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Canadian Historic Sites: Occasional Papers in Archaeology and History No. 1
Archaeological Investigations of the National Historic Sites Service, 1962-1966
by John H. Rick
Other Work
Resistivity Survey
During the summer of 1964, the University of
Pennsylvania Museum's Applied Science Center for Archaeology conducted
tests at Fort Lennox of the Geohm resistivity meter and the proton
magnetometer. Elizabeth K. Ralph, Associate Director of the Center, and
Hugh Bergh were in charge of this project. Results with the latter
instrument were unrewarding, but the Geohm meter proved highly
successful in locating buried structures (Rainey and Ralph 1966).
The following year, Albert E. Wilson carried out
further Geohm tests in Newfoundland and Nova Scotia. The Fort Lennox
work had demonstrated the efficiency of the meter on shallowly buried
masonry in sandy soil and the Newfoundland sites were chosen because of
the radically different conditions prevailing there. At both Castle
Graves and Signal Hill, bedrock is very close to ground surface and the
masonry structures are frequently built directly on bedrock. The tests
at Castle Graves were unsuccessful, partly because the masonry remains
were not massive enough to give meter readings which would distinguish
them from bedrock. Furthermore, the fortifications occupy the entire
hilltop and it was not possible to move outside the fort area to obtain
"background" readings against which the surveys over areas of masonry
could be compared. The Signal Hill tests were also unsuccessful, in this
case, primarily because the overburden was so full of broken rock that
no clear resistance patterns could be established. The final tests were
carried out at Fort Anne where soil conditions are similar to those at
Fort Lennox, but where the masonry remains are generally buried several
feet deeper. The results here were very rewarding with many clear and
easily interpretable resistance patterns emerging (Wilson 1965).
While the results of two seasons of testing show some
of the limitations of resistivity surveys, they also indicate the
usefulness of these instruments in the investigation of archaeological
sites. This is particularly true of historic sites where the comparison
of documentary evidence with resistance patterns will frequently permit scientific
identification of buried structures. Admittedly, field operation can be
slow, but, as a means of determining where to dig and what is likely to
be found, the resistivity survey can represent a substantial savings in
time and money over test trenching.
Archaeological Training Program
The simultaneous
development of archaeological research programs by the National
Historic Sites Service and the Fortress of Louisbourg Restoration
Section created a new demand for experienced field assistants which
existing university training resources were able to fill only in part.
Moreover, a number of students trained on small, unstratified
prehistoric sites found some difficulty in adjusting to the problems of
supervising labour crews and recording complex stratigraphy and
architectural features. As a result, the Service has, for the past four
years, conducted a summer training program in archaeological field
techniques. The primary goal has been to create a body of trained students
available for subsequent summer employment by the Service as field
assistants. It is expected that the students selected will obtain the
requisite theoretical background in their regular university courses
and, for this reason, selection is almost entirely limited to those
majoring in history or anthropology. This has the added advantage of
introducing prospective historians to the applications of archaeology to
their discipline and of perhaps convincing anthropology students that
excavation experience gained on large, stratified historic sites is
also applicable to smaller, prehistoric excavations.
Two basic teaching approaches have been tried:
on-the-job training and training in a formal field school situation with
lectures, examinations, etc. The drawback to the former approach is
that problems are dictated by the work situation and not by teaching
requirements; hence, pressures of work may force students to spend an
excessive amount of time on one aspect of excavation to the exclusion of
necessary experience in other phases of the work. In the formal
school situation, this problem is largely eliminated because one can
select for excavation areas which provide a broad range of typical field
problems. One obvious drawback is that the field school is an artificial
environment which may or may not approximate the "real" excavation
situation and this is recognized by, and reflected in the attitudes of,
the students. More importantly, the training function can only be
incidental to the main work of the National Historic Sites Service and
this precludes the field school approach except under certain
conditions such as existed at Fort Lennox in 1964 and 1965. Here, the
site development problems were such that excavating any of a wide
variety of areas was likely to produce useful information and the
development schedule permitted a pace of excavation which could be
geared to student needs. Completion of this phase of the work at Fort
Lennox dictated a return to on-the-job training methods in 1966.
Over the past four seasons, both approaches have
produced comparable numbers of good students. While the field school
students may finish their initial summer with a somewhat broader
knowledge than the others, the differences tend to be minimal by the end
of the second season in the field. Since on-the-job training seems more
compatible with the Service's basic role, it is likely that this system
will continue in use as long as it is considered necessary to carry on
the training program.
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