As one goes to the top of the mountains back of the Parnon house the coarse sandstone part times of conglomerates are very noticeable. The pebbles from the ground and some are as large as half an inch. The Central and Gulf continues the entire Diluvian time passing without break into the Marlins. A less topography prevails to the East for the deposits are essentially limestone, though somewhat impure. This is continued into Crymours but towards the close a higher type- topography begins to appear seen in the chalk hills of the higher Crymours. This becomes more decided in the Maers Plains hill and then the sea becomes very muddy and finally on land. The Lower period in the western Cumberland Gulf prevails while in the east was deposited the Oolite and onto the Oolites the route again becomes gravel throughout the Cumberland Gulf. Elevation of the land continuing to the east on the Predmast slope and the Oolites losses more and more of its lime and becomes sandy and fry a conglomeratic sandstone in deposits. Elevation continues and all becomes land.