Udall's Park Preserve

According to local Native American lore, there once lived on the shores of Long Island Sound two tribes of giants. When they were at war with each other, the tribe on the Connecticut side would break off pieces of their mountains and hurl them at the giants on Long Island.  The Long Island giants, because they had no mountains, would reciprocate by hurling boulders—a strategy that proved successful. The Long Island tribe’s victory is the legend that explains why Connecticut is strewn with boulders for many miles inland, while Long Island has boulders along its northern shore.

Geologists however, offer a different explanation. At various times over the past million years, global cooling caused massive glaciers to form over much of the northern United States. These ice sheets surged southward from Hudson Bay in Canada, collecting boulders, cobbles, gravel, and soil on the way. As temperatures began to rise 15,000 years ago, the last glacier receded from Long Island and debris was deposited throughout the landscape. On Long Island, it created the range of hills along the North Shore—called the Harbor Hill Terminal Moraine. North of these hills other flat-topped hills formed that now project into the Long Island Sound. These are the peninsulas of Great Neck, Bayside, and Douglaston that flank the pre-glacial river valley of Little Neck Bay and Udall's Cove. As the glacier continued to melt, runoff formed streams that cut into the landscape, creating ravines. Here at Udall's Cove, the streams carried sand and silt, which formed shallow intertidal flats that now collect water from throughout the area. The first plants to colonize these flats were a species of salt-tolerant grass. Where the grass thrived, the current slowed, causing more sedimentary accumulation. The cove’s bottom continued to rise, and more plant species were able to take hold. 

The earliest human inhabitants of this area probably arrived about 4,000 years ago, when a deciduous forest first appeared here. The people came during the warmer months, hunting white-tailed deer and game birds such as wild turkey that lived in the forest. Later visitors came to harvest the waters’ clams and oysters. In 1645, the Dutch established the town of Flushing, and land in Little Neck was granted to settlers such as Thomas Hicks and Richard Cornell. The Mattinecock Indians, led by Chief Tackapousha (d. 1694), disputed these claims and brought the issue before Governor Thomas Dongan (1634-1715). Tackapousha was at first able to delay white settlement but after a few years, Thomas Hicks led a force of Europeans in a raid against the Indian settlement, and forcibly took the land.

In 1833, Richard Udall, for whom the cove is named, bought a mill formerly owned by the Allen family on the eastern side of the cove. The mill, now called the Saddle Rock Mill, remained in the Udall family until 1950, when it was donated to the Nassau County Historical Society.  During the 1830s, a shellfishing community developed around the docks at Oldhouse Landing Road (now Little Neck Parkway) and Sand Hill Road. The industry thrived as the demand for oysters and Little Neck Clams grew. But by 1893, the local shellfish industry was finished, a victim of overharvesting, poaching, and pollution. Today, the stanchions and bulkheads at the end of Little Neck Parkway are all that remain of the bygone era. 

The Udall's Cove Preservation Committee initiated the acquisition of Udall's Park Preserve. The group of local residents organized in 1969 in order to prevent development of the land and promote public ownership. Udall's Cove was first mapped as a New York City park on December 7, 1972. The Preserve was created by a cooperative agreement between Parks and the New York State Department of Environmental Conservation; the state owns most of the land, but Parks manages the property.