REPORT OF THE DIRECTOR AND STATE GEOLOGIST 1901 r49 



shore of Hempstead harbor, about a mile west of the Glencove 

 landing. This shale is unquestionably a phase of the clay, prob- 

 ably a result of hardening, due to oxidation of iron, and part 

 of the loose material on the beach represents the same, which 

 has been washed out by the waves. Other specimens represent 

 material that has come from the adjacent bluffs, where it occurs 

 as drift boulders, in connection with other morainal material. 



In the list of accessions all the specimens noted from Glen- 

 cove were collected under one or another of the above con- 

 ditions. 



SPERMATOPHYTA 



Gymnospermae 

 Dammara borvalis^ Heer, Fl. Foss. Arct. v. 6, Abth. 2, p. 54, pi. 37, 



fig. 5. 



Glencove N. Y. 



Angiospermae 



MoMocotyledones 



Serenopsis Jcempii Hollick, Torrey Bot. Club. Bui. 20:169, 



pi. 149. 



Glencove N. Y. 



Fragments of monocotyledons of uncertain affinities 



Glencove N. Y. 



Diootifledones 



Juglcms arctioa Heer (?), Fl. Foss. Arct. v. 6, Abth. 2, p. 71, 

 pi. 40, fig. 2. 



Glencove N. Y. 



SaMoc inaequalis Newb., Fl. Amboy Clays, p. 67, pi. 16, fig. 1 } 4, 6; 

 pi. 17, fig. 2-7. 



Glencove N. Y. 



Ficus willisiana Hollick, Torrey Bot. Club. Bui. 21:52, pi. 176, 

 fig. 2, 5. 



Glencove N. Y. 



Magnolia auriculata Newb., Fl. Amboy Clays, p. 75, pi. 41, fig. 13; 

 pi. 58, fig. 1-11. 



Glencove N. Y. 



Magnolia oapelUm Heer, Phyll. Cre't. Neb. p. 21, pi. 3, fig. 5, 6. 



Glencove and Center island, Oyster Bay N. Y. 



