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Few detailed analyses exist for the majority of the sites that comprise the archaeological record of the 1845 Franklin Northwest Passage expedition. This paper presents the results of new investigations of an Inuit site (NgLj-9) at Erebus Bay on King William Island, Nunavut, containing materials derived from the 1845 Franklin expedition. The complex history of the origin and use of artifacts found at the site and its relationship to other Franklin sites and events associated with the expedition are revealed through the analysis and integration of archaeological, historical, and oral historical data.

On 22 April 1848, after three years in the Arctic, and 19 months spent ice-bound in northern Victoria Strait, the 105 surviving officers and crew of the Franklin Northwest Passage expedition deserted HMSErebusand HMSTerroras the first step of their escape plan. They assembled at a camp south of Victory Point on the northwest coast of King William Island and made the final preparations for the next step, a 400 km trek along the frozen seashores of King William Island and Adelaide Peninsula to the Back River. All of the men died before reaching their destination, and their remains have been found at 35 locations along the route of the retreat. These discoveries have played a central role in reenactments of events thought to have occurred during the failed attempt to reach the Back River and to the disastrous outcome of the expedition. This paper presents a summary of these findings and examines the criteria used to attribute them to the Franklin expedition. It is suggested that approximately one-third of the identifications have been based on information that is inadequate to confidently assign the human remains as those of Franklin expedition personnel.

In 2013, partial skeletal remains from three members of the 1845 John Franklin expedition were recovered from an archaeological site at Erebus Bay, King William Island, Nunavut. The remains included three crania, two of which were sufficiently intact to allow craniofacial reconstructions. Identifications are not proposed for either reconstruction; however, tentative identifications are being explored through DNA analyses currently underway that include samples obtained from both crania.

In the summer of 1845, under the command of Sir John Franklin, 128 officers and men aboard Royal Navy ships HMS Erebus and HMS Terror sailed into Lancaster Sound and entered the waters of Arctic North America. The goal of this expedition was to complete the discovery of a northwest passage by navigating the uncharted area between Barrow Strait and Simpson Strait. Franklin and his crew spent the first winter at Beechey Island, where three crewmen died and were buried. In September 1846, the ships became stranded in ice off the northwest coast of King William Island, where they remained until April 1848. At that time, the crew, reduced to 105, deserted the ships and retreated south along the island’s western and southern shores in a desperate attempt to reach the mainland and via the Back River, to obtain aid at a Hudson’s Bay Company Post. Sadly, not one individual survived. Previous analyses of bone, hair, and soft tissue samples from expedition remains found that crewmembers’ tissues contained elevated lead (Pb) levels, suggesting that Pb poisoning may have contributed to their demise; however, questions remain regarding the timing and degree of exposure and, ultimately, the extent to which the crewmembers may have been impacted. To address this historical question, we investigated three hypotheses. First, if elevated Pb exposure was experienced by the crew during the expedition, we hypothesized that those sailors who survived longer (King William Island vs. Beechey Island) would exhibit more extensive uptake of Pb in their bones and vice versa. Second, we hypothesized that Pb would be elevated in bone microstructural features forming at or near the time of death compared with older tissue. Finally, if Pb exposure played a significant role in the failure of the expedition we hypothesized that bone samples would exhibit evidence of higher and more sustained uptake of Pb than that of a contemporary comparator naval population from the 19th century. To test these hypotheses, we analyzed bone and dental remains of crew members and compared them against samples derived from the Royal Navy cemetery in Antigua. Synchrotron-based high resolution confocal X-ray fluorescence imaging was employed to visualize Pb distribution within bone and tooth microstructures at the micro scale. The data did not support our first hypothesis as Pb distribution within the samples from the two different sites was similar. Evidence of Pb within skeletal microstructural features formed near the time of death lent support to our second hypothesis but consistent evidence of a marked elevation in Pb levels was lacking. Finally, the comparative analysis with the Antigua samples did not support the hypothesis that the Franklin sailors were exposed to an unusually high level of Pb for the time period. Taken all together our skeletal microstructural results do not support the conclusion that Pb played a pivotal role in the loss of Franklin and his crew.

Historical and archaeological records are examined for three archaeological sites at Erebus Bay, King William Island, associated with the 1845 John Franklin expedition. Comparison of 19th century historical descriptions with archaeological data from sites NgLj-1 and NgLj-3 establishes that the identification of NgLj-1 as the site of the 1859 McClintock “boat place” is incorrect and that NgLj-3 is the actual site. An assessment of 19th century oral historical information and contemporary archaeological data from NgLj-2 supports the conclusion that a ship’s boat from the Franklin expedition was once located at the site, but its identification as the second “boat place” discovered by Inuit in 1861 is problematic. The study underscores interpretive risks associated with uncritical acceptance of historical and oral historical accounts and the importance of archaeological research in the reconstruction of events surrounding the fate of the Franklin expedition.

A chert cobble from an archaeological quarry on southern Baffin Island, Canada, was divided and crushed using five different methods: i) agate mortar and pestle, ii) stainless steel shatterbox, iii) tungsten carbide shatterbox, iv) alumina ceramic shatterbox, and v) zirconia ceramic shatterbox. Powders produced by each method were submitted for acid digestion and analysis by inductively coupled plasma mass spectrometry. The trace element results indicate that different crushing media can contribute significant trace element contamination to chert during the grinding process. These results demonstrate the need for an informed approach to the selection of sample preparation methods when submitting archaeological samples for solution or pellet based geochemical analysis.

In 1999 a team of geologists discovered an archaeological site near Cape Southwest, Axel Heiberg Island. On the basis of its location and the analysis of two artifacts removed from the site, the discoverers concluded that it was a hastily abandoned campsite created by Hans Kruger’s German Arctic Expedition, which was believed to have disappeared between Meighen and Amund Ringnes islands in 1930. If the attribution to Kruger were correct, the existence of this site would demonstrate that the expedition got farther on its return journey to Bache Peninsula than previously believed. An archaeological investigation of the site by the Government of Nunavut in 2004 confirmed its tentative attribution to the German Arctic Expedition but suggested that it is not a campsite, but the remains of a deliberately and carefully constructed cache. The finds suggest that one of the three members of the expedition may have perished before reaching Axel Heiberg Island, and that the survivors, in order to lighten their sledge, transported valued but heavy items (including Kruger’s geological specimens) to this prominent and well-known location to cache them, intending to return and recover them at some later date.

Lieutenant William R. Hobson’s 1859 search for traces of the Franklin expedition on the west coast of King William Island resulted in several major discoveries that include an official record containing the dates of Sir John Franklin’s death, of the abandonment of HMS Erebus and HMS Terror , and of the departure of the ship’s company for the Back River. Information derived from Hobson’s report appeared in McClintock’s published account of the expedition, and it has been referenced in other works, but the report itself was never published. Recent investigations of Franklin archaeological sites on the Victoria Strait coast of King William Island by the Government of Nunavut, including sites first discovered by Hobson, served as a catalyst for locating Hobson’s full descriptions of his findings. The report includes general observations on weather, ice conditions, and wildlife encountered, and his detailed descriptions of several Franklin expedition sites are potentially valuable sources of information for ongoing archaeological investigations.

Despite an immediate need for northerners trained in cultural resource management and the strong desire of many northern communities to direct historical research, there continue to be few opportunities for students to receive formal training in heritage research. A promising new approach is the Tungatsivvik Archaeological Project, which since 1991 has been part of the Environmental Technology Program offered through Arctic College's Nunatta Campus in cooperation with the community of Iqaluit. Integrating lectures, field exercises, lab analyses, and community reporting, the program allows students and community members alike to acquire technical knowledge and skills they can use to develop community-based heritage programs. The more than 100 features identified at the site, where excavations in the first two seasons have yielded more than 2000 artifacts and 7000 animal bones, include late prehistoric (Thule culture) dwellings, food caches, kayak stands, and burials. Results of the project are being actively integrated into local educational and interpretative structures, as community members from elders to school children participate in "making history come alive." Key words: Baffin Island, archaeology, Arctic College, community-based research, cultural resource management, heritage training, Nunavut

Two documents were recovered from a cairn located at the northern extremity of Nettilling Lake, Baffin Island. They record the details of J. Dewey Soper's winter expedition to Foxe Basin in 1926 and the travel itinerary of an Inuit hunting party. Key words: arctic exploration, Baffin Island, archaeology, cairns, Dewery Soper, Nettilling Lake