PAR'T II. 



SECTIONS. 



Sand Crekk and White River Sections. 



Sand creek is one of the eastern tributaries of the East fork of 

 White river, and joins that stream sixty miles north of Louis- 

 ville. It crosses the Devonian belt from east to west and along 

 its valley occur some of the northernmost outcrops of the De- 

 vonian limestone to be met with in the state south of the Wabash 

 valley. 



Station 2C. — At Scipio the New Albany shale outcrops just 

 southwest of the Episcopal church at the roadside and contains 

 an abundance of Styliolafissurella. 



A few hundred yards to the southwest of 2C the Devonian 

 limestone outcrops along a ravine. A small amount of colleAing 

 from the limestone a few feet below the Black shale afforded the 

 following species: 



Chonetes yandellanus, Dahnanites s^., Glyptodesma ereSlum, 

 Spirifer acuminatus, Spirifer varicosus, Stropheodonta perplana, 

 Stropheodonta demissa, Tentaculites bellulus. 



Station 2 A. — West of Scipio one and one-half miles, good out- 

 crops of the limestone occur at the side of the wagon road which 

 afforded the following fossils: 



Glyptodesma occidentale , Orthothetes chemungensis arnostriatus , 

 Platyceras carinatuni^ Polypora sp., Proetus sp., Proetus micro- 

 gemma, Spirifer aciwtinatns, Stropheodonta demissa, Stropheo- 

 donta inequistriata, Stropheoda7ita perpiana, Tentaculites s^. 



