Cape Breton Places & Foods

Nova Scotia Nova Scotia stretches 500 kilometres on a southwest-northeast axis from Cape Sable to Cape North, the shape of the province is often compared to that native delicacy, the lobster, with Cape Breton Island representing the outstretched claws, preparing to nip unsuspecting Newfoundland across the Cabot Strait.

The outstanding geographical fact about Nova Scotia is not the land, but the sea. The province is virtually an island connected to the rest of Canada by the narrow Isthmus of Chignecto. No point of land is more than 55 kilometres from the coastline. Cape Breton is an island joined to the mainland by the Canso Causeway. It is the sea that has carved the wild and ragged shoreline of the Atlantic coast and the sea that creates the wondrous tides of the Bay of Fundy. It is the sea upon which the first European settlers arrived and the sea from which they pulled their livelihood in once bursting nets. It is the sea for which they built ships to sail to other seas, bringing back goods rare and precious and tales even stranger. Not surprisingly, it is to the sea that Nova Scotians today are looking for new sources of wealth from offshore oil and gas.

The province can be divided into three distinct physiographic regions - the lowlands, the uplands and the highlands, which in tum may be subdivided into distinct sub-regions. The lowlands include the fertile Annapolis Valley, the low-lying areas around the Northumberland Strait and large parts of Cape Breton Island. The geology is primarily sedimentary and it is in these areas that most of Nova Scotia's rich coal seams are located. These coasts tend to be low and flat, and there are few good harbours. The shoreline is characterized by sandbars and occasional dunes. Bathers can often wade many hundreds of metres on these sandbars when the tide is out.

The Atlantic uplands comprise an area equal to half the province, running from Cape Canso, Guysborough County, to the extreme southern tip, including all of Yarmouth, Shelburne, Queens and Lunenburg counties, and most of Digby, Halifax and Guysborough counties. The uplands are a mass of Pre-Cambrian hard granite and quartzite, interspersed with belts of weaker slate. l'he area has been heavily glaciated with the result that much of the soil has been scraped away and redeposited in numerous glacial formations, the most famous of which is the drumlin that forms Halifax's Citadel Hill.

Nova Scotia The coastline of the uplands region is deeply indented, forming many good harbours, some of which are considered outstanding. Hundreds of islands dot the landscape along the entire Atlantic coast, most notably at St. Margarets Bay and Mahone Bay. Reefs and shoals abound, accounting for the many lighthouses erected along this coast. In many ways the Atlantic uplands coast epitomizes the North Atlantic coastline with its bare granite sheets plunging headlong into the raging surf to produce an awesome cataclysm between land and sea. When people think of Nova Scotia, they usually envisage the rocky granite shores of the uplands.

The highlands are those parts of the province where metamorphosed igneous and sedimentary rocks have either intruded through the preexisting lowland sediments or resisted erosion to a better degree than the surrounding softer rock. The Cape Breton Highlands are the most notable example. The Cobequid Mountains of Cumberland and Colchester counties, the Antigonish highlands, and the North Mountain, which runs parallel with the Fundy shore from Cape Blomidon to Digby Neck, are the other Nova Scotia highlands. Appearing as sharp ridges when viewed from below, the highlands are actually flat tablelands. This may be observed first hand in the Cape Breton Highlands National Park. At Ingonish, and at Cheticamp, the Cabot Trail rises to the tablelands, several hundred metres above the sea level.

The outstanding feature of the highlands is rectilinear coastlines. In contrast with the hundreds of bays and peninsulas of the Atlantic coast, the shoreline of the Bay of Fundy and western Cape Breton are virtually straight. Here, uplifted highland cliffs that soar up hundreds of metres directly from the ocean create stretches of spectacular landscapes. Less well known, but no less spectacular, are the cliffs of the Bay of Fundy coast, which are interspersed with fossils and unusual minerals.


Oaks of the Island

Filed under: Oak Island — admin @ 5:37 pm

Oaks of the Island Some time before 1790, the island became known as Oak Island, because of the very fine grove of large and beautiful oak trees growing upon its eastern end. It is a fact that Oak Island is the only one out of over 300 in Mahone Bay which has on it any oak trees. That they were large and consequently very old in 1795 is well established. Owing largely to the attacks of black ants in the last century, these oaks, which were numerous at one time, have entirely disappeared, the last two or three dying about 1960.

A number of writers, apparently with a view to adding more mystery to their stories, have stated that this species of oak does not grow elsewhere in Nova Scotia, that they are southern trees found no farther north than Louisiana. Some accounts allege that they are of Mexican origin, and on that assumption advance the theory that the treasure is an Aztec hoard.

Other writers have asserted that these oaks are of the variety or species known to the botanist as the “live oak” (quercus Virginia), an evergreen oak found principally in the southern United States. Its leaves are smooth and glossy; its wood hard and heavy, much used in shipbuilding. This assertion cannot be supported, for the oaks on Oak Island undoubtedly are red oaks, found along the same coast of Nova Scotia.

In 1931 one of these oaks, which bore on its surface evidence of having received an injury in earlier life, was cut down and examined critically with a view to determining its age and the cause of injury. Embedded deeply in the tree was found the end of a stout knife blade had broken off at the point of entry into the tree, the “rings” or “layers” were counted and it was determined that the tree was at least 183 years old, or dated from 1748 or earlier.

As we shall see, the presence in the Money Pit itself of platforms of oak logs, one platform above another, to a depth of more than ninety feet (each log six to eight inches in diameter) would indicate that a very extensive grove of trees existed on oak Island when the Money Pit was constructed. As such engineering work must have been carried out previously to 1749 when Halifax was founded, it follows that the tree cut down in 1931 was of a later generation. We have it as the opinion of a forestry expert, familiar with the grounds of oak trees along the south coast of Nova Scotia, that a tree measuring approximately seven or eight inches would be in the vicinity of fifty to seventy-five years of age. The older the tree, the slower it increases in diameter. A sixteen inch oak tree in this area would probably be about 200 years old. Assuming the correctness of this opinion, it fits in with the writer’s theory that the “Pit” was constructed between 1650 and 1750.

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