330 CONNECTION OF THERMAL SPRINGS IN VIRGINIA 



Table II. 



Geological Position. 



In steep anticlinal a.xis 

 of For. \'I. Springs bold 

 and constant ; some gas 

 — Nil. and C. acid. 



N. W. side of anticl. 

 axis of Paddv Mt. from 

 vert, strata of For. VII. 

 Copious and constant. 



S. E. side of anticl. of 

 Red Patcii Mt. From 

 For. VI. Copious and 

 constant. Some iras — 

 Nit. Carb. acid and Ox. 



S. E. side of anticl. of 

 Mill Ml. From I-'or. 

 VI. Copious and con- 

 stant. 



Anticlinal axis of North 

 river Ml. from For. VI. 

 Very bold and constant. 



N. W. side of anticl. 

 of Paddy's cove. Junc- 

 tion of For. Viand VII. 



N. W. side of anticl. of 

 Chestnut Ridge, from 

 For. VIJ. 



N. W. side of anticl. of 

 Big Sandy. From junc. 

 of For VII. and VIII. 



Anticl. axis of Brown's 

 Mt. For. VI. Much 

 gas. Nit. C. acid. 



Axis in For. II. Rocks 

 nearly vertical. Bold. Gas 

 No gas. 



Sleep beds of For. II. 

 Near fault of Draper's 

 valley. Very bold sp'gs. 

 Gas. 



Near N.E. end of great 

 Anticl. of Burk's Gard. 

 From For. VII. 



Anticl. of Little Flat 

 top Ml. For VI. 



Fault ; in F. II. Copi- 

 ous. Much gas. Nit. &:c. 



Inversion of For. II. on 

 III. with fault. Flows 

 from II. Bold. No gas. 

 Inverted axis of For. II. 

 Very copious. 



Inversion of For. II. on 

 III. with fault. Flows 

 from II. Bold. Nit. Ox. 

 and C. acid. 



Junction of For. Lwith 

 Hypogene rocks. 



