angles of elevation or depression 
30000 ). 
Table for computing differences op level f ro, 
(applicable to scale of 1 
f 4. -f /i 2 for angles of elevat ion. 
Pift'oronco of level—j p/ , h for ang i 08 0 f depression. 
P= distance in scale divisions * inch each; a = angle of elevation or depression; li x =60 feet X tan a; 
1 correction for curvature and refraction. 
Argument for h, is a; argument for h 2 is I). 
Scale 
divisions 
Enoxvi llo ,Tsnn.: 
Log .2 4 ,Chi c karaauga series * * 
Loc. 30,Enoxvilie and Shooks Gap road. . 
Loc.31,Chickamauga limestone • • * 
Loc.32, Sevier shales 2 miles south of 
Knoxville * 
Loc.35, one half mile from Loc.34 in 
Beaver Valley • 
• Knoxville and back toward Clinton 
La Follette, Term *: 
regular succession from Lee conglomerate 
down to Knox *. 
Rockwood iron ore at La Foilette sane 
horizon as in Elk Valley * 
Lake Cttosee, Chilhowee Park, Term. 9 Loc*53 • 
Lebanon Is*: 
rocks at big bend of Clinch Biver look like 
Loc. 17,Clinton to Jacksboro,evidently equi¬ 
valent of Lebanon of central Tenn. 
Stones River probably Lebanon,Loc.25,Knox¬ 
ville *••••••• 
in comments on Raccoon Valley • 
most exposures between Iiarriman and 
Spring City, Loc*39a * 
undoubtedly at Loc*39a .... * 
fossils at Loc*76,northeast of 01tewah,of 
usual Lebanon types . 
horizon at Loc*7S,01tewah to Cleveland 
by way of Mahon Gap,looks like • • 
at Loc.80,Snow Hill P*0.,0 ltewah to Cleve¬ 
land . 
at Locs.84-87.section across eastern fork 
Chattanooga band . 
h 2 
h 2 
Feet. 
Scale 
divisions. 
Feet. 
0 
10S0 
GO 
1 
10S9 
61 
2 
1098 
62 
a 
1107 
-* * * .* 
63 
