This week we resume our travels through the archaeological
heritage of Pennsylvania and journey to the northern region of the state to
Potter County. Often refered to as "God's Country", this county is located in
the north central region of the state along the border of New York State in the
Appalachian Plateaus Province. This
region is characterized by narrow, often steep-sided valleys cut into the
rolling plateau surface. The headwaters of the Susquehanna and Allegheny
Rivers originate in this rugged and beautiful section of the Allegheny
Mountains. Major tributaries include Mill and Sinnemahoning creeks and flowing to
the north, the Genesee River. Most of the county is considered as mountainous
upland terrain; interestingly the distribution of archaeological sites is
almost evenly divided between riverine and upland settings.
DCNR map 59 - Glacial deposits of Pennsylvania
The effects of Wisconsinan glaciation are evident in alluvial
deposition in the Allegheny, and its tributary valleys created by downstream
ice-damming of the Allegheny River and the movement of large quantities of soil
and rock downslope attributable to glacier change. The Wisconsin glaciation was so named because
deposits from its glacier were first discovered, described, and named in the
state of Wisconsin. Radiocarbon dating
of material from above and below the deposits of sediment left by the late
Wisconsinan glacier, scientists have firmly established that in the United
States the late Wisconsinan glaciation occurred between about 25,000 and 12,000
years ago. Local testing indicates
that the ice was in Pennsylvania between about 22,000 and 17,000 years ago,
reaching its maximum extent about 20,000 years ago. The glacier ran along the
northwest corner of Potter County then southeasterly to Pine Creek on its
eastern border- basically the northern third of the county.
The stripping
and redepositing of soils from glacial activity exposed bedrock of the Catskill
formation at or near its surface throughout much of the county. This formation consists of sandstone,
siltsone and shale with much of the soil classified by the Dept. of Agriculture
as acidic soils. The glacially deposited gravels, pebbles and cobbles of jasper
and chert- were utilized for tool production as evident in the archaeological
record. Much of the region is forested in maple-beech-birch with some oak and
hemlock. This is a second to third
growth forest- much different than the ‘black forest” recorded by settlers in
the 1800’s.
This
mountainous terrain with its dense tree cover is likely a factor in the low
number of recorded sites in the county, but also the cold temperatures factor during
the short growing season for certain food sources utilized by native peoples.
This would have been especially true prior to the development of agriculture
when such foods as nuts and berries were most important. The Pennsylvania Archaeological Site Survey
file (PASS) lists one Paleoindian site on a terrace above Twelve Mile Creek which
was recorded based on artifact information provided by a private collector. Additional
reference is made to this collection as “four stumpy fluted points of black
flint” by John Witthoft in Foundations of
Pennsylvania Prehistory.
Excavations
conducted at 36PO4 for a major pipeline project found evidence of a short-term
campsite from the late Middle Woodland period. This mixed assemblage of
artifacts includes cord marked pottery, chipped stone and one Adena projectile
point. The archaeologists noted that the absence of primary and secondary flake
debitage indicates that tools were being resharpened as opposed to being made at
this location. Flaked stone material recovered included jasper (1) and local
cherts (15).
Adeana point and Middle Woodland ceramics from 36Po4
Additional
archaeological testing for various highway, water and sewer projects and
pipeline projects have produced little evidence of occupation beyond short term
camps. Lithic materials recovered have
consistently been local cherts, jasper, and quartz. Since the county is sparsely populated there
have been fewer projects requiring archaeological investigations, thus fewer
sites are found, investigated and recorded.
As mentioned
previously, the cold temperatures and short growing season of the region may
have factored into the level of occupation.
A research project conducted in 1986 by William Roberts examined the
growing season of corn in Hebron Township, Potter County. Roberts compared “flour corn” Zea mays
amylacea which takes 130 days to mature, to Zea mays indurate “flint corn”
which matures in 100 days. His
observation of the frost patterns and growing season prompted him to research
why hilltop fields might escape frost damage while low garden areas were
destroyed by frost. Roberts recorded
temperatures at four locations for the growing season in mixed settings
including twos hilltop archaeological sites.
Elevations ranged from 2,500’ to 1800’ ft and covered the period from
April 15 to October 10. The results have
important implications regarding site selection and use during the Woodland
period.
Temperature
inversion as Roberts termed the variation in frost patterns is addressed as
“Air at lower temperatures is heavier than air at higher temperatures. Cold air
consequently endeavors to push itself under warm air. The result, if
opportunity permits, is a circulation of different air bodies until equilibrium
is obtained. Cold air from the high ground flows to the lower places and is
replaced by warmer air from above. This process works best on calm nights where
air pressure is high and and the sky is clear. This allows for “cold islands”
cold lakes” or “frost holes” or whatever local term may be applied.
Roberts research examined the feasibility of
native peoples growing corn here during the Late Woodland and concluded that
the poor soils and cool temperatures (avg. daily temp 46.1) would likely have
restricted the crop to flint corn.
Roberts further compared corn production of Huron maize horticulture
with Iroquois practices. Huron produced
single crops of two maize varieties a flour and a flint corn allowing for the
possibility for crop failure. Roberts
concluded that hilltop forts and adjacent cornfields may warrant additional
examination in better understand their relationship to Native American
settlement patterns.
By the time Ole
Bornemann Bull, the famous Norwegian violinist who toured the United States
purchased land in 1852, the native population had moved out of the county. Ole Bull attempted to develop a series of Norwegian
settlements and assisted in financing many of those who came to Potter County.
Transportation into the area was difficult and the lack of funds forced Bull to
return to violin performance to raise money.
Restrictions placed on the land that Bull had purchased allowed for use
of only steep hillside lands covered in rich pine forests. Unfortunately the lumber boom occurred after
Bull and the other Norwegians had given up hope and moved from the area. Today,
visitors can enjoy the beautiful scenery at Ole Bull State Park.
The lumber
industry and the boom that would greatly increase the population also wiped out
the “black forest” and left hilltops barren due to uncontrolled clear-cutting.
Today the Pennsylvania Lumber Museum located in Galeton offers visitors an
opportunity to view an early logging camp and equipment employed in the lumber
industry.
References
Kent, Barry C., Ira F. Smith and Catherine McCann
Foundations of Pennsylvania Prehistory, Anthropological
Series of the Pennsylvania Historical and
Museum Commission, Number 1. Harrisburg,1971.
Roberts, William L.
Frost Patterns and Their Implications for Aboriginal
Settlement in Potter County, Pennsylvania, Unpublished Master’s Thesis, Pennsylvania
State University, Anthroplogy,1988, housed in Section of Archaeology at The
State Museum of Pennsylvania.
Weed, Carol S., William F. Wenstrom, PhD. and Jeffrey L.
Jones
A Cultural Resources Survey of the Proposed Transcontinental
Gas Pipe Line Corporation Expansion of the Wharton Lateral Extension Natural
Gas Pipeline, Potter County, Pennsylvania. Unpublished Manuscript, Section of Archaeology.
For more information, visit PAarchaeology.state.pa.us or the Hall of Anthropology and Archaeology at The State Museum of Pennsylvania .
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