Welcome to the Lenoir Preserve! Located in Yonkers, New York, the estimated 40 acre preserve features upland woodlands, a large lawn, nature center, butterfly garden, an old mansion and old ruins scattered throughout.
Heading out, we pass a picture of a map of the preserve including the route we will be taking today.
Lenoir Preserve Trail Map
Ready to begin?
White Trail Trailhead
Heading west from the nature center we find the trail-head of the estimated .70 of a mile White Trail under a stand of dense evergreen trees.
Heading southeast into the forest we pass by the trunk of a massive Tulip Tree. Found throughout the forest of the Lenoir Preserve, the Tulip Tree is native to the Eastern United States and is one of the tallest trees found on the eastern seaboard.
Building near White Trail
Continuing southeast on the white trail a large apartment building appears straight ahead through the trees. This will be the last reminder of the modern urban environment as we trek through the woods.
Old Manmade Pond
Continuing our walk we find an old man-made pond. The pond still fills with water from an old pipe buried underground.
As we walk a twisty looking plant known as Wineberry is found all around us. Wineberry is native to Asia and an established invasive plant in the United States.
A little further on a yellow trail has joined the White Trail from the west.
Stone Steps Wooden Bridge
Let’s head west briefly on the yellow trail for a moment to see where it goes.
The Yellow Trail leads right to the Croton Aqueduct trail which is a New York State Park. This trail goes over a huge old masonry water tunnel which once provided water to thirsty New Yorkers until 1965. The trail was created in 1968.
Stairs Yellow Trail
Leaving the Croton Aqueduct and heading east we temporarily pass the White Trail. Old stairs appear to the east leading to terraces. Let’s go take a look.
Archway Yellow Trail
An ancient Archway appears near the end of the yellow trail. I don’t know about you, but I feel a pair of eyes watching us.
It’s a Song Sparrow! Song Sparrows favor brushy areas such as where we spotted this one or should I say it spotted us.
Yellow Trail Beginning
Let’s head back down the Yellow trail to continue our journey on the white trail in Lenoir’s forest.
White Trail Rock Path
As we walk more ruins appear as the sun filters through the leafless trees.
White Trail Ruins
This may have been part of a fireplace of the destroyed “Ardenwold” Mansion which once existed in the site. The Ardenwold Mansion was destroyed by fire in the 1970’s.
White Blaze on Black Birch
Nearing the southern border of the Lenoir Preserve the White Trail turns east.
We’ve been spotted and the alarm has been sounded! A Northern Mockingbird is keeping careful watch over the woodlands of the Lenoir Preserve.
Leaving the woodlands an old ruined wall with an ancient looking gazebo gazes mournfully at us. We have reached the southern border of the Lenoir Preserve. The ruined wall and gazebo are part of the Alder Manor which was built around 1912 by William Boyce Thompson. The manor is private property operated by the Tara Circle, an Irish Cultural Center.
Alder Mansion Garden
Peaking through an old iron gate we see an expansive old garden.
Crows Chasing Hawk
Leaving the White Trail and heading north to the Great Lawn we spot some commotion in the open sky above. American Crows are chasing an unidentified Hawk.
Now heading north through the great lawn, the expansive Lenoir Mansion appears to our right. The mansion was built between in the mid-to late 1800’s for presidential candidate Samuel J. Tilden from granite quarried on site.The mansion is named after Lenoir, North Carolina by a later owner by the name of C.C. Dula who added additional wings to the mansion.
As we walk pass the Lenoir Mansion heading north a mournful sound fills our ears. It’s source is this Mourning Dove keeping watch over us as we walk.
An old stone gazebo appears just north of the mansion as we walk. What’s that sound?
Just west of the gazebo is a massive butterfly garden which was created in 1995 by volunteers of the Hudson River Audubon Society. The garden is named after a Beverly Smith who came up with the idea to plant the garden. The garden has showcased a rare Rufous Hummingbird in the past. The Rufous Hummingbird normally occurs in the far west of North America and winters in Mexico.
Heading back towards the nature center a curious looking spotted bird is seen on the ground. It’s a Northern Flicker! Northern Flickers, such as this one, spend a lot of time searching for food in the form of ants and other insects on the ground.
Bird Feeders Rain Garden
We’ve reached the back of the nature center where bird feeders tempt hungry birds and a rain garden is present during the growing season. With that we’ve concluded our walk of the preserve. Thank you for joining me today. It is my hope that this virtual tour inspires you to visit the Lenoir Preserve to check it out for yourself!
Click below to see a list of plants found at the Lenoir Preserve!
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
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.
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.
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.
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.
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!
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!
Let’s carefully and slowly proceed west on the jointly blazed Sterling Lake/Sterling Valley trail watching where we step.
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.
Leaving the sandy beach and the now vanished turtle behind we cross an earthen causeway separating the pond above from Sterling Lake.
Taking a closer look at the pond reveals an active beaver lodge.
Continuing west past a former boat launch a movement on a rock catches our eye. A 5-Lined Skink! Native to the Eastern US, the 5-Link Skink is one of the most common lizards found in the Eastern Forest.
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
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 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!
Silas Condict Park was dedicated at 200 acres in 1964. In 2005, additional purchases of adjacent land brought the total acreage to 1,581. The centerpiece of the park is Canty’s Lake which is formed from an impoundment of a Stone House Brook tributary (which itself is a tributary of the C1 classifiedPequannock River, one of the cleanest rivers in New Jersey)
Silas Condict Park White Trail Virtual Tour
Today we are going to explore the Bear Mountain area in the southern section of Silas Condict Park via the estimated 3 mile White Blazed Trail (aka “the Bear Trail”) following the below trail map (taken from the NYNJ Trail Conference).
Ready? We’ll begin our hike by following Canty’s Lake which will be to our left as we walk north from the parking area. Before we go any further let’s see what’s hanging around Canty’s Lake.
We got company! Ring-Necked Ducks! You would think this duck would be called the Ring-Billed Duck due to a white band around its beak but the duck actually has a chestnut colored ring around its neck which is only visible at close range.
While we are chatting about Ring-Necked Ducks a bird just flew by with white tail feathers. It’s a Dark-Eyed Junco! Dark-Eyed Junco belongs to the Sparrow family and prefers forest and shrub lands. The Dark-Eyed Junco stays in New Jersey for the winter and migrates further north during the growing season.
White Trail Trailhead (Near Canty Lake)
Leaving the shore of Canty’s Lake we walk a bit north and find ourselves in front of the White Trail trail-head. We are going to be following the white trail in a loop fashion. Nice! Loop trails are always my favorite.
Silas Condict County Park Forest
Let’s enter the forest and leave civilization behind for a bit.
Mountain Laurel greets us as soon as we enter. The deciduous forest of winter is primarily colorless other than evergreen shrubs such as Mountain Laurel and the American Beech tree. American Beech (particularly young American Beech) hold onto their leaves until spring when new leaves emerge. As we walk we hear the paper like leaves blowing in the wind.
We are proceeding in a southwest direction and climbing in a zig-zag fashion on the White Trail. American Crows are sounding the alarm that we are in their forest. White-Breasted Nuthatches and Tufted Titmouse are having their own conversations as we start to climb on the trail.
East Facing View
We’ve come to the first viewpoint! Here, we are looking east. Though it’s covered with snow, we can take a seat if we want to rest after our brief climb to this view. After taking in the views we descent passing interesting rock formations.
Numerous fresh blow-downs are present throughout the forest which most likely fell during Hurricane Sandy.
Newly Created Vernal Pond Habitat
We may feel sad seeing big trees toppled over but the good news is the hollowed out area where the root structure was now becomes prime vernal pond habitat. Vernal ponds are temporary pools of water that are free of fish and provide valuable areas for amphibians such as Wood Frog to lay eggs.
As we walk Mountain Laurel becomes abundant with adjacent Chestnut Oak.
Chestnut Oak Mountain Laurel
Proceeding through the Mountain Laurel, we have entered a Chestnut Oak forest punctured here and there with Pitch Pine, a tree normally associated with the NJ Pine Barrens.
Pitch Pine grows here on thin, dry and generally infertile soil. These Pitch Pines found on this mountain are exposed to frequent ice storms in winter and strong winds year round.
Chestnut Oak is usually found on dry slopes at high elevations such as where we are right now. Shrubs such as lowbush blueberry and black huckleberry are common in Chestnut Oak forests. However, given we are in late winter, the only shrub we are encountering today is the abundant evergreen Mountain Laurel.
We’ve now started our second climb up a snow covered path.
Our efforts are rewarded with a wonderful western view of the NJ Highlands!
Pitch Pine Western View
The western view is continuous as we continue south and pass an interesting balanced boulder with the White Trail Blaze painted on it.
Balanced Rock with White Trail Blaze
We now start to descend as the trail turns east. It’s a bit tricky going down the snowy trail so be sure to watch your step!
White Trail Blaze leading to Rock Tunnel
As we continue to follow the White Trail we find it is leading us to a rock tunnel.
Let’s squeeze through to the other side!
Looking back at Rock Tunnel
Whew! We made it out! But now we have to watch our footing. We have a snow covered boulder field to walk through!
As we carefully meander through the boulder field we find ourselves following the White Trail on a slippery rock outcrop.
Whoops! We slipped!
Thankfully we’re ok.
Let’s brush ourselves off and keep moving-that Turkey Vulture flying over us seems to have ideas about us.
Trout Brook Stream Crossing
We’ve now arrived at Trout Brook and its surrounding wetlands. Trout Brook drains Canty’s Lake and is a tributary to Stone House Brook. Let’s carefully cross the stream by jumping on rocks.
Bridge over Trout Brook
As we continue on the White Trail we have yet another crossing of Trout Brook-but this time there’s a brand new wooden bridge present which makes for easy walking.
As we leave the bridge we see a massive rock outcrop before us and see the White Trail Blaze lead straight up the outcrop! Let’s watch our step and climb.
At the top we find we have left the footpath and are now following a gravel road (steep in places).
Albino White-Tailed Deer
As we walk we are suddenly surprised by a blur of white! An Albino White-Tailed Deer! The deer is so white it matches the snow around. Amazing!
Bear Mountain Silas Condict County Park
Leaving the deer and the gravel road we are back on a foot path where we see views of Bear Mountain, which we just finished climbing.
Canty’s Lake View from the White Trail
Continuing on a little further we now find a bench with a wonderful view of Canty’s Lake. We are almost at the end!
We did it! We are now at the end of the White Trail back at the parking lot near where we started!
I hope you enjoyed this virtual hike and that it inspired you to check out the hike in person!
Silas Condict Park is located at 100 Kinnelon Road, Kinnelon, NJ.
Check out some great books below to learn more about NJ’s plants and wetlands!
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.
Torne Mountain Norvin Green State Forest
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.
NJ Highlands 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.
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.
Entrance to Torne Trail
Starting from near the Otter Hole Road Parking area, head south to the trailhead of the red blazed Torne Mountain Trail.
To the Blue Trail (Hewitt-Butler Trail)
Once on the Torne trail, signs advertising the blue-blazed Hewitt-Butler Trail will appear.
Hewitt Butler Trail Blaze
Head southwest then south on the blue blazed Hewitt-Butler Trail to Climb Torne Mountain.
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.
View from Stone Living Room
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.
Rocky Ravine Torne Trailhead
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.
Distant Wanaque Reservoir View from Osio Rock
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 found along the trail includes the below 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!
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).
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.
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.
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:
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 Eastern Red Cedar.
Prickley 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/Eastern Red Cedar Woodland:
Eastern 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.
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.
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.
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.
2020 Update – Please note the trail system has changed since this post was written. An updated map was posted to the NY NJ Trail Conference. You can access it here.
The below trail description was as I found the trails in High Mountain when I wrote this post in 2012.
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.
2020 Update – Reminder, the above trail map is no longer accurate.
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.
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 Mountain
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.
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 I’ve spotted during my hikes at High Mountain Park include:
Scarlet Tanager (Female)
Black Rat Snake
Eastern Tiger Swallowtail Butterfly
Eastern Cottontail Rabbit
High Mountain Park Preserve provides much needed habitat to the threatened Long-Eared Bat which has been found roosting in the forest.
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!