Mountainview Nature Park was acquired as a gift from the Winston Perry family by Rockland County in 1979.
Geology
Diabase Rocks
The land comprising Mountainview Nature Park is part of the Palisades ridge. The Palisades extend from Staten Island NY to Mount Ivy NY. The rocks are known as diabase. Diabase was formed around 200 million years ago by molten magma intruding into softer sedimentary rocks.
Virtual Hike
Mountain Trail Trailhead
From the parking area on Strawberry Hill Lane we find ourselves at the trailhead of the orange blazed Mountain Trail. At 1.15 miles, the Mountain Trail is the longest trail found in Mountainview Nature Park. We will use this trail map to help guide us. Ready? Let’s go!
Bridge over Hackensack River Tributary
Heading east on the Mountain Trail, we cross a Hackensack River tributary on a wooden bridge.
NY Thruway
Dipping south we see (and hear) the NY State Thruway straight ahead near another Hackensack River tributary.
Rock Wall Mountain Trail
Turning north on the Mountain Trail we see several old stone walls of farms that existed here at one time.
Goat Path Trailhead
Continuing north on the Mountain Trail the white-blazed trailhead of the .60 mile Goat Path appears to our right. Let’s take it!
Pileated Woodpecker (a bit on the blurry side)
Heading southeast on the Goat Path a large American Crow size bird with a bright patch of red on its head flies over us. It’s a Pileated Woodpecker! This guy is on the ground poking through fallen snags for its favorite food: carpenter ants.
Goat Path Climb
Leaving the Pileated Woodpecker behind we continue southeast on the Goat Path and start to climb uphill.
Building near Goat Path
Coming to the edge of the eastern border of Mountainview Nature Park with a building visible straight ahead, the Goat Path turns left climbing northwest along the edge of a hillside.
Goat Path Hillside
Careful! We have to really watch our footsteps here. Whew! We’ve arrived near the top.
Just ahead we come to an intersection with the orange blazed Mountain Trail we left awhile ago. But for now, let’s head south on the Overlook Spur section of the Goat Path.
White-Tailed Deer
As we walk on the Goat Path we spot a White-Tailed Deer to our left watching us.
Goat Path Trailend
Leaving the deer we continue southwest to the Goat Path terminus.
Palisades Center Mall & NY Thruway with Ramapo Mountains in distance
Let’s take a breather to see the view. Directly in front of us is the Palisades Center Mall with the NY Thruway heading west towards the distant Ramapo Mountains. Ready to continue on? Let’s turn back and head back to the Mountain Trail intersection.
Mountain Trail
We are now leaving the white blazed Goat Path and heading east on the Mountain Trail.
Bear Swamp Trailhead
Just to the left of the Mountain Trail is the western trailhead of the blue blazed .28 mile Bear Swamp Trail loop. Let’s go explore it!
Bear Swamp
The Bear Swamp Trail loops around Bear Swamp and will take us back to the Mountain Trail. Bear Swamp, which is seasonally flooded, is a hardwood swamp dominated by Red Maple, one of the more common trees found in the eastern forest. Shrubs such as Spicebush are quite abundant in the understory.
Royal Fern
Ferns such as Cinnamon and Sensitive Fern are also abundant in Bear Swamp. While they are gone since we are in late fall, we still see the remains of Royal Fern.
Bear Swamp Trailend
Completing our loop, we find ourselves back on the Mountain Trail at the eastern entrance to the Bear Swamp trail. We can either continue heading east (which leads to Mountainview Avenue and the Long Path) or we can retrace our footsteps and head west. Since it’s getting late, let’s head west on the Mountain Trail.
Mountainview Nature Park Mountain Trail
Passing the Goat Path we are now heading west on the Mountain Trail.
Decaying Log
As we walk we pass by numerous blow downs and old decaying logs. These old logs play an important ecological role in the forest. Decaying logs retain moisture and release nutrients into the ground that aid in new plant growth.
Posted Private Property
Heading southwest on the Mountain Trail, we pass near the northern boundary of the park near private property.
Hudson River Mountain Trail
Walking southwest on the Mountain Trail we can just catch glimpses of the distant Hudson River through the remaining leaves on the trees to our left.
Mountain Trail Descent
We’ve now begun our climb down the western border of the hill we climbed earlier on the Goat Path. This trail will take us back down pass the trailhead of the Goat path and back to our car.
Mountain Trail End
We made it back to our car. Thank you so much for joining me today on this virtual hike of Mountainview Nature Park. I hope that it inspires you to visit and hike the park yourself in person!
Welcome to Sterling Forest State Park! Established in 1998 and located in Tuxedo and Warwick NY, the park is one of the newest additions to the New York State Parks in the past 50 years. Most of the woodland is located in NY State but a portion of it extends into NJ and is known as Tranquility Ridge County Park.
Sterling Forest
The almost 22,000 acre park features diverse ecological communities including:
Foot Trail Maintained by Volunteers NY-NJ Trail Conference
Today we are going to hike the estimated 4.2 Blue Blazed Sterling Lake trail (maintained by volunteers from the NYNJ Trail Conference) which starts at the Sterling Forest State Park visitor center. The visitor center is named for the late Frank R. Lautenberg who helped preserve the forest for future generations. The Sterling Lake Lake trail loops around Sterling Lake, a natural lake formed during the last ice age.
Inside there are dioramas on the Sterling Forest mining industry history, fauna exhibits and a huge model of Sterling Forest itself.
From the visitor center let’s head east into a brief section of forest on a footpath.
Old Forge Road Crossing
After rambling through this portion of the trail we follow the Sterling Lake Loop trail east crossing Old Forge Road near private residences.
McKeages Meadow Connector
After crossing Old Forge Road the orange triangle blazed McKeages Meadow Connector trail appears to our right.
Truck Trailers Sterling Lake Loop
Continuing straight ahead on the Sterling Lake Trail, the trail turns from a footpath to a woods road as we pass old trailers to our left near private property.
Old Railroad Causeway
Wetland
From here we follow the Sterling Loop trail as it crosses a wetland via an old mining railroad embankment.
Second Old Forge Road Crossing
Long Meadow Road appears ahead but the trail turns north just missing the busy road. Crossing Old Forge Road for the second time we find ourselves heading north climbing.
Dead Hemlock
We have reached an Eastern Hemlock dominated forest but unfortunately many of the Hemlocks are dead or dying due to the Woolly Adelgid, a non-native pest from 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.
Pine Meadow Trail Connector Trailhead
As we head northwest, the 0.3 Mile Orange Blazed Pine Meadow Connector Trail appears to our right.
Sterling Lake Loop Grassy Trail
Our feet are in for a treat as the trail becomes a soft grassy road as we continue heading north on the Sterling Lake Loop.
First view of Sterling Lake
Our first glimpses of Sterling Lake appears to our left as the trail turns northwest.
Sweetfern
Whew! Let’s take a quick breather and take time to look at some of the vegetation growing near the trail. Here’s some Sweetfern native to the Eastern US. Its name is misleading as Sweetfern is not a fern at all but a deciduous shrub. The “sweet” in Sweetfern is correct as the leaves give off a sweet odor when crushed. Sweetfern typically grows in dry upland habitat.
Hog Peanut
Hey! Is this Poison Ivy? It’s got the whole “leaves of three leave ’em be” look. Nope, it’s a vine known as Hog Peanut. Hog Peanut is a member of the Bean Family (unlike Poison Ivy which is a member of the Cashew Family) and helps out plants growing nearby by correcting Nitrogen levels in the soil. Hog Peanut is common in both dry and mesic (moist) forest types.
American Chestnut
Here’s American Chestnut. The American Chestnut tree was an important member of the eastern forest found in the United States. A wide variety of wildlife fed on its chestnuts. Mature American Chestnuts began to die off in 1904 due to imported Chestnut Blight from Asia. The blight, imported to the US via Asian chestnut trees, is a fungus dispersed by spores in the air, raindrops and animals. American Chestnut now survives only in the understory as shoots sprouting from old roots (which are not affected by the blight). The American Chestnut sprouts reach about twenty feet before the blight strikes. The roots then shoots up new sprouts and the process repeats itself. The American Chestnut Foundation is currently working to restore the once great American Chestnut back to its native range. Check out the book American Chestnut : The Life, Death, and Rebirth of a Perfect Tree for more information. Click here!
Powerline Cut
Milkweed in Bloom
Continuing north we reach a Powerline cut in the forest. Powerline cuts create permanent Shrubland which provides habitat for flora such as Milkweed, an important wildlife plant (especially for Monarch Butterflies) which does not grow in the dense shade of the forest floor.
Heading south a portion of the Yellow Blazed 6.2 mile Sterling Valley Trail joins the Sterling Lake Loop trail from the north.
Looking down as we walk on the jointly blazed Sterling Lake Loop & Sterling Valley Loop we spot movement. Tiny toads!
Little Toads (Most are circled-see if you can find ones I missed!)
Let’s carefully and slowly proceed west on the jointly blazed Sterling Lake/Sterling Valley trail watching where we step.
Sterling Lake
We have now arrived at the northern tip of Sterling Lake.
Approaching a small sandy beach we spot a turtle digging in the sand.
Turtle heading back to Sterling Lake
But, as soon as we spot this turtle it takes off with surprising speed to Sterling Lake…..
…where it quickly disappears under the water.
Pond
Leaving the sandy beach and the now vanished turtle behind we cross an earthen causeway separating the pond above from Sterling Lake.
Beaver Lodge
Taking a closer look at the pond reveals an active beaver lodge.
5-Line Skink
Continuing west past a former boat launch a movement on a rock catches our eye. A 5-Line Skink! Native to the Eastern US, the 5-Link Skink is one of the most common lizards found in the Eastern Forest.
Blueberries
Heading south on the jointly blazed Sterling Lake Loop and Sterling Valley Loop we spot some blueberries growing along the side of the trail. The blueberries provide a refreshing treat as we continue our hike.
Sterling Valley Trail Exits
As we continue south Sterling Lake now appears to our left and the Yellow Blazed Sterling Valley Trail exits.
Continuing south on the Sterling Lake Loop trail we see beautiful views of Sterling Lake.
Sterling Forest Fire Tower Connector Trail
As we walk we find the woods road the trail has been following has ended and the trail now follows a paved road (West Sterling Lake Road) passing the Fire Connector trail to our left.
Lakeville Ironworks Trail
Ruins
As we walk on the pavement we pass ruins of Lakeville Ironworks and the trailhead of the 3/4 of a mile mile Lakeville Ironworks trail. These buildings are remnants of former mining operations.
Located in the Highlands geologic region, the hills of Sterling Forest were mined for iron ore known as magnetite beginning in 1730 and ending in the 1920’s when the last of the mines shut down.
Help Save New York’s Ash Trees
As we walk we notice signs tied to nearby White Ash trees. The signs are in relation to the Emerald Ash Borer, a destructive pest from Asia which threatens all ash trees. The mature emerald ash borer does not pose a threat. It is the larva of these borers which eat away at the heartwood of ash trees.
Sterling Lake Outlet with Sterling Furnace in distance
Heading east on a footpath back in the forest we are now crossing the outlet of Sterling Lake near its dam. The Sterling Lake dam was originally built in the mid 1700’s to provide water power to the the Sterling Furnace. The dam raised the water level of Sterling Lake by 8 feet. A mine (now completely filled with water) was located directly below Sterling Lake.
Sterling Furnace
Sterling Furnace was used until 1804 to create Pig Iron. Later, raw iron ore was shipped by trail to PA to be smelted using large coal deposits. The furnace was rebuilt by the City Investing Corporation in the 1950’s.
Remains of Lakeville Church
Near the visitor center we pass the foundation of Lakeville’s Church. Well, we are now back at the visitor center and have completed our virtual hike of Sterling Lake! I hope you enjoyed your journey and that you check out this hike in person! Click here for directions!
3. Don’t miss The Highlands: Critical Resources, Treasured Landscapes! The Highlands exemplifies why protection of New Jersey’s Highlands is so important for the future of the state. It is an essential read on the multiple resources of the region.
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.
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
ECEC Front Desk
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)
Renewable Energy
Once inside, there are various exhibits regarding topics such as renewable energy.
Wind Energy
After taking in the information, pick up a trail map, it’s time to explore the trails!
Start of Interpretive Trail
Head outside the center and turn right on the Lenape Trail.
Welcome to the Lenape Trail
Throughout the exploration numbered wooded posts will be encountered. These posts correspond to the trail map pictured below (taken from the Essex County Environment Center Website) which we will review as we proceed.
Essex County Environmental Center Trail Map
Sweetgum Leaf
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.
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 Mother Log
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.
Deer Fence
Behind this marker a tall deer proof fence will appear.
Habitat Restoration Area Please Stay on Trail
The fence was constructed to keep hungry white-tailed deer out so native vegetation may grow.
Frog Pond
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!
Create a 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.
Head toward Eagle Rock Avenue to Marker # 5 found at the start of the White Blazed Patriots Path.
Garlic Mustard
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):
White Tail Deer
Eastern Gray Squirrel
Eastern Chipmunk
After passing marker six it’s time to leave the Patriot trail by heading left to a wooden boardwalk.
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).
Poison Ivy
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.
Passaic River Canoe and Kayak Access
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.
Passaic 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.
Pollinator Garden
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).
Busy Bees at Work
The Essex County Beekeepers keep a selection of Honeybees here. Bee careful not to disturb it!
Marker 12 Lenape Life
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.
Wigwam
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.
Red Oak
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.
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
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
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!
Marker 15 Ferns
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.
Bird Lane Trail
We’ve now come to the beginning of the blue blazed Bird Lane Trail.
Bird Lane Trail Trailhead
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.
Old Equipment
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.
Bird Lane What will you find?
Well, we’ve now reached the end of the Bird Lane Trail!
Bird Lane Trail End
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!
The Great Swamp Outdoor Education Center (GSOEC) consists of a 44 acre portion of the Great Swamp managed since 1963 by the Morris County Parks Department. The GSOEC hosts guided nature walks, school, scout and public educational programs.
Herp Study in Progress
The GSOEC hosts periodic studies of the flora and fauna to determine the overall health of the Great Swamp.
Great Swamp National Wildlife Refuge
The estimated 7,768 acre Great Swamp National Wildlife Refuge (GSNWR) abuts the GSOEC to the west. The GSNWR is one of 553 refuges administered by the Department of the Interior’s U.S. Fish and Wildlife Service. Lands comprising a National Wildlife Refuge are managed for the protection of wildlife and its habitat.
History of the Great Swamp
The origin of the Great Swamp begins with the melting and subsequent retreat of the Wisconsin Glacier around 25,000 years ago. Debris from the glacier blocked the passage of an ancient river creating an enormous lake known as Lake Passaic. Lake Passaic is thought to have been 30 miles long and 10 miles wide. Over time, an outlet was formed near Little Falls NJ draining the lake via the Passaic River. This drainage is still occurring today. Today the Great Swamp forms a remnant component of the once great Lake Passaic.
GSOEC Forest
In the late 1950’s the area now known as the Great Swamp was identified by the NYNJ Port Authority as an ideal location for a new jetport. The Great Swamp Conservation Foundation mobilized volunteers to protect the Great Swamp. The result was the establishment of the Great Swamp National Wildlife Refuge. The Great Swamp Conservation Foundation later became the North Jersey Conservation Foundation and then finally known as New Jersey Conservation Foundation.
Trails:
GSOEC features four short loop trails. Two of the four trails (Orange & Red) are interpretive and follow 16 markers listed in a self guided trail booklet available at the education center. Click here for a trail map!
The total length of the trails is 1.4 miles.
Virtual Tour:
Ready to take a virtual tour of the Great Swamp Outdoor Education Center? Let’s Go!
Stop by the kiosk near the parking lot to pick up a trail map. From the kiosk, head to the education center to view the exhibits on the flora and fauna of the Great Swamp.
Outdoor Education Nature Center with Kiosk
Mammals of The Great Swamp
Endangered in New Jersey
After checking out the exhibits inside, it’s time to start our hike.
Orange Trail Trailhead
Let’s begin our virtual hike by taking the Orange Blazed trail located to the south of the education center. The Orange Trail at .61 Miles is the longest trail present in the GSOEC. It contains Markers 1-10 from the self guided trail.
Marker 1
The first marker, regarding the Red Maple tree, appears shortly after the beginning of the orange trail. Red Maple is the most common tree in the Great Swamp as well as the eastern deciduous forest.
Red Maple Leaves
Red Maple’s flowers are red in the spring and the leaves turn a brilliant red in the fall. Though the Sugar Maple may come to mind when it comes to maple syrup, Red Maple can be tapped for syrup as well. Red Maple should be tapped before budding occurs as the buds change the chemical makeup of the syrup.
Marker 2
Continuing on the orange trail, marker #2 comes into view on the right where a large depression may be found.
Large Depression
The large depression is known as a vernal pond. Vernal ponds do not support fish and may be dry or filled with water. Due to the lack of predators (i.e. fish) the vernal pond provides a safe haven for amphibians such as Wood Frogs, Spring Peepers and Blue-Spotted Salamanders among other species to breed and lay eggs. Continuing past the vernal pond, two fenced areas appear shortly after on the left.
Marker 3 with Deer Enclosure in background
Marker # 3 explains that these sections of the GSOEC were fenced in 2009 to study how plant communities recover from the damage caused by an overpopulation of white tail deer.
Marker 4 EcoTone
Marker #4 describes an Ecotone. An Ecotone is anywhere two habitats meet and create an edge. The Ecotone present here was created by the Power line right of way. The positive aspects of this man-made Ecotone is the creation of suitable nesting habitat for the local turtle population in addition to providing a valuable hunting ground for birds of prey. On the flipside, the disturbed ground caused by the creation of the power lines have provided ideal habitat for invasive plants as Autumn Olive, Multiflora Rose, Garlic Mustard, Wineberry & Japanese Barberry.
Marker 5 The Pond
Continuing in a southwest direction, the dirt path changes to a boardwalk as the trail traverses the wetland area.
Orange Trail Boardwalk
A short boardwalk appears to the right of the main boardwalk which leads to the Pond which is marker #5.
The Pond
Ponds are usually less than 18 feet deep. Eventually as plant matter and other organic material decays, the pond will begin to become a marsh, progress to a forested wetland and finally upland habitat after many years.
Continuing on the trail leads to Marker #6 which describes Poison Ivy which is seen here growing as a hairy vine. Poison ivy contains a clear liquid known as urushiol which causing a burning itching rash in many people. In addition to a hairy vine Poison Ivy can be found as a shrub reaching over three feet tall or as a trailing vine on the ground.
Several rhymes exist warning of the dangers of Poison Ivy:
At this point of the hike you may notice abundant Mountain Laurel. Marker # 7 appears here.
Marker 7 The Browse Line
Its purpose is to briefly touch upon “the browse line”. The over abundant white- tail deer have stripped all leaves of vegetation from six feet down. If the current trend continues, there may not be a forest here in the future.
From this area, the trail head of the .23 of a mile Blue trail loop appears.
Blue Trail Trailhead
Let’s take a brief break from the interpretive trail to explore this short trail.
Blue Blaze Swamp Chestnut Oak
The Blue Trail Loop goes through an upland area consisting of mostly Mountain Laurel and Swamp Chestnut Oak.
Dried Vernal Pond Blue Trail
The trail encircles a small vernal pond (the vernal pond, seen here at the end of September 2012 was dry).
Blue Trail trailend
Completing the Blue Trail Loop, head back to the Orange Trail and to Marker # 8 which describes the function of a rotting log in the forest.
Rotting Log
Standing dead trees or snags play an important role in the eastern deciduous forest. Woodpeckers including Pileated, Downy and Red-Bellied among others excavate holes in the dead trees searching for tasty insects. These excavated holes in turn create habitat for birds including Black-Capped Chickadee. Fungus will usually invade the dead wood further softening it. Eventually, the tree will fall to the forest floor where it will continue to decay creating a rich organic soil which will support future species of trees.
Marker 9 Phragmites Marsh
Proceed east to Marker # 9 The Phragmites Marsh. Phragmites (aka Giant Reed) is a giant species of grass which can grow from 10-20 feet. Phragmites thrives in disturbed areas. Phragmites found in the Great Swamp are native to the eastern deciduous forest. Phragmites are considered invasive because of its aggressive growth and tendency to overwhelm all other vegetation.
Marker 10
Outdoor Study Area
From here the trail leaves the boardwalk and heads south to marker # 10 which passes an outdoor study area and leads to a Wigwam replica.
Wigwam
The Lenape Native Americans (the original people) created Wigwams as shelter from saplings, tree bark and Cattail Mats among others. This replica would have been big enough for two people. Marker #10 is the last marker for the orange trail.
Orange Trail Trailend
After heading back from the Wigwam, turn right on the Orange Trail and follow the trail a brief distance to its terminus.
Prayer of the Woods
The “Prayer of the Woods” sign is found right before the start of the Red Trail. After reading the Prayer and taking in its message, turn right to start hiking the .39 mile Red Trail to continue the interpretive trail.
Red Trail Trailhead
The first marker on the Red Trail is #11 which identifies trees found in the Eastern Deciduous Forest.
Marker 11 Deciduous Forest
Trees found in the Eastern Deciduous Forest include the below among others:
The term “deciduous” indicates that the trees comprising this type of forest lose their leaves each fall and grow new leaves in the spring.
Marker 12 Transmission Lines and Marsh
Continuing on the red trail leads Marker #12 “Transmission Lines and Marsh”.
Red Trail Power Cut
Here, vegetation is periodically removed or trimmed back so as to not interfere with the power lines. This wet marsh provides habitat to Wood Ducks, Mallards, Muskrats and Red-Wing Blackbirds among others.
Red Trail to Education Center
From here turn left at the sign leading to the education center to go to Marker # 13.
Marker 13 Stream
The Red Trail approaches Marker #13 as it crosses a stream.
Red Trail Stream Crossing
Sediments and rocks on the stream bottom provides habitat for a variety of Crayfish and Macro-invertebrates. Marco-invertebrates lack backbones and can be seen without the aid of a microscope. Certain macro-invertebrates such as Caddisflies are pollutant intolerant. Presence of pollutant intolerant macro-invertebrates are one way to indicate the health of a stream. Macro- invertebrates eat many different things depending on the species-there are predators, scavengers, and herbivores among them. In turn, macro-invertebrates are a source of food for various turtles, fish and frogs.
Marker #14 The Wet Meadow
Continuing on the red trail leads to Marker #14 which discusses“The Wet Meadow”. The Wet Meadow is a man-made habitat created by a power-line cut and is home to field mice, star-nosed moles and various hawks & owls among others.
Marker #15 American Beech
Marker #15 leads to an American Beech Tree. The smooth gray bark of the American Beech Tree usually invites individuals to carve their names and other messages into the trunks. Carving in a tree trunk is similar to a cut on your finger. However, unlike your injured finger, a tree cannot put a band-aid on its wound. The carved bark is an open door for disease.
Beechdrops
Beechdrops, seen here in this picture, lack both leaves and chlorophyll and is a parasitic plant of the American Beech Tree.
#16 The Swamp
Marker #16 The Swamp
The final marker on the red trail briefly discusses the importance of the Great Swamp. The land comprising the Great Swamp is a mix of meadows, upland woods, marsh and brush covered swamps. Only 40% of the Great Swamp is wet either part of the year or all year long whereas 60% of the Great Swamp consists of upland forest & meadows.
Red Trail End
You are now at the end of the Red Trail.
Green Trail Blaze
At the end of the red trail head north to catch the beginning of the short .20 of a mile Green Trail near the parking area. The Green trail traverses in a short loop in an upland portion of the GSOEC.
Mushrooms Green Trail
Check out these mushrooms found growing in September 2012!
Asian Long Horn Beetle Detector
In the parking area near the end of the Green Trail you may notice a black box hanging from a tree. The Black boxes are used to detect for the presence of the Asian Long-Horn Beetle, an invasive species from Asia.
Wildlife Blind
After the Green Trail is complete, it’s time to visit the Observation Blind located off the parking lot which views the Pond looking west.
Turtles on the Pond from Wildlife Blind
This concludes our virtual hike! I hope you enjoyed it and it inspired you to take a trip to see the GSOEC for yourself!
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.
Green Acres
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.
Funding Provided by Passaic County Board of Chosen Freeholders
Ecological communities featured in High Mountain Park include:
Rocky Headwater Stream:
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 Swamp (Fall)
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.
False Hellebore
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
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:
Trap Rock Glade- Outcrop Community (Winter)
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
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:
Red Cedar
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.
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.
American Beech
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:
Wooly Adelgid on Hemlock Needles
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:
Preakness Brook
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 by the NJ DEP. According to the NJ DEP Website “Category One (C1) designation protects waterways from any discharge that produces a measurable change in the existing quality of the water”. 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.
Red Trail Trailhead College Road Parking Lot
The trailhead of the 1.7 mile Red Trail is accessible from the small parking lot off of College Road.
Red Trail
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.
Massive Boulder on Red Trail
After entering the forest, a large boulder is visible to the west near a sign advertising High Mountain.
To High MTN
From here, the Red Trail passes a stream & wetlands.
Wetlands near Red Trail
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.
Waterfall off of Red Trail
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.
Reservoir Drive Red Trail End
White Trail Trailhead
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.
North Jersey Country Club
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.
North Jersey Country Club Reservoir
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.
White Trail End
Yellow Trail Trailhead from Red Trail
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.
High Mountain Grassy Summit Yellow Trail
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.
Summit of High Mountain View of NYC with Black Cherry Tree in Bloom Yellow Trail
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.
Reservoir Drive Franklin Lakes NJ
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.
Swamp Beech Mountain Yellow Trail
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.
View of Point View Reservoir with Distant NJ Highlands from Yellow Trail Beech Mountain
The Yellow Trail continues northwest past another Preakness Brook Tributary and heads south and west past the parking lot for JVC Corporation.
Back of JVC Building on Yellow Trail
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.
Yellow Trail 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.
Buttermilk Falls Orange Trail Blaze
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.
Buttermilk Falls
Pancake Trail Trailhead
The 2.8 mile Blue Trail (aka the Pancake Hollow Trail) trailhead is located off of Chickapee Drive in Wayne.
Blue Trail Blaze
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.
Lean-To off of Blue Trail
Once past the housing developments, the trail traverses the “pancake hollow” section of High Mountain Park.
Stream along Blue Trail
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.
Blue Trail End
Horizontal White Blaze Trailhead
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:
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.”
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!
Outdoor wildlife exhibits include two Barred Owls and a Red-Tailed Hawk. These raptors were previously injured prior to coming to the nature center and cannot survive on their own in the wild. Other attractions include the the John A. Redfield Building which includes the Stephen Minkoff Memorial Library and indoor animal exhibits.
John A. Redfield Building
Indoor Animal Exhibits
The nature center provides public & after school programs as well as a summer day camp. There is also a butterfly garden, backyard habitat exhibit, picnic area and an outdoor education pavilion.
Education Pavilion
History
Tenafly Nature Center & Lost Brook Preserve
The land that was to become the TNC & LBP was sold in lots by 1874. Over time, the land owners could not afford the taxes and the lots reverted back to the town. The land was purchased from Tenafly by developers in the 1950’s. In 1958, a plan to construct 225 houses was approved by Tenafly but the plan lapsed. Developer Bernard Gray proposed building a million dollar country club in 1960 but later backed out.
In 1962, NY developer Norman Blankman proposed to build 300 homes and a golf course on the land. Tenafly swapped 60 acres of land with Blankman in 1963 to consolidate his land and the boroughs. The 60 acres became the Tenafly Nature Center. Soon after the consolidation, Blankman abandoned his original proposal and created a plan to develop 5 office buildings and a golf course. This development was rejected by Tenafly’s planning board. After other development ideas came and went, Blankman sold the land to Centex Developers in August of 1973 for 9 million. Centex proposed the construction of 1,780 houses, town homes and apartment complexes on the land. The land, valued at around 8.5 million dollars, was condemned by Tenafly which wanted to purchase the property for preservation purposes.
Green Acres Land & Water Conservation Fund
Tenafly completed the purchase of the land in 1976 using Green Acres funding, bonds and donations from the public. The new preserve became known as the Lost Brook Preserve. Tenafly Nature Center took over management of the Lost Brook Preserve in 2005 bringing the total acreage of TNC & LBP to 380 acres.
In 2009, the Bergen County board of chosen freeholders announced a $900,000 grant to the Borough of Tenafly to acquire once acre of land adjacent to the nature center. The nature center’s intent is to let the land revert to forest via succession. The acre is uphill of Pfister’s Pond whose streams drain into the Tenakill Brook, an important tributary of the Oradell Reservoir which is a source of drinking water for a large percentage of Bergen County.
Trails
An estimated 7 miles of blazed trails are waiting to be explored at the TNC & LBP.
Map of the Tenafly Nature Center
The picture above shows all the trails in the Tenafly Nature Center section of the preserve. Click here for a map that also includes trails found in the Lost Brook Preserve. All trails are directly or indirectly accessible from the estimated .55 of a mile Main Trail which can be accessed from the parking lot of the Tenafly Nature Center.
Main Trail
The Main Trail is the unpaved continuation of Hudson Avenue which heads from the parking lot down to Route 9W. The yellow, white (De Filiipi) and Bischoff Trail are accessible to the north of the Main Trail and the Red Trail, Allison Trail and Little-Chism Trail are accessible to the south of the Main Trail. The Main Trail passes by the historic Lambier House (private property) where Lambier Brook dead ends to the south of the trail. Beautiful viewpoints of the 3 acre Pfister’s Pond are visible to the north of the Main Trail. Wild Geranium grows along the side of the trail in springtime.
Yellow Trail Trailhead
The 1/3 of a mile interpretive Yellow Trail is the best introduction to the TNC & LBP. Numbered markers found throughout this trail match with this booklet providing excellent information on the flora & geology of the TNC & LBP including topics such as American Chestnut, New York Fern, Diabase Trap rock and much more.
Numbered Marker on interpretive yellow trail
At the end of the booklet there is a quiz to test your knowledge. The yellow trail follows the western border of Pfister’s pond and features a 50 foot watchable wildlife viewing dock that extends out on the western border of Pfister’s Pond.
Watchable Wildlife Grant Site
The trail then heads east and south to rejoin the Main Trail in a loop fashion.
De Filippi (White Trail)
The eastern side of Pfister’s Pond is accessible via the .4 of a mile white trail (aka De Filippi) trail. The white trail is accessible from the Main Trail or the western terminus of the Bischoff Trail. The trail traverses north near the eastern border of Pfister’s Pond passing the De De Filippi shelter on boardwalks before turning east and then turning south to connect either to the Bischoff Trail to the east or the Main Trail to the south.
View of Pfisters Pond from De De Filippi Shelter
De Filippi Trail Boardwalk
Bischoff Trail
The 0.6 white/red blazed Bischoff trail is accessible from the White trail from the west or off the Main Trail near 9W. From the Main Trail, the Bischoff Trail heads north and passes over a stream draining a small pond.
Bischoff Trail Swamp
From here, the trail turns west and passes to the south of the pond and traverses near Montammy Country Club to the North and the historic (private) Lambier house to the south.
Lambier House
The Bischoff trail then terminates when it meets the white trail.
Red Trail Trailhead
The .3 of a mile Red Trail, accessible from the Main Trail, heads south before turning east and north paralleling the east brook as it empties Pfisters Pond on its way to the Tenakill Brook.
East Brook
Many wildflowers such as Spring Beauty, Dwarf Ginseng, Trout Lily, Canada Mayflower and others appear on this trail in the spring. The purple trail trailhead is accessible to the east of the red trail. The red trail continues north and terminates into the Main Trail.
Purple Trail Trail Head
The .5 of a mile Purple Trail heads southeast from the Red Trail and crosses over the east brook and the Blue Spur (short .2 of a mile trail which leads to Highland Avenue).
Blue Spur Trailhead
Once past the blue spur trail, the purple trail continues southwest crossing over Lambier Brook before terminating into the Allison Trail.
Allison Trail
The yellow blazed 1.4 mile Allison Trail is accessible from the north via the Main Trail, the east and south via the Little-Chism Trail and the west from the purple trail. Heading southwest from the Main Trail the Allison Trail passes wetlands and interesting rock formations.
Massive Rock Formation Allison Trail
These formations are made up of rock known as diabase which was formed when molten lava cooled underground. The trail then traverses southeast where it briefly follows the Little-Chism Trail.
Little-Chism Allison Trail
From here the trail crosses the Green Brook before heading southwest once more paralleling the Green Brook to the west and its wetlands before terminating into the Little-Chism trail near East Clinton Avenue.
Allison Trail End Near East Clinton Avenue
An interesting trail that is accessible from the Allison Trail is the 0.6 of a mile orange blazed Haring Rock Trail.
Haring Rock Trail Trailhead
This trail traverses the western portion of the preserve. Heading south from the Allison Trail, the Haring Rock Trail travels in a meandering fashion passing wetlands to the east. The trail terminates at the Haring Rock.
Haring Rock
The Haring Rock is a glacial erratic named after a Dr. John J. Haring who made sick calls in the area around the turn of the century on horseback. Doctor Haring often stopped at this rock to rest. An interesting fact about this glacial erratic is that it was originally located east of its current position on top of traprock where the Jewish Community Center is located. When the Jewish Community Center was developed the rock was moved to its current location. It was discovered that the rock would not stay put in its original position and was instead cemented in place upside down. The Haring Rock Trail ends at this rock and the Seely Trail begins here.
Seely Trail Trailhead
The 0.3 yellow/orange blazed Seely Trail is accessible from the Haring Rock Trail & connects to the Little-Chism trail once it crosses Green Brook.
Green Brook Crossing Seely Trail
The short trail traverses near East Clinton Avenue in the southern boundary of the preserve.
Little-Chism Trailhead
At 2.1 miles, the red blazed Little-Chism Trail is the longest trail featured in the TNC & LBP. The Little-Chism Trail is accessible from the Seely Trail in the south of the preserve near East Clinton Avenue, the Allison Trail in the southern boundary near Route 9W or from the north off of the Main Trail. Exploring the trail starting from the Seely Trail terminus, the trail heads east near wetlands and turns north briefly leaves the preserve and traverses next to Route 9W before heading back to the forest.
Little-Chism Trail by Route 9W
Continuing north, the trail crosses over Lost Brook where a dam is visible.
Dam on Lost Brook Little-Chism Trail
Lost Brook
The trail joins with the Allison Trail briefly after it crosses Green Brook near more wetlands.
Green Brook Little-Chism Trail
Both the Green Brook, Lost Brook are tributaries of the nearby Hudson River. The trail then passes the trail terminus for the short Sweet Gum Trail (which leads to the nearby members only Greenbrook Sanctuary to the east).
Sweet Gum Spur Trailend
The trail continues heading north crossing over two additional tributary streams before terminating at the Main Trail near Route 9W.
The trail, which opened in October of 1997, follows the path of the former New York Susquehanna and Western Railroad. This particular section of the railroad was created in 1872 and abandoned in 1958. Most of the railroad infrastructure was removed when the line was abandoned but reminders such as moss covered railroad ties can still be found.
Old Railroad Tie
The trail was constructed by hard working dedicated volunteers and named after the Wood Duck, which may be found in the Wallkill River National Wildlife Refuge.
Wood Duck
The trail is flat and makes for very easy walking.
Interpretive signage has been strategically placed throughout the trail informing visitors of the surrounding habitat and its residents.
Wood Duck Interpretive Signage
Beaver Interpretive Signage
In addition to the interpretive nature signs, there are plenty of benches and even a wildlife viewing blind.
Wildlife Viewing Blind
The trail features footbridges over Wallkill River tributaries such as Beaver Run.
Foot Bridge over Beaver Run
Habitats found along the way include red maple dominated swamps located near the beginning of the trail.
Red Maple
Red Maple is one of the most abundant native trees found in eastern North America. It is common in swampy slow draining flats and along small sluggish streams. These habitats can be found throughout the Wood Duck Nature Trail.
This out and back trail runs for about 1.75 miles before it ends at the Wallkill River. Out and back trails always provide the opportunity to see additional wildlife or scenery you might have missed heading in. Future plans for the Wood Duck Nature Trail include a foot bridge over the Wallkill River and extending the trail by another .75 of a mile.
Wallkill River
Wallkill River
The Wallkill River, a tributary of the Hudson River, begins by draining Lake Mohawk in Sparta, New Jersey and flows about 88 miles northeast through a wide glacial valley between the Kittatinny Mountains to the west and the Hudson Highlands to the east. The river is unusual for flowing north in between the south flowing Hudson and Delaware rivers.
Beaver Run as seen from footbridge
The Wallkill River and Beaver Run are labeled FW2-NT. (Fresh Water, Non-Trout). Water with this classification are generally not suitable for trout because of physical, chemical or biological characteristics but may be suitable for a wide variety of other fish.
Wallkill River National Wildlife Refuge Habitat
The Wallkill River National Wildlife Refuge contains one of the last large areas of high quality waterfowl habitat left in northwestern New Jersey. The refuge contains emergent marshes, vernal pools, wet meadows and forested wetlands surrounded by oak covered limestone ridges paralleling the Wallkill River.
Endangered Species
The Bog Turtle Recovery Plan (USFWS 2001) has identified the Wallkill River watershed as a recovery subunit making the refuge one of only two national wildlife refuges that supports the endangered Bog Turtle.
Bog Turtle
Measuring in at only 3-3.9 inches, the Bog Turtle is one of the smallest and secretive of North America’s turtle population. Habitat suiting the bog turtle includes calcareous (limestone) fens and wet, grassy pastures which are all found within the Wallkill National Wildlife Refuge.
Wet Meadows
Just like the interpretive signs of wildlife picture listed below (and found on the Wood Duck Nature Trail), you don’t have to necessarily see physical animals to know they are present.
Signs of Wildlife Interpretive Sign
Animals and birds leave tracks and other signs that they have been in the area.
Given that there are an estimated 40 species of animals living in the Wallkill National Wildlife Refuge, you are bound to come across some clue to key in on what species has been poking around. Animals documented include the following among others:
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!
The Wood Duck Nature Trail trailhead is located on Route 565 in Wantage, New Jersey, approximately 200 yards north of Route 23 near the Sussex Queen Diner on Route 23 North. There is a small parking lot available right outside the Wood Duck Nature Trail trailhead.
Wallkill River National Wildlife Refuge Wood Duck Nature Trail
The refuge contains three other hiking trails in addition to the Wood Duck Nature Trail providing visitors to experience the refuge in and out. If you are in the area, be sure to check it out!
On December 4, 2011, Watershed Advocacy group Bergen SWAN (Save the Watershed Action Network) teamed with naturalist Nancy Slowik to host the first ever Emerson Woods nature walk. Once targeted for intense development, the woods are now preserved and help protect the Oradell Reservoir from non-point source pollution.
Emerson Woods and Oradell Reservoir
Bergen SWAN played a major role in preserving Emerson Woods. Bergen SWAN has fought for almost 24 years to help preserve the remaining forests surrounding upper Bergen County’s reservoirs. The most recent settlement occurred in 2009 with United Water. United Water manages the Oradell, Lake Tappan and Woodcliff Lake Reservoirs in Bergen County. After 5 years of negotiations with Bergen SWAN & the Hackensack Riverkeeper, United Water agreed to granting conservation easements on 3,100 watershed acres to the NJDEP in addition to setting aside $1 million to assist in acquiring and preserving additional land along the Hackensack River and its tributaries. United Water has since become a close ally of Bergen SWAN by helping to sponsor events such as the 2010 “Planting in the Park” in Pascack Brook County Park and allowing Bergen SWAN to host the December 4th nature walk on United Water watershed land-land which is normally not open to the general public.
Nature Tour
Emerson Woods Nature Tour
The tour, led by naturalist Nancy Slowik, started in the United Water recreation parking lot near Lakeview Terrace in Emerson, NJ. Once the group was organized, Bergen SWAN opened up the gate to the Oradell Reservoir providing a rare opportunity to walk along the shore of the reservoir. Nancy directed the tour to the waterfowl present on the open water of the reservoir. Double-crested Cormorant were seen in addition to Hooded Mergansers.
Double Crested Cormorant
Heading away from the shore, the tour passed a stand of American Sycamore with their white peeling bark.
American Sycamore
Early settlers used to make buttons out of American Sycamore seedpods. The “button” is found inside the seedpod. This practice created another name for the American Sycamore: the Buttonwood Tree. Nancy pointed out Poison Ivy growing on a dead Eastern Hemlock tree. Members of the tour were advised to never touch the hairy vine of Poison Ivy as you can still get a painful itchy rash even in winter.
Poison Ivy Rope on Dead Hemlock Tree
Palmolive dish washing liquid was recommended as an inexpensive cure for poison ivy. The tour then led participants up a gas line right of way for about ¼ a mile.
Along the way, White-Tail Deer were seen browsing in the woods west of the right of way.
White Tail Deer
As the group proceeded on, Nancy pointed out large rectangular holes found on a dead tree.
Up ahead on the gas trail was a stand of Northern Red Oak (NJ’s state tree!) with its characteristic “ski slope” bark. Nancy informed the tour that when a Northern Red Oak gets cut it admits a foul odor.
Northern Red Oak
Shortly before turning west onto the Heck Ditch trail, the group happened upon a White Pine plantation.
White Pine Plantation
White pines make excellent habitat for Great Horned Owls and other birds of prey which frequent Emerson Woods.
Possible Hawk or Owl nest in White Pine
Cones of White Pine are sticky with the seeds found inside. Native Americans used to chew on White Pine needles to obtain Vitamin C.
As the group passed the Heck Ditch Nancy pointed out that the oily looking water surface of the ditch was caused by bacteria decomposing leaves.
Heck Ditch
Ground Pine
Ground Pine was found growing in large colonies on the other side of the Heck ditch trail. Ground Pine takes years to become established.
Scouring Rush near Cotton Wood Tree
After walking for about 15-20 minutes on the Heck Ditch trail, the tour headed south on the Equisetum trail which leads back to the United Water Recreating parking lot. Along the way, Nancy pointed out large growths of equisetum growing near massive Cottonwood trees. This collection of Equisetum is thought to consist of the largest stand in New Jersey. Equisetum are members of an ancient order of plants and appeared well before the appearance of the first flowering plants. Equisetum was known to early settlers as “Scouring Rush”-a name given for its ability to clean and scrub pots and pans.
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!
The group headed back to the parking lot as twilight descended. As we walked, we happened upon an abandoned Red-Eyed Vireo nest. The red-eye vireo spends the winter living in South America.
The group proceeded to the parking area and the tour concluded.
Emerson Woods Preserve
A special thanks to Bergen SWAN and Nancy Slowik for offering the opportunity to explore Emerson Woods in great detail. For more information on Bergen SWAN click here.
The Emerson Woods Preserve are accessible from off of Main Street in Emerson or Lakeview Drive. Ample parking is available on Summer Street. Be sure to check out Bergen SWAN if you wish to participate in nature walks, community clean-ups and educational events in Emerson Woods.
Welcome to the Secaucus Mill Creek Marsh! Mill Creek, a tributary of the Hackensack River meanders through the marsh. The estimated 209+ acre marsh was purchased from Hartz Mountain Industries in 1996 by the New Jersey Meadowlands Commission for preservation purposes. The marsh was previously slated for a 2,750 unit housing development.
Mill Creek Marsh
Though the marsh had not experienced direct industrial activities, habitat for wildlife was limited. The marsh had layers of fill and consisted of a monoculture of Common Reed which limited tidal inundation. The New Jersey Meadowlands Commission began enhancement of the marsh in 1998. The purpose of the enhancement was to create an intertidal brackish marsh, upland habitat, mudflats and shallow sub-tidal areas. Islands were created from fill in the marsh and were planted with salt tolerant flora such as Spartina (aka Salt Marsh Cordgrass). Spartina tolerates salt water by excreting excess salt. Two impoundments of Mill Creek (North/South) were created in addition to re-establishing tidal flow.
Stand of Gray Birch next to Mill Creek Marsh Trail
The term “enhancement “is used rather than “restoration” because there is no evidence to support that an intertidal marsh ecosystem with both mud flats and raised islands ever existed naturally in the meadowlands.
Mill Creek Marsh NYC Background
During the enhancement activities, removal of fill exposed old stumps of Atlantic White Cedar which had been buried for many years. It’s estimated that 1/3 of the Hackensack Meadowlands were once covered in Atlantic White Cedar. The decline of these majestic trees in the meadowlands began in the mid 18th century when the durable Atlantic White Cedar wood was used to make roads and houses. Later, swaths of the cedar forest were burned to eliminate hiding places for pirates. The last of the cedars died out with the completion of the Oradell dam on the Hackensack River which severely slowed the influx of freshwater pouring into the swamp and allowed an influx of saltwater into the marshes.
Atlantic White Cedar Stumps in Mill Creek Marsh
Over a short period of time former freshwater marsh became a brackish estuary. These stumps are all that is left of the once extensive Atlantic White Cedar forest in the meadowlands.
Mallards, Yellowlegs, Little Blue Heron
While the eco-system is certainly healthier than it was prior to the enhancement, water quality still has a long way to go. The creation of water channels has allowed for oxygen exchange and greater tidal flushing which has improved water quality. However, coliform bacteria is still present in Mill Creek at elevated levels most likely due to the proximity of a municipal sewage treatment plant near the marsh. Samples of macro invertebrates taken from Mill Creek primarily consists of pollutant tolerant species which is an indicator that water quality is not as healthy as it could become in the future.
Trail
Mill Creek Marsh Trail Map (Trail in Green)
Mill Creek Marsh Trail
A 1.5 mile handicapped-accessible trail was created during the NJMC enhancement activities at Mill Creek Marsh. The trail traverses both the south and north impoundments and ventures near Least Tern Island (one of the artificially created islands) and consists of a gravel footpath and footbridges. The trail offers a multitude of opportunities to view wildlife. Educational signs have been placed throughout the trail providing information to visitors of Mill Creek Marsh.
Example of Educational Signage found along Mill Creek Marsh Trail
The trail can be walked in a looped fashion around the southern impoundment (for a shorter walk) or in a loop around the northern impoundment (for the full 1.5 miles).
Fiddler Crabs and different species of fish populate Mill Creek in addition to turtles such as Diamondback Terrapin. Diamondback Terrapin are the only turtles adapted to life in brackish waters. Muskrats also make their home here.
Flora
Hibiscus
In addition to Common Reed, (which is still present in many locations), Gray Birch, Saltwater Cordgrass, rushes, sedges and other flora flourish in Mill Creek Marsh.
Sunflowers
Mill Creek Marsh
Today the Mill Creek Marsh is an oasis of nature in a sea of overdevelopment. There is no place else that I can think of where you can view ancient stumps of Atlantic White Cedar with the NYC skyline as a backdrop.
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!
Be sure to click here to check out additional great photos of Mill Creek Marsh! (Thanks Hope)
Driving Directions (as stated in the NYNJ Trail Conference Mill Creek Trail Description)
Take the New Jersey Turnpike to Exit 16W and follow signs for Route 3 East. Cross the bridge over the Hackensack River and follow signs for “Secaucus/New Jersey Turnpike South/Exit Only.” Continue past the Turnpike exit and take the next exit (just beyond the underpass) for “Harmon Meadow Blvd./The Plaza/Mill Creek Mall.” Follow Harmon Meadow Boulevard to the third traffic light (Sam’s Club is on the left) and turn left onto Mill Creek Drive. Cross over the New Jersey Turnpike and continue straight ahead (do not bear left) at a sign for “Mill Creek Mall.” Park on the right, at a sign for “Mill Creek Trail.”
Feel free to comment below with any bird sightings, interesting plants, memories or suggestions! Thank you and have fun exploring!
1. The Nature of the Meadowlands – The Nature of the Meadowlands illuminates the region’s natural and unnatural history, from its darkest days of a half-century ago to its amazing environmental revival.
3. Meadowlands: A Wetlands Survival Story – Slowly but surely, with help from activist groups, government organizations, and ordinary people, the resilient creatures of the Meadowlands are making a comeback, and the wetlands are recovering.
The preserve is a cooperative project of the New Jersey Conservation Foundation (NJCF) and the county of Passaic. Passaic County has owned 501 acres of the preserve after purchasing the land from the Borough of Butler with Green Acres funding in 1971. Public Access to the property was limited until NJCF purchased the adjacent Faustini property in 2002 bringing the total acreage to 576. The property was previously going to be developed and would have fragmented a crucial highlands forest and degraded water quality in nearby High Crest Lake. The Faustini property includes an estimated .93 of an acre pond and rock outcrops.
Apshawa Preserve
The forty acre Butler Reservoir is the centerpiece of the Apshawa Preserve and was formed from the impoundment of the Apshawa Brook which flows from the northwest. Once used for the Borough of Butler’s water supply, the reservoir is now only used during emergency drought situations.
Butler Reservoir in fall
From Butler Reservoir, Apshawa Brook continues south through an old mixing pond and cascades until its confluence with the Pequannock River near Route 23.
Apshawa Brook
Samples of macro invertebrates taken from the Apshawa Brook show healthy populations of Mayflies, Stoneflies and Caddis flies. These species are all pollutant intolerant species. Macro indicates that the organism can be seen without the aid of a microscope whereas invertebrate indicates that the organism has no backbone. The presence of these pollutant intolerant species indicates the Apshawa Brook’s water quality is very high. The NJ DEP has classified the stream as Trout Production and labeled the brook with “C1” status which is one of the highest water classifications in NJ. According to the NJ DEP Website “Category One (C1) designation protects waterways from any discharge that produces a measurable change in the existing quality of the water”.
Apshawa Deer Fence
Passaic County Freeholders Forest Restoration Fence
In December of 2010, The New Jersey Conservation Foundation (NJCF) completed construction of a 16,800 feet (3.2 Mile), 8 feet high wire mesh deer fence on three hundred acres of the Apshawa Preserve. The NJCF states that the Apshawa Preserve is at a “deer tipping point” and that the forest is partially degraded. 18 White-Tailed Deer were observed in the fenced 300 acres during a NJCF sponsored deer drive on December 10, 2010. NJCF states that 18 deer on 300 acres equals to about 40 deer per square mile. A deciduous forest becomes degraded when deer density is greater than 20 deer per square mile.
White-Tailed Deer
The purpose of the fence is to keep white-tail deer from over-browsing native herbaceous plants & young tree saplings. The fence will be in place for 10 to 15 years. Assessments of native plant populations found both in and out of the fenced areas will be taken on occasion to determine the effectiveness of the fence. According to the NJCF, so much native vegetation has been consumed by the white-tail deer that non-native plants such as Mugwort, Garlic Mustard, Oriental Bittersweet, Japanese Barberry and Japanese Stiltgrass have taken hold in many areas of the forest where native species once flourished. These nonnative plants crowd out beneficial native plants by forming a monoculture which offers few benefits to native wildlife. Seeds of these plants were carried via foot traffic and illegal ATV use.
Garlic Mustard
The Pequannock River Coalition (PRC) has called the forest restoration project “the fence that makes no sense” and has stated that the design of the fence impedes travel of other animals such as the state endangered Bobcat and Wood Turtle. PRC published a field review of the Apshawa Preserve and fence on November 22, 2010. The report stated that while deer sign was present in the preserve, the PRC did not encounter any deer during a three mile assessment. Greenbrier, which becomes scarce in areas where excessive deer browse is excessive, was found abundant in thickets in many areas. The report goes on to state that many young saplings were present indicating that the forest is regenerating. The biggest threat to new growth appears to be the dense canopy of dense shade and not excessive deer browse. The report concluded that several smaller enclosures would be more feasible to manage. 2019 Update: Please note that the Pequannock River Coalition is now defunct and the field review report is no longer available online.
Apshawa Deer Fence Gate
However, NJCF stated that managing many small enclosures is too expensive and that the design of the fence can be modified. The fence was placed tight to the ground in many places which prompted the NJ DEP to state that amphibians and snakes may have difficulties getting through to critical food supplies or breeding grounds with the current design of the fence. To accommodate, sections of the fence have been raised 7 inches high and 12 inches wide every 15-20 feet depending on the terrain. NJCF has stated that the purpose of the fence is to minimize deer presence but acknowledges that it is impossible to keep deer completely out. The PRC stated that studies have proved that hungry deer have been shown to squeeze in areas 7 inches high and 12 inches wide.
Deer Fence Animal Crossing Apshawa Preserve
Other methods to ease animal crossing include old snags (dead trees) placed over the top of the fence (seen in the picture above) to help animals such as Bobcats to cross over to the other side.
Black Bears have made a habit of breaking through sections of fence to get to the other side. The NJCF studied areas of high Black Bear traffic in the preserve and placed strategic “Bear Ladders” to aid in their crossing.
Bear Climb
Under NJ law, almost all land modifications where there are stream corridors are governed by N.J.A.C. 7:13 aka the flood hazard control act. Fences are only exempted from this act if they are located outside of a floodway and if the fence is not designed in a way that will catch debris in a flood.
Stream Crossing Chains
The NJCF responded by placing heavy chains at the bottom of the fence to prevent debris from catching and permitting the flow of water. It is hoped that if White-Tail Deer feel the heavy chains on their heads they will turn around.
Trails
Apshawa Hike 5.29.11 and 6.21.11
There are almost 7 miles of blazed trails to be explored in the Apshawa Preserve. These trails were created with the assistance of volunteers and funding was provided through the National Recreation Trails Program. 2019 Update: Please note the trail descriptions below were from 2011. Trails have been re-blazed since then. If you go (and I hope you do!) please pick up a trail map from the kiosk in the parking lot or print a trail map from the NJ Conservation website.
All trails are accessible from the white trail whose trailhead may be found in the Apshawa Preserve parking lot. Be sure to stay on the marked trails as there are unmarked trails throughout the preserve. There are signs posted letting you know if you are going to stray from the marked trail.
Leaving Trail System
While it is possible to hike (if you start early in the day) the entire preserve in one trip, I find it best to explore the Apshawa Preserve over two separate trips. The best introduction to the Apshawa Preserve is to hike the northern section of the Apshawa Preserve to the scenic Butler Reservoir. Start by taking part of the 2 mile white trail from the parking lot.
White Trail trailhead
The white trail heads northwest and goes through a swamp and traverses to a ridge top providing excellent views of the Butler Reservoir.
One of the views from White Trail
After stopping here for a look at the surrounding highlands, follow the white trail down to shore of Butler Reservoir and look to the left for the start of the 1.25 mile red trail.
Red Trail Trailhead
The red trail traverses along the western shore of Butler Reservoir and crosses over tributaries of the Apshawa Brook located to the northwest of Butler Reservoir. Once the trail passes over the tributaries, the trail heads east to once again meet with the white trail which traverses the northern section of the Butler Reservoir. Continuing to head east, the white trail meets the .5 of a mile yellow trail which encircles an 8 acre pond.
Yellow Trail with Pond
However, I found most of the yellow trail was under water due to Beaver activity when I visited in May 2011. I spoke to a NJCF representative regarding the condition of the yellow trail and was told that a possible reroute may be possible for the future.
Yellow Trail Closed due to Beaver
As of June 2013 the Yellow Trail is closed due to Beaver Activity. Continuing on our virtual tour: Heading west away from the flooded area, the yellow trail connects to the white trail and goes southwest and then east to the parking lot.
The second hike explores the southern portion of the preserve via the 3 mile green trail.
Green Trail
The green trail is the longest trail created in the Apshawa Preserve. From the white trail, the green trail heads south and passes a historic mixing pond and interesting ruins from the time when this property was watershed land for the Borough of Butler.
Dam at Historic Mixing Pond on Green Trail
Ruins on Green Trail
The trail continues northwest and does a switchback climb. There are scenic views here of adjacent protected Newark watershed land which looks great in any season but looks absolutely spectacular in the fall.
View on Green Trail
From here, the green trail continues north until it reaches Butler Reservoir and the red trail. Follow the red trail east and north until you connect back to the white trail. Take the white trail east and southwest back to the parking area.
Flora:
The Apshawa Preserve consists primarily of a oak-sugar maple forest. Before the Chestnut blight, American Chestnut was likely abundant. Saplings of American Chestnut still occur.
American Chestnut
Today there are new threats facing the eastern forest. The Emerald Ash Borer threatens all Ash trees. Purple boxes have been hung in the preserve and throughout New Jersey to detect for the presence of this destructive pest from Asia. The mature emerald ash borer does not pose a threat. It is the larva of these borers which eat away at the heartwood. The color purple attracts the emerald ash borer. Once the insect lands on the box they become trapped on the sticky surface.
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!
