Geography of New Jersey: Difference between revisions

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[[Image:November 2006 - 2 008.jpg|thumb|left|The Delaware Water Gap from Knowlton Township in New Jersey.]]
[[Image:November 2006 - 2 008.jpg|thumb|left|The Delaware Water Gap from Knowlton Township in New Jersey.]]
[[Image:New Jersey shaded relief map.png|thumb|Shaded relief map]]
[[Image:New Jersey shaded relief map.png|thumb|Shaded relief map]]
The Appalachian Valley and Ridge lies in the northeastern corner of the valley and includes the [[Kittatinny Mountains]], several smaller valleys and the popular [[Delaware Water Gap]]. The state's highest point, the aptly named [[High Point]] is within this area, at 1,803 feet. Most of the state's section of the [[Appalachian Trail]] runs through this area. The province is bounded on the southeast by an [[unconformity]] between [[Cambrian]] and [[Precambrian]] formations.
The Appalachian Valley and Ridge lies in the northwestern corner of the state and includes the [[Kittatinny Mountains]], several smaller valleys and the popular [[Delaware Water Gap]]. The state's highest point, the aptly named [[High Point]] is within this area, at 1,803 feet. Most of the state's section of the [[Appalachian Trail]] runs through this area. The province is bounded on the southeast by an [[unconformity]] between [[Cambrian]] and [[Precambrian]] formations.


===Highlands Physiographic Province===
===Highlands Physiographic Province===

Revision as of 11:10, 21 December 2007

Location of New Jersey in the world
Location of New Jersey in the U.S.A.

New Jersey is a state within the United States of America that lies on the eastern edge of the North American continent.

The State of New Jersey shares a land border with the state of State of New York along the north. Along the east, New Jersey is flanked by the Atlantic Ocean, and is separated from New York, in particular the boroughs of the Bronx and Manhattan in New York City by the Hudson River, and from Staten Island by the Kill van Kull and the Arthur Kill. On its west, New Jersey is flanked by the Delaware River that forms its border with the Commonwealth of Pennsylvania and Delaware Bay which separates New Jersey from the State of Delaware. However, due to a fluke in a colonial land grant for the city of New Castle, Delaware (called The Twelve-Mile Circle), the state of Delaware possesses a small amount of land in New Jersey at Finns Point and a pier near Penns Grove, both adjacent to Salem County.

New Jersey's geography has contributed largely to its development, its economy and its rich history.

Area

New Jersey is the most densely populated state in the U.S.

New Jersey is ranked 47th of the fifty states that comprise the United States of America in terms of area. The total area of the state is 8,729 square miles, of which 14.9% or 1,304 square miles is water, and 85.1%, or 7,425 square miles, is land. New Jersey spans 70 miles (110 km) at its widest, and 130 miles (240 km) in length.

Due to its small size, New Jersey, which ranks tenth in the nation in terms of population with 8,414,350 people, ranks first in population density, with 1,134 people per square mile. However, while this offers the impression that New Jersey is entirely urban or suburban, it is not. Large swaths of northwestern and southern New Jersey are extremely rural. For example, Walpack Township in Sussex County, has a population of only 39 and an area of 26 square miles.

Political geography

New Jersey Counties

The State of New Jersey is divided into 21 counties, which contain a total of 566 municipalities. Like many New England states, all land in New Jersey is incorporated. New Jersey municipalities have a strong tradition of independent home rule which, as a result, means that county government is comparatively weaker than in other states and more open to criticisms of waste and ineffectiveness.[1]

Climate

New Jersey has a humid continental climate, vastly affected by its proximity to the Atlantic Ocean.

Average daily low temperature in January
  • Winter is typically cold. The lows usually hover in the 10s and 20s °F (down to -10 °C) and can frequently dip below 0 °F in the northwestern sections of the state. New Jersey winters often feature snowstorms known as Nor'easters that can paralyze the area with over a foot of snow. However, a variation in the climate also occasionally renders winter mild and almost snowless in sections of South Jersey near the Atlantic coastline.
  • Springs are mild, averaging in the 50s °F (10 to 15 °C) in late March to the lower 80s °F (25-30 °C) in early June. The weather is unpredictable and brings relatively cool summers as an occasional surprise, and huge snowstorms arriving as late as the second week in April (significant snow after mid-March is fairly rare though). Thunderstorms are common in spring.
Average daily high temperature in July
  • Summers in New Jersey tend to be hot and humid, with temperatures often exceeding 90 °F (32 °C), although high temperatures above 100 °F (38 °C) are about as rare as subzero (F) lows in winter. Humidity levels are usually quite high in July and August. Thunderstorms are common in summer. Hurricanes are considered to be a major threat to the area (and especially the Jersey Shoreline communities in Monmouth, Ocean, Atlantic and Cape May counties). While relatively infrequent compared to areas south and east, a direct hit could cause large loss of life and billions of dollars in damage due to the high population in coastal areas.
  • Autumns are comfortable in New Jersey and similar to spring in temperature. However, the weather is notably unpredictable and travelers are advised to check forecasts and bring several layers of clothing in late fall and in the early spring months (e.g., November, March, April) as temperatures do fluctuate quickly at these times of year.

The temperatures vary greatly from the northernmost part of New Jersey to the southernmost part of New Jersey. For example, these are the average high and low temperatures for Cape May, near the state's southernmost ocean-facing point, Sussex, in the mountainous northwest, and Trenton, the state capital located roughly midway between the two:

Sussex Trenton Cape May
High Low High Low High Low
January 34 14 38 24 42 27
February 38 16 41 26 43 28
March 47 25 51 33 51 35
April 59 35 61 42 60 43
May 70 45 71 52 69 53
June 78 54 80 61 78 62
July 83 59 85 67 84 67
August 82 57 83 65 83 66
September 74 49 75 57 77 60
October 63 37 64 45 66 49
November 51 30 54 37 56 40
December 39 21 43 28 47 31
(Temperatures above are Fahrenheit)

Data source: [2]

Rivers

New Jersey rivers includes streams formally designated as rivers. There are also smaller streams (i.e., branches, creeks, drains, forks, licks, runs, etc.) in the state. Major rivers include the Manasquan, Maurice, Mullica, Passaic, Rahway, Raritan, Musconetcong, and Delaware rivers. Historically, the Delaware and Raritan rivers have provided transportation of goods and people inland from the Atlantic Ocean, and were once connected by the Delaware and Raritan Canal. Today, these rivers, and the streams that feed them, provide sport and recreation for many people.

Physiographic Provinces

Physiographic Provinces of New Jersey

New Jersey is a region with a high variety of geographical features in a small area. The area can be broken into five regions, corresponding roughly to geological zones. These regions from north to south are the Appalachian Valley and Ridge, Highlands, Newark Basin Piedmont, Inner Coastal Plain, and the Outer Coastal Plain.

Appalachian Valley and Ridge Physiographic Province

File:November 2006 - 2 008.jpg
The Delaware Water Gap from Knowlton Township in New Jersey.
Shaded relief map

The Appalachian Valley and Ridge lies in the northwestern corner of the state and includes the Kittatinny Mountains, several smaller valleys and the popular Delaware Water Gap. The state's highest point, the aptly named High Point is within this area, at 1,803 feet. Most of the state's section of the Appalachian Trail runs through this area. The province is bounded on the southeast by an unconformity between Cambrian and Precambrian formations.

Highlands Physiographic Province

The Highlands Physiographic Province is a geological formation composed primarily of Precambrian igneous and metamorphic rock running from the Delaware River near Musconetcong Mountain, northeast through the Skylands Region of New Jersey along the Bearfort Ridge and the Ramapo Mountains. Numerous abandoned mines dot the region, dating from the 18th and 19th centuries when iron, copper, zinc and other minerals were extracted from the formations. The glaciated northern half of the province has an abundance of lakes and reservoirs which serve as water supplies for the urban areas to the east. The region's watershed is protected by the Highlands Water Protection and Planning Act.

Newark Basin Piedmont

USGS map of the Newark Basin showing major highways

The Newark Basin is a region in northern New Jersey defined by the boundaries of a sediment-filled rift basin. This basin was formed when the supercontinent Pangaea began to split approximately 220 million years ago, causing several large depressions to form due to extension, which then filled with sediment. The basin itself extends from Rockland County in the southern tip of New York to south-eastern Pennsylvania. It lies within the broader region known as the Piedmont, a crescent-shaped area characterized by smooth topography and large volumes of sediments. Like the Piedmont, the Newark Basin has gentle topography consisting of red bed clastic sediments with occasional igneous rock formations, such as the Palisades Sill and the Watchung basalt flows; these igneous features are responsible for the dramatic elevation changes observed in the region, such as The Palisades and the Watchung Mountains, respectively. The boundaries of the Newark Basin, as well as major highways, are shown on the map at right.

For the geological history of the region, see Newark Basin.

Inner Coastal Plain

The Inner Coastal Plain province consists of lowlands and rolling hills underlain by Cretaceous deposits. The region's northwest border lies along the Piedmont fall line. Fertile, loamy soil makes the land ideal for agriculture and is responsible for New Jersey's nickname of the "Garden State". Its deposits of Greensand marl containing potash were used since colonial days by farmers to fertilize their fields.

Beach at Avalon.

Outer Coastal Plain

The outer coastal plain consists of unconsolidated Tertiary deposits of sands, silt, and gravels. The soils are sandy with less clay than the inner coastal plain, and are more acidic and dry. The lack of fertility makes much of the region unsuitable for agriculture and large areas remain undeveloped. The sandy Pine Barrens, an area that is agriculturally poor but species rich, occupy the center of the province. Blueberries and cranberries have been cultivated in lowland bogs that have accumulated depths of organic matter.

Along the coast, sandy beaches attract a recreation industry, and the offshore barrier islands are popular vacation destinations.

Cultural regions

Historical emigrations

New Jersey's ethnic communities today

New Jersey has one of the fastest growing Asian American communities in the United States. Immigrants from China, Taiwan, South Korea, and India, as well as their native-born children, have transformed towns like Fort Lee, Edison, Iselin, East Brunswick, Palisades Park, and West Windsor[citation needed].

Regional cultural divisions

Although it is a small state, New Jersey has significant regional cultural divisions. South Jersey culture is influenced by its proximity to Philadelphia as well as its extensive shore and beaches. North Jersey culture (particularly northeastern New Jersey) is influenced by its proximity to New York City. Sandwiched in between are the towns of Central Jersey, which are more suburban than their northern counterparts but much less rural than towns in the south.

See also

References

Citations

Books and background references

External links