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ORIGINAL ANTIQUE MAP NAUTICAL CHART Baffin Bay canada greenland Lancaster Sound

$ 76.55

Availability: 69 in stock
  • Country/Region of Origin: Canada
  • Original/Reproduction: Antique Original

    Description

    ORIGINAL ANTIQUE MAP NAUTICAL CHART
    [Thismap is not a reproduction or from a scan, and it's printed on a thick papermatting surface. My Map collection, passed down by my grandfather, has beenstored flat and folded]
    Baffin Bay canada greenland, Bylot Island, Lancaster Sound, Borden Penisula
    See Photos for condition.
    Baffin Bay
    (
    Inuktitut
    :
    Saknirutiak Imanga
    ;
    [3]
    Greenlandic
    :
    Avannaata Imaa
    ;
    [4]
    French
    :
    Baie de Baffin
    ),
    [a]
    located between
    Baffin Island
    and the west coast of
    Greenland
    , is defined by the
    International Hydrographic Organization
    as a
    marginal sea
    of the
    Arctic Ocean
    .
    [6]
    : Art.23
    It is sometimes considered a sea of
    North Atlantic Ocean
    .
    [1]
    [2]
    [7]
    It is connected to the Atlantic via
    Davis Strait
    and the
    Labrador Sea
    . The narrower
    Nares Strait
    connects Baffin Bay with the
    Arctic Ocean
    . The bay is not navigable most of the year because of the
    ice cover
    and high density of
    floating ice
    and
    icebergs
    in the open areas. However, a
    polynya
    of about 80,000 km
    2
    (31,000 sq mi), known as the
    North Water
    , opens in summer on the north near
    Smith Sound
    .
    [8]
    Most of the aquatic life of the bay is concentrated near that region.
    The
    Borden Peninsula
    [1]
    is a
    peninsula
    on northern
    Baffin Island
    , in
    Nunavut
    , Canada. It lies some 80 km south of
    Devon Island
    (Cape Warrender), from which it is separated by
    Lancaster Sound
    . Northeastern Borden Peninsula is home to
    Sirmilik National Park
    .
    Bylot Island
    [
    pronunciation?
    ]
    lies off the northern end of
    Baffin Island
    in
    Nunavut
    Territory, Canada.
    Eclipse Sound
    to the southeast and
    Navy Board Inlet
    to the southwest separate it from Baffin Island.
    Parry Channel
    lies to its northwest. At 11,067 km
    2
    (4,273 sq mi) it is ranked
    71st largest island in the world
    and
    Canada's 17th largest island
    . The island measures 180 km (110 mi) east to west and 110 km (68 mi) north to south and is one of the largest
    uninhabited islands
    in the world. While there are no permanent settlements on this
    Canadian Arctic island
    ,
    Inuit
    from
    Pond Inlet
    and elsewhere regularly travel to Bylot Island. An Inuit seasonal hunting camp is located southwest of
    Cape Graham Moore
    .
    The island's
    mountains
    are part of the
    Byam Martin Mountains
    , which is part of the
    Baffin Mountains
    of the
    Arctic Cordillera
    . In addition to
    Angilaaq Mountain
    ,
    Malik Mountain
    ,
    Mount St. Hans
    , and
    Mount Thule
    are notable. Tay Bay is on the west coast. Vertical cliffs along the coastline are made up of
    Precambrian
    dolomite
    . There are numerous glaciers. The western shore faces Navy Board Inlet. The island's north shore, facing
    Lancaster Sound
    , is a
    polar bear
    maternity den area.
    [1]
    Beluga
    ,
    bowhead whale
    ,
    harp seal
    ,
    narwhal
    , and
    ringed seal
    frequent the area.
    The island is named for the
    Arctic
    explorer
    Robert Bylot
    , who was the first
    European
    to sight it in 1616.
    [2]
    The whaling captain William Adams was the first to prove the island's insular nature in 1872.
    [3]
    In the 2000s, Baffinland Iron Mines Corporation, began to develop a
    tote road
    from its Mary River Mine, and harbour infrastructure in
    Milne Bay
    —a small, shallow arm of at the confluence of Eclipse Sound and Navy Board Inlet which separates Bylot Island from
    Baffin Island
    .
    [4]
    [5]
    Milne Inlet flows in a southerly direction from Navy Board Inlet at the confluence of Eclipse Sound.