Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Salveston gets its water out of artesian dry
wells about 8-10 miles N. of W. of the city.
Baker tells me that the Hurricanes flowing in
from the Gulf pile the water 14 feet above ordinary
sea-level. This is definitely proven since at the
Duelphin Mine sea water came to the 14 foot elev...
tion. This is an important matter to bear in mind
regarding other phenomena. Also that formerly the present
shore is about six city blocks further out than it was
before the hurricane. It is again building out to sea.
The land goes very gradually into the sea, and
the wind waves roll in very gently, probably make no
higher than 12 inches - so shallow is the shore out to
sea. The sand is very fine, even graded, and
taell from the strand where dry the winds blow it into
dunes. These dunes flow higher toward the
Air Grande. Beneath the surface the sands
are replete with from 15-30 species of small pele-
cyphos and some gastropods. Cray are lived by
gastropods. Sea snails are practically absent. Chitinos
worm tubes with shells glued all over them are
common. See these samples of sand and worm
tubes.