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In 2016 the USGS led two geophysical surveys of the Queen Charlotte-Fairweather fault off the coast of southeast Alaska, using multibeam sonar to map the ocean floor in detail, and multichannel seismic reflection to image deeper layers of sediment.

This article is part of the January-February 2017 issue of the Sound Waves newsletter.

Two maps; the left hand one shows brown land, blue water, and red arrows. The right hand one shows colored survey tracklines
Left: Key features in and around the Gulf of Alaska. A black rectangle outlines our 2016 study area along the Queen Charlotte-Fairweather fault. Red arrows indicate relative tectonic plate motions. Right: A shaded relief map of the 2016 study area. Rainbow colors show seafloor depths acquired by the USGS in 2015 and 2016. Red indicates shallower depths. Purple zigzag lines show where we collected seismic-reflection data in 2016.

In the spring and summer of 2016, the USGS led two geophysical surveys of the Queen Charlotte-Fairweather fault off the coast of southeast Alaska. We used multibeam sonar to map the ocean floor in detail, and multichannel seismic reflection to image deeper layers of sediment. Our goals included determining how fast the two sides of the fault move past each other (slip rate) and deciphering the history of the fault. We also want to better understand how large earthquakes might trigger potentially dangerous underwater landslides.

The Queen Charlotte-Fairweather fault extends more than 1,200 kilometers (750 miles) from offshore of Vancouver Island, Canada, to the Fairweather Range of southeast Alaska. This fault can be considered a sister to California’s San Andreas fault: both separate the Pacific tectonic plate from the North American plate; both are right-lateral strike-slip faults (one side moves to the right relative to the other); and both can generate large, dangerous earthquakes.

Scientific equipment is mounted on a metal wing on a research vessel shown at sea.
Reson 7160 multibeam echosounder on a hydraulic wing attached to the R/V Medeia. During operations, the wing flips down to place the yellow sonar head underwater. TerraSond designed the custom wing.
A group of scientists pose on the dock in front of a ship with a blue hull.
Ship’s company at the end of the R/V Medeia survey in 2016. Left to right, kneeling and sitting: David Maggio (TerraSond), Danny Brothers (USGS), Jackson Currie (USGS), Jared Kluesner (USGS), Becky Wilson (Alaska Department of Fish and Game [ADFG]), Captain Jim deLaBruere (ADFG), and Cedar Stark (ADFG). Back row standing: Brian Andrews (USGS), Uri ten Brink (USGS), Doug MacGillivray (TerraSond), Craig Conger (ADFG). Missing: Rob Wyland (USGS) and Peter Haeussler (USGS).

This project began in 2015 with two geophysical surveys along the northernmost submerged section of the fault (see “Investigating the Offshore Queen Charlotte-Fairweather Fault System”). This year we expanded the project by extending the survey area 325 kilometers (200 miles) to the south. We continue to work with last year’s partners—the Alaska Department of Fish and Game, the Geological Survey of Canada, and the Sitka Sound Science Center—and have added a new partner: the University of California, Santa Cruz. We are also collaborating with USGS geologists studying on-land segments of the fault (for example, see “Uncharted: Exploring one of America’s fastest faults”). Scientists from both the onshore and offshore projects presented results at the American Geophysical Union Fall Meeting in December 2016.

First cruise: 25 days of around-the-clock work pay off

The first survey in May and June of 2016 (USGS Survey 2016-625-FA) was a cooperative effort between the Alaska Department of Fish and Game (ADFG) and the USGS, using ADFG’s research vessel R/V Medeia out of Juneau, Alaska. Scientists Danny Brothers, Jared Kluesner, Jackson Currie, and Rob Wyland from the USGS Pacific Coastal and Marine Science Center; Uri ten Brink and Brian Andrews from the USGS  Woods Hole Coastal and Marine Science Center; and Peter Haeussler from the USGS Alaska Science Center worked with four R/V Medeia crewmembers from Fish and Game, and two hydrographic surveyors from the TerraSond LLC. The team used a Reson 7160 multibeam echosounder to map bathymetry (seafloor depth) and backscatter (an indicator of seafloor texture and composition). A high-resolution seismic-reflection system—consisting of a 32-channel hydrophone streamer and a sparker sound source—was used to collect seismic-reflection profiles (vertical images of sediment layers beneath the seafloor). Both systems ran simultaneously throughout the cruise.

We began gathering data along the northwest coast of Chichagof Island, where we had mapped 75 kilometers (50 miles) of the Queen Charlotte-Fairweather fault in 2015 (see “Investigating the Offshore Queen Charlotte-Fairweather Fault System in Southeastern Alaska, and its Potential to Produce Earthquakes, Tsunamis, and Submarine Landslides”), and then continued southward along the fault for an additional 325 kilometers (200 miles). The 110-foot R/V Medeia proved an excellent platform for field operations, allowing us to collect data in less-than-ideal weather conditions. At the midpoint of the survey, we docked in nearby Sitka for one night to resupply and exchange personnel. Only once did we stop for bad weather, when seas of 4 to 5 meters (13 to 16 feet) and 40-knot winds with 65-knot gusts forced us to head into safe harbor on Baranof Island. In total, we completed 25 days of 24-hour operations.

Remarkable results

Three panels with bright colors showing underwater bathymetry features
Perspective views of multibeam bathymetry data acquired by the USGS aboard the R/V Medeia. Shallower depths in red. Arrows point to the distinct line in the seafloor associated with the Queen Charlotte-Fairweather fault.

Despite the often-difficult weather and sea conditions, we collected more than 4,600 square kilometers (1,700 square miles) of multibeam bathymetry and backscatter data. The bathymetric data provide remarkable new views of the shape and extent of the Queen Charlotte-Fairweather fault. We immediately saw several previously unknown features, including a series of subtle bends and steps in the fault that appear to form basins within the fault zone. Perhaps the most intriguing aspect of the new imagery is the continuous and truly “knife-edge” character of the fault for the entire length of the 400-kilometer (250 mile) survey area.

Each time the Queen Charlotte-Fairweather fault ruptures in a large-magnitude earthquake, the seascape on either side moves horizontally. Where the fault slices through submarine canyons, ridges, and slopes, the cumulative movement over several thousand years leads to a mismatch of those features. The offset landforms, or “piercing points,” are important indicators that we can use to calculate the average rate of fault motion and the typical recurrence interval for large earthquakes.

Other interesting features we observed include broad glacial troughs, moraines, and channels near the edge of the continental shelf, which probably deliver a tremendous volume of sediment to the continental slope. We also mapped hundreds of small underwater landslides as well as several larger slides. The team will evaluate the potential links between earthquakes, glacial sediment supply, and underwater landslides along the continental margin. This is an important task since earthquake-triggered landslides can generate dangerous tsunamis in southeast Alaska communities. For example, an earthquake-triggered rockfall in 1958 produced a deadly tsunami in Lituya Bay.

Second cruise: two weeks of nearly ideal weather

During the handful of summer weeks we had back in the office between cruises, we pushed hard to process and interpret the data collected on the R/V Medeia. We needed the results to plan for the second expedition aboard the privately owned R/V Norseman (USGS Survey 2016-656-FA). Scientists from the USGS Pacific Coastal and Marine Science Center (Danny Brothers, Amy East, Jackson Curie, Alicia Balster-Gee, and Daniel Ebuna, a University of California, Santa Cruz student contractor), and the USGS Woods Hole Coastal and Marine Science Center (Nathan Miller and Eric Moore) arrived in Seward on August 6 to set up equipment.

Left: close shot of scientists on the ship's deck preparing equipment; right: scientists connect cables to equipment on deck
Left: Jackson Currie and Alicia Balster-Gee connect hydrophone streamer sections aboard the R/V Norseman. Right: Jackson Currie (kneeling) and Dan Ebuna connect depth-control “birds” to the green and blue cables of the hydrophone streamer. The hydrophones record sounds bounced off sediment layers beneath the seafloor.
Brown lines across the image describe the fault, with labeled features, depth, and width
Multichannel seismic-reflection profile across the Queen Charlotte-Fairweather fault, acquired aboard the R/V Norseman in August 2016. Dashed red line in enlarged section at lower right is the Queen Charlotte-Fairweather fault. m, meter; km, kilometer; ms, millisecond.

The cruise began on August 8 with a short trip to Resurrection Bay near Seward to test the 80-channel hydrophone streamer and sparker sound source. After equipment testing and an unscheduled rescue operation (see bottom of page), we crossed the Gulf of Alaska for a two-week survey of the Queen Charlotte-Fairweather fault.

Early results look promising

We began at the south end of the study area near Noyes Canyon and worked our way northward. The team spent three days mapping fault-bounded basins offshore of Chatham Strait, near Sitka and the Mount Edgecumbe volcano, and the Yakobi Sea Valley. We endured a few days of 3-meter (10 foot) seas but otherwise had ideal weather and collected about 2,100 kilometers (1,300 miles) of seismic-reflection profiles.

Continuing the journey

Our inveterate team of explorers will use the 2015 and 2016 data to guide fieldwork in 2017, including multibeam mapping and seismic-reflection surveying in other areas of the fault zone. Collaborating with the Geological Survey of Canada and the Sitka Sound Science Center, we plan to use the mapping and seismic data to guide selection of sites for sediment coring. Back in the lab, we will use radiocarbon dating of core samples to measure sediment ages.

A group of scientists stand together on the deck of the research vessel for a photo
Scientists on the fantail of the R/V Norseman, with the hydrophone streamer (blue and green cables) and depth control birds (white cylinders) at their feet. Left to right: Amy East, Alicia Balster-Gee, Dan Ebuna, Danny Brothers, Jackson Currie, and Nathan Miller.

These sediment ages enable us to date fault activity during the past 10,000 years—the Holocene epoch. The ages also will help us understand links between long-term (1,000 year) fault movement and motions observed during major historical earthquakes.

The radiocarbon dates could help us establish when glaciers melted back from the edge of the continental shelf. In the late Pleistocene, more than 10,000 years ago, sea level was lower and Alaskan glaciers were much longer, extending across areas of the continental shelf that are now submerged. Some researchers think that humans migrated from Asia to North America along an ice-free coast before using an inland route. Knowing how long ago those glaciers retreated could determine when that coastal migration might have started.

Exciting discoveries continue to roll in with each field effort along the Queen Charlotte-Fairweather fault. We look forward to continuing the journey toward better understanding of the geologic, geohazard, and even ethnographic history of this continental margin.

Rescue of Three Stranded Boaters Opens August Research Cruise

Two researchers work on the deck of a large ship surrounded by cables
Dan Ebuna (USGS student contractor from University of California, Santa Cruz; left) and Jackson Currie (USGS) work on the R/V Norseman amid thick fog on Resurrection Bay. They are preparing to test equipment that will image sediment layers beneath the seafloor.

By Helen Gibbons and Danny Brothers

Scientists from the USGS were testing equipment in Resurrection Bay, Alaska, on August 8, 2016, when their research vessel received a distress signal from a small boat about 3 miles away. The privately-owned R/V Norseman steamed to the location and found three people stranded on a rocky beach after their skiff capsized in the surf. Two smaller vessels had attempted a rescue before the Norseman arrived, but large swells breaking off the beach nearly capsized them as well. The water was frigid, and so three Norseman crewmembers tossed survival suits into a rubber raft, lowered it into the water, and headed toward the beach.

Rather than motoring through the breaking waves and tricky currents, one of the crewmembers swam ashore. Wearing his own survival suit, he towed three more, plus a rope attached to the raft. The rescuer helped the stranded people suit themselves up, and one by one the crewmembers pulled the boaters through the surf and onto the raft. The operation took about an hour.

A fog-shrouded bay surrounded by lush green forested mountains.
Resurrection Bay on August 8, 2016. The water appeared calm in the shelter of the inner bay, but closer to the entrance, swells coming in from the Gulf of Alaska were breaking on a small beach where the three boaters had capsized.

“The guys working on the raft and in the water were exhausted when they made it back to the ship,” said Danny Brothers, a USGS geophysicist and lead scientist on the expedition. “Those survival suits aren’t exactly designed for strenuous exercise.”

Crewmembers welcomed the boaters aboard the Norseman, wrapped them in blankets, and gave them hot coffee. The ship dropped the rescued party off in Seward, then departed on time for a two-week expedition to map the Queen Charlotte-Fairweather fault off southeast Alaska.

“The survey was very successful, despite a few days of rough seas,” said Brothers. “I think the rescue gave us good karma.”

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