111

J Hall Vol VI. p 173 (Ed. Transact) has seen clay stuff enough for potters to use in which great knife formed crystals of ice were formed (like my gypsum case) shows power of segregation & has heated angular fragments of rock, which returned thus angles sharp – yet with character completely altered, & a crystalline structure superinduced

Lyell on Sweden p. 5 & 7 richest shale from decomposed muscles.

Smith of Jordanhill has seen same thing

 

147

When I come to treat of the age of the Pampas Deposit: I may properly remark on the superiorly of Lyell's classification to that of Phillips as given p. 13 Vol II Lardner's Treatise

Phillips in Lardner Vol II p 73: some remarks on veins:

Phillips in Lardner Vol II p 80 – some remarks on dikes applicable to Cordillera

Phillips in Lardner Vol II p 81 & 83 some remarks on thinness of coast as implied by meeting with granite everywhere

Phillips in Lardner Vol II p 125 good discussion on mineral veins

p 125 to 129 & p. 135 – 160 & 162

[Phillips, John. 1839. The cabinet Cyclopædia. Conducted by Rev. Dionysius Lardner, etc. Treatise on geology. Vol. II. London: Longman, Orme, Brown, Green & Longmans, John Taylor, and A. Spottiswoode.]