The landslide on the Lamplugh Glacier on Thursday, July 7, 2016. (Jillian Rogers)

The landslide on the Lamplugh Glacier on Thursday, July 7, 2016. (Jillian Rogers)

The mammoth landslide that buckled from a mountaintop and spilled out onto the Lamplugh Glacier last week in Glacier Bay has caused quite a stir. The story has traveled around the globe and back again as scientists continue gather samples and data from the site. But the magnitude of the slide is hard to put into words. KHNS’s Jillian Rogers took a ride with pilot Paul Swanstrom to see the slide for herself.

It’s 2 p.m. on a sunny Thursday. The wind is calm and we’re told it’s perfect flying weather.

In the stout, shiny 1956 de Havilland Beaver, there are six of us, plus Swanstrom. He owns Mountain Flying Service with his wife Amy, and was the first to discover the slide, last Tuesday morning. Today, we’re heading to the site, cruising along at an easy 115 miles an hour with gasp-worthy vistas as far as the eye can see.

“We’re going on an East and West Arm Glacier Bay flight from Haines, over the Chilkat Mountains. We’re gonna kind of go over and through them and go out to the West Arm of Glacier Bay and look at our new landslide among other things,” says Swanstrom.

As we make our way over and around the craggy, snow-capped peaks, Swanstrom says he’s not surprised the story of the slide has taken off. It is one of the largest in the area at approximately six-miles long and more than a mile wide. It rocked the earth with the equivalent force of a magnitude 5.5 earthquake. Swanstrom says he hasn’t much time to really stop and absorb the media attention.

“I’ve been pretty busy to even understand it.” he says. “A lot of people have commented, I see there was something in the New York Times and the ADN, and everything but we’ve been so busy flying that I haven’t really looked at any or taken the time to read them. Jillian: Has the business been getting calls? Paul: Yeah, yeah … we’ve gotten calls from Fox News, New York Times, all kinds of people.”

As we buzz along, Swanstrom identifies peaks and glaciers. He’s got a story or a nugget of information about most all of them. And his captive audience is eating it up with eyes wide and mouths agape.

After about 30 minutes, the slide comes into sight. It is humongous. It looks fluid, like thick black paint spilled on a white canvas. The contrast is stark and the size is simply astonishing.

“Whoa, look at that!”

That’s John DeRosa. KHNS’s sound engineer, who was along for the ride.

“Wow, it just keeps going. How is that possible? How is it possible that those rocks moved that far?”

The rest of us were speechless for a while. Swanstrom piloted closer around the top of the mountain to the breakaway zone. Dust is still rising from the area because chunks and boulders are still sloughing off.

“You can see how it bulldozed snow up at the bottom of it there,” Swanstrom says.

John: “This is remarkable, Paul! This is remarkable!”

Colin Stark is a geophysicist at Columbia University’s Lamont-Doherty Earth Observatory in New York. He says the amount force in this slide totaled 28 giganewtons and spit out around 120 million metric tons of rock debris. He says this is the largest recorded slide anywhere in the world this year.

Stark just got back to New York from Southeast Alaska. He visited the site on Monday and Tuesday with the help of Haines pilot Drake Olson. Stark says there were two big discoveries upon closer inspection of the slide. One is that the slide is still very much active.

“There’s been rock falling 24-7 since last Tuesday,” Stark says. “It has not stopped. It’s quite amazing. When you look at the lower slope from the ground, you can see individual boulders crashing down that are probably the size of a very large car.”

Those smaller slides, which are still huge, mind you, create little plumes of dust, which rise and gather into a bigger dust cloud over the area. Stark says the constant slides are really loud. They sound like fast flowing streams, he says, but “crunchier.”

The second detail, that Stark noticed was that when the slide let loose, it did so with such unbridled force, that it pushed rock and dirt up the sides of the valley almost 300 feet. So, it’s left a ring on the flanks of the valley. Like a ring of grime leftover in a bathtub.

“Rock and ice slide, with all that momentum it was going down the glacier, but when it hit the valley walls it climbed up, very steeply up the rock wall and then slid back after reaching a maximum,” Stark says. “And then what you see now is the remnant of the highest point that the dirt got to.  And it’s clinging, but it won’t be for long, because we could see rock fall coming off there, too.”

Stark says these slides are becoming more prevalent in the area, which, as a researcher is good for him. But not great for the rest of us in terms of what it could mean.

“Glacier Bay and St. Elias together are the most active rock avalanche places in the world. So, you guys have the worst of it. Or the best of it, depending on how you look at it. Because of glacier retreat and warming, the situation is getting worse. Or from my perspective, better.”

Back on the beaver, we circle around the peak and continue to marvel at the epic event still moving beneath us. Eventually we head back to Haines trying to really understand what we just saw. Tourists are now requesting the flight over the landslide as the news travels. But Swanstrom says, even though he flies over it a few times a day he never gets tired of looking at it.


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The slide at the top of the Lamplugh Glaicier dwarfs a cruise ship at the bottom. (Jillian Rogers)

The slide at the top of the Lamplugh Glaicier dwarfs a cruise ship at the bottom. (Jillian Rogers)

The breakaway zone. (Jillian Rogers)

The breakaway zone. (Jillian Rogers)