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Digby Neck - A Peninsula EarthCache

Hidden : 7/13/2020
Difficulty:
3.5 out of 5
Terrain:
2.5 out of 5

Size: Size:   other (other)

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Geocache Description:


Digby Neck - A Peninsula


Digby Neck (peninsula) is the western extension of the North Mountain range from the Annapolis Valley and is made of two thick lava flows. It is separated from the eastern portion of the North Mountain by a deep, tidal channel, the Digby Gut. Digby Neck, along with Long Island and Brier Island, forms the northwest shore of St. Mary's Bay. On the north side of the peninsula is the Bay of Fundy.  The western most community on the Digby Neck is East Ferry, opposite Tiverton on Long Island to the west. The "Petit Passage" separates Long Island from the Digby Neck.


A peninsula is a landform surrounded by water on the majority of its border while being connected to a mainland from which it extends. The surrounding water is usually understood to be continuous, though not necessarily named as a single body of water.



Geology


The ridge (North mountain)  traces its history to the Triassic period when this part of Nova Scotia occupied the center of the supercontinent Pangaea. It is a 201 million year old sequence of tholeiitic basalts, which contains columnar jointing. The basalts also extend under the Bay of Fundy. 



North Mountain is a narrow southwest-northeast trending volcanic ridge on the mainland portion of southwestern Nova Scotia, stretching from Brier Island to Cape Split.  The ridge traces its history to the Triassic period when this part of Nova Scotia occupied the center of the supercontinent Pangaea. It is a 201 million year old sequence of tholeiitic basalts, which contains columnar jointing. The basalts also extend under the Bay of Fundy and parts of it are exposed on the shore at Five Islands, east of Parrsboro on the north side of the bay.  Numerous sediment-filled fissures are present near the upper surface of North Mountain. The hard ridge of basalt resisted the grinding of ice sheets that flowed over the region during past ice ages, and now forms one side of the Annapolis Valley in western part of the Nova Scotia peninsula.



To log this Earthcache visit the viewing location.  Please answer the following questions and send in a timely manner to my geocaching profile or email. Answers not received will result in deleted logs.


Note: No need to cross on the ferry to complete the Earthcache.


Questions:


1. Elevation at ground zero and Elevation at top of ridge, what is the difference?


2. What is the length of the peninsula, kilometers?


3. What is the width of Petite Passage at the end of the Peninsula (ground zero)?


4. Post a picture in your log with a personal item or hand in picture to prove you were there.


[REQUIRED] In accordance with the updated guidelines from Geocaching Headquarters published in June 2019, photos are now an acceptable logging requirement and WILL BE REQUIRED TO LOG THIS CACHE. Please provide a photo of yourself or a personal item in the picture to prove you visited the site.



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