East Bay (Nova Scotia)

Last updated
East Bay
East Bay in October.jpg
East Bay in October
Nova Scotia topographic map.png
Red pog.svg
East Bay
East Bay in Nova Scotia
Canada relief map 2.svg
Red pog.svg
East Bay
East Bay (Canada)
Location Cape Breton Island, Nova Scotia
Coordinates 45°53′52″N60°37′17″W / 45.89778°N 60.62139°W / 45.89778; -60.62139 Coordinates: 45°53′52″N60°37′17″W / 45.89778°N 60.62139°W / 45.89778; -60.62139
Type Bay
Part of Bras d'Or Lake
Ocean/sea sources Gulf of Saint Lawrence, Atlantic ocean
Basin  countries Canada
Max. length22 nautical miles (41 km; 25 mi)
Max. width5.2 nautical miles (9.6 km; 6.0 mi)
Settlements Cape Breton Regional Municipality

Communities include (from northwest to the bay's eastern terminus to southwest):

Contents

References Geographical Names of Canada - East Bay

East Bay [1] is a bay of the Bras d'Or Lake on Cape Breton Island [2] in the Canadian province of Nova Scotia. It lies entirely within Cape Breton County.

East Bay at sunset 20130810 East Bay, Nova Scotia at sunset.jpg
East Bay at sunset

Description

East Bay is one of three long narrow arms that extend to the east of the main body of the Bras d'Or Lake, the others being St. Andrews Channel and Great Bras d'Or Channel. [3] As East Bay is part of the Bras d'Or Lake system and the lake is essentially a fiordal system connected to the North Atlantic via two restricted channels at the Great Bras d'Or Channel north of Boularderie Island and the Little Bras d'Or Channel to south of Boularderie Island, the waters of East Bay are brackish, partially fresh/ salt water.

East Bay opens to the south-west directly onto the Bras d'Or Lake and lies between the Boisdale Hills to the north and the East Bay Hills to the south. The bay measures 8.3 kilometres (5.2 mi) wide at its mouth, between Benacadie Point to the north, and Middle Cape to the south and runs easterly 41 kilometres (25 mi) to its terminus at Portage. East Bay has 77.9 kilometres (48.4 mi) of shoreline. [4]

The bay's shores are generally heavily wooded and consist mainly of bold and rocky shorelines interspersed with numerous barrachois (barrier) points and beaches. Glacial drumlin deposits form a group of islands along the northern shore of East Bay. The narrower eastern end of the bay is bridged by the East Bay Sandbar, running east–west 1.25 kilometres (0.78 mi).

The name

The present day name for the bay, "East Bay", appears in written accounts as early as 1829, [5] and on maps of the area at least as far back as 1855, [6] though both current and former names (previously "St. Andrews Channel") appeared together on maps as late as 1890. [7] The earlier name "St. Andrews Channel", is now used to identify the adjacent arm of the lake to the north falling between the Boisdale Hills and Boulardarie Island.

Oceanography

East Bay's limited connections to the open ocean through the relatively narrow and shallow Great and Little Bras d'Or channels and the Barra Strait result in limited tidal movement. [8] This, in combination with high freshwater runoff, results in relatively low salinity of 20-21 p.p.t.in surface waters at the east end of East Bay. A thermocline and halocline develop at 10–20 metres (33–66 ft) during the summer and probably deepen in the winter. Measurements of oxygen and salinity indicate that lake water is a mix of Atlantic water and local runoff, with an insignificant contribution from groundwater. The bay is at least partially covered by ice most winters, with water temperatures warming by more than 10 °C from May to July. [3]

East Bay shows a typical estuarine water circulation, with brackish near-surface waters tending to flow toward the open lake to the west, and deep saline water tending to flow into the bay. The long fetch offered by West Bay to the south-west can result in sizeable waves and swells to develop during southwest or northeast gales. [3]

The view from the Ben Eoin Provincial Park Lookoff 20150926 Ben Eoin Provincial Park Lookoff.jpg
The view from the Ben Eoin Provincial Park Lookoff

Geology and seabed morphology

Much of the coastal topography around the bay is very steep, rising almost immediately from the shoreline to elevations of 180 to 200 metres (590 to 660 ft). Like the other major channels of the Bras d'Or Lake (St. Patricks, Great Bras d’Or, Little Bras d’Or and St. Andrews), East Bay has a northeast – southwest orientation. Rifting and regional tectonic plate movements some 360 million years ago formed this directional series of small fault bounded basins between highlands of resistant crystalline rock. The northern shoreline suggests that the bay is largely underlain by Carboniferous Windsor Group sedimentary rocks, principally shale, sandstone and gypsum. The southern shoreline is generally the elongated block of Precambrian rocks known as the East Bay Hills, composed of volcanic deposits of the Fourchu Group (ash and lava interleaved with marine sediments) and earlier Paleozoic era intrusive granite and quartzite. This is some of the oldest surficial geology visible around the Bras d'Or Lake, yet soft Windsor Group rocks form a narrow band along the bay's southern shore and extend out as the lake floor.

East Bay occupies a regional lowland that developed in soft Windsor Group rocks before the Quaternary glacial period. The main excavation of the deep channel (81–82 metres (266–269 ft)) in East Bay appears to be a consequence of glacial erosion, probably over hundreds of thousands of years through the Quaternary. The cliffs bordering the lake are unusual because they preserve organic sediments predating the last glaciation that provide a window on earlier environmental conditions. [3]

The morphology of the lake floor is influenced by the deposition of glacial till and pre-glacial silty muds that occurred during the last retreat of ice. A series of recessional moraines are visible on the floor of East Bay, with pre-glacial silty muds thickening eastward. [3] [9] [10]

Post-glacial history

The shallowness of the links between the Bras d'Or Lake and the Atlantic Ocean have resulted in a complex post-glacial history. Final melting of glacial ice probably occurred about 10,000 years after the Younger Dryas climatic oscillation. The first sediments deposited above glacial till in the central part of the lake, probably 10,000 to 9,000 years ago, contain dinocysts that indicate some penetration of marine water into the lake. The relatively high sea level inferred at this time reflects the continuing depression of the land from loading by glacial ice. Rebound from this depression cut off marine-water influx from about 9,000 to 4,500 years ago. As a result, for many thousands of years the Bras d'Or Lakes were fresh and relatively stable in size, water level and shoreline and were divided into a series of smaller lakes connected by rivers. East Bay was for the most part dry land during this period but the deeper area in the western part of the present bay was even then a significant bay off the main body of the largest of these lakes. Well-preserved and recognizable submerged coastal landforms are common in this part of East Bay. Clearly discernible tombolos, spits, and barrier beaches are present at this former coastline, 25–23 metres (82–75 ft) below present lake water levels. To the east, the present deep section of the bay east of the McPhee Islands was also a small lake, separated from the other lakes by a section of dry land, connected by a stream. [9] Late Holocene subsidence resulted in a renewed influx of marine water in the last 4,500 years. The effects of this subsidence are seen in the transgressive character of many of the shoreline features. [3] [9] [10]

Sediments

Sediment distribution in the Bras d'Or Lake is similar to that found in many of the larger coastal inlets on the southern shore of Nova Scotia. Deeper areas of the lake are floored by mud, except for the sands found in some areas flushed by tidal currents. Coastal erosion of glacial sediments has led to the formation of many sandy and gravelly barrier beaches and spits. [3]

Plants

Seaweed species are similar to those of the Gulf of St. Lawrence. In both areas, seaweeds usually found in intertidal zones occur only in deeper water as the result of winter ice activity, and the rockweed Ascophyllum nodosum is found subtidally. Sheltered bays have marginal salt to freshwater marsh vegetation. [3]

Animals

East Bay is one of the areas where the American Oyster is found, owing to warmer water temperatures suitable for growth and reproduction. A significant population of sand shrimp, a southern species, exists here. The polychaete fauna is Virginian in character but also includes some arctic-boreal species. Other invertebrate populations include lobster (Homarus americanus), Atlantic rock crab (Cancer irroratus), the invasive species Green crab (Carcinus maenas), sea urchins (Strongylocentrotus droebachiensis), starfish (Asterias vulgaris), sand dollars (Echinarachnius parma) and periwinkles. [11]

A varied fish fauna includes blueback herring, blackspotted stickleback, American eel and a southern population of Greenland cod. A feral population of rainbow trout is present in the bay as well. These support strong populations of great blue heron, double-crested cormorant, and bald eagle. [3] [12] [13]

Cultural environment

Most cultural use of East Bay is related to shore-based activities. The area is of high cultural significance to the Mi'kmaq people. Eskasoni, a Mi'kmaq reserve, is the largest community on the bay, situated on the bay's northern shore.

The East Bay Regatta, held the last weekend in July since 1984, features races and other social events. In some years as many as 40 boats participate. 20090726 East Bay Regatta 0088.jpg
The East Bay Regatta, held the last weekend in July since 1984, features races and other social events. In some years as many as 40 boats participate.

The bay is important for recreational boating. [3] Sailboat racing is a long tradition in East Bay. The East Bay Regatta, held the last weekend in July since 1984, features races and other social events. In some years as many as 40 boats participate. [14] A marina for local and visiting boaters was completed and opened in the spring of 2013 at the community of Ben Eoin as part of the existing ski hill and golf course complex. [15] [16]

Ben Eoin Marina, Ben Eoin, Nova Scotia Ben Eoin Marina, Ben Eoin, Nova Scotia.jpg
Ben Eoin Marina, Ben Eoin, Nova Scotia

There is a popular public swimming beach at the East Bay Sandbar, just to the north of the small community of East Bay, and another in the community of Big Pond, opposite St Mary's Catholic Church. [17]

Communities

Communities along the shoreline of East Bay include (from northwest to the bay's eastern terminus to southwest):

Cape Breton County

See also

Related Research Articles

<span class="mw-page-title-main">Cape Breton Island</span> Island in Nova Scotia

Cape Breton Island is an island on the Atlantic coast of North America and part of the province of Nova Scotia, Canada.

<span class="mw-page-title-main">Gulf of St. Lawrence</span> Outlet of the North American Great Lakes via the St. Lawrence River into the Atlantic Ocean

The Gulf of St. Lawrence is the outlet of the North American Great Lakes via the St. Lawrence River into the Atlantic Ocean. The gulf is a semi-enclosed sea, covering an area of about 226,000 square kilometres (87,000 sq mi) and containing about 34,500 cubic kilometres (8,300 cu mi) of water, at an average depth of 152 metres (500 ft).

<span class="mw-page-title-main">Cape Breton Highlands National Park</span> National park in Nova Scotia, Canada

Cape Breton Highlands National Park is a Canadian national park on northern Cape Breton Island in Nova Scotia. The park was the first national park in the Atlantic provinces of Canada and covers an area of 948 square kilometres (366 sq mi). It is one of 42 in Canada's system of national parks.

<span class="mw-page-title-main">Bras d'Or Lake</span> Lake in Nova Scotia, Canada

Bras d'Or Lake is an irregular estuary in the centre of Cape Breton Island in Nova Scotia, Canada. It has a connection to the open sea, and is tidal. It also has inflows of fresh water from rivers, making the brackish water a very productive natural habitat. It was designated the Bras d'Or Lake Biosphere Reserve by UNESCO in 2011.

<span class="mw-page-title-main">Cape Breton Highlands</span>

The Cape Breton Highlands, commonly called the Highlands, refer to a highland or mountainous plateau across the northern part of Cape Breton Island in the Canadian province of Nova Scotia.

<span class="mw-page-title-main">St. Peter's, Nova Scotia</span> Village in Nova Scotia, Canada

St. Peter's is a small incorporated village located on Cape Breton Island in Richmond County, Nova Scotia, Canada.

Boularderie Island is an island separating the Cabot Strait from Bras d'Or Lake on the eastern coast of Cape Breton Island, Nova Scotia, Canada. It takes its name from Louis-Simon le Poupet de la Boularderie, who was granted the area as a concession from the King of France.

<span class="mw-page-title-main">Mira River (Nova Scotia)</span> River in Nova Scotia, Canada

The Mira River is a Canadian river located in eastern Cape Breton Island, Nova Scotia.

<span class="mw-page-title-main">Sydney River</span> River in Nova Scotia, Canada

The Sydney River is a short river located in Cape Breton County, Nova Scotia, Canada. Historically, it was also referred to as the Spanish River from the 18th century French name for its estuary, Baie d’Espagnols. It separates the communities of Coxheath and Westmount, on the north bank of the river, from Howie Centre, Sydney River, and Sydney on the south and east banks.

The Bras d'Or Lakes Scenic Drive is a scenic roadway on Nova Scotia's Cape Breton Island. It extends around the perimeter of Bras d'Or Lake.

<span class="mw-page-title-main">Geography of Nova Scotia</span>

Nova Scotia is a province located in Eastern Canada fronting the Atlantic Ocean. One of the Maritime Provinces, Nova Scotia's geography is complex, despite its relatively small size in comparison to other Canadian provinces.

<span class="mw-page-title-main">Nova Scotia peninsula</span> Peninsula in Nova Scotia

The Nova Scotia peninsula is a peninsula on the Atlantic coast of North America.

The East Bay Hills refer to a 'fault ridge' of ancient rock on the south side of the East Bay of the Bras d'Or Lake, located on Cape Breton Island, Canada, and are an extension of the Appalachian mountain chain. The East Bay Hills lie in Cape Breton County.

<span class="mw-page-title-main">Ben Eoin</span> Unincorporated community in Nova Scotia, Canada

Ben Eoin is a community in the Canadian province of Nova Scotia, located in the Cape Breton Regional Municipality.

Portage is a community in the Canadian province of Nova Scotia, located in the Cape Breton Regional Municipality on Cape Breton Island.

<span class="mw-page-title-main">Barra Strait</span> Body of water

The Barra Strait is a 1.22 km (0.76 mi) wide channel located in the Canadian province of Nova Scotia. It connects the northern and southern basins of Bras d'Or Lake, an inland saltwater body that dominates the centre of Cape Breton Island. The border between two of Cape Breton Island's counties runs through the strait; the community of Grand Narrows, in Cape Breton County, is situated on the eastern shore while the community of Iona, in Victoria County is situated on the western shore.

<span class="mw-page-title-main">Ben Eoin Provincial Park</span> Provincial park in Nova Scotia, Canada

Ben Eoin Provincial Park is a small secluded provincial park on an old farm against hardwood-covered hills in the community of Ben Eoin, Nova Scotia, Canada, on the south side of the East Bay of the Bras d'Or Lake, on Cape Breton Island. This picnic and hiking park is managed by the provincial Department of Natural Resources and is situated on a heavily wooded 225 acres (91 ha) parcel of Crown land. A short distance into the park there are several large neatly mown clearings with picnic tables under the trees at the edge of the small fields. Pit toilets and disposal areas for hot coals are available onsite.

<span class="mw-page-title-main">Grand Narrows Bridge</span> Canadian railway bridge

The Grand Narrows Bridge is a Canadian railway bridge crossing between Victoria County, Nova Scotia, and Cape Breton County. At 516.33 m (1,694 ft), it is the longest railroad bridge in the province. The bridge incorporates a swing span at its eastern end to permit the continued passage of marine traffic through the strait.

St. Patricks Channel is an arm of the Bras d'Or Lake located on Cape Breton Island, in the Canadian province of Nova Scotia. St. Patricks Channel lies entirely within Victoria County.

<span class="mw-page-title-main">Bras d'Or Lake Biosphere Reserve</span> UNESCO Biosphere Reserve in Nova Scotia, Canada

Bras d'Or Lake Biosphere Reserve is a UNESCO Biosphere Reserve located at Bras d'Or Lake, Cape Breton Island, Nova Scotia, Canada. It consists of a salt-water estuary watershed inland sea with three passages to the Atlantic Ocean. The Holocene transgression flooded a complex river-lake system of diverse geology, creating the small, deep inland sea with 12 significant watersheds draining both highlands and lowlands.

References

  1. "Geographical Names of Canada - East Bay" . Retrieved 6 June 2018.
  2. "Nova Scotia Geographical Names Database entry for "East Bay, County of Cape Breton" (includes map)". Government of Nova Scotia. Retrieved April 23, 2012.[ permanent dead link ]
  3. 1 2 3 4 5 6 7 8 9 10 "The Natural history of Nova Scotia - Bras d'Or Lake". Nova Scotia Museum of Natural history. Archived from the original on January 28, 2006. Retrieved April 23, 2012.
  4. "UINR 2007 State of the Bras d'Or Lakes: Marine Environmental Water Quality Background Report 2007-03-01" (PDF). Unama’ki Institute of Natural Resources. Retrieved October 13, 2013.
  5. An historical and statistical account of Nova-Scotia, Volume 2, by Thomas Chandler Haliburton. J. Howe, 1829. p.  241 . Retrieved April 23, 2012. East Bay.
  6. "Belcher's map of the Province of Nova Scotia, including the Island of Cape Breton - David Rumsey Historical Map Collection (includes map)". C.H. Belcher, Halifax, 1855. Retrieved April 23, 2012.
  7. "Mackinlay's map of the Province of Nova Scotia, including the island of Cape Breton - David Rumsey Historical Map Collection (includes map)". A. & W. Mackinlay, Halifax, 1890. Retrieved April 23, 2012.
  8. "Canadian Technical Report of Hydrography and Ocean Sciences 230, Modelling the tides of the Bras d'Or Lakes" (PDF). Fisheries and Oceans Canada, Ocean Sciences Division. Retrieved October 11, 2013.
  9. 1 2 3 "A History of Change in the Bras d'Or Lakes Since the Last Ice Age-- John Shaw". Unama’ki Institute of Natural Resources. Retrieved October 11, 2013.
  10. 1 2 "SENSITIVITY OF THE COASTS OF THE BRAS D'OR LAKES TO SEA-LEVEL RISE -- John Shaw, Robert B. Taylor, Eric Patton, D. Patrick Potter, George S. Parkes, and Scott Hayward". Geological Survey of Canada (Atlantic), Bedford Institute of Oceanography. Retrieved October 18, 2013.
  11. "Lobsters and Other Invertebrates in Relation to Bottom Habitat in the Bras d'Or Lakes" (PDF). Fisheries and Oceans Canada, Bedford Institute of Oceanography. Retrieved October 13, 2013.
  12. "Ecosystem Overview and Assessment Report for the Bras d'Or Lakes, Nova Scotia". Fisheries and Oceans Canada, Oceans and Coastal Management Division, Oceans and Habitat Branch, Maritimes Region. Retrieved October 11, 2013.
  13. "Distribution, prevalence and intensity of Anguillicoloides crassus in the American eel, Anguilla rostrata, in the Bras d'Or Lakes, Nova Scotia" (PDF). Unama’ki Institute of Natural Resources. Retrieved October 14, 2013.
  14. "East Bay Regatta set for weekend". Cape Breton Post. Retrieved 3 June 2018.
  15. "Four-season resort village discussed at Ben Eoin meeting". Cape Breton Post. Archived from the original on October 11, 2013. Retrieved April 23, 2012.
  16. "$3.5-million marina proposed for Ben Eoin". The Chronicle Herald. Retrieved April 23, 2012.
  17. McKay, Wayne. "5 Best Beaches in Cape Breton". goCapeBreton.com. Retrieved 6 June 2018.
Notes