Fig. 1 (202-8369). Chipped Point made of Chalcedony. From the surface, near the head of Priest Rapids. ½ nat. size.
Points Chipped out of Stone. Many implements used in procuring food were found. In general, they are similar in character to those found in the Thompson River Region.[41] The most numerous perhaps, were points of various sizes and shapes, made by chipping and flaking, for arrows, knives and spears. Many of these are small and finely wrought and most of them are of bright colored agates, chalcedonies and similar stones. As before mentioned, several small quarries of such material with adjacent workshops were found. A very few specimens were made of glassy basalt, and it will be remembered ([p. 21]) that this was the prevailing material for chipped implements in the Thompson River region to the north, where there was perhaps not such a great variety of material used.[42] In the Nez Perce region to the east, according to Spinden, a great variety of forms of arrow points chipped from stone of many kinds is found,[43] and the extreme minuteness of some of them is noteworthy. The war spear sometimes had a point of stone, usually lance-shaped, but sometimes barbed.[44] He further states that iron supplanted flint and obsidian at an early date, for the manufacture of arrow-heads.[45]
No caches of chipped implements were found in the Yakima region. Judging from the collections which I have seen, I am under the impression that chipped points are not nearly so numerous in this region as they are near The Dalles and in the Columbia Valley immediately south of this area, and perhaps not even as numerous as in the Thompson River country to the north. We found no fantastic forms such as were rather common in the Thompson River country.[46] It will be remembered[47] that the art of chipping stone was not extensively practised on the coast of British Columbia or Washington, no specimens having been found in that area north of Vancouver Island except at Bella Coola, where only two were discovered. They were frequent at Saanich and in the Fraser Delta and became still more common as one approached the mouth of the Columbia on the west coast of Washington where, on the whole, they seem to resemble, especially in the general character of the material, the chipped points of the Columbia River Valley in the general region from Portland to The Dalles.
Fig. 2 (202-8364). Chipped Point made of Chalcedony. From the surface, near the head of Priest Rapids. ½ nat. size.
Fig. 3 (202-8336). Chipped Point made of White Chalcedony. From the surface, near the head of Priest Rapids. ½ nat. size.
Fig. 4. Serrated Chipped Point made of Petrified Wood. From Priest Rapids. ½ nat. size. (Drawn from a sketch. Original in the collection of Mr. Mires.)
The range of forms and sizes is well shown in Figs. 1 to 6 and in [Plates I] and [II].[48] The specimen shown in [Fig. 1] is very small, apparently made from a thin flake of chalcedony that has not been much chipped. Its edges are slightly serrated and it was found on the surface near the head of Priest Rapids. Deeply serrated points are found in the Nez Perce region to the east, but they are unusual.[49] The one shown in [Fig. 2] is also made of chalcedony and is from the same place. It is larger and the barbs are not so deep. The specimen shown in [Fig. 3], chipped from white chalcedony was found at the same place and may be considered as a knife point rather than as an arrow point. The one shown in [Fig. 4] is made of petrified wood and has serrated edges. It was found at Priest Rapids and is in the collection of Mr. Mires. [Fig. 5] illustrates a point with a straight base chipped from obsidian, one of the few made of this material that have been found in the whole region. This is also from Priest Rapids in the collection of Mr. Mires. The straight based arrow-head is very common in the Nez Perce region.[50] The specimen shown in [Fig. 6] is leaf shaped, the base being broken off. It is made of chert, was collected at Wallula near the Columbia River in Oregon by Judge James Kennedy in 1882 and is in the James Terry collection of this Museum. [Plate I] shows a rather large and crudely chipped point made of basalt, from the surface near the head of Priest Rapids on the bank of the Columbia River. The second is made of red jasper and the third of white chert. They were found near the head of Priest Rapids, the latter also on the bank of the river. These three specimens may be considered as finished or unfinished spear or knife points. The specimens shown in [Plate II] are more nearly of the average size. The first is made of buff jasper and was found on the surface at Kennewick. It is slightly serrated. The second is made of brownish fissile jasper and was found in grave No. 10 (5) in a rock-slide near the mouth of the Naches River. The third, chipped from mottled quartz was found in grave No. 28 (21) near the skull in a rock-slide about three miles west of the mouth of Cowiche Creek. The fourth of white quartzite is also from grave No. 28 (21) near the skull. The breadth of the base of these last two specimens and the notches would facilitate their being fastened very securely in an arrow-shaft, while the basal points would probably project far enough beyond the shaft to make serviceable barbs. The fifth specimen, chipped from brown chert was found among the refuse of a fire in grave No. 1, in a rock-slide of the Yakima Ridge. The sixth is made of glassy basalt and is remarkable for having two sets of notches. It is rather large, which suggests that it may have served as a knife point. It is from the head of Priest Rapids and was collected and presented by Mrs. J. B. Davidson. Double notched arrow points are found in the Nez Perce region.[51] The seventh is chipped from pale fulvous chalcedony and is from the surface at the same place. The eighth is chipped from similar material and was found near by. The ninth is made of opaline whitish chalcedony and is from the same place. The tenth is chipped from yellow agate, and somewhat resembles a drill, while the eleventh is of brown horn stone, both of them being from the surface near the head of Priest Rapids.