Date: July 7, 2019
Location: Lat: 36.35208°, Lon: -74.62602°
Dive Depth Range: 1,469 - 1,642 meters (4,820 - 5,387 feet)
Access Dive Summary and ROV Data
Today we dove about 70 miles off the coast of North Carolina, at the base of a portion of the Currituck Landslide. This submarine landslide is estimated to have occurred between 25,000-50,000 years ago, when sea level was about 200 meters (656 feet) shallower. As the eastern seaboard is not immune from this kind of geologic activity in the future, it is important to characterize this kind of activity in order to ground-truth geohazard models as scientists attempt to understand what could trigger such activity, and what the impacts of such an event could be.
Our dive was delayed by a couple of hours due to high winds, waves, and currents during the drift test this morning, but fortunately, conditions improved and we were able to launch the remotely operated vehicle (ROV) at approximately 10:00 ET. We reached the seafloor near the base of the feature and dove a vertical track up the wall at the steepest slope indicated by bathymetry. The first part of the dive was over soft, fine sediment with some rocks and boulders scattered on the seafloor. A number of ophiuroid brittle stars, sea pens (Umbellula sp. and Kophobelemnon sp.), urchins, and fish (notably halosaurs, sorcerer eels, cusk eels, macrourids, and eelpouts) were seen among the soft sediment.
As the bottom below us became slightly more rocky, a number of Flabellum cup corals were observed, and one specimen was sampled using the suction sampler. A benthic ctenophore attached to a remnant stalk was also sampled. At a depth of approximately 1,550 meters (5,085 feet), the bottom became steeper and more rocky. A number of brisingid starfish were seen on the rocky outcrop, in addition to some sponges and anemones. Surprisingly, the rock surface did not have as much sessile organism settlement as we might have expected in such an area. Towards the top of the feature, a geologic rock sample was collected. Upon inspection, it appeared that the underlying rock is a relatively soft mud or siltstone with a large number of burrow holes.