22 



INTRODUCTION 



Carpinus caroliniana, 

 Betida nigra, 

 Fagus grandifolia, 

 Quercus rubra, 

 Aristolochia Serpentaria, 

 Tovara virginiana, 

 Liriodendron tidipijera, 

 Cimicifuga racemosa, 

 Anemone virginiana, 

 Ranunculus hispidus, 

 Thalictrum revolutum, 

 Menispcrmum canadense, 

 Sanguinaria canadensis, 

 Micranthes pennsylvanica , 

 Micranthes virginiensis, 

 Henchera americana, 

 Geum canadense, 

 Agrimonia pubescens, 

 Cassia marilandica, 

 Meibomia nudiflora, 

 Ionoxalis violacea, 

 Ca th a rtolin u m virginianum , 



Sanicida marilandica, 

 Angelica villosa, 

 Cynoxylon floridum, 

 Fraxinus pennsylvanica, 

 Menyanthes trifoliata, 

 Phlox macidata, 

 Scutellaria pilosa, 

 Scutellaria galericidata, 

 Koellia flexuosa, 

 Cunila origanoides, 

 Chelone glabra, 

 Pedicularis lanceolata, 

 Pedicularis canadensis, 

 Galium circaezans, 

 Viburnum prunifolium, 

 Triosteum perfoliatum , 

 Campanula aparinoides, 

 Aster macrophyllus, 

 Erigeron pulchellus, 

 Senecio aureus. 

 Cynthia virginica, 

 Lactuca spicata, 



34. The distribution of Tsuga canadensis in lower New Jersey is, 

 it seems to me, directly attributable to the glacial terraces found 

 along the small depression areas in the lower Delaware River 

 where the tree is now found. It is known only at one other station 

 elsewhere on the coastal plain, in Maryland, but is, of course, 

 common northward. There are a few more plants with a some- 

 what similar distribution in southern New Jersey, notably Cercis 

 canadensis, which ranges southward, east of the Alleghanies, from 

 these New Jersey and Pennsylvania stations. 



35. Of the peculiar flora of the eastern side of the pine-barrens, 

 called by Stone the "coastal strip," it is difficult to do more than 

 give the list of species found there. None of these are known 

 in the pine-barrens, some are found in the region of glacial terraces 

 in the western part of the Cretaceous region, and others further 

 north. That the coastal strip was ever affected by glacial material 

 in any way seems very doubtful, as the drainage from the front 



