Fig. 56.—Celt, showing “bell shape” and roughening for handle.

Fig. 57.—Celt, showing rectangular section.

H. Rectangular section, occasionally with the corners sufficiently rounded to give a somewhat elliptical section; top flattened or rounded; sides straight and parallel or nearly so, sometimes very slightly curved. Most have polished surfaces; only three or four show any battering, or roughening for handle. A large one of hornblende from Lauderdale county, Tennessee, has the edge dulled and polished by use. Length is from 2 to 9 inches. [Figure 57], of argillite, from a mound in Monroe county, Tennessee. The distribution of this class of celts is wide, as shown by the following table:

District.ABCDEFGHIJ
Eastern Tennessee1010211
Western Tennessee1
Northeastern Kentucky11111
Green River, Kentucky1
Southwestern Illinois21
Miami valley, Ohio2211
Kanawha valley, W. V.18441
Northwestern Georgia1
Savannah, Georgia1
Central Arkansas1
Northwestern North Carolina1
KEY:
A = Sandstone.
B = Argillite.
C = Porphyry.
D = Granite.
E = Sienite.
F = Diorite.
G = Hornblende.
H = Limestone.
I = Jasper.
J = Serpentine.

I. Thickest at top (wedge form), section elliptical or nearly rectangular; sides straight or curved, widest at edge or nearly parallel. A few are roughened for handling, and one or two are battered at top by hammering; most are small. The type is shown in [figure 58], of granite, from Carroll county, Indiana. This class of celts also is widely distributed and diverse in material.

District.ABCDEFGHIJ
Eastern Tennessee341
Northeastern Arkansas11
Southeastern Arkansas11
Butler county, Ohio1
Green river, Kentucky1
Northeastern Kentucky311
Crawford county, Wis.1
Southwestern Illinois31
Savannah, Georgia2
Kanawha valley, West Virginia175152
KEY:
A = Hornblende.
B = Granite.
C = Sienite.
D = Comp. quartzite.
E = Argillite.
F = Greenstone.
G = Sandstone.
H = Diorite.
I = Porphyry.
J = Basalt.

Fig. 58.—Celt, showing wedge-shape.