LNG Partners LLC, of Houston, one of the backers of Douglas Channel Energy, the BC LNG Douglas Channel Project, a partnership between LNG firms and the Haisla Nation, has signed a preliminary deal with Golar LNG for two tankers.
On October 10, Golar entered into a 90 day Vessel Charter Option Agreement with LNG Partners LLC (Houston, TX) for the provision of two newbuild LNG carriers under long term contract to deliver LNG production from the Douglas Channel LNG Project in British Columbia (BC), Canada.
The Douglas Channel Project, in which LNG Partners is an equity owner, is a proposed liquefaction facility on the west bank of the Douglas Channel, within the district of Kitimat, BC. In addition to prospectively providing two vessels, the agreement confers certain preferential rights for Golar to participate in the project with LNG Partners LLC by way of infrastructure investment or LNG offtake.
In the same report, Golar LNG reported operating income of $70.2 million for the third quarter of 2012, an increase of 21 per cent from the second quarter.
Golar, which has its headquarters in Hamilton, Bermuda, says that since 2001, it has grown from a fleet of six LNG Carriers focused on LNG transportation, to a fleet of 13 vessels (with 13 newbuilds due from quarter three 2013), dedicated to both LNG transportation and midstream floating solutions.
The latter means that Golar is working on what the industry calls Floating Storage & Regasification Units (FSRU). LNG is transferred to the FSRU either for storage or where the low-temperature liquified natural gas is heated back to a gaseous state.
The FSRU storage tanks are generally made from aluminium.
Golar’s report also reflects the weakness in the LNG markets, a factor that is slowing development of the Kitimat LNG projects.
Golar says “a bearish cargo market [for shipping] prevailed in the third quarter with falling prices and weak demand in the Far East. Chartering activity remained thin and lacked direction and consequently, short-term charter rates experienced a correction from rates seen earlier in the year.”
It goes on to say:
Looking to the fourth quarter, weak Far East demand may result in additional vessels being released into the market, however, with limited available modern undedicated vessels a resumption in interest from buyers could very easily pull rates upward again.
As for the world LNG market, Golar says “downward pressure on pricing was experienced primarily due to high inventory levels that persisted East of Suez.”
It also says that more LNG projects are coming onstream which could provide potential competition for Kitimat:
New LNG supply will soon be coming to the market with the commissioning of Angola LNG in the Atlantic Basin. Despite delays at the West African project during the third quarter, exports are expected to start early in the New Year. This represents a set-back of about ten months from the original target date for the country’s first LNG project.
In the Far East, ConocoPhillips and Origin Energy announced the sanctioning of a second train at its Australia Pacific LNG project. The project is planning to bring the first train on late in 2015 with the second train following in 2016. Both trains will be sized at 4.5 million tonnes. Additionally, during the quarter Chevron made positive statements about proceeding with a fourth train at its Gorgon LNG project in Barrow Island, Western Australia. There are currently three trains at Gorgon under construction totalling 15.6 million tonnes.
In addition to Angola, given imminent start-up of the project, supply projects under construction in both the Atlantic and Pacific Basin have reached close to 100 million tonnes, with construction officially beginning at Cheniere’s Sabine Pass LNG export facility.
It was the decision by Cheniere to sell LNG to the Far East markets based on North American prices rather than the higher Japanese price that led to a further delay by Apache earlier this year to give the final go-ahead for the Kitimat LNG project.
A follow up study by the Department of Fisheries and Oceans on the discovery of prehistoric slope failure tsunamis in Douglas Channel concludes that the events would have had minimal impact on Kitimat but would have destroyed Hartley Bay.
The DFO follow up study was aimed at better understanding the dynamics of tsunamis during the two slope failure events on the southern end of Hawkesbury Island during the mid-Holecene period, between 5,000 and10,000 years ago.
The wave dynamic model study does not address the discovery by the Geological Survey of Canada of a possible fault line along Hawkesbury Island which could have been the cause of the slope failures.
The study estimates that the wave amplitude of the first tsunami reaching the proposed Enbridge Northern Gateway terminal site near Kitimat would have been about .09 to .12 metres. Since the actual wave height hitting land from a tsunami is one half of the amplitude, the height of tsunami waves reaching Kitimat at the time would have been about 60 centimetres or 23 inches. At Hartley Bay, on the other hand, the maximum estimated wave amplitude from the second tsunami would have been 15 metres, meaning a wave height of 7.5 metres or about 25 feet.
The main reason for the difference is that both the submarine slope failures occurred south of the dogleg in Douglas Channel at Gertrude Point. That meant the configuration of the channel from Gertrude Point up to Kitimat would lessen the amplitude whereas because Hartley Bay was so close, it would be hit by a higher amplitude. The report says that because of their relatively short wavelengths, the tsunami waves undergo multiple reflections that the “high degree of scattering from the complex shoreline and bottom topography in Douglas Channel” would “combined with the flux of tsunami energy through adjoining waterways and channels” have caused a rapid decrease in the energy of the waves with distance south and north of the slide area.
The study also points out a crucial difference between the ancient slides and the two that occurred near Kitimat in 1974 and 1975, while the land near the head of the Kitimat arm were largely composed of material laid down by the glaciers, the large slope failures on Hawkesbury Island were blocks of an extremely hard igneous rock called diorite. Each of the prehistoric slides would have consisted of about 65 million cubic metres of rock.
The DFO report says
Coastal British Columbia is an area of steep slopes, extreme seasonal variations in soil moisture, large tidal ranges, and the highest seismicity in Canada. Hazards of this form have been well documented for the coastal region of British Columbia, and other fjord regions of the world’s oceans, including Alaska and Norway. These factors increase the potential for both submarine and subaerial slope failures in the region. Such events generally take place in relatively shallow and confined inner coastal waterways, and can present hazards in terms of tsunami wave generation.
The two prehistoric submarine slides are located about 10 kilometres apart on the
slope of southern Douglas Channel, near the southern end of Hawkesbury Island
The report says:
The failures are defined by scallop-shaped hollows located along the edge of the fiord wall and appear to be associated with detached blocks that extend out several hundred metres into the channel. The two block slides identified in Douglas Channel are characteristic of rigid-body submarine landslides, which differ considerably from the well-documented viscous submarine landslides with a lower specific gravity (density relative to water) of about 1.5 that occurred to the north of Douglas Channel along the inner slope of Kitimat Arm in 1974 and 1975.
The report’s modelling is “considered minimum values” because the do not include debris that would have spread into the fiord after initial slide. That debris is now buried by a thick layer of post-slide sediment.
The reconstruction model shows that the head of the more northern slide began at a depth of around 60 to 100 metre, while that of the more southern slide began at a depth of 75 to 120 metres.
The slides would have moved down slope at about 25 metres per second, coming to rest after about 30 seconds, 250 to 350 metres from the slope at a depth of 400 metres.
The northern slide, called by the scientists Slide A:
would have generated extremely large waves in the immediate vicinity of the failure
region within a minute of the submarine landslide. Waves in the numerical simulations reach amplitudes of 30 to 40 metres at the coast near the slide area
Submarine landslides cause delays between the arrival of the first waves and the arrival of subsequent higher waves, increasing in distance from the slide, because of “reflections and non-linear interaction” along the shoreline. For Slide A, the maximum wave amplitudes at Hartley Bay would have been six metres (meaning three metre waves) “Large amplitude waves with typical periods of around 50 seconds would continue for several tens of minutes.”
The leading tsunami waves generated by Slide A reach Kitimat Arm in roughly 20 min and have small amplitudes of only a few centimetres. Although later waves have higher amplitudes, the maximum wave amplitudes (which occur 50-55 minnutes after the failure event) are still only around 0.09 to 0.12 metres.
The southern slide on Hawkesbury, called Slide B by the scientists, would have moved 400 metres before stopping. It stared at a greater depth than Slide A, with not as much vertical displacement than Slide A. That means Slide B was slower than Slide A.
Slide B:
would have generated large waves in the vicinity of the failure region. Simulated waves reach the coast adjacent to the slide region within a minute of the failure event, with wave amplitudes of up to 10 metres. The waves also hit the opposite site of the channel within a minute of the failure event and then take an additional minute to reach Hartley Bay where waves reach amplitudes of 15 metres/ Powerful oscillations in the bay last for tens of minutes.
Waves with high amplitudes (more than 2 metres) also occur in the southern part of Douglas Channel, and in certain locations of Verney Passage.
According to the models, the leading tsunami waves would have reached the Kitimat Arm 22 minutes after the start of the slide. The maximum waves would have had amplitudes of 0.08 metres to 0.3 metres (6 inches), reach the Kitimat Arm 45 to 60 minutes after the start of the failure event.
The the tsunami waves generated by Slide B that impact Kitimat Arm, although still of low amplitude, were somewhat higher than those generated by Slide A, despite the fact that Slide B was located further to the south and generated less energetic waves in the source region than Slide A.
This seeming paradox is explained by the slower motion of Slide B, which causes it to generate more wave energy in the low frequency band…Due to their reduced scattering and reflection, the relatively long and lower frequency waves generated by Slide B propagate more readily through the complex fjord system than the relatively short and higher frequency waves generated by Slide A.
Specifically addressing the proposed site of the Enbridge bitumen terminal, as well as potential tanker traffic in Douglas Channel, the detailed explanation of the modelling accompanying the DFO report says:
If similar submarine slides were to occur again somewhere in the same general area, they could present a significant risk to navigation and to nearby shore installations and coastal communities….
As with the tsunami generation regions, the highest waves and strongest currents in any particular region of the coastal waterway would occur near the shoreline. Based on the numerical findings, tsunamis generated by submarine landslides of the form identified for the southern end of Douglas Channel would have heights and currents that could have major impacts on the coastline and vessel traffic at the time of the event throughout much of Douglas Channel, but a minor impact on water levels, currents and hence vessel traffic in Kitimat Arm. Hartley Bay, at the southern end of Douglas Channel, would be impacted by high waves and strong currents, whereas Kitimat, at the northern end of Kitimat Arm, would experience negligible wave effects. Additional modelling would be required to assess the characteristics of possible tsunamis originating beyond the area of the two identified slope failures.
At the estimated propagation speeds of about 65 metres per second, the detailed model says it takes roughly 10 to 15 minutes for the simulated waves to propagate approximately 40 to 45 kilometres to the intersection of Douglas Channel and Kitimat Arm, where peak wave amplitudes would be diminished to less than one metre. It takes another 15 minutes for the waves to reach sites near the proposed Enbridge facilities in Kitimat Arm where wave amplitudes would be reduced to a few tens of centimetres and associated currents to speeds less than a few tens of centimetres per second.
Kitimat, BC and New York City had one thing in common this week, the misuse and use of social media, Twitter and Facebook, that spread both accurate warnings and dangerous misinformation about an impending disaster. In the case of New York and the surrounding area, it was Superstorm Sandy that caused widespread devastation. For Kitimat it was the tsunami warning after the 7.7 earthquake off Haida Gwaii and no damage but a lot of worry for residents.
New York has a population of millions, it is the media centre for the United States, and much of the U.S. Northeast coast is still recovering from the horrendous damage from Superstorm Sandy.
Kitimat has a population of about 8,000 and my home town is off the media radar except when the Enbridge Northern Gateway pipeline issue pops up on the national assignment desks. If the October 27, 2012 tsunami from the Haida Gwaii earthquake did come up Douglas Channel to Kitimat harbour, it was so minimal that any water rise was scarcely noticed.
In one way New York (the state and the city) plus New Jersey and other states were ahead of Kitimat. In the US, there were numerous official sources on Twitter and Facebook, as well as those ubiquitous live TV news conferences with New York Mayor Michael Bloomberg or various state governors.
On October 27, neither Kitimat nor the nearby town of Terrace had any official emergency outlets on social media. In Kitimat, that may change as early as this Monday when District Council considers what happened last Saturday night.
It has been documented that there was no official response from Emergency Management British Columbia (still largely known under its former name Provincial Emergency Program) until an hour after the first earthquake report from the US Geological Survey. Only sometime later did BC’s provincial emergency officials hold a short conference call with reporters. (At the time the BC Liberals were holding a policy convention at Whistler. After the conference call, TV reporters at the convention in Whistler were doing live reports with taped clips of Attorney General Shirley Bond. It should have been easy for Bond and other senior government officials, including Premier Christy Clark–who is plummeting the polls– to hold a live news conference just as US state governors and mayors did later in the week when it came to Superstorm Sandy)
So in that hour of silence from the BC government, one question that has to be raised is: Were the tsunami warnings so completely uncoordinated–at least as far as the public is concerned– that that was one cause of the misinformation and inaccurate information on Twitter and Facebook? Or did confusing information from authorities simply compound and amplify the social media misinformation that was already spreading across British Columbia and around the world?
Here in the northwest, the two area fire chiefs Trent Bossence of Kitimat and John Klie of Terrace have said after the quake that landline phones and some cell phones were out, in some areas up to an hour after the first shock. Klie told CFTK’s Tyler Noble on Open Connection that after the landline phones came back up the Terrace fire department was flooded with calls from people “who wanted it now.” The ability of firefighters to get information was then delayed “because so many people were trying to get through.”
Kitimat has the advantage of being a small town. Emergency services already had scheduled a volunteer recruiting session last Monday night (October 29) for Emergency Social Services–the folks who run, coordinate and work in reception centres during an emergency–so it was easy to turn that meeting into a earthquake/tsunami warning post mortem. (Imagine that happening in New York?)
The most important issue on Saturday night was the false information on both Facebook and Twitter that the Kildala neighbourhood was being evacuated due to the tsunami warning. Other false information on social media indicated that the giant Bechtel work camp at the Rio Tinto Alcan Kitimat Modernization Project was also being evacuated.
As Kitimat’s Emergency Plan Coordinator Bob McLeod told the earthquake post mortem about the information on Facebook and Twitter:
Kitimat Emergency Coordinator Bob McLeod at the earthquake postmortem Oct. 29, 2012 (Robin Rowland/Northwest Coast Energy News)
“Your aim is to be saving people, and you’re not saving people. There was one case where someone was going around banging on doors in Kildala, telling them to get out. I think it was over when he was in the lockup that night. But this is the type of foolishness that goes on. You have people going on Facebook saying ‘Alcan’s been evacuated. they’re evacuating Kildala.’ I am going to be generous and say it is misinformation… It was a blatant lie. And that does not help.”
(For those outside Kitimat you can check the town on Google maps) As seen on this screen grab, Kildala is a low lying part of town. The area north of Highway 37 is higher on a hill. Closer to the ocean at Douglas Channel are the Bechtel/RTA Kitimat Modernization Project work camps.
After driving from the village to the town, McFarlane told the meeting that he stopped at the town viewpoint where “people were telling me they had already been evacuated out of the Kildala neighbourhood, so my first stop after that was the fire department.” The fire hall is about a couple of blocks from the viewpoint, so it was easy to get accurate information from the fire department.
McFarlane continued, “I found the night of the earthquake that no information is just as bad as wrong information. People were calling me on my cell saying why does the Kitimat Daily say we have to evacuate.” That is because the Daily republished a warning from the Pacific Tsunami Warning Centre that “said tsunami warning, evacuation for the north coast. People were saying we’re on the north coast, we got to go.”
I was about fifteen to twenty minutes behind McFarlane in reaching town. (I did not leave Kitamaat Village until after we heard the first tsunami warning.) As soon as I got to back in cell range, my cell phone started to beep with saved messages from my TV and radio news clients calling for information. When I got to my home office, my landline was still dead and would be for about another twenty minutes. The only source of information at that point was Google News, Facebook and Twitter.
I saw the initial, and it turns out general, warning from the Pacific Tsunami Warning Center. Soon I was also getting what I hoped was more specific information on my marine radio from the Canadian Coast Guard Prince Rupert communications station.
But that, too was somewhat confusing. That Coast Guard advisory mentioned various zones, for example, Zone A and Zone B, but there was little specific context and that point I had no idea what Zone A meant. Prince Rupert Coast Guard Radio then went on to say evacuate low lying coastal areas. (transcript below)
With that confusion, and mindful of “when in doubt, leave it out,” I did not mention the zone system in any information I posted on Facebook and Twitter that night. I only retweeted official information or tweets from reporters I knew and trusted (and I did not see any tweeted official information from the province with a link to the page that identifies the official tsunami zones)
From the interview on CFTK, it appears that both the Kitimat and Terrace fire departments were also getting inadequate information.
“We went to our normal place to look EM BC (Emergency Management BC) and there was nothing there,so we went to Plan B to get information and went on from there,” Bossence told Tyler Noble.
Klie said: “We struggle with that every disaster big or small. Social media, I think emergency organizations are trying to tap into more and more. Up north we may be a little behind the eight ball but sure enough Twitter and Facebook information is out there instantly. Looking at Facebook with my son, I saw that they were evacuating whole cities and I knew that was not true. Because of my experience I can filter some of the information, but there is so much information out there that it’s hard to filter what’s real and not real. It’s an area where emergency coordinators have to get into because its the fastest way of getting information out.”
“Once the phone system came back online at the Fire Hall we got a flood of phone calls,” Bossence told CFTK, “it was nonstop and it was people wanting to know. ‘What’s going on? What are we going to do? Are we leaving?’ and they’re giving us ‘This is what is what I’m reading, this is what I’m being texted, on Facebook they’re saying we’re supposed to evacuate’ adding to that we had an individual going around claiming he was a fire department, he was going door to door and telling people to evacuate. That was the added issue we had to deal with. It was definitely misinformation and a sense of urgency that was coming out through the social network (and eventually the media) was big problem for us.”
In Kitimat, I was told about the man going door to door with inaccurate information and as soon as I confirmed it with reliable official sources, I posted that on both Twitter and Facebook, emphasizing there was, at that time, no evacuation order.
But every situation is different. In contrast, in Superstorm Sandy, another story about men going door to door in Williamsburg, a section of Brooklyn was not true, as can be seen in an article summing problems with Twitter in New York, where Jared Keller of Bloomberg reported
I experienced this firsthand during Hurricane Sandy. After retweeting a message warning about muggers in Williamsburg dressed as Con Ed workers as an experiment, I received two sceptical responses checking the claim within 15 minutes, both from people who work in the media industry and spend a significant amount of time on Twitter. Within an hour, I received a mass text message from friends of mine who aren’t completely plugged into the social Web with the same warning: “I just read a news alert of two separate reports of people posing as coned workers, knocking on people’s door and robbing them at gunpoint in Williamsburg. I just want to pass along the info. Stay safe and maybe don’t answer your door.” Two other friends responded with thanks.
Keller goes on to stay “I know a lot of people, especially on Facebook, who end up believing whatever they see first,” says Kate Gardiner, a social media journalist. “It’s almost impossible to track something back to its point of origin there.”
With the earthquake and tsunami warning Saturday night, Twitter misinformation spread internationally. The first hashtag I saw was #bcquake, but as the the tsunami warning gained traction (especially after the warning was extended from BC and Alaska to Washington, Oregon and California and then to Hawaii) the more common hashtag #tsunami became prominent. As people outside BC began tweeting, they began using #Canadaquake and soon #prayforcanada also began to trend. Completely inaccurate information spread on #prayforcanada (believed to have originated in Indonesia) that it was Vancouver, not the north coast that had been hit by the 7.7 magnitude earthquake.
Are you in the Zone?
At this point, one question has to be asked. The spread of information, first the well-intended but wrong, second just rumour and third, the deliberately misleading, has been seen in social media not only during the earthquake and tsunami on the West Coast last weekend, and during Superstorm Sandy on the East Coast but all the way back to the 2004 Christmas tsunami in Southeast Asia.
For the west coast in 2012, however, how much of the problem of misinformation on social media during the earthquake and tsunami warning was the fault of confusing information from the authorities? Just how were people going to interpret such general terms as “north coast” and “low lying areas.”?
From the BC Provincial Emergency Program you have to ask “What is Zone A?” It turns out by checking a day or so later that the province of British Columbia has created Tsunami Identification Zones.
Before October 27, it is likely no one outside of the provincial bureaucracy had ever heard of the provincial tsunami zones. At that time no one in BC, either on Twitter or Facebook or through the media was identifying the BC Tsunami Zones for the public. Later on, the television networks put up maps showing Zones A and B —but that was only good if you had power and were watching the right channel. Kitimat Daily and Terrace Daily posted an official update at 10:42 long after the danger was past explaining the Zone system. It was no good at all if you were listening to news reports on radio or to Prince Rupert Coast Guard Radio on a fishing boat and had no access to the actual maps.
Compounding the confusion is that the US system appears to be very different from the Canadian.
Also the US system has two levels of warning. The Pacific Tsunami Warning Center sends out general warnings but hands over for a more specific warning map from the Alaska -based West Coast and Alaska Pacific Tsunami warning centre. It uses its own system of lettered and numbered zones for the west coast of North America. (See the Oct 27 tsunami advisory here Note it is a Google maps plugin.)
Fisheries management zones as defined by the Department of Fisheries and Oceams (DFO)
So in case of a tsunami warning, Kitimat is in Zone B for the province of British Columbia and the Provincial Emergency Program and in Zone BZ921 for the West Coast and Alaska Tsunami Warning Centre. For the much more familiar fisheries management areas Kitimat is in Zone 6 (which of course has nothing to do with a tsunami, it’s simply the coastal zone system everyone is familiar with)
Adding to the confusion is the fact that the EM British Columbia map shows Terrace, far inland up the Skeena River is considered in Zone A, along with Prince Rupert for tsunami warnings (if a tsunami was big enough to reach Terrace along the Skeena River valley, then I can only assume that much of the west coast of North America would have already been wiped out).
The Monday Post mortem
At the Monday, October 29 post mortem, when McLeod outlined the events of October 27, he began by looking back three weeks, saying, “I have feeling of frustration about a couple of things. October 7, I took 4,000 brochures [How Prepared Are you if Disaster Strikes?] down to the post office to mail out to the residents of Kitimat, They were all delivered by the post office. On Sunday, I had people coming to me and saying what are we supposed to do in the case of an earthquake? It is really, really difficult to get people interested.”
McLeod said that after he felt the earthquake, he went online to check information and then went up to the fire hall, which is Kitimat’s emergency coordination centre. There he met Fire Chief Bossence, his deputy, the RCMP detachment commander Staff Sergeant Steve Corp and representatives from Bechtel and the Rio Tinto Alcan modernization project.
“For the first little while we were going on line trying to get information. The usual method of dissemination getting information it comes from the West coast and Alaska tsunami warning system, then it goes to Victoria, Victoria gives it to the geophysical specialists and they will confirm or deny what ever the information and then it goes to the Provincial Emergency Program and they shoot it out to coastal communities.
“While in this case you’re working with what you find out from different sources and you are trying to determine how reliable these sources are.”
“In our case, for me the first thing you do when you get word of an impending tidal wave [tsunami] action is check the tide. If you’re on a high tide, it’s a different situation than a low tide
“The movie version of a tidal wave is this 50 foot mountain of water roaring along and this is not what is going to happen particularly in Douglas Channel because of the depth. So you are going to see a surge such as we saw in Japan and it will be an increasing surge of water.
“We were told that potentially some sort of surge hitting Langara [the northern most island in Haida Gwaii) at 9:16, 9:16 came and went and there was no notification of a noticeable surge of water. So were down to a non event and we were on a receding tide.” (See advisory below)
“Misinformation going out is not helpful,” McLeod said. “You’ve got to set up a stream of how you get information out to people and it’s a valid point. The District Website, the Facebook page, something like that can get information out. But again if you lose power where do get it? Text can work even locally with cell phones. if you’re in a dead area with a cell phone, you can still get text”
McLeod then asked the audience, mainly people ranging from their thirties to seventies if they text. Only four or five people put up their hands. “You people are going to be saved, the rest of us…” McLeod quipped.
If a conclusion can be drawn from the earthquake and tsunami warning in the Kitimat region on October 27, it’s not just that in an emergency inaccurate, incomplete or malicious information can spread a the speed of light on social media, it’s worse that incomplete, inadequate and confusing information from the authorities is amplified and distorted by rapid posting on social media. That concept is not new for anyone who has tried the phone chain game where the outcome is often completely different from the start.
If Gardiner is correct when she says “I know a lot of people, especially on Facebook, who end up believing whatever they see first,” the BC government delays made everything worse. People Tweeted the first thing they saw and the first thing people saw came from multiple and often conflicting sources. Add that to those Tweets that were exaggeration, rumour and lies.
The problem in 2012 it is not one person talking to one person talking to one person, it is a Tweet or Facebook posting that go out to thousands, or millions of people and that’s a lot more dangerous.
McLeod said the post mortem who said emergency services is trying to get more information out to public, but he added. “The unfortunate part is that if you publish it this week, by Christmas no one will remember. If you start throwing it out every week, it becomes like a stop sign at the end of the street. Nobody sees it.”
(Coming next. If Kitimat had to evacuate)
Transcript of Prince Rupert Coast Guard Radio tsunami warning.
Pan pan. Pan pan. This is Prince Rupert Coast Guard Radio, Prince Rupert Coast Guard Radio. Warning for coastal British Columbia issued by Environment Canada on behalf of the British Columbia Provincial Emergency Program at 2057 Pacific Daylight Time Saturday 27 October. Tsunami warning for Zone A, the north coast and Haida Gwaii,Zone B, the central coast and including Bella Coola, Bella Bella and (unintelligible). A tsunami warning has been issued, if you are in a low-lying area coastal area, you are at risk and must move to higher ground or inland now.
Do not return until directed to do so. Closely monitor local radio stations for additional information from local authorities. Please minimize phone use in affected areas, for further information contact the provincial emergency program at website www. papa echo papa period bravo charlie period charlie alpha.Prince Rupert Coast Guard Radio over.
TSUNAMI BULLETIN NUMBER 003
PACIFIC TSUNAMI WARNING CENTER/NOAA/NWS
ISSUED AT 0341Z 28 OCT 2012
THIS BULLETIN APPLIES TO AREAS WITHIN AND BORDERING THE PACIFIC
OCEAN AND ADJACENT SEAS…EXCEPT ALASKA…BRITISH COLUMBIA…
WASHINGTON…OREGON AND CALIFORNIA.
… TSUNAMI INFORMATION BULLETIN …
THIS BULLETIN IS FOR INFORMATION ONLY.
THIS BULLETIN IS ISSUED AS ADVICE TO GOVERNMENT AGENCIES. ONLY
NATIONAL AND LOCAL GOVERNMENT AGENCIES HAVE THE AUTHORITY TO MAKE
DECISIONS REGARDING THE OFFICIAL STATE OF ALERT IN THEIR AREA AND
ANY ACTIONS TO BE TAKEN IN RESPONSE.
AN EARTHQUAKE HAS OCCURRED WITH THESE PRELIMINARY PARAMETERS
ORIGIN TIME – 0304Z 28 OCT 2012
COORDINATES – 52.9 NORTH 131.9 WEST
DEPTH – 10 KM
LOCATION – QUEEN CHARLOTTE ISLANDS REGION
MAGNITUDE – 7.7
EVALUATION
NO DESTRUCTIVE WIDESPREAD TSUNAMI THREAT EXISTS BASED ON
HISTORICAL EARTHQUAKE AND TSUNAMI DATA.
HOWEVER – THE WEST COAST/ALASKA TSUNAMI WARNING CENTER HAS
ISSUED A REGIONAL WARNING FOR COASTS LOCATED NEAR THE EARTHQUAKE.
THIS CENTER WILL CONTINUE TO MONITOR THE SITUATION BUT DOES NOT
EXPECT A WIDER THREAT TO OCCUR.
THIS WILL BE THE ONLY BULLETIN ISSUED FOR THIS EVENT UNLESS
ADDITIONAL INFORMATION BECOMES AVAILABLE.
THE WEST COAST/ALASKA TSUNAMI WARNING CENTER WILL ISSUE PRODUCTS
FOR ALASKA…BRITISH COLUMBIA…WASHINGTON…OREGON…CALIFORNIA.
BULLETIN
PUBLIC TSUNAMI MESSAGE NUMBER 2
NWS WEST COAST/ALASKA TSUNAMI WARNING CENTER PALMER AK
834 PM PDT SAT OCT 27 2012
THE MAGNITUDE IS UPDATED TO 7.7. THE WARNING ZONE REMAINS THE
SAME.
…THE TSUNAMI WARNING CONTINUES IN EFFECT FOR THE COASTAL
AREAS OF BRITISH COLUMBIA AND ALASKA FROM THE NORTH TIP OF
VANCOUVER ISLAND BRITISH COLUMBIA TO CAPE DECISION
ALASKA/LOCATED 85 MILES SE OF SITKA/…
…THIS MESSAGE IS INFORMATION ONLY FOR COASTAL AREAS OF
CALIFORNIA – OREGON – WASHINGTON AND BRITISH COLUMBIA FROM
THE CALIFORNIA-MEXICO BORDER TO THE NORTH TIP OF VANCOUVER
ISLAND BRITISH COLUMBIA…
…THIS MESSAGE IS INFORMATION ONLY FOR COASTAL AREAS OF
ALASKA FROM CAPE DECISION ALASKA/LOCATED 85 MILES SE OF
SITKA/ TO ATTU ALASKA…
A TSUNAMI WARNING MEANS… ALL COASTAL RESIDENTS IN THE WARNING
AREA WHO ARE NEAR THE BEACH OR IN LOW-LYING REGIONS SHOULD MOVE
IMMEDIATELY INLAND TO HIGHER GROUND AND AWAY FROM ALL HARBORS AND
INLETS INCLUDING THOSE SHELTERED DIRECTLY FROM THE SEA. THOSE
FEELING THE EARTH SHAKE… SEEING UNUSUAL WAVE ACTION… OR THE
WATER LEVEL RISING OR RECEDING MAY HAVE ONLY A FEW MINUTES BEFORE
THE TSUNAMI ARRIVAL AND SHOULD MOVE IMMEDIATELY. HOMES AND
SMALL BUILDINGS ARE NOT DESIGNED TO WITHSTAND TSUNAMI IMPACTS.
DO NOT STAY IN THESE STRUCTURES.
ALL RESIDENTS WITHIN THE WARNED AREA SHOULD BE ALERT FOR
INSTRUCTIONS BROADCAST FROM THEIR LOCAL CIVIL AUTHORITIES.
EARTHQUAKES OF THIS SIZE ARE KNOWN TO GENERATE TSUNAMIS.
AT 804 PM PACIFIC DAYLIGHT TIME ON OCTOBER 27 AN EARTHQUAKE WITH
PRELIMINARY MAGNITUDE 7.7 OCCURRED 25 MILES/40 KM SOUTH OF
SANDSPIT BRITISH COLUMBIA.
EARTHQUAKES OF THIS SIZE ARE KNOWN TO GENERATE TSUNAMIS.
IF A TSUNAMI HAS BEEN GENERATED THE WAVES WILL FIRST REACH
LANGARA ISLAND BRITISH COLUMBIA AT 916 PM PDT ON OCTOBER 27.
ESTIMATED TSUNAMI ARRIVAL TIMES AND MAPS ALONG WITH SAFETY RULES
AND OTHER INFORMATION CAN BE FOUND ON THE WEB SITE
WCATWC.ARH.NOAA.GOV.
TSUNAMIS CAN BE DANGEROUS WAVES THAT ARE NOT SURVIVABLE. WAVE
HEIGHTS ARE AMPLIFIED BY IRREGULAR SHORELINE AND ARE DIFFICULT TO
FORECAST. TSUNAMIS OFTEN APPEAR AS A STRONG SURGE AND MAY BE
PRECEDED BY A RECEDING WATER LEVEL. MARINERS IN WATER DEEPER
THAN 600 FEET SHOULD NOT BE AFFECTED BY A TSUNAMI. WAVE HEIGHTS
WILL INCREASE RAPIDLY AS WATER SHALLOWS. TSUNAMIS ARE A SERIES OF
OCEAN WAVES WHICH CAN BE DANGEROUS FOR SEVERAL HOURS AFTER THE
INITIAL WAVE ARRIVAL. DO NOT RETURN TO EVACUATED AREAS UNTIL AN
ALL CLEAR IS GIVEN BY LOCAL CIVIL AUTHORITIES.
PACIFIC COASTAL REGIONS OUTSIDE CALIFORNIA/ OREGON/ WASHINGTON/
BRITISH COLUMBIA AND ALASKA SHOULD REFER TO THE PACIFIC TSUNAMI
WARNING CENTER MESSAGES FOR INFORMATION ON THIS EVENT AT
PTWC.WEATHER.GOV.
THIS MESSAGE WILL BE UPDATED IN 30 MINUTES OR SOONER IF
THE SITUATION WARRANTS. THE TSUNAMI MESSAGE WILL REMAIN
IN EFFECT UNTIL FURTHER NOTICE. FOR FURTHER INFORMATION STAY TUNED
TO NOAA WEATHER RADIO… YOUR LOCAL TV OR RADIO STATIONS… OR SEE
THE WEB SITE WCATWC.ARH.NOAA.GOV.
$$
Did the media over react to the earthquake and tsunami warning?
There were also numerous Tweets on October 27, accusing the media of over reacting. The Haida Gwaii quake was 7.7 magnitude. Compare that to the Haiti earthquake on January 12, 2010 which was 7.0. The Christ Church, New Zealand earthquake on February 27, 2011 which caused major damage was 6.3 magnitude. So the Haida Gwaii earthquake was a major event. The tsunami warning that eventually reached as far off as Hawaii had to be taken seriously.
Fortunately Haida Gwaii is sparsely populated and there was minimal damage largely because most of the houses and buildings are wood and can absorb some of the shaking from an earthquake.
Given the tsunami damage in Southeast Asia in 2004 and in Japan in 2011, no media organization could ignore the developing story.
If there is justifiable criticism, it is that some media over hyped the story in the beginning, rather acting to reassure the public in a responsible manner. But the media that over hyped the earthquake and tsunami are the kind that would over hype any story. That is generally the result of management listening to “TV doctors” and media consultants who urge over hyping to increase ratings. (It often works). But those who, quite early in the event, who tweeted that the media was overreacting, were themselves guilty of overreaction in their Tweets.
The Northern Gateway Joint Review panel has allowed the Department of Fisheries and Oceans and Natural Resources Canada to delay a report on historic tsunamis and a possible fault line on Douglas Channel until November 16, 2012.
The report was scheduled for release on October 31.
In a ruling released by the JRP on November 1, the panel noted:
In Ruling no. 105 dated 24 September 2012, the Panel stated that the Department of Fisheries and Oceans (DFO) could provide “modelling of the potential wave heights and speeds that may have resulted from two previously unrecognized submarine slope failures in the Douglas Channel” (Modelling) and that it should do so by 31 October 2012. The letter from Justice Canada seeks an extension to 16 November 2012 as DFO “requires additional time to complete the peer review and approval processes related to this additional written evidence.”
The Panel believes the Modelling to be relevant, as noted in Ruling no. 105. The Panel is also ofthe view that there is unlikely to be any undue prejudice to any party by permitting its filing to be delayed to 16 November 2012.
Accordingly, the Federal Government Participants’ motion is granted and DFO is permitted to file the Modelling on or before 16 November 2012
The Department of Justice filed the request with the JRP on Monday Oct. 30, 2012, less than 48 hours after a major earthquake of magnitude 7.7 struck off Haida Gwaii just after 8 p.m. Pacific Daylight Time, on Saturday Oct. 27, shaking much of northern BC. There have been numerous aftershocks since the main quake.
A map from the USGS shows that the latest 5.1 aftershock from the Oct. 27 earthquake occurred east of Haida Gwaii, in Hecate Straight. (USGS)
The latest aftershock from the 7.7 magnitude earthquake off Haida Gwaii occurred east of the islands, according to preliminary data released by the US Geological Survey. Canadian data, however, shows the quake west of Haida Gwaii.
The USGS marked the aftershock at 52.500°N 131.100°W at a depth of one kilometre or .6 mile. No tsunami warning was issued.
Natural Resouces Canada data puts the quake at 52.4 North 132.4 West, adding the earthquake “was felt at Queen Charlotte City and Skidegate. There are no reports of damage, and none would be expected.”
The NRC map shows the aftershock on the Queen Charlotte fault line. However, if the USGS map is correct, an aftershock on the east side of Haida Gwaii could raise questions of the potential hazard for Douglas Channel.
Both services said the aftershock occurred at 3:15 am November 1, using Universal Time. An automatic bulletin from the Canadian earthquake centre recorded the quake as 5.0 20:15 PDT. Oct, 31, 97 km SSW of Queen Charlotte City.
No tsunami warning was issued.
According to the USGS the aftershock was
181km (112mi) SSE of Masset, Canada
208km (129mi) SSW of Prince Rupert, Canada
278km (173mi) SW of Terrace, Canada
493km (306mi) NW of Campbell River, Canada
679km (422mi) SSE of Juneau, Alaska
Northwest Coast Energy News will update this story if newer data is available Thursday morning. Although no tsunami warning was issued, tonight’s event is another example of the confusion that can result from automatically generated earthquake data. If the event east of Haida Gwaii is confirmed, it means that the level of tsunami hazard for Douglas Channel will have to be reconsidered.
Rio Tinto Alcan has reopened Hospital Beach, the nearby boat ramp and Moore Creek and the Moore Creek falls for public use.
RTA took out an ad in a local newspaper Wednesday, Oct. 12, 2012, to make the announcement which came after a meeting members of the District of Kitimat Council on Oct. 4.
The RTA statement reads, in part:
Both Rio Tinto Alcan and the District of Kitimat understand the value and importance of ocean access to residents of the area while at the same time, continuing to respect and ensure that safety is the number one priority.
Over the last few months, while hearing the disappointment and concern about Hospital Beach, the KMP [Kitimat Modernization Project] Construction Team took action to mitigate the public safety risk. The massive rock trucks hauling heavy loads will be re-routed; a new bridge over Anderson Creek has been installed; new traffic lights will be installed near the Construction Village; and an extra construction road has been built from the former Eurocan Haul Road. All these measures have enabled the decision to accommodate the wishes of the community to access Hospital Beach, the boat ramp and Moore Creek safely.
It is important to remind residents however, Rio Tinto Alcan is in the middle of constructing a mega project to modernize and sustain the aluminium smelter business in Kitimat for the benefit of us all. This is the highest priority with many demands and intense focus. To that end, Rio Tinto Alcan will continue to assess traffic patterns and will likely need to make short term closures again as construction dictates. It is imperative that residents respect the company’s right to manage activities on its private property as it deems in the best interest of its business, including the KMP and public safety.
Rio Tinto Alcan and the District of Kitimat have committed together to work toward finding long term solution to ocean access. Thank you all for your patience, support and cooperation.
Prince Rupert residents wanting to walk along the road adjoining the ocean past Rotary Waterfront Park will notice new barriers and signs alerting them that they would be trespassing should they do so.
The barricades and signs were put up yesterday, and CN regional manager of public affairs Emily Hamer says it is due to safety concerns with the public on the railway’s property.
Prince Rupert acting mayor Anna Ashley told the Northern View the city expected some restrictions during construction and said the city planned to talk to CN about the issue.
In an e-mail to Northwest Coast Energy News after the October 4 meetingm Kitimat mayor Joanne Monaghan, while hinting then that a solution to the restrictions was coming, said that industry has been faced with so many lawsuits that safety is becoming a bigger issue.
Councillor Corinne Scott also said that the meeting with RTA stressed that “Large businesses are putting safety as a higher priority.” (She also noted that council agreed to have regular meetings with RTA “.communication lines are open and we look forward to a continued good working relationship between the District of Kitimat and RTA. “)
In both cases, it appears that waterfront access is a legacy issue, left over from an earlier era of industrial development that gave little thought to either the environment or community.
Now it is also apparent that liability lawyers, who probably live thousands of kilometres away from the northwest, have, so far, been driving this issue, with little regard for the needs of local residents.
Make no mistake, safety should be a high priority, but arbitrary restrictions that may look good on legal brief, could actually mean that people would simply try to get around the restrictions, to the determent of safety. It is well known that RTA Plant Protection was finding people at Hospital Beach during the summer, especially at night, despite the publicized restrictions, barriers and warning signs.
Today with a strong need for jobs in northwestern British Columbia, future community needs for access to waterfront and green space (even in such a wide green area as northern BC) must be taken into consideration in municipal and corporate planning. If that planning isn’t done, that will mean that while there could be jobs, the northwest could be in a situation as it was this summer, with no way to enjoy the advantages of waterfront life in northern BC.
A map from the Geological Survey of Canada showing the line of a possible seismic fault on Douglas Channel (Geological Survey of Canada)
Updates with statement from Natural Resources Canada, new filings by Enbridge Northern Gateway and the Attorney General of Canada (in box below)
The Geological Survey of Canada has identified a tsunami hazard and a possible seismic fault in Douglas Channel near Kitimat. A scientific paper by the Geological Survey and the Department of Fisheries and Oceans says there were once two giant landslides on Douglas Channel that triggered major tsunamis and that the landslides were possibly caused by an earthquake on the fault line.
Kitimat is the proposed site of the Enbridge Northern Gateway project and at least three liquified natural gas projects.
If the projects go ahead, hundreds of supertankers with either bitumen or LNG will be sailing in the channel for years to come.
A filing by the Attorney General of Canada with the Northern Gateway Joint Review Panel is asking the JRP for leave to file late written evidence long after the original deadline of December 2011. The Attorney General’s motion was filed on August 17, but went unnoticed until the Kitimat environmental group Douglas Channel Watch brought the matter up with District of Kitimat Council tonight (Sept. 17).
Appended to the Attorney General’s motion is a copy of a scientific paper from the Geological Survey “Submarine slope failures and tsunami hazards in coast British Columbia: Douglas Channel and Kitimat Arm” by Kim W Conway, J.V. Barrie of the Geological Survey and Richard E. Thomson of the Department of Fisheries and Oceans.
The report says the scientists discovered “evidence of large submarine slope failures in southern Douglas Channel.”
It goes on to say: “The failures comprise blocks of bedrock and related materials that appear to have been detached directly from the near shore off Hawkesbury Island.” Hawkesbury Island and many of the other islands in Douglas Channel are built up with material left over from the ice age glaciers and thus are vulnerable to displacement and landslides.
The research identified two slides, one estimated at 32 million cubic metres and a second of 31 million cubic metres. The report goes on to say that the discovery of an “apparently active fault presents the possibility that they may have been triggered by ground motion or surface rupture of the fault during past earthquake events.”
The slope failure landslides are covered with thick layers of mud, and that, the scientists say, could mean that the failures could be ancient, possibly occurring 5.000 to 10,000 years ago. Further research is needed to confirm the date of the giant slides.
What is worrying about the discovery is that fact that there were two recent submarine slope failures on the Kitimat Arm of Douglas Channel. both creating tsunamis. The first slope failure occurred on October 17, 1974, triggering a 2.4 metre tsunami at low tide. Then on April 27, 1975 there was a second slope failure near low tide on the northeast slope of the Kitimat Arm that generated an 8.2 metre tsunami. The 1975 tsunami destroyed the Northland Navigation dock near Kitimat and damaged the Haisla First Nation docks at Kitamaat Village.
The paper says that “Additional geological research is required to better delineate the age of the submarine failures, their triggers, and their mechanisms of emplacement.”
Urgent new research is underway and the filing by the Attorney General says when the Department of Justice requested leave to file late evidence says it anticipates that the further research by DFO is expected to be completed by November 1. The Natural Resources Canada Earth Sciences Sector began a national assessment of submarine slope failures in Canada in late 2011 and completion of the Pacific portion of this assessment is targeted for December of 2012.
The Attorney General’s filing says that DFO is now modelling “potential wave heights and speeds that may have resulted from the two previously unrecognized submarine slope failures in the Douglas Channel.” The model will use high resolution scans of the Douglas Channel seafloor to create the models.
The survey of Douglas Channel in 2010 suggests the possible existence of a fault immediately to the south of the second ancient slide on Hawkesbury Island.
The GSC paper says that evidence for a continuous fault was observed by aligned stream beds and fractures on the south end of Hawkesbury Island, about four kilometers from the site of the second ancient slide. The possible fault then appears to terminate far to the south near Aristazabal Island on the Inside Passage. The Geological Survey says that eleven small earthquakes, all less than magnitude three, have appeared with 20 kilometres of the suspected fault over the past 25 years.
The paper says that the scientists conclude that the slides appear to have left very steep slopes at or near the shoreline that could be susceptible to future failure events.
A large potential slope failure has been identified near one of the ancient slides….
in the absence of additional evidence, the fault must be considered a potential trigger for the submarine failure events….the triggers for the failures have not been defined; however, their proximity to a potentially active fault represents one potential source. The failures probably generated tsunamis during emplacement and conditions exist for similar failures and associated tsunamis to occur along this segment of Douglas Channel in the future.
The scientists say that detailed tsunami modelling is underway to
provide an improved understanding of the generation, propagation, attenuation, and likely coastal inundation of tsunami waves that would have been created by slides… or that could be generated from similar future events. Only through the development and application of this type of tsunami modelling will it be possible to gauge the level of hazard posed by the identified submarine slope failures to shore installations and infrastructure, or to devise ways to effectively mitigate the impacts of future such events.
The filing by the Attorney General offers to bring the scientists to the Joint Review Panel to appear as witnesses sometime during the final hearings.
The filing notes that the current evidence tendered to the JRP by Enbridge, and other parties does demonstrate the potential for marine geohazards and associated tsunami events. Enbridge’s design of the proposed Northern Gateway marine terminal and its operational plans took into consideration the current state of knowledge of geohazards including earthquakes and tsunamis at the time of filing. Enbridge has said it would undertake further geological survey during the detailed design phase for the terminal.
At the time Natural Resources Canada noted that the information provided for the Environmental Review was sufficient at that time, now the Attorney General says:
the geographic scope for potential landslide induced tsunami hazards is now better understood to extend beyond the Kitimat Arm. NRCan and DFO seek by this motion to ensure that this Panel, and the Parties before the Panel, have the most up to date information on geohazards in the Douglas Channel.
Updates: DFO report in October will clarify the tsunamis in Douglas Channel.
Statement from Natural Resources Canada
Natural Resources Canada sent this statement to Northwest Coast Energy News on September 20, 2012.
In reference to the opening paragraph of your September 18th editorial entitled Geological Survey of Canada identifies tsunami hazard: Possible fault line on Douglas Channel, we would like to clarify the following. Although the ancient large submarine slope failures which our scientists have identified may have caused tsunamis, this is not a certainty. It is important to note that Fisheries and Oceans Canada is currently studying this information to model potential wave heights and speeds.
As our report states, only through the development and application of this type of tsunami modelling will it be possible to gauge the level of hazard posed by the identified submarine slope failures to shore installations and infrastructure, or to devise ways to effectively mitigate the impacts of future such events.
Northern Gateway response filed on August 31, 2012
Enbridge Northern Gateway filed this response to the Attorney General’s motion on August 31.
This motion of the Federal Government Participants requests permission to file late evidence consisting of a report entitled “Submarine Slope Failures and
Tsunami Hazard in Coastal British Columbia: Douglas Channel and Kitimat Arm” regarding tsunami hazard and additional modelling work based on that report.
Northern Gateway does not object to the filing of this late intervenor evidence.
It may be relevant and Northern Gateway accepts that theevidence could not be filed earlier. However, Northern Gateway would like the opportunity to conductits own additional modelling work which it would be prepared to provide to DFO for comment prior to the filing of any modelling work by DFO in this proceeding.
Attorney General response to Enbridge on September 10, 2012.
The Attorney General of Canada responded to Enbridge by saying:
Attorney General responds DFo is prepared to await filing its subseqent modelling work in these proceedings until such time as it has received, reviewed and commented upon additional modelling work as proposed by NGP Inc.
DFO nots howeverand wishes to alert the JRP that the NGP INc proposed may occasion a delay in the filing of the DFO moedling work which is now proposed for filing on or about October 31, 2012. Delivery of DFO comments as requested will depend on when DFO received the NGP Inc modelling work, the time and resources required by DFO to study and provide comments on the NGP modelling work and unforeseen factors which may have an impact upon completion the commentary. As such,
DFO is prepared to file its modeling work on or about October 31, 2012, but subject to any further direction or request by the panel.
Geological Survey of Canada map of Douglas Channel showing the area surveyed which discovered the landslides and possible fault line. (Geological Survey of Canada)
;
;
Map from the Geological Survey of Canada showing the landslides on the Kitimat Arm which triggered tsunamis in 1974 and 1975 (Geological Survey of Canada)
;
;
Map from the Geological Survey of Canada showing the giant slide on the southern tip of Hawkesbury Island. (Geological Survey of Canada)
;
Map from the Geological Survey of Canada showing the second giant slide on the coast of Hawkesbury Island on Douglas Channel (Geological Survey of Canada)
A map, released by the BC government, shows the area of Crown land covered by the Haisla Framework agreement that could lead to another LNG project in Kitimat. (Govt of BC)
The Haisla Nation and the BC government have signed an agreement that will lead to a third liquified natural gas project near Kitimat.
The “Haisla Framework Agreement” allows for the lease or sale of up to approximately 700 hectares of Crown land near the Douglas Channel, and for the foreshore lease of submerged lands of up to 102 hectares for a berthing facility.
The area is just north of the Haisla Reserve land at Bish Cove where the KM LNG project will be located, but south of the proposed BC LNG and Enbridge terminals. It is all undeveloped and unserviced land within the boundaries of the District of Kitimat.
That could mean, if all projects go ahead there the west side of Douglas Channel from Kitimat almost to Jesse Falls would see three, perhaps fourm hydrocarbon facilities and terminals.
The agreement provides the Haisla with the options for up to a 60-year lease or the possibility of purchasing of the land outright.
The agreement also commits both parties to start work on land-use planning for areas around the Douglas Channel, which, the BC government says, has tremendous potential as a marine port.
A news release from the BC government today does not specify the backer of the terminal, While the most obvious candidate could be the Shell project LNG project (last fall Shell purchased the old Methanex site and the associated marine terminal at Kitimat) there is now media speculation that there could be other players involved, possibly another giant Exxon Mobile.
A news release from the BC government says that the “framework agreement” is a “significant step toward government’s commitment to have three terminals and their connecting pipelines operating by 2020, creating more than 1,400 ongoing jobs and generating an estimated $600 billion in economic activity over 30 years.”
The release says the agreement “provides the structure for a land purchase or lease that will allow the Haisla to partner with industry to develop a liquefied natural gas (LNG) facility and marine export terminal on the west side of the Douglas Channel in the areas around Haisla Reserve #6.”
The release quotes, Ida Chong, BC Minister of Aboriginal Relations and Reconciliation as saying:
Our government is working with First Nations like the Haisla to create new jobs and opportunities throughout British Columbia. This agreement builds on our strong partnership with the Haisla Nation, and it is the key to unlocking the vast potential of a whole new natural gas export industry in British Columbia which will provide long-term stability for families and communities.
It also quotes Ellis Ross, Chief Councillor of the Haisla Nation: –
This agreement allows the Haisla to look at the land on the west side of the Douglas Channel in a different light. This gives the Haisla and associated projects the certainty needed for the LNG proposals and other projects coming forward for our territory. If we are able to do this, the Haisla people will benefit, as will all British Columbians and Canadians.
Ida Chong and Ellis Ross sign the Haisla Framework Agreement in Vancouver, Sept.14, 2012 (Govt of BC photo)
The release goes on to say that the agreement signals a closer working relationship between the Haisla and BC in and around the Kitimat and Douglas Channel area. It commits both parties to start work on land-use planning for areas around the Douglas Channel, which has tremendous potential as a marine port. This certainty will allow other development projects in the area to proceed.
The agreement says the Haisla will work independently to find a suitable partner for the development of the land. Details of the lease or sale are expected to be finalized this fall.
Map from the United States Federal Energy Regulatory Commission showing LNG export terminal projects in North America (FERC)
What is it about the islands in Douglas Channel? First, Enbridge gets in to a lot of hot water, so to speak, for erasing the islands in Douglas Channel in an animation promoting the Northern Gateway Pipeline. See for example The Vancouver Sun on back on Aug. 16, 2012, when it picked up a story from the Times Colonist – Enbridge map sinks islands, angers critics. The controversial video segment showed Douglas Channel wide open for navigation, rather than marked with about one thousand square kilometres of mountainous islands. This map, created by the Leadnow.ca and Sumofus.org websites was widely used by the media to show the difference. Enbridge later amended its video with a disclaimer that it is “broadly representational.” A video by Shortt and Epic Productions “This is Not An Enbridge animation” showing the beauty of northwestern BC quickly went viral.
As this was happening, the United States government Federal Energy Regulatory Commission issued a map that shows Liquified Natural Gas import and export terminals across North America, a map that adds an island to the Channel–“Douglas Island.”
In fact, the map manages to get a lot about Canadian LNG projects wrong. It locates the BC LNG project on the non-existent Douglas Island. The company’s name Douglas Channel Energy Partnership actually gives the proper location this way
south of the Moon Bay Marina, within the District of Kitimat and the asserted traditional territory of the Haisla Nation. The site is approximately 10 km southwest of Kitimat and 7 km north of Bees Cove Indian Reserve 6 (Bish Cove)
The small cove where BCLNG will put its barges to create the LNG is often locally called North Cove.
The FERC map also misplaces the Shell LNG project, now known as LNGCanada, in Prince Rupert, even though Shell confirmed the Kitimat location on May 15, 2012. It also calls it Prince Rupert Island, although the town of Prince Rupert is actually located on Kaien Island.
The map does apparently get the KM LNG project somewhat correct, attributing it to Apache Canada, but leaving off Apache’s partners, Encana and EOG.
The map recently also appeared on the website of Oregon Public Broadcasting in an article Five Keys To The Pacific Northwest’s Natural Gas Export Debate by reporter Amelia Templeton, which outlines the growing controversy over the plans to export US LNG through Coos Bay, Oregon via the Jordan Cove Project.
It appears that in Oregon, the Coos Bay LNG project is becoming as controversial as the Northern Gateway project is in Canada.
The issues outlined by Templeton include the threat of expropriation (called “eminent domain” in the US and also a key issue in the debate over the Keystone XL pipeline on the plains). There are arguments on jobs versus the environment, especially the perceived threat to wild rivers and salmon spawning grounds. Finally one issue that is lower on the agenda in northwestern BC but a big worry in Oregon, the potential for a devastating earthquake along the Cascadia fault.
During the NEB hearings on the KM LNG (Apache/EOG/Encana) project in June, 2011, many of the “expert” witnesses urged that that first Kitimat project go ahead quickly because of perceived competition from Oregon.
Unlike in Oregon, LNG projects are generally perceived positively in the northwest and all three are going ahead, although not as quickly as originally planned due to market volatility among prime potential customers in Asia.
There’s one question about the Enbridge Northern Gateway project that many people ask and few can answer: Who is responsible for the port of Kitimat? Who would be liable should there be a disaster in the port? Nobody really knows.
Unlike many harbours in Canada, the port of Kitimat is “private,” although as the District of Kitimat says, “Transport Canada and other federal agencies continue to regulate navigation, security and environmental safety.” Kitimat has promoted that private status as an economic advantage.
If there’s a dispute, the question of responsibility and liability would probably end up in the Supreme Court of Canada, with the justices sorting out a historic puzzle. Or perhaps that historical puzzle could mean that the future of the port of Kitimat might be decided by the next B.C. provincial election.
Most of the other harbours in Canada are the responsibility of Ports Canada, a branch of Transport Canada or run by (usually not-for-profit) semi-public port corporations or local harbour commissions.
To find out why Kitimat is one of the few private ports in Canada, the first thing to do is watch Eliza Kazan and Bud Schulberg’s classic 1954 multiple Oscar winning movie, On the Waterfront, starring Marlon Brando, about how the mob ran the New York docks.
What has On the Waterfront got to do with Kitimat? It goes back to when the then Aluminum Company of Canada/Alcan (now Rio Tinto Alcan) was planning the Kitimat project; much of that work was done in New York both by employees and consultants. It was in 1949, that Malcolm Johnson, a New York Sun reporter, wrote a Pulitzer Prize winning series of investigative reports called “Crime on the Waterfront,” exposing corruption and Mafia involvement with the docks and the longshoremans’ union. The movie was based, in part, on that investigative series.
So in its planning, Alcan was determined that the longshore unions would not be involved in running the docks in Kitimat. The publicly stated reason has always been that Alcan wanted a seamless 24/7 operation that would be integrated with the aluminum smelter. Alcan would sign a collective agreement with the United Steelworkers that covered both the smelter and the docks. (CAW 2301 now represents most of the workers at the Kitimat smelter.)
When the Kitimat project was being finalized in 1949 and 1950 at the height of the Cold War, aluminum was a strategic commodity, security was high on the agenda, and it was not just the Soviet bloc but the mob as well that worried the authorities.
Add two factors. First, in 1949 the province of British Columbia was anxious to promote what would today be called a “mega-project.” Second, in the post-war era when corporations were relatively enlightened compared to today, Alcan was determined not to create the traditional “company town.”
To promote private-sector development of both hydro-electricity and aluminum, B.C. signed a rather loosely worded agreement with Alcan, noting that the project was going on “without investment by or risk to the government.” That agreement was implemented by the Legislative Assembly of B.C. by an equally wide open Industrial Development Act. One aim of both was try to ensure that future “socialists” would not expropriate the project.
Industrial township
With the province handing over the Crown land at the head of Douglas Channel at a very nominal price to Alcan, next came the creation of the District of Kitimat. With the town under construction, with few buildings and a small population, under normal B.C. practice, the area would be “unincorporated” and would not have a municipal government. But Alcan and the province came up with a new concept, which they called “an industrial township,” which would allow a municipal government to be established in anticipation of future growth.
The act that established the District of Kitimat put the boundaries outside the land owned by Alcan (excluding land reserved for the Haisla Nation).
The District of Kitimat has some legal responsibility for “wharfs” at the port of Kitimat. At council meetings, the environmental group, Douglas Channel Watch, has raised the question of the district’s responsibility and liability in case of an Enbridge incident but there’s been no definitive response from district staff. There is no municipal harbour commission as there is in other jurisdictions.
Up until recently, it was a convenient arrangement for everyone involved. Alcan, Eurocan and Methanex ran their dock operations without any interference, beyond standard Transport Canada oversight.
Things began to change in 2007, when the Rio Tinto Group bought Alcan, creating Rio Tinto Alcan. A couple of years ago, a senior staff source in the Canadian Auto Workers explained it to me it this way. “Alcan was a big corporation, but Alcan was a corporation with a big stake in Canada. As a union, we could do business with them. Rio Tinto is a transnational corporation with businesses in lots of countries but no stake in any of them. So it’s a lot harder now.”
With the Rio Tinto acquisition of Alcan, things tightened up in Kitimat. Negotiations between the District and RTA for the District to obtain more land stalled. Access to the estuary and other RTA lands that had been somewhat open under Alcan became more restrictive. In 2010, the Eurocan paper mill shut down along with its dock. In 2011, Rio Tinto bought the dock from West Fraser, owner of Eurocan. The Kitimat community noted that when the dock was repainted, it said just “Rio Tinto.” not “Rio Tinto Alcan” and that led to lots of gossip and wondering about what the Rio Tinto Group really plans for Kitimat. Last fall, Shell Canada purchased the former Methanex dock for part of its liquified natural gas operations.
With the Enbridge Northern Gateway project, the BC LNG project at North Cove and the KM LNG project at Bish Cove all along the shore of Douglas Channel and within the boundaries of the District of Kitimat which extends as far south as Jesse Lake, the question that has to be asked is, what happens now? If the Enbridge project is built, it will start just beyond the boundaries of the land owned by Rio Tinto Alcan.
That old arrangement between Alcan and the District of Kitimat is facing many new challenges.
The district once had a harbour master, but the position was eliminated because he had nothing to do. Alcan owned its docks, Alcan managed the docks and Alcan union employees worked on the docks. Later came the Eurocan (now owned by Rio Tinto) and Methanex (now owned by Shell) docks, again owned and operated by private corporations.
The District of Kitimat, nominally in charge, was content to sit back and collect taxes.
With the Enbridge Northern Gateway project, the B.C. LNG project at North Cove and the KM LNG project at Bish Cove all along the shore of Douglas Channel and within the boundaries of the District of Kitimat, the question that has to be asked is, what happens now? If the Enbridge project is built, it will start just beyond the boundaries of the land owned by Rio Tinto Alcan.
In Canada, ports and harbours are normally under federal jurisdiction and Transport Canada has oversight. But Alcan’s “private port” and the District of Kitimat were created by acts passed by the B.C. government.
The original agreement between the province and Alcan mentions an “aluminum plant” and “low-cost electrical power,” it doesn’t mention bitumen or liquified natural gas. Those provincial acts do not cover bitumen, supertankers and liquified natural gas.
B.C. Opposition Leader Adrian Dix has made it clear that his New Democratic Party opposes the Northern Gateway project. The federal government has said the province can’t really do anything to stop Enbridge Northern Gateway once Stephen Harper has decided that the pipeline project is in the national interest.
At this moment, Dix is a “contender” for the premiership, with Christy Clark and the B.C. Liberals dropping in the polls and with key members of her government deciding not to run in the election next spring.
So, if, as expected, Adrian Dix becomes the next B.C. premier, he has one very strong hand to play. Any act can, with proper legal advice, be amended by the B.C. legislature. That means the “socialists” so feared by Alcan and the premier of the day, Byron “Boss” Johnson, could alter the 1949 law. That in turn may upset the decades-old arrangement that created the private port which Enbridge is banking on.
Golar LNG, which describes itself on its website as “one of the world’s largest independent owners and operators of LNG carriers” said in its interim results report to shareholders on November 28:
