Synopsis of geological phenomena. 
SOURri'S OF EVIDEXC 
UEDUCTIONS. 
Pishes in ab 
Petrified she 
Cyrstalsblu 
liviucniiy SUCH loicc; was ueueciiiu uy primuive i gei 
rocks, and further as th2 matter formed, locally — J cumstances was adequate to th 
the elevating force reitiiiiiing greatest at greatest I ual elevation of land, 3 or 4 
depths of water \ higher than the ordinary level. 
origin of HILLS which w 
bro- the hquid matter of 
, of land animals mi? 
Earth was dry and inhabited. 
By thebouldered 
s surface, ' , There h 
!i''nfiStllTf.iH''.!tEf ''''''^'^ !■ We ascertain the way of action -THE DELUGE. 
By the height to which tlic boulder: 
We get the force of action and height of the v 
ILLUSTRATIVE EFFECTS OF THE DELUGE. 
Hyalmn-sb. 
Brthe\a?n, 
By the abiL 
ByShjpfellyi 
By sea shells 
Hyscas shells 
Bv romtdcd c 
I ODsideofditto.fromnorthof Ireland . 
j Vale of Taunton and below Bristol, on the hil! 
" ■ ■ ■■ Bath, Cricklade common, 
* ■ ■ I N'orthamptonshire, Rutland and Huntingdoi 
. . . Ashby dc la Zouch, and vale of Trent 
. - . Needwood Forest, 
:.late I Moughton Fell, (see papers on Craven rock' 
1 ftet abavc the slate. 
I Current deflected. 
I uplaying force. 
•ifiinal docunieni this read "and c 
To face page 175. 
