History is never completely written. There are always new discoveries, new understanding.
NOAA historian John Cloud recently sent Coast Survey an intriguing report:
Yesterday I was looking for some historic Chesapeake Bay T sheets [topography drafts]… Anyway, down in the bottom of a folder, there was a zipped file, dated 2009, never unzipped. I thought: well, since I have noticed this now, why don’t I unzip it? It turned out to be two overly rescaled jpgs, but using my Keith Bridge tricks [a technique developed by a former Coast Survey historical chart expert] I found the two full-scale originals. It was one chart, with a small part cut off to make two separate files: the original 1838 hydrography for New Haven Harbour!
This is the basis for the 1838 engraved chart for Congress, the second published Coast Survey chart. (The first was based on Lt. Gedney’s partial survey of Newark Bay, NJ and the mouth of the Hackensack River, 1837.) The New Haven work was 1838. In 1839, the same Lt. Gedney and company captured the slave ship Amistad and brought the ship and captives to New Haven, claiming the escaped slaves as property. [UPDATE, 10/27/2016: Delving deeper into Gedney’s actions, it turns out he docked the ship in New London, while the captive Africans were brought to New Haven.] Then later, John Quincy Adams persuaded a judge they had freed themselves on the boat and were no longer slaves.
Unzipping the files happened within an hour or so of getting an email from Michelle Zacks, a scholar of marine environmental history who has explored historic Coast Survey field survey notebooks as sources for her ongoing project on the antebellum oyster industry and the lives of enslaved and free African Americans in the Chesapeake region. That research helped lead to her new job, as the associate director of the Gilder Lehrman Center for the Study of Slavery, Resistance, and Abolition, at Yale, which is in: New Haven!
It all happened just like that! Like the chart “wanted” to emerge back into the Amistad story.
We weren’t able to trace the origination of that zip file, but it was obviously created by someone who didn’t realize the value of the historical images. And this, ladies and gentlemen, is why we value historians.
National Weather Service image of Hurricane Matthew near Port Canaveral, Florida on October 7, 2016.
As Hurricane Matthew bore down on Florida, Georgia, and South Carolina, Coast Survey pre-positioned hydrographic survey vessels for immediate deployment, to help speed the reopening of commercial shipping at ports hit by high winds and storm surge.
Currently, our Central Coast Gulf navigation manager, Tim Osborn, embedded in Port Canaveral, Florida, and our Southwest navigation manager, Kyle Ward, are coordinating marine transportation system recovery priorities with the U.S. Coast Guard and port stakeholders in Florida, Georgia, South Carolina, and North Carolina.
Speeding the resumption of commercial vessel traffic has important human and economic considerations. For instance, Port Canaveral experienced winds over 60 knots and wave heights over 30 feet. Cruise ships are awaiting port entry and with about 3,000 passengers per ship, that is over 30,000 passengers (~15,000 crew) waiting for the port to be re-opened.
Video: Port Canaveral experiencing high winds from Hurricane Matthew on October 7, 2016.
An additional aid in the preparation for a hydrographic survey response is anticipating where and how big the storm surge will be along the coast. Just prior to the arrival of Hurricane Matthew, NOAA’s nowCOAST™ updated its system with the National Hurricane Center’s (NHC) potential storm surge flooding map which depicts the risk associated with coastal storm surge flooding resulting from tropical cyclones.
NHC’s first potential storm surge flooding map for Hurricane Matthew on nowCOAST.
On September 15, 2016, President Obama designated the first marine national monument in the Atlantic Ocean. The Northeast Canyons and Seamounts Marine National Monument includes two areas: one that includes four undersea mountains, called “seamounts” – Bear, Mytilus, Physalia, and Retriever; and an area that includes three undersea canyons – Oceanographer, Lydonia, and Gilbert – that cut deep into the continental shelf. These sea features have monumental histories.
Coast Survey cartographer Leland Snyder used several data sources to create this map of the Northeast Canyons and Seamounts Marine National Monument.
Bear, Mytilus, and Physalia Seamounts were discovered by oceanographers with Woods Hole Oceanographic Institution, and they were named for small Woods Hole vessels that began making forays into the deep sea in the 1950s. The Bureau of Geographical names does not know the origin of the name “Retriever Seamount,” but NOAA historian Skip Theberge thinks it was probably discovered and named for the Cable Repair Ship Retriever, which started service in 1961 working off the East Coast. The canyons were named in the 1930s, for U.S. Coast and Geodetic Survey ships. (C&GS is the earliest NOAA predecessor agency.) Oceanographer Canyon was named for the C&GS Ship Oceanographer, which discovered many canyons incising the continental slope between the Georges Bank area and Cape Hatteras; Gilbert Canyon was named after the C&GS Ship Gilbert, which took an active part in the survey of the Georges Bank, 1930-32; and Lydonia Canyon was named for the C&GS Ship Lydonia.
The monument, which encompasses 4,913 square miles, has been the subject of scientific exploration and discovery since the 1970s. But the original discoveries of the canyons were made more than 80 years ago, when the U.S. Coast and Geodetic Survey surveyed the canyons with TNT bombs.
Yes, you read that right.
Some of the C&GS ships in the 1930s were anchored-station vessels, hanging a hydrophone over the side at a well-determined point. TNT bombs were thrown over the sides at about fifteen minute intervals. The explosion being “time zero,” the sound waves traveled through the water to the hydrophone, which in turn activated an automatic radio signal back to the survey vessel. The time interval between reception of radio signal and time of explosion, times the velocity of sound in sea water, gave the distance. This system, called “radio-acoustic ranging,” was developed by C&GS as the first non-visual survey system.
The survey of these canyons, using (for then) modern methods gave an unprecedented view of the seafloor generating debates as to the cause of the canyons, and in a larger sense, generating the birth of marine geology. Indeed, Dr. Francis Shepard, recognized by many as the “father of marine geology,” got his start on these surveys.
This excerpt from International Aspects of Oceanography, a National Science Foundation publication, was written by Wayland Vaughn of the Scripps Institution of Oceanography in 1937. He describes the contribution of both echo-sounding and the navigation system termed “radio-acoustic ranging” to the mapping of the seafloor. C&GS developed RAR and used it to survey U.S. continental margins in the 1930s.
The history of these early explorations is fascinating. So as not to give it short shrift, we are going beyond our normal blog post format and including a full-length article contributed by NOAA’s historian, retired Capt. Skip Theberge.
♦ ♦ ♦
A History of Exploration and Discovery in the Northeast Canyons and Seamounts Marine National Monument
By Capt. Albert “Skip” Theberge, Jr., NOAA (retired), Acting Chief of Reference, NOAA Central Library
The recent designation of the Northeast Canyons and Seamounts Marine National Monument is the culmination of over eighty years’ involvement in this area by NOAA and its predecessor agencies. It is no accident that the canyons in this area were named for ships of the U.S. Coast and Geodetic Survey (C&GS), NOAA’s oldest ancestor agency. Oceanographer, Gilbert, and Lydonia Canyons were named for three of the four ships that conducted surveys of the area between the years 1930 and 1932. The fourth ship, Welker, is commemorated by the naming of Welker Canyon, just to the west of the new monument boundaries, and a fifth ship, Hydrographer, was commemorated by the naming of the next canyon to the west of Welker Canyon. These ships completed the first comprehensive survey of the continental slope in this area, using the most modern equipment available: a combination of advanced echo-sounding equipment and the radio-acoustic ranging system, the first survey-quality non-visual navigation system. This system was developed in the Coast and Geodetic Survey.
C&GS map of submarine valleys on Georges Bank, 1932
Besides being used for navigational charts, the data from these surveys was used in a number of scientific publications, first by Francis Shepard, known as the father of marine geology. Although going on to become a famous Scripps Institution of Oceanography scientist, some of his earliest work was initially published in the Bulletin of the Field Engineers of the Coast and Geodetic Survey. However, the greatest work associated with these surveys was a paper published in 1939 by the geologist A.C. Veatch and the brilliant C&GS officer Lieutenant Paul Smith. This paper was titled “Atlantic Submarine Valleys of the United States and the Congo Submarine Valley” and was Geological Society of America Special Papers Number 7. Included in this paper was a beautiful map that extended from Lydonia Canyon on its northeast corner to Norfolk Canyon off Chesapeake Bay at its southern limit. Shown on this map were thirteen named canyons as well as a number of other canyons incised in the continental shelf.
This map served to call the attention of the geological community to the rugged and grand nature of the seafloor, previously believed by many to be bland and featureless. It also served to ignite a fierce debate in the scientific community regarding the mode of formation of canyons. There were two competing theories. The first theory was that the canyons formed sub-aerially with sea level dropping as much as 10,000 feet worldwide. The second theory was that sediment-laden density currents carved out the canyons. Both theories had influential backers but, ultimately, as a result of Woods Hole Oceanographic Institution (WHOI) sediment sampling in the early 1950s on the oceanic extension of Hudson Canyon, the density current theory won out as layers of poorly graded sands and gravels were found far at sea. This, combined with knowledge of the sequential breaking of further downslope submarine cables over a period of 13 hours following the 1929 earthquake on the Grand Banks, served to prove the concept of density currents.
The Second World War brought new studies in this area as the continental shelf and slopes of the United States were the locus of fierce submarine warfare. Woods Hole Oceanographic Institution and the Coast and Geodetic Survey combined efforts to map the location of known shipwrecks and bottom sediment types on a series of charts extending from east of Georges Bank to the tip of Florida. This was not WHOI’s first work in the area, as Maurice Ewing had conducted early seismic reflection and refraction experiments in this area before the war.
C&GS issued chart 1107-A in 1943, showing names of canyons. This was a restricted chart (used in anti-submarine warfare) overprinted with bottom characteristics and known shipwrecks.
Following the war, WHOI sent numerous expeditions into the Atlantic and discovered three of the seamounts included in the Northeast Canyons and Seamounts National Marine Monument. These three were Bear, Mytilus, and Physalia and were named for small inshore vessels operated by WHOI. Although the earliest mention of these seamounts in the unclassified literature was in 1962, John Ziegler of WHOI first discovered and named these features in 1955 on a classified survey. A prototype Heezen-Tharp physiographic diagram that was probably produced in the mid-1950s clearly shows the New England Seamount Chain and seamounts in the vicinity of the three Woods Hole seamounts of the monument. The fourth seamount in the monument, Retriever Seamount, was probably discovered by and named for the cable repair ship Retriever which operated off the east coast of the United States in the early 1960s.
Geological discovery and interpretation of the canyons and seamounts dominated research until the late 1960s. At this time, studies began of the dynamic oceanography of Oceanographer and other New England canyons. The first manned submersible dives into the canyon also occurred at this time, with 1966 Alvin dives followed in 1972 and 1974 by dives in the Navy’s nuclear research submersible NR-1. Oceanographer Bruce Heezen was aboard and suggested a “balanced concept in which canyons are created by some tectonic forces or drowned river valleys, are shaped and kept alive by the tides and are coursed by turbidity currents at certain long term intervals when especially large supplies of sediment are delivered to the heads of their system.” In the late 1970s and early ‘80s, there were sporadic efforts to begin studying the biology of the canyon systems, which has continued up to the present day. Since 2000, there has been a significant increase in studies related to these systems. The first dive on a seamount of the new monument was made on July 24, 1968, on Bear Seamount, by K. O. Emery in the submersible Alvin. Minimal information was obtained, but in 1974 a series of dives was made from the vicinity of Corner Seamount to Mytilus Seamount under the direction of James Heirtzler as chief scientist. In his words, this was the first time that “man had directly viewed the expanse of the earth between the Mid-Atlantic Ridge and the North American continent.” Dive 7, the final dive, was made on Mytilus Seamount; it was described as “unique” as it is capped by approximately 300 meters of shallow water reef material. As this occurs at a depth of over 3,000 meters, it is apparent that this seamount has subsided over two miles while being rafted to the northwest from its original location over the Great Meteor hotspot.
Biological studies of these seamounts did not begin in earnest until 2000, when NOAA Ship Delaware II made 20 exploratory trawls in the vicinity of Bear Seamount. Over 270 species were collected including 115 fish species, 26 cephalopod species, and 46 crustacean species. Over the next thirteen years, NOAA’s Office of Ocean Exploration and Research (OER) followed up the fisheries cruise with a number of expeditions to the vicinity of the newly designated national monument. The first of these cruises was the 2003 Mountains in the Sea Expedition which, following in the footsteps of Heirtzler years earlier, used the submersible Alvin to dive on Manning and Kelvin seamounts and conduct multibeam surveys of Bear Seamount. As opposed to the primarily geologic emphasis of the earlier dives, though, these concentrated on the remarkable biological diversity of the New England Seamount Chain. This expedition was followed by Mountains in the Sea 2004, in which the use of robotic vehicles instead of a manned submersible was used to conduct explorations. 2004 saw Retriever, Balanus, and Bear Seamounts explored and the acquisition of hundreds of spectacular photos of the seafloor. 2005 saw the North Atlantic Stepping Stones expedition which, although not studying seamounts in the national monuments, did explore a number of seamounts of the New England Chain. In 2012, NOAA ocean exploration ship Okeanos Explorer returned to the northeast continental shelf and slope area on the Northeast and Mid-Atlantic Canyons mapping expedition. This expedition was primarily concerned with multibeam mapping of the various canyons, including those in the monument, as preparation for the 2013 Northeast U.S. Canyons Expedition that investigated Oceanographer, Lydonia, and Gilbert Canyons, other large canyons of the regions, and Mytilus Seamount. This expedition marked the first use of NOAA’s 6,000 meter-rated remotely operated vehicle, Deep Discoverer and its accompanying Seirios camera sled which enabled telepresence ocean exploration. With this technology, OER was able to provide scientific and public audiences onshore a real-time view of ocean discovery in the grand canyons and hidden mountains of our Atlantic Ocean frontier.
Over eighty years of discovery and exploration, much of it accomplished by NOAA, its predecessor agencies, and academic partners have led to President Obama’s presidential proclamation of the Northeast Canyons and Seamounts Marine National Monument. The monument will assure that the unique ecosystems of this fragile area will be protected for posterity.
By Ensign Michelle Levano
NOAA Ship Rainier recently arrived in Uganik Bay, off of northwest Kodiak Island, to complete hydrographic survey operations in Uganik Passage and Uganik Bay, including the Northeast Arm, North Arm, and South Arm. Rainier has spent 2013 through 2016 surveying areas around North Kodiak Island, including Kizhuyak Bay, Whale and Afognak Passes, Kupreanof Strait, and Viekoda and Terror Bays. The ship will remain in Uganik Bay until the end of October.
Rainier completed project areas H12916, H12919, and H12848 in the spring. They are now surveying H12693 south through H12849 and H12918.
Rainier is using multibeam sonar technology to acquire high-resolution seafloor mapping data to provide modern chart updates that support Kodiak’s large fishing fleet and higher volumes of passenger vessel traffic. Some of the data appearing on NOAA’s charts in this area are from surveys conducted between 1900 and 1939. (See the source diagram in the bottom left corner of NOAA chart 16597.) However, this is not Rainier’s first visit to Uganik Bay. In the early 1970s, Rainier was in the same vicinity performing survey operations and installing survey stations at Broken Point, Uganik Bay, and Shelikhof Strait.
Rainier crew at Broken Point, Uganik Bay, in the 1970s
Commissioned in 1968, NOAA Ship Rainier has a 48-year history in NOAA’s fleet of research ships and aircraft. Homeported at NOAA’s Marine Operations Center-Pacific in Newport, Oregon, she is operated and managed by NOAA’s Office of Marine and Aviation Operations. The 231-foot Rainier is one of four hydrographic survey ships in the NOAA fleet that support the nautical charting mission of NOAA’s Office of Coast Survey to keep mariners safe and maritime commerce flowing. The ship, her four aluminum survey launches, and other small boats collect data that is used to update nautical charts and inform decisions on coastal science and management.
NOAA Ship Rainier at anchor, in Uganik. Photo by Ensign Dylan Kosten
One of Rainier‘s four launches at work in Uganik Bay.
Each of Rainier’s small boat launches has modern sonar systems that gather data nearshore as well as offshore. Additionally, the ship itself has a sonar system mounted to her hull for offshore operations. This information can provide bottom seafloor habitat characterization for sustainable fisheries initiatives, and provide data for ocean tourism and recreational fishing.
If you happen to be in the area, and see a white hull with S-221 painted on her bow, please do not hesitate to contact the ship to acquire more information regarding the ship and her mission. Rainier monitors VHF channels 13 and 16. Or, email Rainier’s public affairs officer at firstname.lastname@example.org.
By Ensign Max P. Andersen
Formed by retreating ice sheets over 14,000 years ago, the Great Lakes have long represented one of the most valuable fresh water resources in North America. They contain more than one-fifth of the world’s supply of fresh surface water, and the vast size is easily visible from space. From Native American hunting routes to French fur-trade exploration to influential battles in the War of 1812, the Lakes have proved a key platform for numerous historical events that shaped the development of the country.
Uniquely, these bodies of water served as the gateway to connect the booming production of an expanding population in the Midwest from 1825 to 1925. During this time, a broad range of wooden, sailing, and steam-powered ships trekked across the lakes, carrying coal, grain, and passengers. Due to unpredictable weather conditions, fire, ice, high-traffic areas, and an ever-increasing pressure to meet shipping quotas, hundreds of ships were lost in collisions and accidents. These incidents have earned this period the nickname “Shipwreck Century.” Today, the history of the “Shipwreck Century” is presented at Thunder Bay National Marine Sanctuary’s visitor’s center, the Great Lakes Maritime Heritage Center, in Alpena, Michigan.
Thunder Bay is located in Lake Huron, near one of the most historically dangerous areas of navigation in the Great Lakes. The sanctuary covers 4,300 square miles. In this area, over 200 shipwrecks are known to exist, and 92 have been discovered and accurately charted. The staff provides continual archaeological monitoring to ensure the preservation of the sites.
Much of this archaeological work is completed aboard research vessel (RV) Storm. Storm is operated by the NOAA Great Lakes Environmental Research Laboratory (GLERL) and is dedicated to supporting Thunder Bay National Marine Sanctuary. Storm is suited for a diverse range of projects and is equipped with multibeam and side scan sonar for survey projects, compact crane for using remotely operated underwater vehicles, and drop-down transom for handling diving equipment. Additionally, her use of B100 fuel – engine and hydraulic oil manufactured from vegetable oils – and redesign with recycled materials qualify her as one of NOAA’s “green ships.”
Traditionally, the survey systems on Storm have been primarily used to provide accurate locations and high-resolution acoustic imagery of shipwrecks. Using these positions and contextual images, teams of Thunder Bay NMS archaeologists can complete dives to see the submerged cultural resources that lie beneath the surface. They share that information with the public at the Great Lakes Maritime Heritage Center.
A side scan sonar provided this acoustic image of W.C. Franz shipwreck.
With recent increases in multibeam and side scan sonar proficiencies, the sanctuary has started a new collaboration with the Office of Coast Survey. This summer, Coast Survey physical scientist Tyanne Faulkes and Ensign Max Andersen assisted Capt. Travis Smith and maritime archaeologists John Bright and Phil Hartmeyer in a new project. The team was tasked with surveying two unique sites: an Air Force and Air National Guard live-fire testing range, and a high-traffic area that needed updated navigational charts. The teams used RV Storm as a “vessel of opportunity” (a vessel not normally used for charting surveys) to conduct surveys to charting specifications. As such, some of Storm’s survey equipment needed to be “tuned” to meet those stringent hydrographic requirements. After some trial and error, Storm’s Applanix POSMV, Reson 8101, Klein 3000, Castaway CTD, Hypack 2016 machine were operational and ready for data acquisition.
NOAA marine archaeologist Phil Hartmeyer acquired survey data for the project.
The survey operations were a tremendous success. Throughout the month of August, Storm completed a series of acquisition voyages – as weather permitted – including a 36-hour operation on August 17 and 18. They acquired charting data covering 28 square nautical miles, along 418 linear nautical miles.
Projects like this show the great gains for the scientific community when different partners collaborate. We are looking forward to using more vessels of opportunity to expand on nautical chart updates in the Great Lakes region.
The two project survey areas for chart updates are shown by the colored bathymetry. The area on the right (in blue and green) was surveyed in response to a military request.
Just over a year ago, Coast Survey began testing the use of small unmanned surface vehicles (USV) to survey the shoalest depths, areas along the shore where NOAA ships and their launches are unable to reach. These USVs proved beneficial not only for mapping shallow, murky waters, but also for improving the efficiency of our hydrographic operations. So what is the next step in evaluating USV technology? Testing larger, longer-lasting USVs and taking them beyond shallow waters.
This September, Coast Survey is partnering with the National Centers for Coastal Ocean Science (NCCOS), the Office of Marine and Aviation Operations (OMAO), NOAA Ship Nancy Foster, and ASV Global, an unmanned vehicle manufacturer, to conduct an operational evaluation of a USV, called the C-Worker 5, during a bathymetric and marine habitat survey offshore of the Carolinas.
A USV is an unmanned small boat that can be remotely operated and monitored from a control station aboard the host ship, and can also be programmed to drive pre-planned survey lines while operators monitor vehicle and data collection systems.
The C-Worker 5 is 5.5 meters and powered by a 57 horsepower diesel engine and can operate for up to five days before requiring recovery and refueling. It is equipped with a Reson 7125 multibeam bathymetric sonar system, similar to systems carried by Nancy Foster, and each can survey a swath of ocean that is about four times as wide as the water depth.
The C-Worker 5 USV is being operated remotely by ASV Global personnel aboard Nancy Foster during testing prior to departing for offshore survey operations.
Video and navigation data from the C-Worker 5 is streamed to the ship by telemetry where shipboard technicians keep the vessel safe while monitoring its performance and data quality.
During the cruise, Coast Survey personnel, with support from ASV Global, are evaluating the operational capabilities of C-Worker 5 as it conducts hydrographic survey operations in coordination with Nancy Foster. Coast Survey will use the experience to create a transition path for using USVs in support of routine hydrographic surveys. OMAO will evaluate the shipboard requirements for hosting and operating unmanned systems. The data collected will support NCCOS’s mission to conduct ecological characterizations of hard bottom and rocky reef essential fish habitats in the southeast U.S. Atlantic waters to guide ecosystem management and ocean planning.
The C-Worker 5 USV recovery alongside the Nancy Foster on Saturday, 9/10, after conducting a multibeam sonar system calibration test, known as a patch test.
NOAA Ship Nancy Foster as seen from the C-Worker 5 USV. During this mission, the USV and Nancy Foster surveyed approximately three km apart from each other and will continue for three to four days before the USV is recovered to fuel and exchange data storage drives.