Tourism Guide
Total Page：16
File Type：pdf, Size：1020Kb
Load more
Recommended publications
-
Kittatinny Valley Is the Name Given to That Part of the Great Appala Chian Valley
BULLETIN OF THE GEOLOGICAL SOCIETY OF AMERICA PALEOZOIC LIMESTONES OF KITTATINNY VALLEY, NEW J E R S E Y * BY HENRY B. KUMMEL AND STUART WELLER ( Read before the Society December 28, 1900) CONTENTS P a g e Kittatinny valley............................................................................................................... 147 Hardiston quartzite........................................................................................................... 149 Relations and character............................................................................................ 149 Previous views............................................................................................................. 151 Kittatinny limestone......................................................................................................... 151 Stratigraphic and macroscopic characters............................................................ 151 Chemical composition................................................................................................ 152 Fauna of the Kittatinny lim estone........................................................................ 152 Previous views............................................................................................................. 154 Trenton formation............................................................................................................. 154 Basal conglomerate............................................................................................................ -
Sparta, New Jersey, Flood of August 11-14, 2000
USGS science for a changing world SPARTA, NEW JERSEY, FLOOD OF AUGUST 11-14, 2000 More than 14 inches of rain fell in a small area of southeastern Sussex and northwestern Morris County in northwestern New Jersey during August 11-14, 2000. Flood peaks at some U.S. Geological Survey gaging stations on Lake Hopatcong, Musconetcong River, Green Pond Brook, Rockaway River, and Russia Brook tributary were the highest ever recorded. About 2,700 homes and businesses in Sussex, Morris, Warren, and Hunterdon Counties were flooded, and about 2,600 people were evacuated. Many bridges, dams, and roads were damaged or destroyed. Damage was estimated at $179 million, and Sussex and Morris Counties were declared Federal disaster areas. The U.S. Geological Survey (USGS), in cooperation with the Federal Emergency Management Agency (FEMA), conducted a study of the flood that occurred in the Sparta, New Jersey, area during August 11-14, 2000. This Fact Sheet documents precipi tation amounts, peak flows and stages, indirect measurements of peak flow, and damage that resulted from the flood. Precipitation 20 KILOMETERS Unusually large amounts of rain produced by a series of EXPLANATION 2 Line of equal rainfall. Interval is variable, in inches. Dashed where thunderstorms deluged parts of northwestern New Jersey during approximate the period August 11-14, 2000. Rainfall was greatest in parts of Location of rain gage. Number is total rainfall, in inches southeastern Sussex County and northwestern Morris County Figure 1. Total rainfall at 41 rain gages in northern New Jersey, (fig. 1). More than 10 inches of rain fell in a limited area August 11-14, 2000. -
Life Around the Lake
LIFELIFE AROUNDAROUND THETHE LAKELAKE Lake Hopatcong Games and Activities It’s great not to swim into trash Look how healthy our lake is! Hope kids learn how to keep our lake clean LakeHopatcongFoundation.org BY THE NUMBERS The Lake Hopatcong Watershed A lake is not just like a huge bucket of water. There’s a lot more to it than that. The life of a lake includes hills, slopes, plants, trees, streams, rivers… pretty much every part of the land surrounding it. It’s called a watershed. A watershed is an area of land that drains into a body of water. Watersheds come in all shapes and sizes. Some are as small as a backyard that drains into a pond, others are thousands of acres in size. No matter where you are, you are in a watershed! Lake Hopatcong is in the Middle Delaware–Musconetcong Watershed. Lake Hopatcong is the largest of the more than 3,500 lakes, reservoirs and ponds in New Jersey! It drains into the Musconetcong River and has more types of game fish than any other lake or waterway within the state. Let’s take a look at Lake Hopatcong and its watershed by the numbers: 4: Towns that border Lake Hopatcong (Hopatcong, Jefferson, Mount Arlington and Roxbury). 9: Length of Lake Hopatcong, in miles, a distance that would take about three hours to walk. Size, in pounds, of the largest rainbow trout ever caught in New Jersey at Lake Hopatcong—about 13: as heavy as 1½ gallons of milk. 28: Fish species found in a recent fishery study of Lake Hopatcong. -
A Century of Forest Stewardship in New Jersey 1905-2005
A Century of Forest Stewardship in New Jersey 1905-2005 Researched and written by Kevin Wright © Kevin Wright 2005 An Introduction to New Jersey’s Natural Parks and Forest Reservations Tucked between blue-hazed mountains and the ocean shore, the State of New Jersey occupies a full cross section of the Atlantic slope with terrains and habitats that vary remarkably mile by mile. The cultural landscape is equally picturesque; what began as the most ethnically and religiously diverse colony has become the most densely populated State in the Union. Consequently a wonderful variety of plant and animal life competes on a daily basis with a spreading suburban population for space and resources. New Jersey’s virgin forests vanished by 1860, having been repeatedly cut over. With such widespread deforestation, even the Highlands “presented a perfectly bare appearance.” By 1900, about 46% of New Jersey’s land area, amounting to two million acres, remained woodland, though its condition was generally poor. Though this forest area was close to lumber markets, its overall value was insignificant, due mainly to repeated and uncontrolled destruction by forest fires. The first generation of professional American foresters, trained mainly in the carefully managed forest reserves of Germany, recommended the practice of scientific forestry to restore the exhausted condition of New Jersey’s remnant woodlands after centuries of exploitation. They believed that even the poor sandy soils of the Pine Barrens might yield crops of “commercially valuable trees … at a more rapid rate than is the rule on the average forest soil in the East, due to a favorable climate.”1 They not only advocated the creation of an organized firefighting force, but also a system of state-owned demonstration forests to promote reforestation. -
November/December 2007
www.nynjtc.org Connecting People with Nature since 1920 November/December 2007 New York-New Jersey Trail Conference — Maintaining 1,700 Miles of Foot Trails In this issue: Crowd Builds RPH Bridge...pg 3 • A Library for Hikers....pg 6 • Are Those Pines Sick, Or What?...pg 7 • Avoid Hunters, Hike Local...pg 12 revamped. There was an enormous amount BELLEAYRE Trail Blazes of Glory of out-blazing the old markers, putting up new markers, closing trails, clearing the By Brenda Freeman-Bates, Senior Curator, Ward Pound Ridge Reservation trails of over-hanging and fallen debris, Agreement Scales reconfiguring trails, walking them in the different seasons, tweaking the blazes, and Back Resort and having a good time while doing it all. A new trail map has also been printed, Protects Over with great thanks and gratitude to the Trail Conference for sharing its GPS database of the trails with the Westchester County 1,400 Acres of Department of Planning. The new color map and brochure now correctly reflect Land in New York N O the trail system, with points of interest, I T A V topographical lines, forests, fields, and On September 5, 2007, Governor Spitzer R E S E wetlands indicated. announced an agreement regarding the R E G This amazing feat would never have been Belleayre Resort at Catskill Park develop - D I R accomplished so expeditiously without the ment proposal after a seven-year legal and D N U dedication of volunteers. To date, a very regulatory battle over the project. The O P D impressive 928.5 volunteer hours have agreement between the project sponsor, R A W : been recorded for this project. -
Beyond the Exit
New Jersey Road Trips Beyond the Exit ROUTE 80 Mountain Magic NJ TURNPIKE Bridge to Bridge ROUTE 78 Farm to City ROUTE 42 Wine Trail GARDEN STATE PARKWAY Down the Shore BY THE ROUTE: Six major road ROUTE 40 Southern trips across the River to state where you Shore can stop along the way and experience New Jersey’s best! Due to COVID19, some attractions may be following adjusted hours and attendance guidelines. Please contact attraction for updated policies and procedures. NJ TURNPIKE – Bridge to Bridge 1 PALISADES 8 GROUNDS 9 SIX FLAGS CLIFFS FOR SCULPTURE GREAT ADVENTURE 5 6 1 2 4 3 2 7 10 ADVENTURE NYC SKYLINE PRINCETON AQUARIUM 7 8 9 3 LIBERTY STATE 6 MEADOWLANDS 11 BATTLESHIP PARK/STATUE SPORTS COMPLEX NEW JERSEY 10 OF LIBERTY 11 4 LIBERTY 5 AMERICAN SCIENCE CENTER DREAM 1 PALISADES CLIFFS - The Palisades are among the most dramatic 7 PRINCETON - Princeton is a town in New Jersey, known for the Ivy geologic features in the vicinity of New York City, forming a canyon of the League Princeton University. The campus includes the Collegiate Hudson north of the George Washington Bridge, as well as providing a University Chapel and the broad collection of the Princeton University vista of the Manhattan skyline. They sit in the Newark Basin, a rift basin Art Museum. Other notable sites of the town are the Morven Museum located mostly in New Jersey. & Garden, an 18th-century mansion with period furnishings; Princeton Battlefield State Park, a Revolutionary War site; and the colonial Clarke NYC SKYLINE – Hudson County, NJ offers restaurants and hotels along 2 House Museum which exhibits historic weapons the Hudson River where visitors can view the iconic NYC Skyline – from rooftop dining to walk/ biking promenades. -
LAKE HOPATCONG, JULY 2, 1898. , Nolan's Point, Lake Hopatcong, N
LAKE HOPATCONG, JULY 2, 1898. , Nolan's Point, Lake Hopatcong, N. J. Long Distance Telephone Pay Station. J. L. ALLEN & CO., Proprietors. Twenty New Fishing Boats and Twelve New Natural Finished Skiffs as handsome as are built, in the boat livery to rent. Full line of Groceries, Meats, Fresh Vegetables and Fruits, In their departments, kept always on hand, and only the best in every line, at Market Prices. OPEN ALL THE YEAR ROUND. RIVER STYX, - - - LAKE HOPATCONG, N. J. Within 75 Feet of the Lake, with New Annex of Twenty Rooms. Accommodates 60 Guests. Boating, Bathing and Fishing. RATES—Per Day, $1.50; Per Week, $8.00 to $10.00. Take Steamboat from Hopatcong Station on Delaware, Lackawanna and Western Railroad, or Lake Hopatcong Station, on New Jersey Central Railroad to Ithanell Pier. J. COCKS, Proprietor, P. O. ADDRESS, LANDING, N. J. Hillside Lodge. Situated on the boulevard, one-half mile from the Hotel Breslin, four minutes walk from the Lake at American House Pier, and five minutes from Minnisink Station on Central Railroad. Accommodates 30 Guests. Excellent Table and Service. Meals Served to Transients. Large New Dining Room added thia seasoD. Kitchen entirely separate from house. From D., L. & W, Railroad, take Steamboat at Hopatcorjg Station to American House Pier. For terms apply to Hopatcong Post Office, Morris County, N, J. MRS. G. A. BURKHART. WESTMORELAND, Lake Hopatcong's Model Hotel. OPEN ALL THE YEAR. KATES—$10 to $15 per week. D. L. BKYANT, Proprietor; A. 8. BRYANT, Manager. Livery Connected with the hotel. Telephone, Post Office and Telegraph.; LAXDIKG, MORRIS COUNTY, N. -
The Nature of Boulder-Rich Deposits in the Upper Big Flat Brook Drainage, Sussex County, New Jersey
Middle States Geographer, 2009, 42: 33-43 THE NATURE OF BOULDER-RICH DEPOSITS IN THE UPPER BIG FLAT BROOK DRAINAGE, SUSSEX COUNTY, NEW JERSEY Gregory A. Pope, Andrew J. Temples, Sean I. McLearie, Joanne C. Kornoelje, and Thomas J. Glynn Department of Earth & Environmental Studies Montclair State University 1 Normal Avenue Montclair, New Jersey, 07043 ABSTRACT: The upper reaches of the Big Flat Brook drainage, northwest of Kittatinny Mountain, contain a variety of glacial, pro-glacial, and periglacial deposits from the Late Quaternary. The area is dominated by recessional moraines and ubiquitous ground moraine, along with meltwater deposits, drumlins, and possible post- glacial periglacial features. We have identified a curious boulder-rich deposit in the vicinity of Lake Ocquittunk and Lake Wapalanne on upper Big Flat Brook. The area where these boulder deposits occur is mapped (1:24,000 surficial geology) as till. As mapped and observed, larger cobbles and boulders within the till are quartz-pebble conglomerate, quartzite, sandstone, and shale. The boulder-rich deposits differ from the typical till, however. Unlike the local till, which is more mixed in lithology, the boulder deposits are nearly exclusively Shawangunk conglomerate. The deposits are discontinuous, but appear to occur at a topographic level above the meltwater stream terraces. The boulders in the deposits lie partially embedded in soil, but are very closely spaced. The boulders range in size from ~20cm to over 100cm, and present a subrounded to subangular shape. There appears to be a fabric orientation of the boulders, NE-SW, with subsidiary orientations. As the boulder deposits differ from other mapped features in the area, we attempt to ascertain the origin for the deposits. -
Lower Paleozoic Carbonates: Great Valley
LOWER PALEOZOIC CARBONATES: GREAT VALLEY Frank J. Markewicz and Richard Dalton New Jersey Department of Environmental Protection, Division of Water Resources, Trenton, New Jersey INTRODUCTION The purpose of this field trip is to demonstrate the The Lower Cambrian Leithsville Formation named subdivision of the Cambro-Ordovician carbonate se by Wherry (1909) in Pennsylvania is the equivalent of quence as proposed by the field trip.leaders. In addition, the Tomstown Formation described by Miller and there will be discussions on environmental, others (1939) in eastern Pennsylvania and New Jersey, hydrogeologic, and engineering problems in these car bonates and how this subdivision has "opened the Avery Drake, (1961, 1967b) mapped the Leithsville doors" in understanding how everyday problems from Formation on the Frenchtown and Bloomsbury man's activities can affect or be affected by certain lit,hie Quadrangles and Markewicz (1967) used the term units within the carbonate sequence. This understanding Leithsville on the High Bridge Quadrangle. Wherry of the interaction between man's activities' and how it (1909) assigned a Lower-Middle Cambrian age to the lflight affect or be affected by critical aquifers, thin or Leithsville, whereas Willard (1961) infers that it is Mid thick soil horizons, and specific lithologies by septic dle Cambrian. No fossil evidence had been found to waste loads, ground water pollution, building founda establish its age until the discovery of the Lower Cam tion loading, landfills, etc'., has become extremely im-' brian fossil Hyolithellus micans in the early part of the portant in the land development process. 1960's, Markewicz (1964 unpublished), in rubbly dolomitic beds of the basal Leithsville at Califon, New We anticipate this field trip will not only relate the Jersey and also near Monroe in southern New York carbonate subdivision but will point out how important State. -
Monument Trail Loop from Steeny Kill Lake
Monument Trail Loop from Steeny Kill Lake Overview This loop hike goes along two scenic lakes and climbs to two ridges of Kittatinny Mountain, with panoramic views. Details Time: 3 hours Difficulty: Easy to Moderate Length: 5 miles Driving Directions Follow Route 208 North to I-287 South. Take Exit 52B of I-287 (Route 23 North), and proceed north on Route 23 for about 35 miles to High Point State Park. Continue for 1.4 miles beyond the main park entrance, turn right at the Steeny Kill Boat Launch, and proceed for 0.1 mile to a small parking area on the left. Description From the parking area, follow a gated road which heads east, towards Steeny Kill Lake. Bear left at the lakeshore and follow the light-blue-circle-on-white-blazed Steeny Kill Trail, which runs along the dam on the north side of the lake. At the end of the lake, cross the outlet stream and follow the trail through the woods. After a short climb, the Steeny Kill Trail ends at a junction with the red/green- circle-on-white-blazed Monument Trail. Turn right onto the Monument Trail, which continues to climb, using switchbacks and stone steps (built in the 1930s by the Civilian Conservation Corps) for part of the way. After a short level stretch, the trail emerges on a paved road, with a stone building - the park's Interpretive Center - just ahead. Follow the trail as it turns left, descends on the paved road, and crosses Kuser Road to reach the northern end of Lake Marcia. -
Backpacking the Long Path
Backpacking the Long Path By Ed Walsh Afoot and light-hearted I take to the open road, Healthy, free, the world before me, The long brown path before me leading wherever I choose. —Walt Whitman This guide is written to assist hikers who wish to hike the Long Path from end to end in a single trip. It may also be useful to anyone planning a shorter backpack on the Long Path. Until recently it was almost impossible to hike the Long Path in a single trip, although a few intrepid backpackers have done it. The stretches of pri- vate property crossed by the trail and the long road walks necessitated by the closing of sections of the trail, made a continuous trip a major undertaking. However, the opening of the Shawangunk Ridge Trail (SRT) and the co- alignment of the Long Path with the Appalachian Trail to reach the SRT have made such a trip feasible. It is now possible to backpack the entire length of the trail, but it still re- quires quite a bit of planning. It is not possible to camp out along the trail for its entire length. Some nights it will be necessary to hike to a motel or a nearby campground. This section will tell you which sections of the trail are open for camping and will list facilities nearby where overnight camping or other accommoda- tions are available for those sections where camping is not allowed. Just be- cause a motel or campground is listed in this booklet does not guarantee its quality. -
LEAGUE NEWS the Newsletter of the League of Historical Societies of New Jersey
LEAGUE NEWS The Newsletter of the League of Historical Societies of New Jersey Vol. 37 No. 3 www.lhsnj.org August 2012 PRINCETON BATTLEFIELD AMONG Summer Meeting MOST ENDANGERED PLACES Friends of Waterloo On June 6, the National Trust for Historic Preservation named Princeton Village Battlefield in Princeton, N.J., to its 2012 list of America’s 11 Most Endangered October 20, 2012 Historic Places. This annual list spotlights important examples of the nation’s ************************* architectural, cultural, and natural heritage that are at risk of destruction or irrepa- Article, registration rable damage. More than 230 sites have been on the list over its 25-year history, form, and directions, and in that time, only a handful of listed sites have been lost. p. 23, 24 Princeton Battlefield is the site of a pivotal Revolutionary War battle where General George Washington rallied his forces to defeat British troops. Waged 235 years ago, the battle at Princeton was a crucial turning point in America’s War of Independence, marking one of General Washington’s first victories over professional British soldiers. Not only did Washington’s success inspire countless soldiers to renew their commissions, but it also reinvigorated financial and political support for the war effort throughout the colonies. Many historians believe that this battle, along with the Battle of Trenton, saved the American Revolution and changed the course of world history. A portion of the battle site is now threatened by a 15-unit housing development planned by the Institute for Advanced Study. As proposed, the project would radically alter the integrity of the historic landscape, which has never been built upon, burying or destroying potential archeological resources and dramatically changing the topography of the terrain — an important element of the battle and essential to interpreting the battle today.