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About Ballard Park
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Ballard Park is a wild and natural open space of 13 acres located near the intersection of Hazard and Wickham Roads, directly across from Rogers High School in Newport, Rhode Island. The park was deeded as a gift to the City of Newport in 1990 by Carol C. Ballard. It has been designated by deed as an area to be used for conservation, education and passive recreation. Its unique features include two 19th century quarries and a diverse variety of native and introduced plant (see list below) species. Ballard Park allows for unobtrusive observation of the abutting 54 acre wildlife refuge by providing paths suitable for walking and bird watching. The park is remarkably diverse. It forms an unfragmented block of habitat and open space with the contiguous 54 acre wildlife refuge, Gooseberry Beach, Newport Country Club and Brenton Point State Park. In the Spring, Cooper Hawks and Northern Harriers (both state listed species) scan the meadow quarry for prey. Deer use the tall grass of the quarry meadow to bed and turtles amble into the meadow to lay their eggs in the summer months. In addition to high rocky ledges and thickly wooded ravines, the park is home to a vernal pond and several small, seasonal streams. Parts of Ballard park have spectacular views out to the Atlantic Ocean. Native trees, glades of ferns and wildflowers are also present creating glimpses of Aquidneck Island's 17th century past. In fact, in a city which has been continuously occupied since the earliest Colonial days, Ballard park contains an unusually pristine landscape which has both esthetic and historical value. |
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PLANT LIST FERNS Cinnamon Fern Hay-scented Fern Lady-fern Marginal Wood Fern Spinulose Wood Fern Common polypody New York Fern Sensitive Fern ANGIOSPERMS - Monocots GYMNOSPERMS |
ANGIOSPERMS - Dicots |
Common St. Johnswort |
GEOLOGY
All three basic types of rocks -- Igneous, Sedimentary and Metamorphic --are found in Newport’s Only Nature Preserve, Ballard Park. SEDIMENTARY In Ballard Park, the one Puddingstone boulder is about the size of a small car and basically oval shaped located between the Southwest and Valley Trails. It is composed of many smaller, rounded stones, pebbles, cobbles and sand cemented together. METAMORPHIC The Price Neck Formation outcrop looks like a hill of stone off to the side of the Swamp Maple trail near where the board walk ends. The rock is gray and composed of very fine minerals, much finer and smaller than the minerals that make up the Newport Granite or the Puddingstone. IGNEOUS The majority of rock found in Ballard Park is Newport Granite. There are also slight differences in the sizes and shapes of the minerals making up the Newport Granite throughout the park, these are the result of differences in the conditions when the granite first formed.
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