Welcome! Today we are going to hike two of the four Pompton Aquatic Parks trails. We will use the below trail map (provided by thePompton Lakes Open Space Committee) to guide us.
We will have views of the adjacent Pompton River and a hike through a preserved floodplain forest. Ready? Let’s go!
Blue-Blazed Pompton Aquatic Trail
Starting from Woodlawn Avenue in Pompton Lakes we will head straight going west at the intersection near the trailhead of the .59 of a mile Pompton Aquatic Park Trail. The entire trail is through fresh water wetlands. Its good we picked the month of August to walk through when it is nice and dry! In fact, if we didn’t look at the vegetation growing we might not even know we were walking through wetlands. Common wetland vegetation growing along the trail as we walk include:
All of the above flora are native except for Purple Loosestrife and Japanese Knotweed which are considered invasive plants, that is, they displace and prevent native plants from growing because there are no natural predators native to the US to stop the spread of these plants.
Intersection of the Blue Blazed Pompton Aquatic Trail with the Yellow Blazed Rivercrest Trail
From here we will follow the 1 mile yellow blazed Rivercrest Trail which is the longest trail found in Pompton Aquatic Park. We will head north on this out and back trail (meaning we will retrace our steps). Out and back trails are a good way to verify if you missed something as you walked.
And there is the Pompton River! The Pompton River formed just north of Aquatic Park through the confluence of the Pequannock, Wanaque and Ramapo Rivers. The river above the park is technically still called the Pequannock River. The Pompton River is classified FW2-NT (fresh water non-trout production or maintenance) by the NJ DEP. The Pompton River is a major tributary to the Passaic River.
Painted Turtles in the Pompton River
As we walk along we spot some painted turtles bobbing in the Pompton River. Don’t they have the life! Not a care in the world!
Invasive Mile-a-Minute Plant
We see jumbles of arrow shaped leaves everywhere. It’s a Mile-a-Minute Plant another invasive. It is native to Asia.
We’ve been spotted! A white-tailed deer family is watching us closely. Let’s keep going!
Well, we have made it to the end of the Rivercrest Trail at Joe’s Grill Field (which is part of the Pompton Lakes park system.). Time to head back the way we came to get to our cars. Glad you could make it! It is my hope that this ‘virtual tour’ of Pompton Aquatic Park inspires you to visit and check it out for yourself!
Feel free to comment with any memories, wildlife sightings or any other comments about Pompton Aquatic Park! Thank you and have fun exploring!
The trailhead discussed in this post is located off of Woodlawn Avenue in Pompton Lakes NJ.
Check out some great books below to learn more about NJ’s plants and wetlands!
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!
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 this trail map.
Silas Condict Park White Trail Area
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’s 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-Tail Deer
As we walk we are suddenly surprised by a blur of white! An Albino White-Tail 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. Directions may be found here.
Feel free to comment below with any bird sightings, interesting plants, memories or suggestions! Thank you and have fun exploring!
The 2013 Pequannock River Coalition (PRC) Winter Hike took participants on an exploratory hike through the Pequannock River Watershed. Led by PRC Executive Ross Kushner, the 4 mile hike promised education & exercise.
Pequannock Watershed Forest
Started in 1995, the Pequannock River Coalition provides a crucial voice in protecting the watershed of the Pequannock River, one of the cleanest rivers in New Jersey and a tributary of the Passaic River.
PRC 2013 Winter Hike
Ah, there you are! Welcome! Ready for the 4 mile hike? There’s plenty of snow on the ground to help us look for animal tracks.
Ross Kushner of the Pequannock River Coalition
Let’s begin by meeting Ross Kushner, the Executive Director of the Pequannock River Coalition. He’s going to lead the hike today!
We will be exploring the area just north of Copperas Mountain in nearby Rockaway Township. Ross has just taken attendance and now we are heading southwest on Green Pond Road and will be heading into the woods of the vast Pequannock watershed!
What happened here? These trees appear to have collapsed like dominoes. The fallen trees were part of plantations planted in the 1930’s by the Civilian Conservation Corps and were to be maintained (i.e. trimmed) every 10-15 years. With the onset of WWII the plantations were all but forgotten. Fast forward to 2012, we now have a tangle of trees growing close to one another. Hurricane Sandy came and knocked the trees down. Ross explained that in general other than habitat for Northern Goshawks and Red Squirrels, plantations are a monoculture and do not provide the diversity most wildlife require.
Hardwood trees that fell during the hurricane have become popular with White-Tail Deer who enjoy nibbling on sections of tree normally inaccessible.
Ross Kushner Praying Mantis Egg Case
Leaving the fallen tree and coming to a small field, Ross has just found a curious looking egg pouch attached to a plant in a frozen field. This is a Praying Mantis egg case.
Praying Mantis Egg Case
You can purchase Praying Mantis egg cases and use them as a natural “pesticide” for pests such as Japanese Beetles.
Heading back to Green Pond Road, Ross points out a stand of deciduous conifers near the side of the road and has identified them as American Larch. American Larch needles turn orange in the fall and fall off in winter.
Phragmites Marsh at Base of Green Pond Mountain
Heading back on Green Pond Road, we’re now walking over a Pequannock River Tributary near Deerhaven Lane. The Pequannock River Tributary draining the marsh in the foreground was straightened to drain the marsh. Phragmites, a common plant which thrives in disturbed wetlands, is abundant.
Green Pond Mountain
Around 10,000 years ago the Wisconsin Glacier piled boulders on the north side and sheared off the southern side of mountains in the NJ Highlands. As the glacier retreated at the end of the ice age, they tended to melt in place. The sheered cliffs visible on Green Pond Mountain were testimony to that theory.
Walking along Green Pond Road
We’re now continuing our journey down Green Pond Road. It’s been about a quarter of a mile but we are now again entering the Pequannock River Watershed forest.
What are these ruins we are looking at? Ross is now explaining that when the City of Newark acquired the land in the early 1900’s people were living throughout the watershed property and had been for over a hundred years. Their property was taken by imminent domain to protect the water supply. Back in the 1890s and early 1900s Newark’s population was dying as their water supply was derived from the Passaic River in Newark. This section of the Passaic River was and is severely impaired.
Running Deer Tracks
Walking a bit further in the snow Ross has suddenly stopped. “Look at the space between these deer prints!” he says. “This guy was flying, but not from us-these are old prints”. There must be 20 feet present between the gaps of the prints!!
Bear Tree (American Larch)
What is Ross looking at? It’s another American Larch tree with a good portion of its bark missing. Ross states “The bark has been taken off over the decades by Black Bears biting and rubbing their backs on the tree. The higher the bite, the bigger the bear. Sort of a territorial thing-every bear that comes by can determine what other bears have been in the area”.
Ross walks a bit further into the woods and suddenly stops.
We just happen to be by Deerhaven Lake where a number of White Pines are standing. These pines grew naturally. Though we don’t spot any today, there have been reports of Great Blue Heron nests in these pines. Ross turns around and starts heading back to Green Pond Road.
Near the beginning of the trail we see tiny footprints heading to a log. They belong to an Opossum.
American Beech Eye of the Forest
It looks like we are now leaving the Four Birds Trail and are walking by a rather large American Beech with marks that look like eyes keeping watch over the forest. American Beech is considered a climax species in succession and is an indicator that the forest present here has not been disturbed in a long time.
Ross Kushner American Beech Black Bear Claw Mark
Ross Pointed out black bear claw marks and noted that they are perfectly spaced.
Beaver Lodge Deerhaven Lake
Looking northwest towards Deerhaven Lake we see a large active beaver lodge with several others in the distance. Ross stated that the primary predator of beavers is the gray wolf which has been extirpated from New Jersey. Time to stop for lunch!
After eating our lunch Ross spots a White Oak tree covered with Black Bear claw marks. White Oak acorns are sweeter than other oaks such as Black or Red Oak. Black Bears love White Oak acorns so much that they will go up into the tree to retrieve them before they fall.
While checking out the claw marks we spot an out of season Firefly on the White Oak. Apparently it was tricked by the abundant sunshine.
River Otter droppings containing fish scales were spotted near an outlet of a Pequannock River tributary leaving Deerhaven Lake. River Otters are usually active near the outlet of a beaver pond and the droppings are indicators of River Otter territorial tendencies.
Otter Sliding Marks
We even see the slides they made on the ice!
Ross is taking us on a shortcut back to our cars near the Pequannock River.
What’s this? A stonefly! Soneflies are a sure indicator of the good water quality found in the C1 Trout Production Pequannock River.
Well, we’ve reached our cars and the tour has concluded. I hope this virtual hike has inspired you to explore your local forest.
Welcome to the Passaic River Coalition’s Butler Forest Preserve & Butler Raceway! Both preserves are contiguous and have a combined acreage of 14.9 acres of which four are deciduous wooded wetlands. Located in Butler, NJ, The Butler Forest Preserve and Butler Raceway were purchased to prevent the development of townhouses and provide protection of the Pequannock River.
Butler Forest Preserve & Butler Raceway
The Passaic River Coalition was established in 1969 and provides stewardship for the preservation and protection of over 1,000 miles of waterways associated with the Passaic River. The Pequannock River, a tributary of the Passaic River is labeled C1 indicating the water consists of some of the highest quality in the state of New Jersey.
American Beech Butler Forest Preserve
This was how the Butler Forest Preserve and Butler Raceway appeared when I explored it near the end of September 2012, nearly a month before Hurricane Sandy arrived. I find Jericho Road to be the best entrance to the Butler Forest Preserve & Butler Raceway.
Pequannock River Tributary
Entering the forest here I noticed a stream to my left (an unnamed Pequannock River Tributary) and plenty of American Beech. American Beech is part of the Beech-Sugar Maple climax forest community and are a sure indicator that this forest has not been disturbed for a very long time.
I carefully followed the woods down a somewhat steep slope while a steady roar increased. Thinking it was urban noise coming from nearby Route 23 and housing developments I was somewhat surprised to see the source was far more natural: The Pequannock River rushing by.
I noticed the river just as my eye caught old ruins. These ruins were part of the Butler Raceway which once provided water from the Pequannock River to power machinery to what was once the country’s largest rubber factory. The historic function of the raceway was to provide water from the Pequannock River to power machinery at the Butler Rubber Factory. The rubber factory was destroyed by fire in 1957.
Waterfall on Pequannock River
Near the ruins is a beautiful man-made waterfall on the Pequannock River.
Carefully scrambling over the ruins I made it to the Raceway just in time for a Great Blue Heron to fly by (unfortunately too fast for me to get its picture).
After admiring the Heron I came across an abandoned motorcycle.
Continuing east Yellow Birch appeared in good numbers. Yellow Birch favors north facing slopes.
Pre-Cambrian Rocks along Butler Raceway
Rock Outcrops of Precambrian origin appear occasionally to the right of the path. The Butler Raceway ends near Gifford Street. To get back to Jericho Avenue, simply turn around on the Raceway and proceed west until you come back to the cement ruins. Proceed south going up the hill until you reach Jericho Road.
The 2011 Pequannock River Coalition Fall (2019 Update: Pequannock River Coalition is now defunct) Hike took place in West Milford’s Kanouse Mountain located in the Newark Watershed lands.
Attendees of 2011 PRC Fall Hike near trail entrance off Route 23
The 1,100 foot Kanouse Mountain is located off of Route 23 North near Echo Lake Road in the Newfoundland section of West Milford. Dense woodlands surround the mountain to the north, Echo Lake is to the north east, Kanouse Brook is to the west, the Echo Lake Channel is to the east and Route 23 is to the south and southeast.
Kanouse Brook Tributary
Kanouse Brook has a naturally regenerating trout population and drains into the Pequannock River.
Attendees of the hike parked off of Old Route 23 near the NJ Transit Park & Ride and walked to the entrance of the trail off of Route 23 North near the entering Newfoundland sign.
The hike took place on unmarked wood roads starting in a northeast direction to the summit of Kanouse Mountain where a large star, American flag and outstanding views were present.
Star on top Kanouse Mountain
US Flag on top of Kanouse Mountain
View of Charlottesburg Reservoir from top of Kanouse Mountain
Views of Route 23
View of Copperas Mountain (Foreground) & Green Pond Mountain (Background)
Charlottesburg Reservoir was formed from the impoundment of the Pequannock River which is given C1 water classification. The C1 classification is used to indicate that the river is relatively unspoiled in comparison to other rivers in NJ.
As with all Pequannock River Coalition Hikes, Ross Kusher (the executive director of PRC) discussed different points of interest along the hike including ecology and geology. This interesting information makes a hike much more than a physical journey. The information provided by Ross’s expertise boosts the strength of your mind as you learn new aspects of your surroundings.
The geology of Kanouse Mountain and the surrounding highlands is estimated to be between 400-435 million years old and thought to be from the Silurian Period of the Paleozoic Era. Past glacier activity courtesy of the Wisconsin Glacier is evident by gentle slopes on the north side of the mountain and a sudden drop on the south side. As the Wisconsin glacier moved through the area 10,000 years ago it pushed rocks and carved out hillsides creating this phenomenon present throughout the highlands region.
Small trace amounts of copper have been found alongside the much more abundant iron in the highlands region. It is said that nearby Copperas Mountain was named so because of the copper that was once taken from it.
Occasionally the group came across muddy areas when the trail crossed through wetlands. These muddy spots are prime spots to look for animal prints. Ross pointed out this Eastern Coyote print found in the picture above.
The group found this Wood Frog near the trail. Though hard to tell from this photo, wood frogs generally look like they have a robber’s mask on due to the dark patch which extends backward from their eye. These frogs are often found in moist wooded areas.
American Chestnut Leaf
American Chestnut saplings were found periodically in the forest. Once a dominant tree in the forest canopy, the Chestnut blight has reduced the tree to the shrub layer. Once the American Chestnut reaches about twenty feet or so the blight strikes and kills it. The tree may die, but the root structure is still alive and sends up new sprouts. The American Chestnut Foundation is working to defeat the blight and restore its former footprint.
Kakeout Reservoir, at 150 acres, was constructed in the 1930’s by the works progress administration by impounding Stone House Brook (a Pequannock River Tributary) over an old roadway connecting Butler and Kinnelon. Most of Stone House Brook, a Pequannock River tributary, is classified by the NJ DEP primarily as 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.
Stone House Brook
Kakeout Reservoir holds up to 950 million gallons of water and serves an estimated 9,600 people in Butler, West Milford and Kinnelon. Fishing in Kakeout Reservoir is allowed by permit only.
Fishing by Permit Only
While it is possible to do a loop around the reservoir, I prefer to take the blue blazed Butler-Montville trail north of Fayson Lake Road to Kakeout dam and back. This trail is maintained by volunteers of the New York New Jersey Trail Conference.
Blue Blaze Butler-Montville Trail
If you take the Butler-Montville Trail south of Fayson Lakes Road it will lead to Pyramid Mountain and its famous Tripod Rock. Taking this trail north of Fayson Lakes Road goes slightly west with views of the reservoir and a small island.
Canada Goose on Mini Island
The trail then heads north to a bridge which goes over Stone House Brook.
Footbridge over Stone House Brook
Once you cross over Stone House Brook, the trail turns to the east and passes Kakeout Mountain to the northwest. The trail then hugs the Reservoir until you reach the dam.
Kakeout Reservoir Dam with Wetlands
There are wetlands beyond the dam where Stone House Brook once again narrows to form a stream which flows northeast. Stone House Brook (also called Kakeout Brook at this location) becomes C1 trout production from Lake Edenwold downstream. C1 is one of the highest classifications given to a stream in the state of NJ.
Once you reach the dam, turn around and follow the trail back to Fayson Lakes Road where the hike began.
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!
Echo Lake West is one of the most beautiful trails I’ve ever been on. The Echo Lake West trail follows the western shore of Echo Lake. Another trail exists (Echo Lake East) on the other side of the lake. It is not possible to do a loop around the lake due to houses located on the north eastern border of the lake. Echo Lake West follows the Highlands Trail , a NYNJCT Trail Conference project. The trail head is located at the office of the NWCDC located near Echo Lake Road.
The trail passes near Camp Watershed a summer camp for the City of Newark youth. The beginning of the trail is gravel covered but then changes to a rough nature trail.
Echo Lake is part of the Newark Pequannock watershed lands. The lake is an estimated 270 acres and is fed by the Macopin River. The Echo Lake channel and Macopin River drain from the lake and into the Pequannock River. The lake, with the exception of the northeast corner is completed surrounded by upland forest and wetlands. Kanouse Mountain sits to the west of the lake. Kanouse Mountain is around 1,100 feet in elevation.
One of the great things about hiking is you never know what is around the corner. For example, we saw this tree completely covered with claw marks and (though you can’t see it in this photo) black bear fur. Black bears do this to mark territory.
We also saw the Southern Leopard Frog pictured below. The Southern Leopard Frog is usually found near freshwater.
Flora found on the trail included:
Aside from a few muddy spots, the Echo Lake West trail is mostly dry until you reach near the end when wetlands abound.
It was near here that I found one of my favorite plants: Jewelweed
Our goal for the hike was to make it to this rock (shown below) rest a bit and head back.
However, due to what appears to be beaver activity, the old (white blazed) Echo Lake West trail which led from the Highlands Trail to this rock is impassable and the trail now ends near the wetlands section.
For me, one of the more unusual finds of the day was finding what appeared to be the shell of a freshwater clam in Echo Lake.
Freshwater Clam Shell
This trail is mostly flat and is located in the heart of the NJ highlands. For more information on Newark Watershed hiking trails and obtaining a Newark watershed permit click here.
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 2010 Pequannock River Coalition Spring Hike took place on May 2nd. The hike took place near Dunker Pond in the NJ Highlands Newark Watershed lands.
The group traveled on an old carriage road (and nope, no carriages were on it today!) which used to have cow pastures to the side. Old barb wire from over a hundred years ago was still embedded in some old shade trees on the side.
100 Year old barb wire embedded in an old shade tree