Cape Cod : $b its natural and cultural history : a guide to Cape Cod National Seashore, MassachusettsUnited States. National Park Service. Division of Publications
History
Cape Cod : $b its natural and cultural history : a guide to Cape Cod National Seashore, Massachusetts
United States. National Park Service. Division of Publications
Cape Cod National Seashore (Mass.) -- Guidebooks
Even more valued by these early Cape Cod farmers were the salt
marshes, or salt meadows. In a place of little natural grassland,
marshes were prized for grazing. During the spring and summer cows
were pastured on the marshes, with boys sent along to keep them from
falling into the tidal creeks or potholes, called “pannes.” In fall
the salt hay was scythed, stacked in ricks on raised wooden platforms
called “staddles,” and hauled to the barns by oxen or horses wearing
special wide wooden shoes to keep them from sinking into the peat.
The Cape’s numerous bays, inlets, salt ponds, and estuaries were also
early recognized as marine cornucopias. Foot-long oysters, scallops,
crabs, eels, flounder, diamondback terrapins, striped bass, mackerel,
and other fish were taken for local use, and clam shells provided the
lime for plastering colonial walls.
Still, despite the many uses these early settlers made of the marine
riches around them, they did not truly become men of the sea until
they were forced to by the land’s limitations and by their own
mismanagement of it. The Cape’s once-abundant woodlands were cut and
burned for farm and pasture land and consumed for a seemingly endless
array of local uses and industries: heating homes; boiling seawater
for salt; building boats, gristmills, houses, and barns; firing tar
kilns; and trying out whale blubber, to name just a few.
[Illustration: _The Atlantic cod typically weighs 10 to 25 pounds but
ranges up to 200 pounds. Its bountiful numbers sparked Massachusetts’
first major maritime industry in the 1600s. A bottom dweller, the cod
soon attracted Cape fishermen to the Grand Banks off Newfoundland and
to Georges Bank off Cape Cod._]
The thin glacial soil, exhausted by repeated cropping and left
unprotected by deforestation, soon blew away. In Provincetown,
unregulated cutting and grazing in the Province Lands let loose the
dunes, which threatened to bury the town and fill up the harbor. By
1800 dune ridges were advancing at a rate of 90 feet a year. In 1847
Massachusetts geologist Edward Hitchcock, visiting the Lower Cape,
felt as if he were “in the depths of an Arabian or Libyan desert.”
Though the Cape’s soil was never very rich, the waters around it
teemed with abundance, and in the sea Cape Codders found their
true destiny. Thrust some 30 miles out into the Atlantic, the Cape
partakes of two distinct marine environments. Cape Cod Bay is part of
the larger Gulf of Maine ecosystem, a cold-water habitat influenced
by the south-flowing Labrador Current. The waters of Nantucket Sound,
averaging some ten degrees warmer, are influenced primarily by the
northward-flowing Gulf Stream.
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