Preliminary Report: Evaluating the Potential of Archaeogeophysical Surveying on Viking Age and Medieval Sites in Greenland, 2 – 16 August, 2010

The primary goal of this research is to begin to overcome biases in the Greenlandic Norse archaeological record. Assessing the establishment dates and organization of Norse sites in Greenland is difficult because substantial cultural deposits can be hidden under deep windblown sand deposits as well as later occupations. Shallow geophysical methods were used to help recover information on the nature, extent and depth of subsurface cultural deposits. Assessing these site characteristics is a first step in overcoming the bias towards the later, the larger, and the more visible sites in the archaeological record. Norse Greenland presents a relatively visible medieval landscape with many ruins preserved on the surface. Survey archaeologists have taken advantage of these conditions to do comprehensive surveys of Norse settlements producing inventories of farm buildings and settlements (Guldager, et al. 2002; Keller 1990). Coring surveys and excavation at known sites have demonstrated that some sites are buried under significant aeolian deposits and that areas within many other sites can be deep and contain ruins that are not visible on the surface. In many cases Viking Age deposits cannot be accessed by archaeological excavation, as this would damage later occupational phases. In these cases, application of archeogeophysics may be the only way to assess this unique cultural history. The identification, characterization, and dating of these subsurface architectural remains are critical to systematic survey programs and to the production of regional settlement patterns and chronologies that can help explain the ecological and political dynamics of Norse colonization, land use, and the eventual demise of Norse Greenland. Over the past 10 years the Skagafjörður Archaeological Settlement Survey (SASS) has developed an intensive subsurface survey protocol to systematically recover, date, and characterize Viking Age landscapes in Iceland. While we believe the SASS subsurface protocol can be effective in Greenland there are many questions that must be resolved before any wide-scale application of the methods can be developed. The project set out to address two basic questions: (1) what is the actual subsurface record at Norse sites, and (2) which methods work best and how are they most effectively employed? In this initial investigation, we tested and adapted this protocol to conditions in Greenland. We hope that the preliminary test of these methods will significantly expand the range of sites and periods accessible to researchers working in Greenland and allow for new questions regarding the long-term political and environmental histories of the region. The successful integration of archaeogeophysics with archaeological survey and excavation will result in a more holistic approach to the preservation of Norse archaeological sites in Greenland. These sites suffer from increased modern impacts resulting from mineral exploitation, sheep farming, and tourism. Additionally, there is now total summer sub-surface thaw and conditions that were once ideal for preserving organic remains are now deteriorating, especially in well-drained areas. In the coming years the Greenland National Museum will begin a program of scheduling and protecting some of these sites. We believe that the application of archaeogeophysics could be a great asset in determining which sites are in danger and worthy of preservation

Results of Archaeogeophysical Surveying at the Great Friends Meeting House in Newport, Rhode Island

Archaeogeophysical surveys were carried out in October 2010 over a 30 x 50 m grid that was established immediately to the north and west of the north end of the Great Friends Meeting House (GFMH) in Newport, RI. The surveys were conducted using a Geonics EM-38 RT ground conductivity meter and a Malå X3M Ground Penetrating Radar (GPR) system that was equipped with 500 and 800 MHz antennas. In addition, a resistance survey was performed over a much smaller central area using a Geoscan RM15 resistance meter. From this work three types of geophysical anomalies have been identified: those associated with individual features, structures, and graves. There may be one large structure to the north of the GFMH with a similar alignment. Forty-two anomalies were identified that are consistent with graves. There are many more anomalies that have not been specifically interpreted as graves because they did not meet enough of our criteria but may indeed be graves. We recommend that additional archaeogeophysical surveys be performed as well as a series of follow-up excavations to ground truth the interpretations

Egg on Hegranes: Geophysical Prospection, Coring, & Test Excavations—Report 2016

This report describes the 2016 archaeological work at the farm of Egg is in the southernmost part of Hegranes, North Iceland

Unconfined Aquifer Flow Theory - from Dupuit to present

Analytic and semi-analytic solution are often used by researchers and practicioners to estimate aquifer parameters from unconfined aquifer pumping tests. The non-linearities associated with unconfined (i.e., water table) aquifer tests makes their analysis more complex than confined tests. Although analytical solutions for unconfined flow began in the mid-1800s with Dupuit, Thiem was possibly the first to use them to estimate aquifer parameters from pumping tests in the early 1900s. In the 1950s, Boulton developed the first transient well test solution specialized to unconfined flow. By the 1970s Neuman had developed solutions considering both primary transient storage mechanisms (confined storage and delayed yield) without non-physical fitting parameters. In the last decade, research into developing unconfined aquifer test solutions has mostly focused on explicitly coupling the aquifer with the linearized vadose zone. Despite the many advanced solution methods available, there still exists a need for realism to accurately simulate real-world aquifer tests

Results of Archaeogeophysical Investigations of the Fowler - Clark Farm Mattapan, Boston, Massachusetts

Ground penetrating radar (GPR) and Frequency-Domain Electromagnetic (FDEM) surveys were employed over an extensively modified 50 m x 65 m city lot containing a farmhouse initially constructed between 1786 and 1806 and a later barn. Both geophysical methods suggested that most of the lot had experienced substantial disturbance and that there was limited sub - surface preservation. Both the GPR and EM surveys indicated a scatter of metallic debris and other disturbance s in the back yard at depths up to 1 m. Most of the front yard also presents as disturbed, except for two unusual but limited buried surfaces that were identified in the GPR. Three 50 cm x 50 cm shovel test pits in these two areas confirmed the presence of preserved surfaces or at least archaeological deposits, under more than 65 cm of unremarkable fill

Keflavík on Hegranes: Cemetery Excavation—Interim Report2015

The summer of 2015 was the first of three planned years of excavations at the early Christian cemetery at farm Keflavík on Hegranes in the region of Skagafjörður, North Iceland. The excavation is the third phase of Skagfirska kirkjurannsóknin (Skagafjörður Church Project) and is a collective effort of the Skagafjörður Heritage Museum and the Fiske Center of the University of MassachusettsBoston. The collective project goes by the name Skagafjörður Church and Settlement Survey (SCASS). The excavation season started on the 6thof July and finished on the 14thof August. The first two weeks were spent cleaning the surface and removing a 20thcentury rubbish heap overlying the western part of the cemetery, the actual cemetery excavation extended over four weeks

Hegranesþing on Hegranes: Geophysical Prospection Interim Report 2013 – 2015

Geophysical surveys were conducted at Hegranesþing on Hegranes in North Icelad during the summers of 2013 and 2015

Data from: Encoding of wind direction by central neurons in Drosophila

Wind is a major navigational cue for insects, but how wind direction is decoded by central neurons in the insect brain is unknown. Here we find that walking flies combine signals from both antennae to orient to wind during olfactory search behavior. Movements of single antennae are ambiguous with respect to wind direction, but the difference between left and right antennal displacements yields a linear code for wind direction in azimuth. Second-order mechanosensory neurons share the ambiguous responses of a single antenna and receive input primarily from the ipsilateral antenna. Finally, we identify novel “wedge projection neurons” that integrate signals across the two antennae and receive input from at least three classes of second-order neurons to produce a more linear representation of wind direction. This study establishes how a feature of the sensory environment—wind direction—is decoded by neurons that compare information across two sensors

Të dhëna mbi kronologjinë absolute të arkeologjisë shqiptare: datime radiokarboni AMS nga Apollonia dhe Lofkëndi / Towards an Absolute Chronology of Albanian Archaeology: AMS Radiocarbon Dates from Apollonia and Lofkënd

Damiata Brian N., Papadopoulos John K., Gracia Amore Maria, Morris Sarah, Bejko Lorenc, Marston John M., Southon John. Të dhëna mbi kronologjinë absolute të arkeologjisë shqiptare: datime radiokarboni AMS nga Apollonia dhe Lofkëndi / Towards an Absolute Chronology of Albanian Archaeology: AMS Radiocarbon Dates from Apollonia and Lofkënd. In: Iliria, vol. 33, 2007. pp. 135-185

Quantifying surplus and sustainability in the archaeological record at the carthaginian-roman urban mound of zita, tripolitania

Cultural ecological theory is applied to a spatially and temporally bounded archaeological data set to document long-term paleoeco-logical processes and associated sociopolitical behaviors. Volumetric excavations, treating the material culture of an archaeological matrix similar to an ecological core, can yield quantifiable frequencies of surplus goods that provide a multiproxy empirical lens into incremental changes in land use practices, natural resource consumption, and, in this case, likely overexploitation. Archaeological methods are employed to quantify cultural ecological processes of natural resource exploitation, industrial intensification, sustainability and scarcity, and settlement collapse during the colonial transition between Carthaginian and Roman North Africa. The data indicate that overexploitation of olive timber for metallurgical fuel taxed the ecological metabolism of the Zita resource base, likely contributing to a collapse of the entire local economic system. © 2021 by The Wenner-Gren Foundation for Anthropological Research. All rights reserved.12 month embargo; published online 20 July 2021This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at [email protected]