Projectiles, Tools and
Knives
Plus a Little Bit of Pre-History
from The Enumclaw
Plateau
Western Washington
State
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Ethno History
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The Native American Indian groups inhabiting the area of present day King
County were first encountered by Euro-American explorers beginning in the
late 18th century and by traders in the first half of the 19th century. The
major tribal groups associated with King County have been known since
historic times as the Snoqualmie, Duwamish, Muckleshoot, Puyallup, Skykomish, and possibly the Suquamish. All of these groups are
closely
related both culturally and linguistically. In ethnographic literature they
are known as belonging to the Southern Puget Sound branch of the Coast
Salish. Linguistically, these tribal groups are known as Lushootseed
speaking peoples.
Although there are traditional locations at which groups
erected villages, hunted, fished, and gathered food and resources,
certain territories may have been in common use or their usage changed with
developments in intertribal relations. Tribal or extended family bands
occupied winter villages, seasonal camps, and territories according to their
individual needs as well as their fortunes in intertribal relations,
alliances and wars.
Although exact population figures are unknown, there were an estimated several
thousand persons in the area in late prehistoric times. It is believed that
Euro-American-spread epidemics in the late 18th and early
19th centuries were responsible for depopulating Puget Sound by as much as 80%
of its indigenous peoples. Attacks by seagoing Tlingits and Haidas from
southeast Alaska, which occurred as late as the Historic Period,
further reduced and disrupted the local tribal groups. Historic accounts of
occasionally brutal intertribal warfare among Puget Sound groups up to the
Historic Period may also have been a factor in local population decline.
The Snoqualmie were known to have had major villages at or near Fall City,
Tolt (Carnation), North Bend, and other sites along the Snoqualmie River from
the Cascade Crest to an area north of Duvall. In historic times they
also lived on the eastern shore of Lake Sammamish.
The Duwamish are reported to have had villages along Black River and Cedar
River near Renton, along the valley of the Duwamish, at its mouth and
immediately southeast of Pioneer Square in Seattle. Related groups
extended up along Shilshole, Salmon, and Union Bays. The Lower White (now
Green) River and shorelines of Lake Washington were also traditional village
sites or areas of influence. Several accounts place closely related bands on
Lake Sammamish and the Sammamish River. The Duwamish were also known to have
used sites at Alki Point (West Seattle) and at several points farther south on
the Puget Sound shoreline.
The Puyallup-Nisqually are said to have had large villages in and around the
present City of Tacoma, but usedsites on Vashon-Maury Islands and along the
southern Puget Sound shoreline of King County.
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ENUMCLAW PLATEAU
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Burgundy and Red Jasper Leaf or Pre-form Projectiles |
Several bands of the Muckleshoot lived at sites along the upper White and
Green Rivers and on the Enumclaw Plateau. The Muckleshoot were believed to have
had close cultural and linguistic ties through intermarriage with
Sahaptin-speaking Yakamas and Klickitats of eastern Washington.
It was noted
The Stevens Pass area of King County was once the hunting territory of the
Skykomish who lived downstream, with a village in the Sultan Creek area of
Snohomish County. The small number of Skykomish are believed to be largely
absorbed into other groups, possibly the Tulalip, Snohomish, and Snoqualmie.
Puyallup families were known to have made
extensive use of sites around Quartermaster Harbor on Vashon and Maury Islands,
especially in the Late Historic Period. Summer villages are believed to
have been located at several sites in the islands including Tahlequah and
Manzanita on Maury Island and between Burton and Portage on Vashon Island.
All of the major Native American groups erected split cedar houses or
longhouses for their more permanent villages. Old Man House (part of a Suquamish
Village near Poulsbo), reportedly the largest longhouse on Puget Sound, was
nearly 700 feet long and housed as many as several hundred people. Seasonal
camps were constructed of woven mats and poles. Several varieties of finely
crafted cedar dugout canoes were used for transportation, and they were
extensively used by the earliest pioneers. Stone working and woodworking
technologies were well developed before the widespread use of smelted metals
most of which were introduced by Euro-American trade in historic times. In King
County, Indian groups harvested the incredible runs of salmon which have been
documented by the early settlers. Other dietary items included shellfish,
waterfowl, large and small mammals, roots, herbs, and berries. Among the
Duwamish and other groups, cultivation of the Hudson’s Bay potato had begun
before the arrival of the settlers. Many of the clearings later occupied by the
County’s first pioneers were apparently naturally occurring prairies which were
occasionally burned off by the Indians to increase the berry harvest and hunting
of small game. Trade was routinely conducted across the mountain passes,
especially in late summer.
Most King County Indian groups had some form of
contact, trade, cultural affinity or blood relationship to tribes across the
Cascade Mountains. Trails and trade routes across the Cascades are known to
exist, NACHES PASS was a common route taken by the plateau Indians, and lithic material from Eastern Washington is known from a number of sites
around the plateau and Puget Sound region.
The
Yakama followed these trans-Cascades trails to secure supplies of various
natural resources available in the region of Rainier Park as well as to enter
the country of their friendly Northwest Coast neighbors and share their food
resources. For example, they fished for red salmon in the Cowlitz River. According to one of Smith's Muckleshoot informants, the
Yakama also journeyed westward through Naches Pass into Muckleshoot territory to
catch and dry fish. On occasion, coastal groups passed east of the Cascades to
secure local foods. For example, the Muckleshoot traveled through Naches Pass to
Yakama country to obtain things they could not obtain in their own territory,
including certain roots, berries, and other products.
The Wilkes expedition
did make the first recorded trip over Naches Pass, following an Indian trail
around the northern flank of Mount Rainier. This was done by Lieutenant Robert
E. Johnson in command of a contingent of six members of the expedition. They
were allowed eighty days for the trip across the mountains to Fort Colville,
Fort Okanogan, and other posts east of the mountains, but they did it in less
time, "leaving Nisqually on May 19, and returning on July 15, a total of
fifty-seven days." (Meany, 1909, 76).
Overall, the lifestyle of most Indian Groups in the King County area was
characterized by a natural abundance of food and raw materials. Finely crafted
baskets, mats, and woven blankets were in wide use and were also
made for trade. Much of the remaining material culture of local Indian groups
is now in museums, with many of the earliest collections located in other
counties or states.
With the influx of American settlers beginning in the early 1850s,
pressures increased on the U.S. government to solve the problem of land tenure
for the new arrivals. THE REBELLION "INDIAN WARS OF 1854-1856"
The solution, following the federal policies used to
acquire territories across the continent, was to negotiate treaties ceding
Indian lands to the Federal government in exchange for limited reservation
parcels, some services, and compensation. The DONATION
LAND ACT, was created.
The Puyallup, Muckleshoot, and Suquamish eventually acquired reservation lands
within their traditional areas of influence. The Snoqualmie and Duwamish were to
be relocated, out of the County, to reservation lands,
which essentially were overstrained by the numbers of people involved and
sometimes inhospitable to their traditional ways of life. Some Tribal members
refused to leave their traditional homes in King County. Others
left the reservation after a short while, and subsequently found work in
pioneer farming and logging operations. The Snoqualmie and Duwamish have not as
yet acquired their own reservations, despite their inclusion as
signatories to the Point Elliot Treaty.
Reference:
OVERVIEW OF KING COUNTY PREHISTORY TO EARLY HISTORY
Historical Paper No. 3
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PREHISTORY OF THE
ENUMCLAW
PLATEAU |
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LOCATION AND CULTURAL ASSESSMENT OF ARCHAEOLOGICAL SITES ON THE
ENUMCLAW PLATEAU IN THE SOUTHERN PUGET LOWLAND
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An Abstract by:
Gerald C. Hedlund |
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Nineteen prehistoric sites have been located, investigated and/or
tested on the Enumclaw Plateau. Most of these sites reflect an
"Inland" adaptation and are located back from major streams on
higher ground. The larger sites also appear to have been developed
on local "prairies" that were deliberately maintained open areas.
Most of the artifacts found were chipped stone since organic
materials were not preserved. Significant numbers of ground and
polished stone were found at only two sites. Evidence of house
structures has been found at one site.
The Enumclaw Plateau is a portion of the Southern
Puget Lowland
terminating on the west approximately 15 km east of Puget Sound (25
km east of Tacoma), and bounded on the east by the foothills of the
Cascade Range. Its relatively flat surface is underlain by glacial
drift, which was further covered and leveled by the massive Osceola
mudflow from Mt. Rainier (35 km to the southeast) some 4900 years
ago (Hedlund 1974:77). Average elevation of the region is around 180
m above sea level, and its total area is about 100 km2•
The plateau is drained by three sizeable rivers--the Green, along
the northern edge, the Puyallup to the southwest, and the White,
which bisects the area.
Nineteen prehistoric archaeological sites have been located and
investigated on the Enumclaw plateau . Six of the 19 sites
have been excavated and/or surface collected in a
systematic manner. The other 13 sites have
been visited, investigated and their collections observed and
examined.
Nine of the sites are located on higher ground with good drainage,
of which eight are located some distance from streams or lakes. Five
of the possible habitation sites, of a total of 10 sites on river or
creek banks, may have been subject to flooding (the Pheasant Farm
Site, 45KI33, the Boise Creek Site, 45KI70, the Cooper's Corner
Site, 45KI71, the Noble Site, 45KI64, and the Mahler Park Site,
45KI13). The Flaming Geyser petroglyphs Site (45KI40), a probable
non-habitation site, would also have been subject to flooding.
Sites located away from
streams and on better drained ground would appear to have been more
generalized in activity and more permanently occupied, while sites
closer to streams, such as the Pheasant Farm, Boise Creek, Noble
and Mahler Park sites, may have been specifically fishing sites.
Sites located at some distance from streams, such as the Jokumsen,
Pedersen, Maris and Connell's prairie sites, show more evidence of
habitation, i.e., have more artifacts, have a greater depth of
deposit and cover greater areas. The Jokumsen, Schodde-Anderson,
Imhof, and Pedersen sites are examples of such extensive
non-specific use sites. The Cooper's Corner Site, on the other hand,
covers a large area over which cultural material is relatively
abundant and is located on a small creek.
Smith
(194e:31)
classifies the prehistoric and early
historic native inhabitants of the Enumclaw Plateau as having a
specific "Inland" cultural adaptation. Gibbs
(1877)
uses a similar term, while Bryan
(1963:91)
referred to this type of adaptation as a
"Trans-Cascadian" culture. The "Inland" or
"Trans-Canadian" terms refer to a generalized adaptation
to the area between the Pacific ()cean or Puget Sound and the Cascade Range. People with
this adaptation had a generalized system of food getting. Most of the larger sites located on
the Enumclaw Plateau appear to have been situated on so-called
"natural prairies," or cleared areas in the coast forest type
vegetation pattern that normally grows in this region. However, it
can easily be demonstrated that there are no "natural prairie"
conditions on the Enumclaw Plateau. The "prairies" were human
caused, or kept open by deliberate burning on a regular basis,
perhaps as often as twice a year (Norton, Boyd, and Hunn). Some of the Connell's prairie sites were certain to have
been located in such cleared areas. Other sites, such as the
Cumberland Sod Farm, Maris, Pedersen Jokumsen, Bohn, Muckleshoot and
Cooper's Corner, may also have been open areas at times. It appears
that such "prairies" may have changed location and expanded or
contracted, due to natural fires and/or burning by humans.
These "prairies" were conducive to
supporting plants and animals not normally found in the area which
the prehistoric inhabitants used in their diets. It is probable that
the deliberate burning of these "prairies" to keep them open
contributed to the presence of such vegetation as oak trees, hazel
bushes, and collectible roots like the camas. Grasses, from which
seed could be gathered, would also have grown in open areas, as
would various kinds of berries, such as blackberries.
Cultural materials found consist
mainly of chipped stone. The majority of the worked
stone is of cryptocrystalline silicate, with basalt and other
volcanic materials also common. Obsidian is found on some 0 f the sites and has been identified
as coming from sources in Central Oregon. Cobble-core choppers and
edge ground cobbles are common to most of the sites, but only two
sites yielded a significant number (two or more) of ground and
polished tools. Mauls were found on only one site. Organic material
is not generally preserved on any of the sites, and artifacts of
bone or wood have not been identified in any significant number. House pits and other structural
remains have been identified at the Jokumsen Site. One house pit is
approximately
Ie
m by 6 m and oval in shape. Further
house evidence is suggested by an alignment of five post molds over
a distance of approximately 12 meters. The potential for further
archaeological research in the area appears to be promising. There
are remains of relatively large undisturbed sites with considerable
cultural evidence, and others will probably be discovered. One site
with excellent potential is the Cooper's Corner Site mentioned
above. Bisected by a small creek, one part of this site is badly
disturbed by the construction of farm buildings. On the other side
of the creek however, there has been little disturbance other than
plowing. Another place with good potential is the Noble Site, which
was investigated by Green River Community College during the summer
of 1988.
Although this site is quite
extensive, it is presently owned by people not especially open to
archaeology. The White River Bank Site is another relatively
undisturbed location that should be preserved or excavated. Other
locations that should be investigated further are the Jokumsen,
Schodde-Anderson and the Bohn sites.
The site least disturbed by
Euro-American cultural activity is the Mahler Park Site. It consists
of three known locations adjacent to Newaukum creek~ suggesting
temporary fishing camp functions. One location of about 15 m maximum
extent was logged, but otherwise the site appears to be undisturbed.
Cultural deposition appears to be surficial. The most disturbed site
in the area is the Boise Creek Site, with several modern houses
built on it. The Tacoma Water pipe Site is also badly disturbed by a
pipeline ditch and by road cuts. Another site, that at Southwood
Elementary School, has been destroyed by grading to level a play
area and by artifact collecting by students and their parents. Near
Buckley, the Maris Site has been badly disturbed by plowing and
digging for numerous artifacts to a depth of .5 m. This large and
important site would be very difficult to excavate systematically
because of the disturbances.
In summary, the Enumclaw
Plateau shows a substantial number of prehistoric sites, nineteen of
which are listed here. The largest sites are generally found on
ridges or slightly elevated areas with good drainage. Most of the
larger sites were probably built on "prairies" which were kept open
by periodic burning. Artifacts found are generally made of chipped
cryptocrystalline silicate or basalt. While edge ground cobbles and
cobble-core choppers are common to most sites, ground and polished
tools are sparse on all but two locations. Mauls occurred on only
one of the sites.
All of the sites were disturbed by
Euro-American cultural activity, including the building of
structures, plowing, logging, road building, ditch digging and
collecting artifacts. Nevertheless, there are several sites which
should be preserved as archaeological resources and others that
should be investigated further before they are completely destroyed.
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Pictures of Site 45KI67 Before
the Internet
The following maps are a
collection representing the Donation Claim of Allen Porter , Now called Porters
Prairie |
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Nov 1st 1853 1st Donation Claim on the
Westside of the White River |
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NORTH |
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WEST |
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EAST>>Cascade Mountains |
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SOUTH |
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NORTH |
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EAST, SE.>>Cascade Mountains |

Looking East
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SOUTH |
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Old Timers Hand Drawn Map Copy of Allen Porters Donation Claim
~ 1872 |
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Picture of a Survey Map Late 1877 |
Early
1900's Donation Claim has been Subdivided |
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Late 1960's Land divisions
Barron Industries was the
beginning
of Sod Cultivation |
Topo. Overview of the Land |
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Here is a current view of Porters Prairie
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HISTORICAL ACCOUNTS OF ALLEN PORTER
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"ALLEN PORTER" WAGON TRAVELS ITS LAST
MILE
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INDIAN REBELLION DOC No.9 March 7th 1856
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"A RACE FOR LIFE"
Part 1
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"A RACE FOR LIFE"
Part 2
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"A RACE FOR LIFE"
Part 3
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ARCHAEOLOGY LOST or PRESERVED
THE CULTURAL
ASSESSMENT
For
100 years this land was being used as a dairy, The more recent 20 years this site was tilled and groomed for the production of Sod.
Annually 3/4 to 1 inches of soil was removed.
This equates to roughly 20" of soil removed.
Also represents every layer of habitation gone! All ended up in a rock pile or part of
the farms road and eventually ended up in someone's backyard.
The next
few pictures represents the last pieces of archaeology saved from the Sod Farm
site.
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WEST
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EAST>>Cascade Mtns. |
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SOUTH |
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INTERACTIVE MAP |
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CLICK ON a section of the map and see the artifact found.
NOTE: JUST Run your cursor over the map and when it changes you found a picture |

Cataloged Site |
The Archaeological Time Frame
Generalized outline of cultural sequences has been
suggested which may provide a simple framework
for understanding the County’s archaeological resources. Three major time
periods may be defined as follows
(bp indicates "before present"):
Late Period < Historic: 250 bp
Prehistoric: 2500-250 bp
Middle Period < Prehistoric: 4500-2500 bp
Early Period < Prehistoric: 8000-4500 bp
These artifacts were disturbed and surface found so I can't date.
I
can say they are no older than 5600 b.p.
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