I 
To Mll'i'hn-rn -ffia Grego^T \Jyo3iiup Avenuaa-^ Gap Fii^st 
aJriTiSHpondlBg lap in Second -;o..nta.ln fnled Py Moraine. 
Mount a 5, 
These gaps mark pi’ 
Rookaway Rivers. 
®®^“g-glaoiai course of the upper paSsaic and 
To Church of Revolutlonpy fame* " '^9 Union, 
anil Woodhridge. Porch Amhoy for night* 
'imhoy 
Jers^. 
RoselleT^WEeaisTejf and Woodhridgc 
Ho to pn__Triag of __ 
foraation in lew Jersey consists of a great thick- 
ness IfTel lhlle, arkosic d 
Hud;o*n ^he^Ld^nts «re nalnly fluvlat le ao=-dM»latad In^n 
SSSIBm S~ 
motmtalne. In ths northeastern gtMktorf Ad lookLong beds 
a“f .elf neS Srfll^aA, Aere ptofcnnd faulting repeats 
the series twlee, ^ oL/SoAtain 
fwl Tlr?ir| time the' lo.er 
O'-’ which (3om©r*'i3.ie peneplain) was v/idely covered with str 
deposits in oaily Ploistoconoo These have been since 
“tiify remfsd and the present dissection acoonpllshed. 
THURSDAY 
Note on Gretaceous of I.T9'v< 
25 fsot 
25<»70 feet 
3(9 
member O^'ICO " 
o5«40 foot 
5-60 ” 
2Qd.35 feet 
aQ 0-55 feet 
^ tf 
feet 
feet 
!^n New Jersey the Cretaceous consists of the 
lianas quan marl 
Rau'jocas group 
’ Tfincen'i/Own sand 
' Rorners t own marl 
Mohiaouth group ^ 4. ^ . 
Rsdbank sand and Tint on sand 
Nave sink marl 
Mount laurel sand 
Matawan group 
Wenonah sand _ 
Marshallt'^’'''® iormation 
Engl is ht own sand 
Woodbury elay 
lierchantvill® <Slay 
- 7 - 
2 G-IOO 
60 
