Minerals
The people of this region are acquainted with few mineral substances, excluding the metals which they obtain from the whites. The most important are flint, slate, soapstone, jade, and a peculiar form of massive pectolite, first described by Prof. F. W. Clarke93 from specimens brought home by our party. Flint, ánma, was formerly in great demand for arrow and spear heads and other implements, and according to Dr. Simpson94 was obtained from the Nunatañmiun. It is generally black or a slightly translucent gray, but we collected a number of arrowheads, etc., made of jasper, red or variegated. A few crystals of transparent quartz, sometimes smoky, were also seen, and appeared to be used as amulets. Slate, ulu´ksɐ, “material for a round knife,” was used, as its name imports, for making the woman’s round knife, and for harpoon blades, etc. It is a smooth clay slate, varying in hardness, and light green, red, purple, dark gray, or black in color. All the pieces of soft gray soapstone, tună´ktɐ, which are so common at both villages, are probably fragments of the lamps and kettles obtained in former years from the eastern natives. The jade is often very beautiful, varying from a pale or bright translucent green to a dark olive, almost black, and was formerly used for making adzes, whetstones, and occasionally other implements. The pectolite, generally of a pale greenish or bluish color, was only found in the form of oblong, more or less cylindrical masses, used as hammerheads. Both of these minerals were called kau´dlo, and were said to come “from the east, a long way off,” from high rocky ground, but all that we could learn was very indefinite. Dr. Simpson was informed95 that the stones for making whetstones were brought from the Kuwûk River, so that this jade is probably the same as that which is said to form Jade Mountain, in that region.
Bits of porphyry, syenite, and similar rocks are used for making labrets, and large pebbles are used as hammers and net sinkers. They have also a little iron pyrites, both massive and in the form of spherical concretions. The latter were said to come from the mouth of the Colville, and are believed by the natives to have fallen from the sky. Two other kinds of stone are brought from the neighborhood of Nu´ɐsŭknan, partly, it appears, as curiosities, and partly with some ill defined mystical notions. The first are botryoidal masses of brown limonite, resembling bog iron ore, and the other sort curious concretions, looking like the familiar “clay stones,” but very heavy, and apparently containing a great deal of iron pyrites. White gypsum, used for rubbing the flesh side of deerskins, is obtained on the seashore at a place called Tû´tyĕ, “one sleep” east from Point Barrow.
Bituminous coal, alu´a, is well known, though not used for fuel. Many small fragments, which come perhaps from the vein at Cape Beaufort,96 are picked up on the beach. Shaly, very bituminous coal, broken into small square fragments, is rather abundant on the bars of Kulugrua, whence specimens were brought by Capt. Herendeen. A native of Wainwright Inlet gave us to understand that coal existed in a regular vein near that place, and told a story of a burning hill in that region. This may be a coal bed on fire, or possibly “smoking cliffs,” like those seen by the Investigator in Franklin Bay.97 We also heard a story of a lake of tar or bitumen, ádngun, said to be situated on an island a day’s sail east of the point. Blacklead, mĭ´ñun, and red ocher are abundant and used as pigments, but we did not learn where they were obtained. Pieces of amber are sometimes found on the beach and are carried as amulets or (rarely) made into beads. Amber is called aúmɐ, a word that in other Eskimo dialects, and probably in this also, means “a live coal.” Its application to a lump of amber is quite a striking figure of speech.