Hopewell Rocks: Difference between revisions
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[[Image:Hopewell_Rocks_Main.jpg|thumb|right|250px|Out of view, a staircase affords access so that visitors can hike down from the cliffs into the bay during low tide.]] |
[[Image:Hopewell_Rocks_Main.jpg|thumb|right|250px|Out of view, a staircase affords access so that visitors can hike down from the cliffs into the bay during low tide.]] |
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The '''Hopewell Rocks''', also called the Flowerpot Rock |
The '''Hopewell Rocks''', also called the Flowerpot Rock are rock formations caused by tidal erosion in ''The Rocks Provincial Park'' in [[New Brunswick]]. |
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They are located on the shores of the upper reaches of the [[Bay of Fundy]] at [[Hopewell Cape]] near [[Moncton]], [[New Brunswick]]. Due to the extreme tidal range of the Bay of Fundy, the base of the formations are covered in water twice a day. However, it is possible to view the formations from ground level at low tide<ref>As the tides are best seen at low tide, check the [[Environment Canada]] website for tide tables</ref>. |
They are located on the shores of the upper reaches of the [[Bay of Fundy]] at [[Hopewell Cape]] near [[Moncton]], [[New Brunswick]]. Due to the extreme tidal range of the Bay of Fundy, the base of the formations are covered in water twice a day. However, it is possible to view the formations from ground level at low tide<ref>As the tides are best seen at low tide, check the [[Environment Canada]] website for tide tables</ref>. |
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Revision as of 23:30, 3 April 2008
The Hopewell Rocks, also called the Flowerpot Rock are rock formations caused by tidal erosion in The Rocks Provincial Park in New Brunswick.
They are located on the shores of the upper reaches of the Bay of Fundy at Hopewell Cape near Moncton, New Brunswick. Due to the extreme tidal range of the Bay of Fundy, the base of the formations are covered in water twice a day. However, it is possible to view the formations from ground level at low tide[1].
The formations consist of dark sedimentary conglomerate and sandstone rock. The large volume of water flowing in to and out of the Bay of Fundy modifies the landscape surrounding it. After the retreat of the glaciers in the region following the last ice age, surface water filtering through cracks in the cliff has eroded and separated the formations from the rest of the cliff face. Meanwhile, advancing and retreating tides and the associated waves have eroded the base of the rocks at a faster rate than the tops, resulting in their unusual shapes.
The vast sediment planes in the basin in Fundy support a variety of biological productivity. Various shore birds are often seen flocking to nest and feed in the area. Visitors are advised to stay for a full tidal cycle to a full appreciation of the formation
Photo gallery
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Low Tide
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High Tide
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Visitors during Low Tide
See also
References
- ^ As the tides are best seen at low tide, check the Environment Canada website for tide tables
External links
45°49.4′N 64°34.4′W / 45.8233°N 64.5733°W
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