82 Origin of the British Flora. 
«Eine Probe aus dem Torflager bei Lauenburg an der 
Elbe? Naturwissensch, Wochenschrift, 4th Nov., 1894.) 
The exact relation of this peat to the Glacial deposits 
is not clear, and Professor Nathorst suggests that more 
than one plant-bed is represented. The occurrence of 
Brasenia suggests an Interglacial date. 
Nymphea alba. Lycopus europeus. 
Brasenia purpurea. ~ Ulmus. 
Corydalis fabacea. Alnus glutinosa. 
Viola. Carpinus Betulus. 
Arenaria trinervia. Corylus Avellana. 
Tilia platyphyllos. Quercus Robur. 
Geranium columbinum. Salix aurita (?). 
Rhamnus Frangula. Salix repens. 
Acer platanoides. Pinus sylvestris. 
Trapa natans. Picea vulgaris. 
Cornus sanguinea. Larix europza. 
Viburnum Opulus (?). Iris Pseudacorus. 
Lysimachia Nummularia (?). Sparganium. 
Vaccinium Oxycoccos. Potamogeton. 
Fraxinus excelsior. Carex Pseudo-cyperus, 
Menanythes trifoliata. 
MUNDESLEY, NORFOLK. 
(Reid, ‘ Geology of the Country around Cromer, pp. 36, 
37, 83, 84, 118, 119, and folding plate, Wem. Geol. Survey, 
1882; also ‘Pliocene Deposits of Britain,’ pp. 166-169. 
2bid@. 1890.) 
At this locality three different plant-bearing deposits 
are represented. The oldest is Preglacial, and belongs to 
the Cromer Forest-bed, which is here divisible into an 
upper and a lower freshwater deposit, between which is a 
mass of estuarine gravel. The lower freshwater bed 
consists of laminated peat, full of fruits of Zrapa natans, 
but containing little else. The middle or Estuarine divi- 
sion, contains bones of extinct mammals, much drift-wood,, 
and cones of Pinus sylvestris and Picea excelsa. The: 
