CHILCOTIN SLIDE UPDATE, 3 P.M., SATURDAY, AUG. 3
The province just held an information briefing about the slide on the Chilcotin River, so since there's obviously interest in it, here's an update about where we are.
Lidar data has established that the slide is 1,000 metres long by 800 metres wide by 30 metres deep. Lidar is a method for determining ranges by targeting an object or a surface with a laser and measuring the time for the reflected light to return to the receiver.
The 'lake' behind the slide site is rising at a rate of about 22 centimetres per hour. This is a slight decrease over the first couple of days, as the water now has more room to spread out behind the slide area.
There is no seepage at the toe of the slide, so overtopping of the slide is the most likely scenario based on what is known/being observed.
Worst Case Scenario: A one-hour breach scenario. In this scenario it would take 1.5 hours for water to reach Farwell Canyon, three hours to reach the confluence of the Chilcotin with the Fraser, 15 hours to reach Lillooet, 21 hours to reach Lytton, 24 hours to reach Boston Bar, and 29 hours to reach Hope (all times measured from the slide site).
In this scenario, peak flow between the slide site and Farwell Canyon would be 6,590 cubic metres per second (typical freshet flow is 300 cubic metres per second). Peak height above current would be 10 metres. At the confluence with the Fraser the peak flow would be 5,545 cubic metres per second and peak height above current would be four metres.
By the time the flow reached Lillooet it would be well below typical freshet flow but 1.8 metres above the current height. Same at Lytton, where it would 1.5 metres above current height; Boston Bar (1 metre above current height); and Hope, where the water would be 0.3 metres above current height.
Best Case Scenario: A 24-hour breach scenario. In this case, the water would take 9.5 hours to reach Farwell Canyon, and 11 hours to reach the confluence with the Fraser, where the peak height would be 2.1 metres above current.
It was stressed that this is an extremely dynamic situation, and that a lot of assumptions have had to be made to create the models. There is confidence, however, that there will be overtopping, and not a breach. Additional field data is being collected continuously, and all possibilities are being prepared for.
Debris may be part of the outflow, which could damage riverbanks and infrastructure. An evacuation order has been issued for properties along the Chilcotin River from Hanceville to the Fraser, and people are being warned to stay clear of the land and air space around the slide.
A question that has been asked is 'Will there be an effect on area highways?' The answer is 'No.' Highways 20, 99, and 1 are either far enough away from, or too high above, the Chilcotin and Fraser Rivers to be affected.
Attached picture (courtesy Marty Lauren/Facebook) shows water and debris backing up behind the slide site (l).
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