Bay of Fundy Rock Hounding: Where Continents Collide!

Hampton Bay Patio - Bay of Fundy Rock Hounding: Where Continents Collide!

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Whilst Fundy's huge tides gradually chip away at the towering coastal cliffs and wash the shores, quite a few important rocks, zeolites and semi-precious stones are revealed day by day. As such, the Bay of Fundy is regarded as a rock hounder's paradise.

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Hampton Bay Patio

On the shores near Parrsboro, Nova Scotia, mineral treasures like, for example, amethyst and agate aren't unusual discoveries. Parrsboro is also the place to find the Fundy Geological Museum, where citizen have a opening to examine mineral terminals, view some of the oldest dinosaur bones in Canada, as well as the earth's first reptiles.

Plan a visit to New Brunswick's Fundy National Park and view two separate tale-telling rock clusters. While the beige and greyish rocks spotted near Owls Head are made of sandstone, the volcanic rocks close to Point Wolfe show the relocation of our continents, and they're made from white colored quartz veins, swirling folds and also criss-crossing cracks. The older rocks in this national park are situated near Point Wolfe. The Caledonia Highlands, which are as old as the Ice Age, may also be seen in Fundy National Park.

Recently, in the Fall season of 2010, a region neighboring St. John, New Brunswick, had the honor to be named as the 1st Unesco acknowledged Geopark in all of Canada and the Usa. The Stonehammer Geopark stretches east along the Fundy Trail Parkway, west at the Lepreau Waterfalls and stretches inland as far as Norton, Hampton and Grand Bay-Westfield.

Stonehammer's tagline is "A Billion Years of Stories" and this could not be more spot-on. From an consideration patio beside Saint John's Harbour Passage, visitors look across the Reversing Rapids gorge to a pair of continents which ran into each other thousands of years earlier. Taking a look across the gorge, the rocks at the left hand side create from the Cambrian duration (somewhere colse to five hundred million years of age) while the lighter grey rocks to the right hand side create from the Precambrian age (seven hundred and fifty million-1.2 billion years old).

Stonehammer contains rocks of the majority of the geologic eras except for the Tertiary and Jurassic eras. Some other Stonehammer Geopark visitors attractions comprise the Irving Nature Park, Rockwood Park, Dominion Park, Tucker Park, Fort Howe and King square West. One can find over two hundred potential sites of geological importance straight through this 2800 km2 region.

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