Knowledge

Hatfield Swamp

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The Whippany River flows into the Rockaway River, at the western end of the swamp. The Rockaway River travels a short distance and then flows into the Passaic River near the center of the swamp. The USGS gaging station is 1.3 miles (2.1 km) downstream of the Rockaway River confluence. At this
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Muskrats are low in population in the swamp due to several factors. The first is the flooding of the area, which fills bank dens with water. The second is the lack of plant foods that the muskrats eat. The third is water pollution. While efforts to clean the rivers of pollution have proven
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The Hatfield Swamp floods several times a year, from heavy rain, snow melt in spring, or the remnants of storms that originated in the tropics. The area is the joining point of three rivers. The frequent flooding makes the swamp a difficult place to live for mammals, such as deer, raccoons,
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The area has a northern deciduous forest consisting of various oaks, maples, sweet gum, and elm. Most trees are from six to ten inches (254 mm), with some going to twenty inches. Due to the constant flooding makes it difficult for hardwood trees to grow.
118:, were confiscated and sold to Cyrus Crane, who operated a mill on the edge of the swamp in what is now West Caldwell. After the death of family member Herbert Crane in the 1960s, the mill was dismantled and moved to 96:
point the Passaic River drainage is three hundred forty nine square miles. This includes the Rockaway River drainage of one hundred twenty five square miles and the Whippany River drainage of sixty nine square miles.
67:. Over millions of years, the rift valley was faulted, tilted, and eroded, until the edges of the hard flood basalt layers formed ridges. Prior to 20,000 years before the present, an ancestral 87:. After thousands of years, the lake drained leaving behind many swamps with various hardwood trees struggling to take hold, including the Hatfield Swamp. 55:
periods, when the North American plate separated from the African plate, an aborted rift system was created. The resulting rift valley, known as the
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lead trips within the swamp throughout the year, while the Essex County Environmental Center provides information regarding such trips.
75:, a massive continental ice sheet which formed during the last ice age, advanced on the region and permanently plugged the gap with 99:
The area is from 180 feet (55 m) above sea level to 160 feet (49 m). Latitude 40.85 N and Longitude 74.32 W
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possums, skunks and fox. Most of these animals live on the fringes of the swamp, where the ground is higher.
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Waterfowl that pass through the area in the autumn stop and rest in the swamp before proceeding south.
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The area of Hatfield Swamp is approximately 2,500 acres (10 km), located in northern New Jersey.
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The swamp is named for Cornelius Hetfield who owned and operated a mill sometime before the
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The wetlands, which help facilitate hiking through their flatness, are a part of
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Fish that inhabit the Rockaway River and Whippany River are carp and catfish.
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flowed through a gap in these ridges. This changed when the
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successful so far, pollutants remain in the soil and water.
27:, forming what might be considered the "second bank" of the 157:, and there are a number of trails open for public 222: 59:, was filled with alternating layers of 161:. Both the Essex County Chapter of the 236:Landforms of Morris County, New Jersey 223: 231:Landforms of Essex County, New Jersey 13: 125: 14: 262: 172: 122:in Monmouth County, New Jersey. 1: 90: 7: 10: 267: 105: 42: 23:area in the U.S. state of 179:Birding at Hatfield Swamp 148: 246:Swamps of New Jersey 184:USGS topographic map 85:Glacial Lake Passaic 207:40.8408°N 74.3283°W 203: /  165:and the New Jersey 112:American Revolution 251:Watchung Mountains 120:Allaire State Park 81:Watchung Mountains 212:40.8408; -74.3283 73:Wisconsin Glacier 19:is a fresh water 258: 218: 217: 215: 214: 213: 208: 204: 201: 200: 199: 196: 47:During the late 266: 265: 261: 260: 259: 257: 256: 255: 221: 220: 211: 209: 205: 202: 197: 194: 192: 190: 189: 175: 167:Audubon Society 155:West Essex Park 151: 128: 126:Flora and fauna 108: 93: 45: 12: 11: 5: 264: 254: 253: 248: 243: 238: 233: 187: 186: 181: 174: 173:External links 171: 150: 147: 127: 124: 107: 104: 92: 89: 77:glacial rubble 44: 41: 17:Hatfield Swamp 9: 6: 4: 3: 2: 263: 252: 249: 247: 244: 242: 241:Passaic River 239: 237: 234: 232: 229: 228: 226: 219: 216: 185: 182: 180: 177: 176: 170: 168: 164: 160: 156: 146: 142: 139: 136: 132: 123: 121: 117: 113: 103: 100: 97: 88: 86: 82: 78: 74: 70: 69:Passaic River 66: 65:flood basalts 63:sediment and 62: 58: 54: 50: 40: 38: 34: 30: 29:Passaic River 26: 22: 18: 188: 152: 143: 140: 137: 133: 129: 109: 101: 98: 94: 57:Newark Basin 46: 16: 15: 210: / 163:Sierra Club 83:), forming 225:Categories 198:74°19′42″W 195:40°50′27″N 51:and early 39:counties. 25:New Jersey 91:Geography 116:Loyalist 53:Jurassic 49:Triassic 31:between 106:History 61:red bed 43:Geology 21:wetland 159:hiking 149:Hiking 33:Morris 37:Essex 35:and 227::

Index

wetland
New Jersey
Passaic River
Morris
Essex
Triassic
Jurassic
Newark Basin
red bed
flood basalts
Passaic River
Wisconsin Glacier
glacial rubble
Watchung Mountains
Glacial Lake Passaic
American Revolution
Loyalist
Allaire State Park
West Essex Park
hiking
Sierra Club
Audubon Society
Birding at Hatfield Swamp
USGS topographic map
40°50′27″N 74°19′42″W / 40.8408°N 74.3283°W / 40.8408; -74.3283
Categories
Landforms of Essex County, New Jersey
Landforms of Morris County, New Jersey
Passaic River
Swamps of New Jersey

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