Despite its close proximity to the Ramapo Mountains which are comprised of Highlands “basement” rocks, Campgaw Mountain comes from a different geological background. With a ridge expanding two miles Campgaw Mountain is comprised of basalt and is part of the Watchung Mountains. Elevations range from 300 feet to a maximum elevation of 751 feet atop Campgaw Mountain.
Campgaw Mountain contains several ecological communities including upland xeric (dry) deciduous forest, mesic (moist) deciduous forest and deciduous forest wetlands. Meadow habitat can be found along the power lines within the boundaries of the park.
The below are a sample of a list of birds that have been spotted within Campgaw Mountain:
Welcome! Today we are going to see eastern views near a ski lift, and explore an interesting pond! Ready? Let’s go!
Let’s start our journey by heading west on the joint .5 of a mile Yellow Blazed Indian Trail and Blue Blazed .90 of a mile Rocky Ridge trail.
Almost immediately the blue blazed rocky ridge trail splits off from the yellow blazed Indian Trail. Let’s take it! We’ll meet up again with the Indian Trail later. On the Rocky Ridge Trail we pass under power lines between two old buildings.
Old Cedar Trail 1
As we walk we go through an intersection with the 2.10 mile Red Blazed Old Cedar Trail.
The Rocky Ridge footpath has now changed to a gravel road which we are climbing. Looking to the sides of the trail we see lots of Japanese Barberry, which has become an established invasive plant in the understory of the forest of Campgaw Mountain.
Old Cedar Trail
As we near the top of our climb the Rocky Ridge Trail has left the gravel road and is now a rocky footpath traveling along the ridge of Campgaw Mountain (hence the trail’s name!) We pass through another intersection with the 2.10 mile Old Cedar trail.
Basalt Rocky Ridge
Turning north on the Rocky Ridge Trail we find the landscape has become even more rocky but pleasant and more open like the environment found among the ridges of nearby High Mountain Park Preserve with basalt appearing now and then.
Dutchman Breeches Rocky Ridge Trail
As we walk on the basalt of Campgaw Mountain, we spot some Dutchman Breeches along with some Hepatica flowers growing to the side of the trail. Dutchman Breeches are named as such because the flowers resembles old-fashioned breeches. Hepatica flowers are named as such because the leaves are said to resemble liver. Both are ephemeral flowers found only in the early spring before the leaves on the trees come back. As we admire the flowers we hear a Red-Tailed Hawk screech overhead.
Shagbark Hickory and Eastern Red Cedar
Looking at some of the trees as we walk we pass by Shagbark Hickory and Eastern Red Cedar. We have now arrived in an open woodland. We spot Wineberry, a common invasive plant from Asia sprouting from the forest floor. As we walk we pass several structures for Frisbee golf (aka disc golf) which is set up throughout the park.
Rocky Ridge Trail End
Arriving near the ski lefts the .50 of a mile yellow blazed Indian Trail we left when we first started reappears.
Eastern View with Ski Lifts
Take a look at the view! Here we can see a clear eastern view of surrounding Bergen County.
Leaving the the Rocky Ridge Trail, we now head east on the yellow blazed Indian Trail and pass the green blazed beeches trail to our left and right.
Skunk Cabbage Wetlands
Looking to our left we spot a good amount of Skunk Cabbage as we go down the Indian Trail. Ahead of us is a swamp. Many people think that any wetland they may see is a swamp but this is not the case. A swamp contains woody vegetation whereas marshes do not.
From the Indian Trail we turn left on the orange blazed Hemlock Trail. The Hemlock Trail follows along the shore of Fyke Pond which was created from the impoundment of Fyke Brook.
As we walk along we pass several smooth bark grey trees. These are American Beech, a slow growing native deciduous tree of the eastern forest.
American Beech Hemlock Trail
Continuing on we pass to our left two massive boulders made of basalt.
Basalt Boulders Hemlock Trail
As we pass the boulders a sudden cry pierces the ear: a Blue Jay has noticed our presence and is sounding the alarm that we are in its forest.
As we walk we pass by many dead and dying trees from which this trail was named after: The Eastern Hemlock. Most of the hemlocks found in Campgaw Mountain County Reserve 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.
Take a look! Some turtles have spotted us from a rock in Fyke Lake. Nice!
Turtle Fyke Lake
Near the end of the Hemlock Trail we scare away a male and female Wood Duck.
Hemlock Trail End
From here it’s a short walk back on the Indian Trail to the parking lot where our car is. I hope you enjoyed this virtual hike of Campgaw County Reservation and that it inspires you to visit it for yourself!
Campgaw Mountain is located at 200 Campgaw Road, Mahwah, NJ 07430
Feel free to comment below with any bird sightings, interesting plants, memories or suggestions!
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!
Welcome to Buttermilk Falls Park! Located in West Nyack, New York, the park features a scenic waterfall and two western views where on a clear day you can see up to 16,000 acres. The 75 acre Buttermilk Falls Park was purchased by Rockland County with additional acquisitions in 1981.
Buttermilk Falls Park is location in a portion of the Palisades ridge north of the Sparkill Gap. The Palisades are located along the western shoreline of the Hudson River in southeastern New York and in north eastern New Jersey. Rocks found in the Palisades are known as diabase and were formed during the Triassic period around 200 million years ago.
Buttermilk Falls consists of a mixed-oak forest community including the following species among others:
Welcome! Today, using this Trail Map, we are going to explore some of the 75 acres that make up Buttermilk Falls Park! Along the way, we’ll see some cascades and check out some cool western views. The total hike is an estimated 1.2 miles. Ready? Let’s go!
Blue Trail Trailhead
From the parking lot we are going to head northeast on 0.9 of a mile blue blazed trail.
Entrance to the Blue Trail
Entering the park on the blue trail, the path starts flat but we find it is deceiving as we start to climb.
But before we start any kind of climbing let’s take a quick scan of some of the flora that’s sprouting near the entrance. What’s this plant that sort of looks like little bamboo shoots sprouting up everywhere alongside the trail? It’s Japanese Knotweed, a obnoxious invasive plant which, once established, is generally there for good. Japanese Knotweed forms monocultures, excludes native plants and does not provide any benefit to wildlife.
Blue Trail Steps
Leaving the Japanese Knotweed for now the Blue Trail is taking us up some wooden steps.
Taking another look at the flora coming up, what’s this 3 leaved spiked covered plant popping up all over the place? It’s Wineberry. Wineberry is native to Asia and is an established invasive plant in the United States.
Blue Trail Climb 2
Continuing on we start hearing the sound of water, a good sign as we must be approaching Buttermilk Falls!
Taking a look around the forest floor we spot the leaves of Trout Lily, a native woodland plant which blooms in early spring. And here you thought all we would be looking at is invasive plants! The “trout” in it’s name is said to come from its mottled leaves which are said to resemble wild trout.
Heading southeast on the blue trail we come to an open area on the trail with Eastern Red Cedar and occasional trap rock.
Continuing southeast on the blue trail we pass the .21 of a mile Orange Trail trail head.
Blue Trail Second Viewpoint 2
Shortly after we pass the orange trail trail head we arrive at the second westerly viewpoint. What a beautiful day! From an ecological perspective we are currently in a traprock glade/rock outcrop surrounded by dry grass and forb-dominated species.
Leaving the second and last viewpoint we continue on the blue trail and pass a small but interesting plant known as Dutchman Breeches. Dutchman Breeches are a native to the eastern US. The flowers (which have since wilted) are said to look like old fashioned breeches hence its name.
Blue Trail Rock Seat
Tired? Want to take a seat? There is a seat carved out of the diabase to our left. Neat!
After a series of switchbacks we have come to the end of the Blue trail at the intersection with the white trail. Turning right on the white trail we walk in a north west direction.
What’s that up ahead? Someone long ago dumped an old car off of the White Trail.
Rock Wall White Trail
Looking to our left we pass by an old rock wall which is a sure sign the land we are walking on was at one time farmland.
Boardwalk White Trail
Looking ahead we spot a boardwalk further down the White Trail.
Swamp White Trail
As we walk on it we come to a Red-Maple Swamp to our left. Red Maple (Acer Rubrum) are one of the most common maples found in the northeast and is a common tree in wetlands.
White Trail end
Just past the swamp we have reached the end of the White Trail at the parking lot where we started our hike. And that concludes our hike! I hope you enjoyed it and that it inspires you to visit Buttermilk Falls County Park for yourself!
Today’s hike will be an estimated 4.2 miles. We will be using this Trail Map to help us find our way through the woods.
Today’s virtual hike will take us pass a lake, the Ramapo River, ruins, scenic overview and a waterfall!
Ready to begin?
Ramapo Valley County Park Kiosk
From the parking area just past the kiosk marks the start of the Orange Blazed 6.5 mile Shuber Trail (the longest trail found in Ramapo Valley County Reservation) and the .8 mile Silver blazed trail (All trails are maintained by volunteers of the NYNJ Trail Conference)
Shuber (Orange) & Silver Trailhead
Heading west on the combined orange blazed Shuber and the Silver trail a bridge appears ahead crossing the Ramapo River.
Continuing west, scenic Scarlet Oak Pond (once part of a former gravel quarry) appears to our right. I think it’s safe to say that the majority of people we will see on our hike will be found here walking their dogs (as this is an extremely popular park to bring your dog) around this beautiful pond.
Shuber Trail Left
Come on, let’s leave the crowds and take the path less traveled. Keeping our eyes peeled to the left we follow the Orange Blazed Shuber Trail as it leaves the Silver Trail heading south west following the Ramapo River through a floodplain forest where Red Maple is the staple tree.
We are lucky today. The trail which travels alongside the Ramapo River is relatively dry. During times of snowmelt and rainstorms this path would be inaccessible.
As we continue heading west on the orange blazed Shuber Trail we pass the 3.0 mile Green on White Blazed Halifax Trail trailend to our right and cross over MacMillan Brook on a wooden footbridge.
Orange Trail Bridge Crossing
At this point as you take in your surroundings you might start to question a couple of items. Is all this beauty actually in New Jersey? In Bergen County? The answer is a resounding yes!
But wait, what’s this before us? Old ruins of a stone cabin built by a church camp which once operated here appears as we turn right on the orange blazed Shuber trail. (update February 12, 2016: the ruins have been removed by the Bergen County Parks Department)
The orange blazed Shuber trail starts climbing to the northwest of the Ramapo River. But don’t get discouraged by the climb, we are in a for a treat! Scenic cascades and pools of the Macmillan Brook parallels the trail to our right.
The Macmillan Brook is a tributary of the Ramapo River.
Orange Trail Silver Trailend
As we continue past the cascades we meet up with the trailend of the .8 of a mile Silver Trail we had originally started with the Shuber trail. As we turn right on the orange blazed Shuber trail, our footpath turns to an asphalt road.
Yellow Silver Trailhead
Leaving the asphalt road and continuing on the orange blazed Shuber trail, the 1.6 mile Yellow Silver Trail appears to our left which traverses an area known as Matty Price Hill.
Passing the trailhead of the Yellow Silver Trail and continuing on the Shuber trail we pass a dam and outlet of Macmillan brook and see the beautiful estimated 13.11 acre MacMillan Reservoir to our right.
Red Trail Marsh Loop Trailhead
Continuing west past the reservoir the red blazed .3 mile Marsh Loop Trailhead appears to the south. Passing this trailhead we continue on our way traveling through an area of the Ramapo Mountains known as the Middle Valley.
Ridge Trail Trailhead
A short distance ahead the 1.9 mile Blue Blazed Ridge trail appears to our right. Let’s take it!
Ridge Trail Macmillan Stream Tributary #1
Heading north and leaving the Shuber trail behind us we carefully walk on rocks over a couple of Macmillan Brook tributaries. I should probably mention here that these rocks and the Ramapo Mountains themselves are situated in a geologic area known as the Highlands Region. Dating from the pre-cambrian time period, these rocks are probably as old as the Earth itself.
Ridge Trail Stream 2
Turning right and heading southeast on the Ridge Trail the .8 Blue on White Havemeyer Trail appears to our left.
Ridge Trail & Havemeyer Blue on White Trailhead
While we will be continuing on the Ridge Trail, the Havenmeyer trail explores a section of the Ramapo Mountains known as the Monroe Ridge. Though we can’t see it, an abandoned mine known as the Nickel Mine is found to the right of the Ridge Trail. The Nickel Mine is said to have been associated with the Hopkins and Dickinson Manufacturing Company which had operations producing bronze locks and iron castings in the 1870s along the Ramapo River. The Nickel Mine was created by digging two pits (both now are filled with water) in a search for nickel-bearing rock (hence the name Nickel Mine).
Ridge Trail Chestnut Oak Forest
As we continue our walk on the Ridge Trail with the Monroe Ridge to our north we have left the forest of Birch and Beech we were passing through and have entered a Chestnut Oak Forest. Chestnut Oak Forest canopies are up to 65% dominated by its namesake species. Associate plant communities of Chestnut Oak Forest include:
Continuing southeast on the Ridge Trail we come across the trailend of the 1.0 mile White Trail which traverses across the Monroe Ridge which is located north of where we are now.
Ridge Trail Overlook Sign
Heading south on the Ridge Trail a sign for a Scenic Overlook appears. Let’s take it!
Following a brief Red Triangle on a blue background we come to outcrops. The outcrops 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. Enough geology for now, let’s take a look at the view! Here we have a great eastern view of the surrounding Ramapo Mountains along with Campgaw Mountain. Though we cannot see it today due to hazy conditions in the distance NYC may be seen on a clear day.
RidgeTrail End Silver Trail
Heading back to the blue blazed Ridge Trail we turn south where the Ridge Trail ends at an intersection with the Silver Trail. Heading South on the Silver Trail we see a sign advertising a waterfall. Let’s check it out!
After a steep descent we come to the base where we have terrific views of the waterfall.
Whew! Believe it or not but we are almost done and it seems like we just got started! Alright, let’s head back to the Silver Trail.
Scarlet Oak Lake Return
Heading south on the the Silver Trail we pass scenic Scarlet Oak Pond where the orange blazed Shuber Trail joins us.
Silver Trail & Shuber Trail End
Well we have come to the end of the jointly blazed silver and shuber trail back at the parking lot where we began our hike. I hope you enjoyed our virtual hike and that it inspires you to check out Ramapo Valley County Reservation for yourself! Thanks for reading!
Wanna Hike Ramapo Valley County Reservation? Click Here for Directions!
Mountainview Nature Park was acquired as a gift from the Winston Perry family by Rockland County in 1979.
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.
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.
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.
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.
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!
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.
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.
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!
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 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:
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.
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.
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.
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:
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!