The Quaker Colonies [36]
Jersey and, while they were not numerous enough to make it a thoroughly Puritan community, they largely tinged its thought and its laws, and their influence still survives.
The difficulty with Jersey was that its seacoast was a monotonous line of breakers with dangerous shoal inlets, few harbors, and vast mosquito infested salt marshes and sandy thickets. In the interior it was for the most part a level, heavily forested, sandy, swampy country in its southern portions, and rough and mountainous in the northern portions. Even the entrance by Delaware Bay was so difficult by reason of its shoals that it was the last part of the coast to be explored. The Delaware region and Jersey were in fact a sort of middle ground far less easy of access by the sea than the regions to the north in New England and to the south in Virginia.
There were only two places easy of settlement in the Jerseys. One was the open region of meadows and marshes by Newark Bay near the mouth of the Hudson and along the Hackensack River, whence the people slowly extended themselves to the seashore at Sandy Hook and thence southward along the ocean beach. This was East Jersey. The other easily occupied region, which became West Jersey, stretched along the shore of the lower Delaware from the modern Trenton to Salem, whence the settlers gradually worked their way into the interior. Between these two divisions lay a rough wilderness which in its southern portion was full of swamps, thickets, and pine barrens. So rugged was the country that the native Indians lived for the most part only in the two open regions already described.
The natural geographical, geological, and even social division of New Jersey is made by drawing a line from Trenton to the mouth of the Hudson River. North of that line the successive terraces of the piedmont and mountainous region form part of the original North American continent. South of that line the more or less sandy level region was once a shoal beneath the ocean; afterwards a series of islands; then one island with a wide sound behind it passing along the division line to the mouth of the Hudson. Southern Jersey was in short an island with a sound behind it very much like the present Long Island. The shoal and island had been formed in the far distant geologic past by the erosion and washings from the lofty Pennsylvania mountains now worn down to mere stumps.
The Delaware River flowed into this sound at Trenton. Gradually the Hudson end of the sound filled up as far as Trenton, but the tide from the ocean still runs up the remains of the Old Sound as far as Trenton. The Delaware should still be properly considered as ending at Trenton, for the rest of its course to the ocean is still part of Old Pensauken Sound, as it is called by geologists.
The Jerseys originated as a colony in 1664. In 1675 West Jersey passed into the control of the Quakers. In 1680 East Jersey came partially under Quaker influence. In August, 1664, Charles II seized New York, New Jersey, and all the Dutch possessions in America, having previously in March granted them to his brother the Duke of York. The Duke almost immediately gave to Lord Berkeley and Sir George Carteret, members of the Privy Council and defenders of the Stuart family in the Cromwellian wars, the land between the Delaware River and the ocean, and bounded on the north by a line drawn from latitude 41 degrees on the Hudson to latitude 41 degrees 40 minutes on the Delaware. This region was to be called, the grant said, Nova Caesarea, or New Jersey. The name was a compliment to Carteret, who in the Cromwellian wars had defended the little isle of Jersey against the forces of the Long Parliament. As the American Jersey was then almost an island and geologically had been one, the name was not inappropriate.
Berkeley and Carteret divided the province between them. In 1676 an exact division was attempted, creating the rather unnatural sections known as East Jersey and West Jersey. The first idea seems to have been to divide by a line running from Barnegat on the seashore to the
The difficulty with Jersey was that its seacoast was a monotonous line of breakers with dangerous shoal inlets, few harbors, and vast mosquito infested salt marshes and sandy thickets. In the interior it was for the most part a level, heavily forested, sandy, swampy country in its southern portions, and rough and mountainous in the northern portions. Even the entrance by Delaware Bay was so difficult by reason of its shoals that it was the last part of the coast to be explored. The Delaware region and Jersey were in fact a sort of middle ground far less easy of access by the sea than the regions to the north in New England and to the south in Virginia.
There were only two places easy of settlement in the Jerseys. One was the open region of meadows and marshes by Newark Bay near the mouth of the Hudson and along the Hackensack River, whence the people slowly extended themselves to the seashore at Sandy Hook and thence southward along the ocean beach. This was East Jersey. The other easily occupied region, which became West Jersey, stretched along the shore of the lower Delaware from the modern Trenton to Salem, whence the settlers gradually worked their way into the interior. Between these two divisions lay a rough wilderness which in its southern portion was full of swamps, thickets, and pine barrens. So rugged was the country that the native Indians lived for the most part only in the two open regions already described.
The natural geographical, geological, and even social division of New Jersey is made by drawing a line from Trenton to the mouth of the Hudson River. North of that line the successive terraces of the piedmont and mountainous region form part of the original North American continent. South of that line the more or less sandy level region was once a shoal beneath the ocean; afterwards a series of islands; then one island with a wide sound behind it passing along the division line to the mouth of the Hudson. Southern Jersey was in short an island with a sound behind it very much like the present Long Island. The shoal and island had been formed in the far distant geologic past by the erosion and washings from the lofty Pennsylvania mountains now worn down to mere stumps.
The Delaware River flowed into this sound at Trenton. Gradually the Hudson end of the sound filled up as far as Trenton, but the tide from the ocean still runs up the remains of the Old Sound as far as Trenton. The Delaware should still be properly considered as ending at Trenton, for the rest of its course to the ocean is still part of Old Pensauken Sound, as it is called by geologists.
The Jerseys originated as a colony in 1664. In 1675 West Jersey passed into the control of the Quakers. In 1680 East Jersey came partially under Quaker influence. In August, 1664, Charles II seized New York, New Jersey, and all the Dutch possessions in America, having previously in March granted them to his brother the Duke of York. The Duke almost immediately gave to Lord Berkeley and Sir George Carteret, members of the Privy Council and defenders of the Stuart family in the Cromwellian wars, the land between the Delaware River and the ocean, and bounded on the north by a line drawn from latitude 41 degrees on the Hudson to latitude 41 degrees 40 minutes on the Delaware. This region was to be called, the grant said, Nova Caesarea, or New Jersey. The name was a compliment to Carteret, who in the Cromwellian wars had defended the little isle of Jersey against the forces of the Long Parliament. As the American Jersey was then almost an island and geologically had been one, the name was not inappropriate.
Berkeley and Carteret divided the province between them. In 1676 an exact division was attempted, creating the rather unnatural sections known as East Jersey and West Jersey. The first idea seems to have been to divide by a line running from Barnegat on the seashore to the