Raymond : The Cma/y Formation' and its Fauna. 



r)2<) 



Bryozoan sp. ind. r, 

 F/cesioiiiys />/a/ys c, 

 RafineS(}uina cliaDif^litiiirusis c, 

 Clitamboiiitcs inulticosfa r, 

 OrtJiidiimi hiDiellosum r, 

 Canierella loiigirostris R, 



llialeops 07'ata r, 

 Aiiiphilic/ias ininga/w/ists r, 

 Plioiitrrops canadoisis, r, 

 Leperditia limatula r, 

 Leperditia canadensis c. 



This fauna indicates tliat these strata belong to Division 2. 



Station A',,^,. This station is at the extreme northern end of the 

 same point. The rock is more impure, containing much clay, and 

 ^^aclllri^cs »iaguus is absent. 



Ph.yllopo7-iiia inccpta r, 

 Hebertclla sp. r, 

 Plccsiomys platys r, 

 Hebertclla borcalis r, 

 Rafiuesqniiia alteruata r, 

 Rafincsqiiina champlainensis c. 



ClitaDibonitcs iniilticosla r, 

 Trochoiievia hudsoiii r, 

 TroclioncDia dispar r, 

 Thalcops ovafa r, 

 Plio/iierops caiiadc7isis r, 

 AniphilicJias minganeiisis r. 



This also belongs to Division 2. 



Station Vj^^.^. This locality is on the first point of rock south of the 

 lower farm-house (Church farm) at Valcour Island. The rock is a 

 rather coarse-grained, but hard limestone, and does not yield the 

 fossils readily. 



Cai/ierclla loiio/'/uislris c, 

 Asaphiis alpha r, 

 Asaphits beta r, 

 Illccmis globosiis r, 

 Pfi'iygoinetopiis aiiiiiilaliis r, 

 P.cperditia ca/iade//s/s c. 



Monotrypella sp. c, 

 Bryozoan sp. ind. c, 

 Plccsiomys platys c, 

 Heberiella borcalis c, 

 Rafinesqtiina chaiiiplainciisis c, 

 Rafincsquina disfaiis r, 

 Caiiiarota'iliia prist in us c, 



This fauna indicates Division 2. 



Station ¥,^3. This station is on the ledges a {qw rods south of 

 V,P2 ^"cl ne«r the fence between the middle and south farms. All the 

 specimens came from a thin layer of ])ure limestone, in which the 

 fossils are well preserved. 



Monotrxpclla sp. r, Conocardiuin bcechcri R, 



Phylloporina incept a c, Ctenodonta pcracuta r, 



Bryozoan sp. ind. c, Judiarpcs antiqnafiis r, 



