132 
TABULAR VIEW OF 
TABULAR VIEW 
OF 
THE EOSSILIFEROUS STRATA, 
SHOWING THE ORHEE OF SUPERPOSITION OR CHRO.NOLOGIOAL SUCCESSION OP THE PRIN¬ 
CIPAL GROUPS, WITH REFERENCE TO THE PAGES WHERE THEY ARE DESCRIBED IN 
THIS WORK. 
POST-TERTIARY. 
POST- 
TERTIARY. 
1 . 
RECENT. 
Shells and mam¬ 
malia, all of 
living species. 
2 . 
POST¬ 
PLIOCENE. 
Shells, recent 
mammalia in 
part extinct. 
EXAMPLES. 
British—C\yde marine strata, with canoes (p. 146). 
Foreign —Danish kitchen middens (p. 146). 
Lacustrine mud, with remains of Swiss lake-dwell¬ 
ings (p. 148). 
Marine strata inclosing Temple of Serapis, at Puz- 
zuoli (p. 146). 
British—lj 02 Lm of Brixham cave, with flint imple¬ 
ments and bones of extinct and living quadru¬ 
peds (p. 157). 
Drift near Salisbury, with hones of mammoth, 
Spermophilus, and stone implements (p. 161). 
Glacial drift of Scotland, with marine shells and 
remains of mammoth (p. 176). 
Erratics of Pagbam and Selsey Bill (p. 182). 
Glacial drift of Wales, with marine fossil shells, 
about 1400 feet high, on Moel Tryfaen (p. 181). 
Foreign —Dordogne caves of the reindeer period (p. 
150). 
Older valley-gravels of Amiens, with flint imple¬ 
ments and bones of extinct mammalia (p. 152). 
Loess of Rhine (p. 154). 
Ancient Nile-mud forming river-terraces (p. 154). 
Loam and breccia of Liege caverns, with human 
remains (pp. 156,157). 
Australian cave breccias, with bones of extinct mar¬ 
supials (p. 158). 
Glacial drift of Northern Europe (pp. 166-188). 
TERTIARY OR CAINOZOIC. 
PLIOCENE. 
3. 
NEWER 
PLIOCENE. 
The shells al¬ 
most all of living 
species. 
4. 
OLDER 
PLIOCENE. 
Extinct species 
of shells forming 
a large minority. 
—Bridlington beds, marine Arctic fauna (p. 
189). 
Glacial boulder formation of Norfolk clififs (p. 190). 
Forest-bed of Norfolk cliffs, with bones of Elephas 
I meridionalis, etc. (p. 191). ^ 
Chillesford and Aldeby beds, with marine shells, 
chiefly Arctic (p. 192). 
Norwich crag (p. 193). 
Foreign—E?Lstevn base of Mount Etna, with marine 
shells (p. 204). 
Sicilian calcareous andtufaceous strata (pp. 205,206). 
Lacustrine strata of Upper Val d’Arno (p. 207). 
. ■ Madeira leaf-bed and land-shells (p. 532). 
British—Red crag of Suffolk, marine shells, some of 
northern forms (pp. 194,195). 
White or coralline crag of Suffolk (p.T97). 
Foreign —Antwerp crag (p. 204). 
Subapennine marls and sands (p. 208). 
