3447 Nanaimo harbour and Departure Bay CHS chart update
82 updated charts for Canada :
- 1312 LAC SAINT-PIERRE
- 1313 BATISCAN AUTO LAC SAINT-PIERRE
- 1317 SAULT-AU-COCHON TO QUEBEC
- 1350A SOREL - TRACY TO RUISSEAU LAHAISE
- 1350B RUISSEAU LAHAISE TO SAINT-ANTOINE-SUR-RICHELIEU
- 1350C SAINT-ANTOINE-SUR-RICHELIEU TO ILE AUX CERFS
- 1350D ILE AUX CERFS TO OTTERBURN PARK
- 1509A RIVIERE DES PRAIRIES ILE BIZARD TO PONT-VIAU
- 1509B RIVIERE DES PRAIRIES PONT-VIAU TO ILE BOURDON
- 2042 WELLAND CANAL ST.CATHERINES TO PORT COLBORNE
- 2318 HERON BAY
- 3053A SHUSWAP LAKE CHASE TO ANGLEMONT
- 3053B SHUSWAP LAKE SALMON ARM TO SEYMOUR ARM
- 3441 HARO STRAIT BOUNDARY PASS AND SATELLITE CHANNEL
- 3447 NANAIMO HARBOUR AND DEPARTURE BAY
- 3463 STRAIT OF GEORGIA SOUTHERN PORTION
- 3477 BEDWELL HARBOUR TO GEORGESON PASSAGE
- 3478 PLANS SALTSPRING ISLAND
- 3479 APPROACHES TO SIDNEY
- 3492 ROBERTS BANK
- 3526 HOWE SOUND
- 3527 BAYNES SOUND
- 3602 APPROACHES TO JUAN DE FUCA STRAIT
- 3603 UCLUELET INLET TO NOOTKA SOUND
- 3902 HECATE STRAIT
- 4002 GOLFE DU SAINT-LAURENT GULF OF ST. LAWRENCE
- 4012 YARMOUTH TO HALIFAX
- 4013 HALIFAX TO SYDNEY
- 4015 SYDNEY TO SAINT-PIERRE
- 4022 CABOT STRAIT AND APPROACHES
- 4023 NORTHUMBERLAND STRAIT
- 4047 ST PIERRE BANK TO WHALE BANK
- 4115 PASSAMAQUODDY BAY AND ST CROIX RIVER
- 4116 APPROACHES TO SAINT JOHN
- 4202 HALIFAX HARBOUR POINT PLEASANT TO BEDFORD BASIN
- 4233 CAPE CANSO TO COUNTRY ISLAND
- 4235 BARREN ISLAND TO TAYLORS HEAD
- 4237 APPROACHES TO APPROCHES DE HALIFAX HARBOUR
- 4275 ST. PETERS BAY
- 4307 CANSO HARBOUR TO STRAIT OF CANSO
- 4320 EGG ISLAND TO WEST IRONBOUND ISLAND
- 4321 CAPE CANSO TO LISCOMB ISLAND
- 4328 LUNENBURG BAY
- 4335 STRAIT OF CANSO AND APPROACHES
- 4363 CAPE SMOKEY TO ST PAUL ISLAND
- 4384 PEARL ISLAND TO CAPE LA HAVE
- 4385 CHEBUCTO HEAD TO BETTY ISLAND
- 4399 PARRSBORO HARBOUR AND APPROACHES
- 4405 PICTOU ISLAND TO TRYON SHOALS
- 4447 POMQUET AND TRACADIE HARBOURS
- 4450 SAINT PAUL ISLAND
- 4462 ST. GEORGE'S BAY
- 4491 MALPEQUE BAY
- 4497 AMET SOUND
- 4498 PUGWASH HARBOUR AND APPROACHES
- 4521 BAIE VERTE
- 4593 SUNDAY COVE ISLAND TO THIMBLE TICKLES
- 4615 HARBOURS IN PLACENTIA BAY PETIT FORTE TO BROAD COVE
- 4616 BURIN INLET AND APPROACHES
- 4625 BURIN PENINSULA TO SAINT-PIERRE
- 4641 PORT AUX BASQUES AND APPROACHES
- 4724 TICORALAK ISLAND TO CARRINGTON ISLAND
- 4820 CAPE FREELS TO EXPLOITS ISLANDS
- 4821 WHITE BAY AND NOTRE DAME BAY
- 4826 BURGEO TO FRANCOIS
- 4831 FORTUNE BAY NORTHERN PORTION
- 4839 HEAD OFFOND DE PLACENTIA BAY
- 4849 PLANS CONCEPTION BAY
- 4850 CAPE ST FRANCIS TO BACCALIEU ISLAND / HEART'S CONTENT
- 4851 TRINITY BAY - SOUTHERN PORTION
- 4854 CATALINA HARBOUR TO INNER GOOSEBERRY ISLANDS
- 4855 BONAVISTA BAY SOUTHERN PORTION
- 4862 CARMANVILLE TO BACALHAO ISLAND AND FOGO
- 4863 BACALHAO ISLAND TO BLACK ISLAND
- 4864 BACK ISLAND TO LITTLE DENIER ISLAND
- 4913 CARAQUET HARBOUR BAIE DE SHIPPEGAN AND MISCOU HARBOUR
- 4920 CHALEUR BAY SOUTH SHORE
- 4956 CAP-AUX-MEULES
- 5138 SANDWICH BAY
- 6023 LAKE OF BAYS
- 7122 CULBERTSON ISLAND TO KOOJESSE INLET
- 8048 CAPE HARRISON TO ST MICHAEL BAY
So 757 CHS charts (1614 including sub-charts) are viewable in the Marine GeoGarage.
Note : don't forget to visit 'Notices to Mariners' published monthly and available from the Canadian Coast Guard both online or through a free hardcopy subscription service.
This essential publication provides the latest information on changes to the aids to navigation system, as well as updates from CHS regarding CHS charts and publications.
New map NZ5219, Approaches to Marsden Point - 1:50000 The entire catalogue of raster charts from Linz has been updated in the Marine GeoGarage.
The 10 following charts have been updated :and some charts have been added :- NZ5219 Approaches to Marsden Point
So the NZ layer is composed of 321 charts (including sub-charts) right now.
Note : don't forget to visit the New Zealand Notices to Mariners (NTMs)
From Steve Szkotak, The Associated Press
A team of scientists will launch an expedition to the Titanic next month to assess the deteriorating condition of the world's most famous shipwreck and create a detailed three-dimensional map that will “virtually raise the Titanic” for the public.
The expedition to the site four kilometres beneath the North Atlantic is billed as the most advanced scientific mission to the Titanic wreck since its discovery 25 years ago.
(Titanic position in the Marine GeoGarage)
The 20-day expedition is to leave St. John's, Newfoundland, on Aug. 18 under a partnership between RMS Titanic Inc., which has exclusive salvage rights to the wreck, and the Woods Hole Oceanographic Institution in Massachusetts. The expedition will not collect artifacts but will probe a 3-by-5 kilometre debris field where hundreds of thousands of artifacts remain scattered.
Some of the world's most frequent visitors to the site will be part of the expedition along with a who's who of underwater scientists and organizations such as the National Oceanic and Atmospheric Administration.
Organizers say the new scientific data and images will ultimately will be accessible to the public.
“For the first time, we're really going to treat it as an archaeological site with two things in mind,” David Gallo, an expedition leader and Woods Hole scientist, told The Associated Press on Monday. “One is to preserve the legacy of the ship by enhancing the story of the Titanic itself. The second part is to really understand what the state of the ship is.”
The Titanic struck ice and sank on its maiden voyage in international waters on April 15, 1912, leaving 1,522 people dead.
Since oceanographer Robert Ballard and an international team discovered the Titanic in 1985, most of the expeditions have either been to photograph the wreck or gather thousands of artifacts, like fine china, shoes and ship fittings. “Titanic” director James Cameron has also led teams to the wreck to record the bow and the stern, which separated during the sinking and now lie one-third of a mile apart.
RMS Titanic made the last expedition to the site in 2004. The company, a subsidiary of Premier Exhibitions Inc. of Atlanta, conducts traveling displays of the Titanic artifacts, which the company says have been viewed by tens of millions of people worldwide.
“We believe there's still a number of really exciting mysteries to be discovered at the wreck site,” said Chris Davino, president of and CEO of Premier Exhibitions and RMS Titanic. “It's our contention that substantial portions of the wreck site have never really been properly studied.”
The “dream team” of archaeologists, oceanographers and other scientists want to get the best assessment yet on the two main sections of the ship, which have been subjected to fierce deep-ocean currents, salt water and intense pressure.
Mr. Gallo said while the rate of Titanic's deterioration is not known, the expedition approaches the mission with a sense of urgency.
“We see places where it looks like the upper decks are getting thin, the walls are thin, the ceilings may be collapsing a bit,” he said. “We hear all these anecdotal things about the ship is rusting away, it's collapsing on itself. No one really knows.”
The expedition will use imaging technology and sonar devices that never have been used before on the Titanic wreck and to probe nearly a century of sediment in the debris field to seek a full inventory of the ship's artifacts.
“We're actually treating it like a crime scene,” Mr. Gallo said. “We want to know what's out there in that debris field, what the stern and the bow are looking like.”
“Never before have we had the scientific and technological means to discover so much of an expedition to Titanic,” said P.H. Nargeolet, who is co-leading the expedition. He has made more than 30 dives to the wreck.
Bill Lange, a Woods Hole scientist who will lead the optical survey and will be one of the first to visit the wreck, said a key analysis will be comparing images from the first expedition 25 years ago and new images to measure decay and erosion.
“We're going to see things we haven't seen before. That's a given,” he said. “The technology has really evolved in the last 25 years.”
“I'm sure there will be future expeditions because this is the just the beginning of a whole new era of these kind of expeditions to Titanic – serious, archaeological mapping expeditions,” Mr. Gallo said.
Geo link to the Marine GeoGarage
If you need to send the display of a specific area containing the nautical map at the scale of your choice :
- move the cursor of the mouse to the left bottom corner of the map
- a small window appears (show in red above)
- click once on the first line (Link) to copy and paste the html address for sending this link via Email or Instant Messaging (IM)
For 'Public' layers (NOAA US, Linz NZ, DHN Brazil ), select at first the chart layer, and this one will be automatically recorded in the Marine GeoGarage link.
Ex.: Fort Lauderdale, Bahia Mar Yacht Club
http://marine.geogarage.com/routes?anonmap=eyJtdCI6MSwicG9zIjp7ImxsIjoiMjYuMTEzMTgsLTgwLjEwNjU1IiwieiI6MTd9LCJvIjp7Ijk1MyI6eyJ0Ijo2OX19fQ==
For 'Private' chart layers (UKHO, CHS Canada, SHN Argentina) , you need to be registered with 'Chart Premium' access
Ex. : Bassin Louise, Quebec (
to view the above CHS chart)http://marine.geogarage.com/routes?anonmap=eyJtdCI6MSwicG9zIjp7ImxsIjoiNDYuODIwNDYsLTcxLjE5OTM5IiwieiI6MTZ9LCJvIjp7IjEwN2EiOnsidCI6NTh9fX0=
Note : you can eventually use the service of some URL shortening services (bit.ly ...) in order to insert your Marine GeoGarage link in a short form for Twitter
Ex. : http://bit.ly/doluXW / http://bit.ly/aV47Zk tied to the above examples
NOAA chart of the Yukon-Alaska border
CHS chart of the Yukon-Alaska border From VancouverSun
Canadian and U.S. government experts met quietly in Ottawa last week to begin trying to resolve a long-standing boundary dispute in the Beaufort Sea, a Canadian diplomat revealed Monday.
News of the surprise talks was disclosed during a briefing by Canadian and U.S. officials on a bi-national seabed mapping mission to be conducted next month in the Beaufort region.
This summer's joint Canada-U.S. survey, the third consecutive year in which researchers from the two countries have agreed to collaborate on mapping the Beaufort sea floor, will also include a sonar probe of the contested area itself for the first time.
The Ottawa talks on the Beaufort controversy, held July 22, followed a pledge earlier this year by Foreign Affairs Minister Lawrence Cannon that Canada intends to actively pursue an agreement with the U.S. over where the maritime boundary should be drawn in an unresolved, Lake Ontario-sized section of the Arctic Ocean north of the Yukon-Alaska border.
Allison Saunders, deputy director of the continental shelf division at the Department of Foreign Affairs, said the gathered specialists in international law, hydrography and other fields had a productive discussion on the technical aspect related to the boundary and that a second meeting has been scheduled to take place in Washington next year.
Beginning Aug. 2, scientists aboard the U.S. Coast Guard cutter Healy and the Canadian Coast Guard icebreaker Louis S. St-Laurent will co-operate in a 42-day mission aimed at generating seabed data across a wide swath of the southern, central and northern Beaufort Sea.
The information is intended to help the two countries prepare their respective claims under a UN treaty for extended authority over submerged territory as well as potential petroleum deposits and other seabed resources.
Canada's submission to the UN agency on continental shelves is due in 2013.
Until now, the two countries have avoided conducting survey work in the disputed zone in the southern Beaufort.
But the federal scientist leading Canada's offshore mapping mission, Natural Resources Canada geologist Jacob Verhoef, said Monday that mapping within the contested area has become necessary to complete each country's broader claims for undersea territory beyond the Beaufort's southern waters.
To secure extensions to their authority over extended stretches of undersea territory, countries must prove that clear geological connections exist between the continental mainland and adjacent stretches of sea floor.
Historically, the key area of dispute was a triangle-shaped, 21,500-sq.-km section of the Beaufort Sea close to the Yukon-Alaska shore. But the joint Canada-U.S. seabed surveys in 2008 and 2009 showed each country's claims could extend much farther toward the North Pole than previously imagined, doubling or even tripling the ultimate size of the dispute zone once continental shelf submissions are made.
The two countries have disagreed since the 1970s over where to draw the ocean border. It's a conflict that flares whenever fisheries management, oil-and-gas exploration or other resource development issues arise in the region.
Canada's position is based on an 1825 treaty between Russian and Britain that was transferred to the U.S. and Canada when the two countries acquired Alaska and the Yukon respectively in the latter half of the 19th century.
That treaty suggests the Beaufort Sea maritime boundary is an extension of the arrow-straight land border between Yukon and Alaska, which follows the 141st meridian.
The U.S. argues the offshore boundary is defined by an "equidistance" principle: the demarcation line at any point is drawn halfway between each country's nearest stretch of coastline.
But because the two countries are working to expand their seabed domains in the central and northern Beaufort — also potential petroleum targets — an area much larger than the traditional dispute zone is coming into play.
Under the U.S. formula for determining the maritime boundary, the looming presence of Canada's Banks Island on the Beaufort's eastern side radically alters where the border between the two countries would be drawn in areas farther out to sea.
According to the U.S. position, Alaska's northward-sloping coastline means the sea's southern maritime boundary veers slightly eastward of the Yukon-Alaska land boundary, giving the U.S. a greater amount of marine jurisdiction.
But the overlap in the northerly expanse of the Beaufort would be much larger and reversed, with the boundary under the U.S. formula swinging far to the west because of Banks Island, giving Canada a greater share of the potentially resource-rich seabed.
Meanwhile, Canada's longitude-line formula for determining the boundary would give the U.S. more seabed territory in the outer Beaufort.
Canada also recently began talks with Denmark to try to resolve an offshore territorial dispute in the eastern Arctic Ocean.
In March, Canwest News Service revealed that the two countries were now actively working to end a decades-old disagreement over a 200-square-kilometre section of the Lincoln Sea, north of Canada's Ellesmere Island and Danish-controlled Greenland.