendsofpresquileGeology/>
When proglacial [[Glacial Lake Iroquois|Lake Iroquois]] drained, leaving the lower Lake Ontario five limestone islands, the largest of which was [[Presqu'ile Island]] reduced the speed of currents carrying sand and silt, causing the dynamic sand spit to grow.  The spit eventually engulfed Presqu'ile Island, and two small islands.  [[Gull Island (Lake Ontario)|Gull]] and [[High Bluff Island (Lake Ontario)|High Bluff]] islands remain unattached. The Tombolo and the two remaining islands form Presqu'ile Provincial Park<ref name=PPP /> and provide a temporary sanctuary for migrating birds.


The Tombolo and the two remaining islands form [[Presqu'ile Provincial Park]], and provide a temporary sanctuary for migrating birds.<ref name="CGNDB"/>
==Notes==
 
==References==
{{Reflist|refs=  
{{Reflist|refs=  
<ref name=friendsofpresquileGeology>
<ref name=friendsofpresquileGeology>
Line 26: Line 26:
</ref>
</ref>


<ref name=CGNDB>
<ref name=PPP>[https://www.ontarioparks.ca/park/presquile Presqu'ile Provincial Park]'s official website.</ref>
{{cite web
 
| url        = https://geonames.nrcan.gc.ca/search-place-names/unique?id=FCIJX
| id          = FCIJX
| title      = Presqu'ile Provincial Park
| publisher  = Geographical Names Data Base, ''[[Natural Resources Canada]]''
| accessdate  = 2013-05-12
}}
</ref>
}}
}}

Latest revision as of 07:25, 11 March 2024

This article is a stub and thus not approved.
Main Article
Discussion
Related Articles  [?]
Bibliography  [?]
External Links  [?]
Citable Version  [?]
 
This editable Main Article is under development and subject to a disclaimer.
Waterfront (142819807).jpg

Presqu'ile is a tombolo on the north shore of Lake Ontario in Northumberland County near the town of Brighton, Ontario.[1] When proglacial Lake Iroquois drained, leaving the lower Lake Ontario five limestone islands, the largest of which was Presqu'ile Island reduced the speed of currents carrying sand and silt, causing the dynamic sand spit to grow. The spit eventually engulfed Presqu'ile Island, and two small islands. Gull and High Bluff islands remain unattached. The Tombolo and the two remaining islands form Presqu'ile Provincial Park[2] and provide a temporary sanctuary for migrating birds.

Notes

  1. Geology and Formation of Presqu'ile, Friends of Presqu'ile Park. Retrieved on 2019-05-06. “In the last few thousand years Lake Iroquois drained somewhat to form our present-day Lake Ontario. As it did so, five islands appeared off-shore of the mainland. These islands are Template:Sic limestone, part of that package of rocks formed so long ago in the Ordovician. This limestone has now been designated as part of the Lindsay Formation and is described as thin, crystalline to nodular limestone with very thin shaley seams (Peterson, 1969). This means that the rocks break up quite easily and form the low rubble cliffs found today on the south shore of Presqu'ile. This also means that the rock is not very suitable for building stone as demonstrated by the fate of the Presqu'ile Lighthouse (see the History section here). This rock is full of fossils, primarily crinoids, brachiopods, trilobites, and cephalopods, in decreasing order of abundance. Most of these fossils are fragments of the animals' shells, as they probably tumbled down a slope on the sea bed before coming to their final resting place to begin the process of fossilization.”
  2. Presqu'ile Provincial Park's official website.