Welcome to the Essex County Environmental Center!
Welcome to the Essex County Environmental Center (ECEC)!
ECEC is part of the Essex County Park System and features about 1 mile of hiking trails, a canoe launch on the Passaic River, frog pond & a Wigwam among other points of interests. ECEC hosts many fine environmental education programs. Click here for more information on ECEC programs! Originally established in 1972 and closed due to funding issues in 1995, ECEC re-opened in 2005 with a new environmentally friendly building.
Partners of the ECEC include the Essex County Nature Photography Club, the Sierra Club, NJ Audubon Society, Essex County Environmental Commission, Essex County Beekeepers Society & the Essex County Recreation & Open Space Trust Fund Advisory Board.
ECEC is located in the 1,360 acre West Essex Park which primarily consists of deciduous wooded wetlands. West Essex Park was created in 1955 when the Essex County Park Commission first acquired a portion of the land. Additional land was purchased from more than 70 additional landowners through the years.
ECEC Virtual Tour
From the parking area, head to the Environmental Center to pick up a trail map and check out the indoor exhibits. (PS this tour took place in September 2012-about 1 month prior to Hurricane Sandy and thus describes the center as I found it at that time)
Once inside, there are various exhibits regarding topics such as renewable energy.
After taking in the information, pick up a trail map, it’s time to explore the trails!
Head outside the center and turn right on the Lenape Trail.
Throughout the exploration numbered wooded posts will be encountered. These posts correspond with this interpretive trail guide (link includes the trail map!) which we will review as we proceed.
The first marker is in regards to the Sweetgum Tree which is found here near its northern natural limit. Sweetgum has star shaped leaves & spiny seedpods. Click here for more information regarding this interesting tree!
Just past marker 1 turn right on a short green blazed trail and come to marker # 2 which has the remains of a Gray Birch. Gray Birch, one of the first trees to grow after a disturbance, is a short lived species. Only the logs (located around the marker) remain of this particular Gray Birch.
Marker 3 appears just after Marker 2 and discusses the old log lying next to the post. The old log is known as a mother log because it is “nursing” the soil by slowly decomposing nutrients therefore creating a richer soil for future vegetation.
Behind this marker a tall deer proof fence will appear.
The fence was constructed to keep hungry white tail deer out so native vegetation may grow.
Continuing to Marker #4, a cool little body of water known as the Frog Pond appears. While we might not see any frogs today, we know they are present. Check out the native vegetation such as cattail and arrow arum growing in the pond!
A sign has been strategically placed so that you can learn how to construct a pond of your own to attract frogs. From the Frog Pond, leave the green blazed trail and pass Garibaldi Hall.
Garibaldi Hall was part of the original environmental center and is still used by the Master Gardeners of Essex County.
Head toward Eagle Rock Avenue to Marker # 5 found at the start of the White Blazed Patriots Path.
The flora identified by this marker is found at your feet. Garlic Mustard is its name, and, at least here in the eastern United States, establishment of itself as an invasive species is its game. White Tail Deer do not eat Garlic Mustard and the plant has no natural predators in the US. Garlic Mustard produces a chemical which suppress mycorrhizal fungi required by most plants to grow successfully. As a result, Garlic Mustard, once established, forms a monoculture in which native plants cannot become established. Heading further on the Patriot Path I encountered these three fellows in addition to a River Birch (Marker #6):
After passing marker six it’s time to leave the Patriot trail by heading left to a wooden boardwalk.
The boardwalk is raised above the Passaic River floodplain.
A wooden box will appear straight ahead near the Passaic River (Marker #7). This box has been placed for nesting Wood Ducks (a species that nests in tree cavities but will also utilize man-made structures).
Be careful of Poison Ivy (Marker #8) as you continue your journey on the boardwalk! Poison ivy contains a clear liquid known as urushiol which causing a burning itching rash in many people. Poison Ivy can be found as a hairy vine, a shrub reaching over three feet tall or as a trailing vine on the ground. It helps to remember the following jingles to remind you of the dangers of this vine:
“Hairy rope, don’t be a dope” & “Leaves of three, leave them be”
Leaving Poison Ivy behind, the Passaic River (Marker #9) appears to the right as we leave the boardwalk.
The river is located southwest behind the Environmental Center Building. This is a great spot to launch a canoe or kayak to go explore the river.
Some quick Passaic River facts: Spanning 80 miles, the Passaic River is the second largest river in NJ and flows through Morris, Somerset, Union, Essex, Passaic, Bergen and Hudson counties. The confluence of the Rockaway River with the Passaic River is located nearby. Fish including bass, herring & shad find a home in the Passaic River.
We now find ourselves back on the Lenape trail and passing a Pollinator Garden (Marker #10). Native plants are being grown here to attract bees which are our next point of interest (Marker #11).
The Essex County Beekeepers keep a selection of Honeybees here. Bee careful not to disturb it!
Wow! What’s this? Why it’s Marker #12 aka Lenape Life. Here you will find behind a gate a Wigwam and other items characteristic of Lenape Life. The Lenape were the original people who found a home in this area prior to European settlement.
Wigwams were created from saplings which were bent to create a dome frame. The frame was then covered with a mixture of animal skins & mats of reeds and rushes. In addition to the Wigwam, the Lenape learning center features a fire pit, meat drying rack, food cache, Lenape Gardens, fishing & tanning rack.
Looping back towards the Environmental Center a Northern Red Oak (Marker #13) appears. The Northern Red Oak is NJ’s state tree and is readily identified by its “ski-slope” bark. Northern Red Oak emits a foul odor when cut down.
Soon after Marker #13 appears Marker #14 (Forest Composition) which describes Musclewood, American Beech & Spicebush.
Smooth gray bark is characteristic of the American Beech. It is this feature that attracts individuals to carve their initials. This practice is detrimental to American Beech as the carvings create opportunities for disease and could very well kill the tree. In winter, American Beech leaves remain until the spring when new leaves bud out. American Beech is usually found in forest in the final stage of succession.
Spicebush is one of the first native shrubs to bloom in spring. Spicebush earns its name from the spicy scent which emits from a broken twig. Spicebush is usually found in deciduous wooded wetlands such as those encountered at the ECEC.
Musclewood (aka Ironwood or American Hornbeam) is a small understory tree usually found in deciduous wooded wetlands. The form of the tree resembles a muscular arm. Straight ahead is the Environmental Center but we’re not quite finished with our tour yet. We still have a whole trail yet to explore!
Let’s turn right on the Lenape to Marker # 15 which discusses three common ferns found in the ECEC forest: Christmas fern, Hay scented Fern & Sensitive Fern. Christmas fern is evergreen and is thought to be given the name due to its leaves having the appearance of a stocking that you would hang on your chimney. Hay scented fern is named such due to its scent resembling, well, hay. Sensitive Fern is an appropriate name indeed as this fern is one of the first to wilt come the first frosts of fall.
We’ve now come to the beginning of the blue blazed Bird Lane Trail.
Let’s take a right to go explore it. The first marker on the Bird Lane Trail is #16 the Fox Grape Vine. Birds such as Northern Cardinal enjoy the grapes this vine produces.
Continuing on we start our loop and see Marker #17 which describes the floodplain forest found at the ECEC. The forest here often will flood (especially in early spring when melting snow contributes to increase water flow in the Passaic River). Species here such as Red Maple flourish in the conditions provided by frequent flooding.
As we start to turn back there is a large rock (Marker #18) visible in the woods. This rock is known as a glacial erratic and was carried to this spot when the last glacier (Wisconsin Glacier) came through the area around 10,000 years ago. This rock was likely carried from the nearby Watchung Mountains.
Continuing back towards the Lenape Trail we pass Marker #19 which describes the past land use of the ECEC. Old farming equipment such as this piece found near this marker tells us that this land was once used as farmland. Looking around you can clearly see the forest has reclaimed the land. Well, we’ve now reached our last marker (#20) which describes the Mayapple plant. The Mayapple plant blooms a single flower in early spring and first emerges before the forest has fully leafed out in springtime.
Well, we’ve now reached the end of the Bird Lane Trail!
And with that, our tour has concluded. I hope it has inspired you to go visit the ECEC to see if for yourself! Click here for directions!
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
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Hiking Kincaid Woods!
Welcome to Kincaid Woods!
Kincaid Woods, a part of Morris County’s Pyramid Mountain, is located mostly in Boonton along Kinnelon Road just after it becomes Powerville Road.
The woods, officially opened to the public circa 2009, were once farmland owned by a local family by the name of Kincaid. Evidence of old farm stone walls can still be found in the woods. The hike is located in the Stony Brook Mountains which are named for the nearby Stony Brook, a tributary of the Rockaway River.
From the kiosk in the parking area, follow the trail as it meanders through a meadow.
(Please keep in mind I took this hike in September 2012 about a month before Hurricane Sandy arrived. The following describes the hike as I encountered it at the time)
The yellow blazes of the Kincaid Trail will appear on wooden posts.
Enter the woods heading east on the Kincaid Trail.
Pass over a stream (a Stony Brook tributary) and through wetlands on a raised wooden bridge.
From here, be on the lookout for the Black-Dot Trail trail head which will appear on the right.
Head southwest on the black dot trail which passes over an old Kincaid Farm stone wall. From here, the Black Dot trail will begin to loop to the northeast.
Come to the end of the Black dot-trail after crossing another old stone wall.
From here turn left back on the Kincaid Trial heading northwest (turning right on the Kincaid trial leads to Pyramid Mountain).
From here a coppice Red Maple with the yellow blaze of the Kincaid trail becomes visible.
Soon a remnant of the Rockaway Valley Mine (aka DeCamp Mine) will come into view. Minerals mined included pyrite & magnetite. Minerals was shipped to the Musconetcong Ironworks in Stanhope NJ via the nearby Morris Canal. Tailings from the old mine may be found scattered about.
From the mine area, continue following the Kincaid trail west back through the wetlands, over the boardwalk and into the meadow where the hike began.
Directions (as taken from the NYNJ Trail Conference Web Site)
Take I-287 South to Exit 47 (Montville/Lincoln Park) and turn left at the bottom of the ramp onto Main Road (Route 202). Continue to follow Route 202 as it turns first sharply left, then sharply right. In 0.6 mile, just before reaching a fire station, turn right onto Taylortown Road and continue for 3.1 miles to a “stop” sign at Powerville Road (after 1.8 miles, Taylortown Road becomes Rockaway Valley Road). Turn right onto Powerville Road (the road is open only for local traffic because a bridge is out ahead, but the parking area for the hike is before the bridge, so you should go around the barricade) and continue for 1.2 miles to Kincaid Road (Powerville Road bears left at this intersection). Turn right onto Kincaid Road and immediately turn right into a gravel parking area.
UPDATE: Per the NYNJ Trail Conference website: The trails followed by this hike are temporarily closed due to the construction by PSE&G of an upgraded power line in the area. It is expected that the closures will remain in effect until the fall of 2013. For more information, please call the Park Visitors Center, (973) 334-3130.
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
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Butler Forest Preserve & Butler Raceway!
Welcome to the Passaic River Coalition’s Butler Forest Preserve & Butler Raceway! Both preserves are contiguous and have a combined acreage of 14.9 acres of which four are deciduous wooded wetlands. Located in Butler, NJ, The Butler Forest Preserve and Butler Raceway were purchased to prevent the development of townhouses and provide protection of the Pequannock River.
The Passaic River Coalition was established in 1969 and provides stewardship for the preservation and protection of over 1,000 miles of waterways associated with the Passaic River. The Pequannock River, a tributary of the Passaic River is labeled C1 indicating the water consists of some of the highest quality in the state of New Jersey.
Virtual Tour
This was how the Butler Forest Preserve and Butler Raceway appeared when I explored it near the end of September 2012, nearly a month before Hurricane Sandy arrived. I find Jericho Road to be the best entrance to the Butler Forest Preserve & Butler Raceway.
Entering the forest here I noticed a stream to my left (an unnamed Pequannock River Tributary) and plenty of American Beech. American Beech is part of the Beech-Sugar Maple climax forest community and are a sure indicator that this forest has not been disturbed for a very long time.
I carefully followed the woods down a somewhat steep slope while a steady roar increased. Thinking it was urban noise coming from nearby Route 23 and housing developments I was somewhat surprised to see the source was far more natural: The Pequannock River rushing by.
I noticed the river just as my eye caught old ruins. These ruins were part of the Butler Raceway which once provided water from the Pequannock River to power machinery to what was once the country’s largest rubber factory. The historic function of the raceway was to provide water from the Pequannock River to power machinery at the Butler Rubber Factory. The rubber factory was destroyed by fire in 1957.
Near the ruins is a beautiful man-made waterfall on the Pequannock River.
Carefully scrambling over the ruins I made it to the Raceway just in time for a Great Blue Heron to fly by (unfortunately too fast for me to get its picture).
After admiring the Heron I came across an abandoned motorcycle.
Continuing east Yellow Birch appeared in good numbers. Yellow Birch favors north facing slopes.
Rock Outcrops of Precambrian origin appear occasionally to the right of the path. The Butler Raceway ends near Gifford Street. To get back to Jericho Avenue, simply turn around on the Raceway and proceed west until you come back to the cement ruins. Proceed south going up the hill until you reach Jericho Road.
The Butler Forest Preserve and Butler Raceway is a great place to explore. Check it out for yourself!
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
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Hiking Torne Mountain! (Norvin Green State Forest)
Welcome to Norvin Green State Forest’s Torne Mountain!
Torne Mountain, standing at 1,120 feet and located in Passaic County NJ, is situated in the southern section of the estimated 4,982 acre Norvin Green State Forest. The land comprising the forest was donated to the State of New Jersey by the nephew of Ringwood Manor’s Abram S. Hewitt in 1946.
Norvin Green State Forest has the largest concentrations of trails in the state of NJ. Most of the trails date back to the 1920’s when members of a local organization known as the Green Mountain Club constructed them.
Geology
Many of the rocks that are encountered during this hike have a rounded appearance due to the Wisconsin Glacier which came through the area around 10,000 years ago. This event is relatively recent as the Highlands rocks were formed over four billion years ago.
The rocks are “basement rocks” as the younger rocks which originally had covered them eroded away over time. Most of the rocks are thought to be comprised of ancient granite-gneiss.
Trails
Below is a brief virtual tour of a section of the 0.4 of a mile Torne Trail and a portion of the 6.4 mile Blue Blazed Hewitt-Butler Trail. Stops include outstanding views and an interesting man-made Stone Living Room. Ready? Let’s do it!
The hike is an estimated 1.5 miles from Otter Hole Road.
Starting from near the Otter Hole Road Parking area, head south to the trailhead of the red blazed Torne Mountain Trail.
Once on the Torne trail, signs advertising the blue-blazed Hewitt-Butler Trail will appear.
Head southwest then south on the blue blazed Hewitt-Butler Trail to Climb Torne Mountain.
The first view will be of Buck Mountain to the north. Continuing southeast views of the Newark Pequannock Watershed land appear to the west.
Near the western viewpoint, a short unmarked trail appears to the left leading to a man-made Stone Living Room. “Chairs” & “Sofas” have been constructed from surrounding rocks. The Stone Living Room is an excellent place to stop for lunch and rest while taking in views.
From the Stone Living Room, head back to the Hewitt Butler Trail. Continuing south, descend Torne Mountain passing a stand-alone Stone chair.
Here you will reach a ravine at the bottom of Torne mountain and the southern trailhead of the red blazed Torne Trail which will be your return back to Otterhole Road.
For now, pass the southern trail-head of the Torne Trail and continue southeast on the blue blazed Hewitt-Butler trail climbing to Osio Rock.
From here, views of the Wanaque Reservoir, the NYC Skyline (on a clear day) and High Mountain of the 2nd Watchung Mountain range may be viewed to the east.
After taking in the views, turn around and head north west to retrace your steps back to the ravine to the red blazed Torne trail trailhead.
Here you will take the Torne trail north back to Otterhole Road where the trail began.
Flora
Flora found along the trail includes the below among others:
Fauna:
Directions: (as taken from localhikes.com)
Hamburg Turnpike to Glenwild Ave. Parking area is next to Bloomingdale/West Milford border (look for Welcome to West Milford sign, or Welcome to Bloomingdale sign depending on which direction you are traveling.
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
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Little Fall’s Morris Canal Preserve!
Welcome to Little Fall’s Morris Canal Preserve!
Walking on Little Falls Main Street, few people would suspect that a preserved woodland and forested floodplain is located behind the stores.
The Morris Canal Preserve is located right above the Passaic River. The river rushes by on fractured basalt . The preserve features a gentle paved path which traverses the edge between the developed landscape of Little Falls and the remnant forested floodplain of the Passaic River.
The paved path leads from a beautiful gazebo and heads in a southwest direction to its terminus near an outflow from the Passaic Valley Water Company.
You might be tempted to think that Little Falls was named after these views, but the real falls were eliminated late in the 18th century to relieve upstream flooding of the Passaic River.
The path features checkerboards, basalt rocks of the second Watchung Mountain and beautiful views along the way.
Morris Canal
A portion of the 102 mile Morris Canal flowed over the Passaic River via an aquaduct created in 1829 of local Little Falls Brownstone.
The Morris Canal was an artificial waterway which connected the coal fields of Pennsylvania’s LeHigh Valley to Paterson, Newark & New York City. Successful at first, railroads eventually replaced the need for the canal. After falling into disrepair, the Aqueduct was dynamited to the ground in 1925.
Flora
Typical examples of flora found along the Morris Canal Preserve include:
Want to learn more about the high diversity of plant life found in the Garden State? Check out Plant Communities of New Jersey.
NJ’s geology, topography and soil, climate, plant-plant and plant-animal relationships, and the human impact on the environment are all discussed in great detail. Twelve plant habitats are described and the authors were good enough to put in examples of where to visit!
Click here for more information!
Directions: (as taken from the NYNJCT Botany Website)
From Route 80 westbound, get off at the Union Avenue exit and bear left to follow Union Avenue for about one mile into Little Falls. Turn left at the light onto Main Street and then go about five blocks looking for Maple Street and Schumacher Chevrolet on the left. Turn left down Maple and continue as for the bus directions.
Alternative route by car: From Rt. 46 westbound, get off at the Great Notch/Cedar Grove exit. Bear left and follow overpass over Route 46 on to Notch Road. At the end of Notch Road turn right at the light onto Long Hill Road. Proceed on Long Hill Road for about one mile where it becomes Main Street. At Schumacher Chevrolet, turn right onto Maple Street and then follow the directions as for the bus. Look for the brick sign for the preserve on the left.
By public transportation: Take NJ TRANSIT 191/195 bus that leaves the Port Authority Bus Terminal, NY (check schedule prior to the trip) and get off on Main Street in downtown Little Falls at the corner of Maple Street Turn right on Maple and walk one block to entrance to the preserve parking lot on the left.
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
Wayne’s High Mountain Park Preserve!
Welcome to High Mountain Park Preserve! The preserve, aka High Mountain Park, is located in Wayne, NJ and consists of over 1,000 wooded acres.
High Mountain Park is owned and jointly managed by the Township of Wayne, the State of NJ and the New Jersey Natural Land Trust. In 2011, the New Jersey Natural Land Trust obtained the Nature Conservancy’s divided and undivided interest in High Mountain Park.
History of Site
High Mountain Park was a tree farm owned by Urban Farms, Inc., a subsidiary of McBride Enterprises of Franklin Lakes, NJ before its establishment as a preserve. On May 19, 1993 the Wayne Council majority in an 8-1 vote accepted a deal to purchase High Mountain from Urban Farms, Inc.
The State of NJ committed $2.6 million in a Green Acres Grant and agreed to a 2% loan of $4 million. $901,943 was provided in other grand funds. The Nature Conservancy obtained a $500,000 state grant to assist in the purchase of High Mountain.
Geology
Situated on the Second Watchung Mountain range, High Mountain Park is the largest forested area east of the NJ Highlands. The 2nd Watchung Mountain range was formed by lava flows extruding over deep sedimentary rock basalt.
Ecological communities featured in High Mountain Park include:
Rocky Headwater Stream:
Rocky headwater stream habitat includes a small to moderate sized rocky stream that lacks persistent emergent vegetation. In other words, few large rooted plants are found but mosses and algae are usually present. The stream flows over bedrock near its origin and contains riffle and pool sections.
Red Maple Swamp:
Red Maple Swamps (as the name suggests) are dominated by Red Maple, a tree that is moderately flood-tolerant. Skunk Cabbage, False Hellebore, Cinnamon Fern and Spice Bush (along with many other species) are found in Red Maple Swamp habitat.
In addition to Red Maple Swamps, Shrub swamps are also found in High Mountain Park. This community consists of temporarily to permanently flooded wetlands usually populated with Skunk Cabbage, Buttonbush, Spicebush among others.
Talus Slope Community:
Talus Slope communities consist of sparse vegetation occurring on exposures of shale bedrock, ledges and talus. Little soil exists on the talus.
Trap rock Glade/Outcrop Community:
The trap rock glade/outcrop community is globally rare and was the principal reason the Nature Conservancy was interested in protecting High Mountain. Trap rock Glade/Outcrop communities, a globally impaired community type, consists primarily of grasses and forbs with occasional red cedar.
Prickly Pear Cactus may also be present. Hickory-Ash-Red Cedar woodland is also dominated in the trap rock glade/outcrop community. Rare Rock Outcrop Plants include Torreys Mountain Mint and Dewey’s Sedge among other rare plants.
Hickory/Ash/Red Cedar Woodland:
This community contains the trap rock outcrop community and consists of Pignut Hickory, Eastern Red Cedar, White Ash and Chestnut Oak with the understory consisting primarily of grasses and forbs. This community along with the trap rock glade/outcrop community harbor a total of 14 rare and endangered plants.
Mixed Oak Forest:
The mixed oak hardwood forest found in High Mountain Park is dominated by White, Red & Black Oak and includes trees such as Shagbark Hickory, White Ash, Yellow birch, Tulip Poplar and Black Birch.
Frequent disturbance is required for the oak-hickory forest to maintain itself. Without disturbance, shade tolerant species such as Sugar Maple and American Beech regenerate replacing oaks over time. Maple-Beech dominated woodland do not provide sufficient quality mast (i.e. acorns, hickory nuts) required for wildlife.
The composition of the present Oak-Hickory forest found in High Mountain Park will likely change as the sapling layer is mostly populated by Sugar & Red Maple with only a few Oak saplings present. This change may be due to fire suppression.
Hemlock-Hardwood Forest:
Most of the hemlocks found in High Mountain Park Preserve are dead or dying due to the Hemlock Wooly Adelgid. Native to East Asia, the adelgid feeds by sucking sap from Hemlock trees. This exotic pest was accidently introduced to North America circa 1924 and is currently established in eleven states ranging from Georgia to Massachusetts. It is estimated that 50% of the geographical range of the Eastern Hemlock has been affected by the adelgid. Biological control (i.e. using adelgid predators to control infestations) has been the major emphasis of control since 1997.
Streams:
High Mountain Park is a part of the Passaic River watershed. All streams that originate or flow through High Mountain Park drain to the Passaic River. Streams include tributaries to the Point View Reservoir found in the western section of the preserve and tributaries of the Molly Ann Brook (the last stream to drain into the Passaic River before the Great Falls in Paterson) found in the eastern portion of the preserve. The headwaters of Preakness (Signac) Brook are located in High Mountain Park and are classified in this location as C1 Trout Production. Numerous tributaries to the Preakness Brook are found primarily in the heart of the preserve.
Trails
There are five blazed trails ranging from 0.2 miles to 4.9 miles waiting to be explored at High Mountain Park. All trails are maintained by volunteers of the NYNJ Trail Conference who have maintained the trails since the 1940’s. Click here for a trail map provided by the Township of Wayne.
The trailhead of the 1.7 mile Red Trail is accessible from the small parking lot off of College Road.
From the kiosk in the parking area, the Red Trail heads east on a gravel trail in an open field adjacent to College Road and enters the woods heading in a north to northwest direction.
After entering the forest, a large boulder is visible to the west near a sign advertising High Mountain.
From here, the Red Trail passes a stream & wetlands.
At half a mile, the southern trailhead of the Yellow Trail is accessible on the east. Past the trailhead of the Yellow Trail, the Red Trail passes the southern trailhead of the White Trail Trailhead to the west .6 of a mile. Once past the trailhead of the White Trail, the Red Trail crosses a stream and wetlands before continuing in a northwest direction.
Another stream with a waterfall eventually appears to the east of the Red Trail. The Red Trail crosses the stream proceeding a short distance to its northern terminus at Reservoir Drive in Franklin Lakes.
The southern trailhead of the 1.6 mile White Trail is accessible from the Red Trail about .6 of a mile from the Red Trail’s trailhead at College Road.
From its trailhead, the White Trail heads west through the wetlands of a Preakness Brook tributary stream. Continuing west the White Trail reaches another Preakness brook tributary and its wetlands.
From here, the White Trail turns north passing the North Jersey Country Club. Continuing north past the North Jersey Country Club, the White Trail passes a reservoir used for the ponds found in the country club.
From here the White Trail continues north and goes through talus slopes while paralleling and eventually crossing another Preakness Brook tributary. The White Trail ends at the Yellow Trail near Beech Mountain.
At 4.9 miles, the Yellow Trail is the longest trail present in High Mountain Park. The southern trailhead of the Yellow Trail is accessible from the Red Trail about ½ a mile from the trailhead of the Red Trail on College Road.
From the Red Trail, the Yellow Trail turns east and crosses a stream and wetlands heading in a northwest and then northeast direction. Soon the Yellow Trail passes the summit of Mount Cecchino to the east. From here the trail begins a steady climb to the summit of High Mountain. At 885 feet, High Mountain is the third tallest peak in the US within 20 miles of the Atlantic Ocean.
The grassy summit is about 1 mile from the Yellow Trail trailhead and provides fantastic views of the Manhattan skyline, Garrett Mountain (1st Watchung) and the distant Ramapo Mountains.
From the summit of High Mountain the Yellow Trail heads west going downhill and crosses a stream.
After crossing the stream, the Yellow Trail comes to an intersection with the Red Trail.
Once past the intersection with the Red Trail, the Yellow Trail heads northwest to a paved circle on Reservoir Drive in Franklin Lakes and briefly travels along Reservoir Drive before reentering the forest near Winding Hollow Drive in Franklin Lakes.
Heading south, the Yellow Trail passes the northern trailhead of the White Trail and then heads south and climbs Beech Mountain. At 875 feet, Beech Mountain is the second highest peak in High Mountain Park.
The Yellow Trail then traverses past a large forested wetland to the west and crosses a Preakness Brook tributary. Turning west, the Yellow Trail reaches a beautiful view found on a basalt outcrop of Pointview Reservoir and the distant NJ Highlands.
The Yellow Trail continues northwest past another Preakness Brook Tributary and heads south and west past the parking lot for JVC Corporation.
From here, the Yellow Trail heads northwest and passes the northern terminus of the Horizontal White Blaze connector trail. The Yellow Trail then turns north and traverses through the Franklin Clove.
The Franklin Clove was formed by glacial action in the last ice age. Continuing north, the Yellow Trail passes by the very short Orange Blazed Buttermilk Falls trail and then ends at Indian Drive in Franklin Lakes.
The 0.2 Mile Orange Blazed Buttermilk Falls trail begins from the Yellow Trail shortly after the Yellow Trail passes through the Franklin Clove. It ends at Scioto Drive in Franklin Lakes. The primary feature of this trail is Buttermilk Falls which spills over fractured basalt.
The 2.8 mile Blue Trail (aka the Pancake Hollow Trail) trailhead is located off of Chickapee Drive in Wayne.
The Blue Trail initially heads east and turns north at the intersection of the horizontally white blazed connector trail. Heading north, the trail passes the Franklin Clove and the headwaters for Preakness Brook to the east. The Blue Trail then turns northwest passing between housing developments to the north and south where a lean-to is present.
Once past the housing developments, the trail traverses the “pancake hollow” section of High Mountain Park.
The Blue Trail continues west crossing over a brook and wetlands. As the blue trail approaches Berdan Avenue at the farthest western portion of High Mountain Park, the trail turns NW and then NE and then continues in a SE direction leaving the Pancake Hollow section returning the hiker in a loop fashion back to the portion of the Blue Trail previously traveled with housing developments to the north and south. From here, the hiker follows the blue trail back to the trailhead at Chickopee Drive.
The 0.2 mile Horizontal White Blaze Connector trail’s western trailhead is accessible from the Blue Trail near the Blue Trail trailhead at Chickapee Drive in Wayne. The Horizontal White Blaze Connector Trail initially heads southeast from the Blue Trail before turning north to connect with the Yellow Trail near the Franklin Clove where it ends.
Fauna:
Fauna I’ve spotted during my hikes at High Mountain Park include:
Directions to College Road Parking Lot: (as taken from the NYNJ Trail Conference Website)
Take Route 208 west to the second Goffle Road exit (towards Hawthorne/Paterson) and turn right at the end of the ramp. At the next light, just beyond the intersection with Goffle Hill Road, turn right onto North Watchung Drive. At a “stop” sign at the top of the hill, turn sharply right onto Rea Avenue, which becomes North Haledon Avenue and then Linda Vista Avenue. At a T-intersection with Terrace Avenue, turn right, then bear left to continue on Linda Vista Avenue, which leads into William Paterson University (Entry 6). At the next “stop” sign, turn right and continue for 0.4 mile to a small parking area on the right, with a sign “High Mountain Park.”
Check out Plant Communities of New Jersey.
NJ’s geology, topography and soil, climate, plant-plant and plant-animal relationships, and the human impact on the environment are all discussed in great detail. Twelve plant habitats are described and the authors were good enough to put in examples of where to visit!
Click here for more information!
Other Resources:
1. 60 Hikes Within 60 Miles: New York City: Including northern New Jersey, southwestern Connecticut, and western Long Island – Packed with valuable tips and humorous observations, the guide prepares both novices and veterans for the outdoors. From secluded woods and sun-struck seashores, to lowland swamps and rock-strewn mountain tops, this practical guidebook contains all the information needed to have many great hikes in and around New York City.
Click here for more information!
2. Take a Hike New York City: 80 Hikes within Two Hours of Manhattan – In Moon Take a Hike New York City, award-winning writer Skip Card shows you the best hikes in and around The Big Apple—all within two hours of the city.
Click here for more information!
3. Eastern Deciduous Forest, Second Edition: Ecology and Wildlife Conservation – This book is a useful tool for anyone who wants to know or hopes to help one of North America’s great natural resources.
Click here for more information!
4. Protecting New Jersey’s Environment: From Cancer Alley to the New Garden State – With people as its focus, Protecting New Jersey’s Environment explores the science underpinning environmental issues and the public policy infighting that goes undocumented behind the scenes and beneath the controversies.
Click here for more information!
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!



















































































































































































































































































































































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