[412] See Smith and Fowke.

The Kalapuya of the Willamette Valley to the southwest, buried their

dead in the earth. One writer described the process as follows:--"When

the grave was dug they placed slabs on the bottom and sides, and when

they had lowered the wrapped body down, placed another over, resting on

the side ones, and filled in the earth."[413] The account does not seem

to indicate whether these slabs were of wood or stone, but in either

case there is a certain similarity to the graves with the stone cyst

found near Tampico.

[413] Lewis, p. 178; Galschet, p. 86; American Antiquarian, IV,

1882, p. 331.

A grave which may be of this type, found about two and one half miles

south of Fort Simcoe was reported to me by Mrs. Lynch who furnished the

following information about it. It was on a low ridge with the usual

cairn of rocks about three feet high covering it. This cairn was made up

of two distinct layers of rocks, both lying above the contents of the

grave which included the skeleton of an adult man estimated to be at

least six feet tall and that of a child about six to eight years of age,

according to identifications made by the physician of the United States

Indian service stationed at Fort Simcoe. The man's skull which was well

preserved though brittle, was found four feet below the ground or

approximately seven feet below the top of the cairn and on the eastern

side of the grave. The pelvis of the child was completely decayed, and

few of the bones were intact except the maxilla which was found in the

western part of the grave between the patellæ of the man. Near them were

found four "links" [beads] of a copper necklace. The maxilla was deeply

copper-stained. The steatite ornament shown in Fig. 119 was found on the

man's manubrium.

_Rock-slide Graves._ The rock-slides on the hill and canon sides as in

the region to the north had frequently been used as burial places. The

graves are found from top to bottom. Some of them seem very old. Others

were proven to be recent by the character of the objects found in them.

The skeletons were in or on the ground and the rocks of the slide had

been piled or caused to slide over them (Fig. 1, Plate VIII).[414] The

skeleton was buried from one to five, six or even ten feet deep. In some

cases, the rocks seemed to have sunk as the body decayed, in others they

formed a pile as if placed there to mark the grave. Some graves were

marked with sticks (Fig. 3, Plate VI). In others, probably always the

older graves, sticks were not seen having doubtless decayed. One of the

graves found rifled 75 feet above the little flat at the edge of the

north side of the Naches River about a mile and a half above its mouth,

seemed to lie walled up with rocks like a well and slabs of a broken

canoe, part of which had been thrown out surrounded a few of the

disturbed bones. The skeletons were always in a flexed position (Fig. 2,

Plate VIII) and objects were found to have been placed in some of these

graves.

[414] See Museum negative no. 44513, 7-3, from the south in base of

rock-slide on the north side of the Yakima River about a mile below

the mouth of the Naches River, see p. 15.

Spinden states that cemeteries are readily located by the heaps of

"river-worn or rock-slide boulders" piled over the graves in the Nez

Perce country.[415] They are usually on the first bench above the river

bottom and are found near the traditional village sites, from which they

can be seen. The more common method of disposing of the dead there, was

by burial in the ground, especially on stony hillsides, and covering the

graves with stones to keep off the wild animals. This seems to have been

the prevailing method throughout the whole Columbia region of which this

is a part.[416] Rock-slide graves were sometimes made in basaltic cliffs

in the Nez Perce region. One of these is known to have been used in

recent times from the presence of a Lewis and Clark medal,[417] and

graves marked by pieces of upright cedar and covered by large piles of

stone are reported by Spinden on the east bank of the Snake River,

beside the mouth of the Grande Ronde.[418]

[415] Spinden, p. 181.

[416] Lewis, p. 190; Lewis and Clark. IV, pp. 366-7, 371, V, p. 99;

Ross, (a), pp. 320-321; Cox, p. 105; Douglas, p. 339; Gibbs, (a), p.

405.

[417] Spinden, p. 181.

[418] Spinden, pp. 181 and 252.

Indian graves filled up with stones are numerous in the vicinity of the

several remains (pp. 29, 54 and 82) near Mr. Turner's home, according to

Mr. J. S. Cotton. Mr. Turner told him that all the graves that had been

excavated contained bones in a greatly decayed condition, which

suggested to him that they were very old. These graves, like the other

remains of the vicinity previously mentioned, have been in the same

condition since about 1874.

The terraces mentioned on p. 13 (Fig. 1, Plate VII)[419] may have been

made to facilitate reaching rock-slide graves in the same slide; while

the pits which were found in the slides (Fig. 2, Plate VII)[420] walled

up on the outer sides like balconies, with the rocks that apparently

came both from the pits and the disturbed slide above them, have been

considered as rifled graves or graves from which the burials had been

removed (p. 13).

[419] See Museum negative no. 44520, 7-10, from the southwest, about

a mile above the mouth of the Naches River, (p. 13).

[420] See Museum negative no. 44519, 7-9. The same slide from the

southwest (p. 13).

The following quotation may refer to rock-slide pits:[421] "In the

eastern part of Marion County, Oregon, there stands an isolated and most

strikingly regular and beautiful butte some three hundred feet in height

and covering nearly a section of land. It was fringed about its base, at

the time of which I write, with fir groves, but its sides and well

rounded and spacious top were devoid of timber, except a few old and

spreading oaks, and perhaps a half dozen gigantic firs, whose weighty

limbs were drooping with age. A meridian section line passes over the

middle of this butte, and four sections corner near its top. While

running this line and establishing these corners in 1851, I observed

many semi-circular walls of stone, each enclosing space enough for a

comfortable seat, and as high as one's shoulders when in a sitting

posture, upon cross-sticks as high as the knee ... the older white

residents said the Indians made them, but for what purpose they could

not say. I became a witness to the use, and was particularly impressed

with the fitness for what I saw. Indians from the North and South

traveling that way generally camped upon the banks of the Abiqua Creek,

a rapid stream of pure, cold water, just issued from the mountains upon

the plain. The butte was near, and this they ascended and, taking seats

within the stone sanctuaries, communed in silence with the Great Spirit.

Bowing the head upon the hands and resting them upon the knees for a few

moments, then sitting erect and gazing to the west over the enchanting

valley interspersed with meadow, grove and stream." The author states

that the place is now called Mount Angel, is surmounted by a Roman

Catholic cathedral and that the Indians called this butte

Tap-a-lam-a-ho, signifying Mount of Communion; and the plain to the west

Chek-ta, meaning beautiful or enchanting.

[421] Pp. 35 and 36 of an article entitled "Extract from T. W.

Davenport's, Recollections of an Indian agent (not yet published)."

The Quarterly of the Oregon Historical Society, March, 1904, Vol. V,

No. 1.

Possibly the burials in the domes of volcanic ash and those in the

rock-slides are practically the results of a common motive by the same

people in the same time and the differences may be due simply to the

difference in the character of the near by topography and the relative

convenience of securing the material to cover the graves. This idea is

strengthened by information given me by Mr. W. H. Hindshaw who stated

that from sixteen to thirty miles above the mouth of the Snake River

where it cuts through canons there are rock burial heaps immediately

above flood level and burials in the flood sand below, both of which he

found to contain human bones and implements. He also stated that graves

are found on the bluff overlooking the river. One was curbed with the

remains of a cedar canoe. The grave had a bottom of plank and a cover

over the body--that of a small child--which was wrapped in a fur,

apparently a beaver skin. There were a number of beads and brass buttons

and a large fragment of the shell of the _Schizothoerus nuttallii_ which

must have come from the coast.

_Cremation Circles._ Rings of stones (Fig. 1, Plate IX)[422] were also

seen and on excavation within them cremated human remains were found

usually several in each circle. In some cases the ring was irregular and

in others assumed the form of a rectangle. None of them are known to be

recent. In such places, dentalium shells, flat shell beads, and shell

ornaments were usually seen. Mr. Teit says that rings of stones were

also put on top of graves in the Thompson River region. Along the

Columbia, below the mouth of the Snake River, vaults or burial houses

like those found among the Upper Chinook were used.[423] A somewhat

similar method was observed even among the Nez Perce.[424] This suggests

that the cremation circles here described, may be the caved-in remains

of earth-covered burial lodges built somewhat on the plan of the

semi-subterranean winter houses.

[422] Museum negative no. 44493, 5-6 of circle no. 14 from the east

on the terrace northwest of the junction of the Yakima and the

Naches Rivers (p. 15 and 157). Cf. also Museum negative no. 44522,

7-2.

[423] Cf. Lewis, p. 190; Lewis and Clark, II, pp. 139-140.

[424] Lewis and Clark, IV, p. 369; Lewis, p. 190.

_Position of the Body._ In all the old graves the skeletons were flexed

and usually on the side (Plate VIII, Fig. 2).[425] The graves where the

body was buried at length with the feet to the east were doubtless

recent and probably placed that way due to the teachings of Christians.

In the Nez Perce region to the east, the body was placed in a variety of

positions, either flexed or at length[426] and sometimes upon the side.

Considering the difference between the costume and objects used by the

men and those by the women, in the Nez Perce region to the east,[427] it

would seem that the contents of the graves in this near by region may be

used to check the determination of the sex of the skeletons.

[425] Museum negative no. 44516, 7-6, see grave no. 22, p. 160.

[426] Spinden, pp. 182 and 252.

[427] Cf. Spinden, p. 216.

_Property with the Dead._ Objects are usually found with the remains of

the dead in all classes of old burials but some of the graves contained

nothing; others very little. There was apparently no radical difference

in the character of the material in the graves in volcanic domes and

those in the rock-slides; but the more modern rock-slide graves seemed,

on the whole, to contain a greater number of objects than the older

graves or the graves in domes. On the coast, objects are found with

recent burials, but rarely in ancient graves. The cremation circles

often contained dentalium shells and bits of shell objects but little

else. In the Nez Perce region to the east a considerable amount of

property, ornaments and utensils is found buried with the dead.[428]

[428] Spinden, pp. 182 and 252.

_Horse Sacrifices._ We discovered no graves containing horse bones or

over which a skeleton of a horse was found, although it will be

remembered that such were found in the Nez Perce region east of

here.[429] There, the killing of horses over the graves of their owners

became the usual practice when horses were plentiful. Sometimes a horse

was buried over the body.[430] In this region, however, we found no

evidences of the horse in connection with the graves other than the

presence of an old Spanish bit in one of the more recent burials.

[429] Spinden, p. 182.

[430] Spinden, p. 252.

_Diseases._ Out of about seventeen complete skeletons and six skulls

secured in this region by our party those of two children (99-4323,

99-4326) and two adults, one of which was apparently a female (99-4336),

exhibited anchylosis of some of the vertebrae. The left ankle bones of

the other skeleton (99-4327) showed anchylosis with the tibia and one of

the ribs was abnormal. The skeleton of a young child (99-4329) with

persistent frontal suture, an example of retarded development was also

found.[431]

[431] Cf. Wounds, p. 82.

CONCLUSION.

The connection, nay partial identity, of this culture with that of the

Thompson River region in the southern interior of British Columbia is

supported by considerable evidence. Small heaps of fresh-water clam

shells are found in both regions. The preponderance of chipped points

over those ground out of stone, bone and antler; the presence of digging

stick handles; pestles with flaring bodies and no striking heads, others

with tops in the form of animal heads; celts; the sites of cache pits,

of circular summer lodges marked by rings of stones; and of

semi-subterranean houses with stones on the encircling ridge; pairs of

arrow-shaft smoothers, and bone tubes, were all found to be common to

both regions. The simple pipe bowl found here, although with one

exception not found among archaeological objects in the Thompson area is

commonly used by the present Indians there. Tubular pipes, modern copper

tubes or beads, incised designs consisting of a circle with a dot in it

and engraved dentalium shells, each of a particular kind, besides

pictographs in red, rock-slide sepulchres, modern graves walled up with

parts of canoes, the marking of recent graves with sticks, and the

custom of burying artifacts with the dead were also found to be common

to both areas. Perforated slate tablets of gorget-form are unknown in

both regions. Circles of stones which mark places where cremated human

remains were found in this region sometimes indicate graves in the

Thompson River region.

Frazer[432] mentions meeting Yakima Indians in the Lillooet Valley which

shows that they travelled even beyond the Thompson River country and

readily accounts for the dissemination of cultural elements.

[432] Fraser, p. 175.

On the other hand, many differences in culture are observable. Thus

objects made of nephrite and mica which occur, the former being common

in the Thompson River valley, were not found in the Yakima area.

Quarries and terraced rock-slides such as were seen here are not known

to us in the Thompson River region. The bone of the whale occasionally

found in the Thompson River country is lacking in Yakima collections.

That glassy basalt was not the chief material for chipped implements, as

it was in the Thompson River region, is probably due to the scarcity of

this material and its use is perhaps as rare in the Yakima valley as on

the coast. Chipped implements were made of a greater variety of stone

than in the interior of British Columbia, and a greater proportion were

of the more beautifully colored materials. No harpoon points made of a

unio (?) shell, such as the object found in the Thompson River region or

other objects made of such a shell, were seen. Notched sinkers and large

grooved sinkers were more commonly found than in the Thompson Valley,

while sap scrapers which were common there, were not found in the Yakima

district. A great number of pestles made from short cylindrical pebbles,

forming a type rather rare in the Thompson River region; many long

pestles, of which only four or five have been found in interior British

Columbia; and one with a zigzag design not represented among the finds

from that region, were found in the Yakima area. Saucer-shaped

depressions marking summer lodge sites were not noted by the writer.

Clubs made of stone were more numerous and all are of a different type.

Clubs or other objects made of the bone of the whale or drilled pendants

either circular or elongated were not found. Petroglyphs, pictographs

in white, and representations of feather headdresses were not found

among the archaeological objects in the Thompson region. Graves in

knolls, some with a cyst made of thin slabs of stones constitute another

distinct trait of the Yakima area.

There is relatively less evidence of contact with the prehistoric people

of Puget Sound and the Pacific coast of Washington, and of southern

British Columbia. Several kinds of sea shells, including dentalium,

haliotis and pectunculus, which must have come from the coast, were

found in the Yakima Valley. Small points chipped from beautiful material

found in this region were occasionally seen on the coast, more

particularly south of Puget Sound. Glassy basalt was used here perhaps

about as much as on the coast. Net sinkers are also about as common here

as on the coast from Gray's Harbor southward. The pestles found in the

vicinity of Vancouver Island are similar to some of the short pestles

found in the Yakima region. Short tubular pipes are found on the coast

in the vicinity of the Saanich Peninsula and the Lower Frazer. The pipe

previously described as clearly representative of the art of the

Northwest coast must have been brought from there or made by a coast

artist, not by one merely familiar with the art of the coast. A portion

of the material indicative of coast culture that was found in the Yakima

Valley may have come up the Cowlitz and down the Toppenish River.

The similarities mentioned are, however, outweighed by marked

differences. Large shell heaps--the chief feature of Coastal

archaeology--have not been found in the Yakima area, while quarries are

unknown to us on the coast. Objects made of nephrite and whale's bone

are lacking in the Yakima Valley. A very great number of points rubbed

out of slate and bone are found on the coast, but none rubbed out of

slate and only a few rubbed out of bone have been found on Yakima sites.

Net sinkers are much more common than on the coast, where they are

plentiful only from Gray's Harbor southward and in the Lower Columbia

Valley. Long pestles with the tops carved to represent animal heads are

distinctive of the Yakima area, while cylindrical pebbles used as

pestles but slightly changed from the natural form, which are quite

common in the Yakima Valley, are rarely found in the Coast country. One

style of club made of stone commonly found in this vicinity has not been

seen anywhere on the coast, although some clubs made of stone are like

specimens from that region. Perforated slate tablets like Coastal

gorgets are unknown to us from the Yakima area. Cairns common on the

coast are not found in the Yakima country, while the reverse holds true

of rock-slide burials. Graves in knolls are unknown on the Pacific, and

artifacts are often found in the Yakima graves but they seldom, if ever,

occur with ancient burials on the coast.

Much of the material from the Yakima region resembles that which I have

seen from the general area including the Columbia Valley between

Umatilla and The Dalles, and possibly extending further down the valley.

There seems to be a greater similarity of the art products of the Yakima

to those of the Thompson River region than to those of the Columbia

Valley below the mouth of the Snake, so far as we understand the latter

region at this time, and this according to Lewis[433] is certainly not

contrary to the belief in an earlier occupancy of this region by the

Salish. The culture here resembles that of the Nez Perce region to the

east in that a considerable variety of material was used for chipped

implements.[434]

[433] Lewis, p. 196.

[434] Spinden, p. 181.

Inter-tribal trade may have been a factor in the production of some

observed similarities. It was seen that pipes of three types, one of

which is found as far east as the Dakota, another as far north as the

Thompson River country, and a third as far west as the Queen Charlotte

Islands are all found in this region. It is clear that the ancient

people from the Yakima region had extensive communications not only with

the region southward as far as The Dalles, but also northward, as far as

the more distant Thompson River tribes. If the products of the sea found

in this region came up the Columbia, as may be inferred from Lewis,[435]

it is a good illustration of how trade as a rule, follows the line of

least physical resistance; although the migrations of the tribes do not

always follow such lines because the lines of trade as a rule are

thickly populated by people who resist the migration of their neighbors.

Lewis[436] states that from the coast inward there was only one trade

route of importance in the Washington-Oregon-Idaho region and this led

up the Columbia River to The Dalles where was found the greatest trade

center in the whole region and whither the tribes were wont to come from

the north and south as well as from the east.[437] Klamath,[438] Cayuse,

Nez Perce, Walla Walla and other Sahaptin and probably Salish tribes

were all in the habit of going there to traffic. He also states that

further east, the Sahaptin in their turn, traded with the Shoshone from

whom they obtained buffalo robes and meat. The center for this trade at

least in later times was the Grande Ronde in eastern Oregon;[439] but

this later center probably came into being after the advent of the

horse. The Okanogan are known to have crossed the mountains to Puget

Sound to trade wild hemp for sea shells especially dentalia as well as

for other small objects.[440] The Yakima also in later times crossed the

mountains and traded with Puget Sound tribes according to Gibbs,[441]

but if this trade were carried on in earlier times its effect in the

Yakima Valley seems to have been slight as indicated by the few

dentalium shells, the shell pendants shown in Figs. 87-94 and the pipe

of coast art, shown in Fig. 127. It is possible that this trade with the

coast became customary only after the horse was introduced. There was a

considerable amount of trade between the Yakima and the Thompson River

and other tribes of British Columbia which was carried on chiefly

through the Okanogan.[442] Lewis[443] states that the Walla Walla who

lived to the south of the Yakima at least in later times visited as far

north as the Thompson River region, and that certain Sahaptin tribes

seem to have moved northward and westward and forced back the Salish

tribes which at the time of Lewis and Clark's visit were on the north

bank of the Columbia and on its tributaries.[444] These tribes were

particularly the Klickitat and the Yakima, an assumption which Lewis

states is supported by the definite assertions of the natives

themselves. A number of old men positively assured Dr. Suckley that they

had pushed their way into the country formerly occupied by the

Salish.[445] The Klickitat, although living in a well wooded region on

the southern slopes of Mt. Adams and Mt. St. Helens are thought to have

been driven by the Cayuse from their earlier home which was further east

and south. Later, they went further west into the Cowlitz Valley.[446]

This may account for the circular pit surrounded by an embankment which

I saw near Rochester in Thurston County and interpreted as the remains

of a semi-subterranean winter house site. Lewis also states that the

Yakima probably lived on the Columbia near the mouth of the river which

now bears their name, and are in fact so located by Cox who places them

on the north and east side of the Columbia. The pressure of neighboring

tribes caused by the coming of the white race no doubt facilitated the

adoption of new cultural details.

[435] Lewis, p. 193.

[436] Lewis, p. 193.

[437] Lewis and Clark, IV, p. 286; Ross, (b), p. 117.

[438] Gatschet, p. 93.

[439] Wilkes, IV, p. 394.

[440] Ross, (a), p. 290; (b), I, p. 44.

[441] Gibbs, (a), p. 408.

[442] Cf. Teit, (a), p. 258.

[443] Lewis, pp. 194-5.

[444] Lewis and Clark, VI, pp. 115 and 119; Mooney, pp. 734-736.

[445] Gibbs, (b), p. 224.

[446] Swan, p. 323.

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