Welcome to the Pequannock River Coalition’s 2013 Spring Hike! 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) since 1995.
Meet Ross Kushner, the Executive Director of the Pequannock River Coalition. He’s going to lead the hike today!
Ross begins by explaining that the Monksville Reservoir was created in 1987 by impounding the 2.8 mile Wanaque River and the .4 mile Beech Brook (a Wanaque River tributary). The land comprising Monksville Reservoir was formerly a river valley. Dead Trees (snags) still poke through the water where dry land once existed.
Looking out at the reservoir a large white bird has caught Ross’s attention. The bird is a Mute Swan, he explains. Mute Swans originated from Europe and are not native to the US. The Mute Swan, according to legend, is silent all its life until right before it dies where the bird sings an achingly beautiful melody known as a “Swan Song“. The real story is Mute Swans are not mute but actually make a deep grunting territorial sound. Click here to hear a Mute Swan for yourself!
Standing near the reservoir Ross points to a stand of Gray Birch Trees across the water. Gray Birch is a pioneer species that is one of the first trees to grow following a disturbance and can be found growing on poor soils. Ross says we’ll see two additional species of Birch on the hike. Let’s begin!
As we walk a Tree Swallow is seen flying erratically over the water. Tree Swallows prefer inland wetland ecosystems and are among the first in the American Swallow family to migrate back after winter. You can hear a Tree Swallow Sing by clicking here!
A second after seeing the Tree Swallow a Red-Winged Blackbird makes its presence known. Red-Winged Blackbirds are usually found in wetlands such as those found in the intact woodlands surrounding Monksville Reservoir. Click here to hear a Red-Winged Blackbird!
Near the northern edge of the reservoir Ross points out an active Beaver Lodge to us. A beaver lodge is the home of the American Beaver and is created from sticks, mud and rocks. A small opening at the top of the lodge provides air.
As we walk closer to the woods we stop in front of an old Eastern Hemlock tree which has been punctured with large rectangular holes. Ross explains that these holes were created by a Pileated Woodpecker looking for one of their favorite foods: Carpenter Ants. Pileated Woodpeckers are North America’s largest living woodpecker and provided the model for the famous cartoon Woody Woodpecker. Their habitat is large mature forest such as the woods which surround Monksville Reservoir. Click here to hear a Pileated Woodpecker!
The 2,100 acre Tranquility Ridge County Park is an extension of New York’s Sterling Forest found just north of where we are now.
Entering the park we are now near the end of the green-blazed Monk’s Connector trail which connects to nearby Monk’s Mountain (part of Long Pond Ironworks State Park) with Tranquility Ridge County Park.
Barely inside Tranquility Ridge County Park, Ross has spotted our second birch: Yellow Birch. Yellow Birch prefers to grow near streams & wetlands. The tree’s characteristic peeling bark is visible to all. The hairy looking vine growing on the Yellow Birch is Poison Ivy.
Ross spots a massive tree in the distance branching out in all directions and surrounded by young trees. Ross explains that trees can only grow sideways or to the top but can’t do both. This “lone wolf” tree will eventually be crowded out by the young trees competing for sunlight.
We are now turning left on the Hasenclever Iron Trail. The creation of the six mile Hasenclever Iron Trail was first conceived in 2001 by the Friends of Long Pond Ironworks. The Hasenclever Iron Trail follows an old Woods Road which dates from the 1760’s. The road connected Long Pond Ironworks with ironworks located in Ringwood. The Friends of Long Pond Ironworks installed nine interpretive signs along the trail in 2007. The installation was funded with a grant from the NJ Recreation Trails Program. We’ll be passing by historical signs #’s 4 through 1 today.
After we cross a tributary to Beech Brook Ross tells us that Beech Brook contains a naturally occurring population of Brook Trout. We have now entered the 6,911 acre Long Pond Iron Works State Park.
We have just passed an unmarked trail to our right and historical marker #4. Marker #4 tells us that the unmarked trail leads to Beech farm which has long been abandoned.
As we walk Ross points out dirt patches in the leaf litter on the ground. This was caused by Wild Turkeys looking for food.
A turkey feather has just been found in the litter. Given all this Turkey sign Ross takes out a device which makes a female turkey sound that hunters use to attract the male turkeys (toms). Ross used the device but the Turkeys have moved on for now and we do not see any.
Ross strongly recommended not to play the device during Wild Turkey hunting season. Want to hear what a Wild Turkey sounds like? Click here to hear!
Ross has stopped at another Eastern Hemlock and says this tree has been designated a “marking tree” by an Eastern Gray Squirrel. Squirrels rub the glands found under their chin on trees as a sign of territory to other squirrels in the other area.
We are now at historical marker #3 which describes Edward Hewitt, who was a member of the last family to own most of Ringwood State Park before it became state land. The Hewitt family also owned hunting and fishing camps which were built in the area we are now standing.
This hike is taking place in early spring and the only plants we see blooming are invasive species like Japanese Barberry and Winged Euonymus (aka Burning Bush) both of which thrive in disturbed areas. Ross explains that invasive species are non-native species which lack natural predation to control their spread. As a result invasive plants crowd out native plants by forming a monoculture.
We’ve now at historical marker #2 which describes the role of limestone in iron making. Limestone was crushed and added to iron furnaces with iron ore where it acted as a fluxing agent to separate impurities from iron.
Ross has just found our third and final species of Birch: Black Birch. Black Birch twigs and bark have a strong scent of wintergreen when scraped. Ross is scraping away some the bark of a Black Birch to take a whiff. Wintergreen oil was derived from Black Birch for commercial purposes in the past.
Ross has stopped in front of an old Shagbark Hickory with an old Grape Vine wrapped around it. Only mature Shagbark Hickories (such as the one we are looking at here) have actual “shagbark”. Young trees have smooth bark. The grape vine wrapped around the Shagbark Hickory is probably as old as the tree itself. Grape Vines prefers to grow where sunshine is plentiful and prefers forest edge habitat.
After a brief climb on the Hasenclever trail we pass near wetlands to our right.
The green leaves of Skunk Cabbage are starting to poke through. Skunk Cabbage is one of the first native flowering plants and generates heat to poke through ice and snow. It generally blooms in February. Skunk Cabbage earns its name due to a foul odor emitted by torn leaves.
We’ve just reached historical marker #1 on the Hasenclever Iron Trail. This is the last marker we will see today. This marker describes Long Pond Village, a long ago industrial village that supported the nearby Long Pond Ironworks.
We are now approaching the Wanaque River. The word “Wanaque” is Native American for “place of the Sassafras Tree”. A good portion of the length of the Wanaque River is impounded to form the Monksville and Wanaque Reservoirs. Ross tells us that a bridge used to cross the Wanaque River to the old Long Pond Ironworks but was washed away when Hurricane Irene struck in 2011. The NYNJ Trail Conference is planning to rebuild the bridge in 2013.
We have now left the Hasenclever Iron trail and are turning north on the joint Sterling Ridge/Highlands Trail. The Blue-on-white 8.6 mile Sterling Ridge Trail leads to Sterling Forest State Park in New York if we kept going straight. Don’t worry! Ross has no plans to take us out of New Jersey today.
We are also sharing the same path with a section of the estimate 45 mile long interstate Highlands Trail. The Highlands Trail is a project by the NYNJ Trail Conference which highlights the unique characteristics of the Highlands region. The Highlands Trail is still a work in progress.
We are now following a tributary of the Wanaque River.
We have stopped just as we enter a cool ravine. Eastern Hemlocks favor this habitat. Indeed, Eastern Hemlocks are all around us!
What is Ross holding in his hand? It’s an old piece of iron slag left over from the iron making operations that took place here over a hundred years ago.
We are heading briefly off the marked trail and walking towards the Wanaque River. The segment of the Wanaque River seen here is draining Greenwood Lake. What a great spot for lunch! After resting we continue to walk leaving the Wanaque River and following a tributary stream.
Tulip Trees grow straight and narrow with fissured bark. The tree’s leaves actually look like Tulip Flowers! It flowers in Mid-May to early June.
We are now walking northeast on an unblazed woods road. This is the same woods road we passed to our right when we first started out on the Hasenclever Iron Trail.
As we walk, we pass a deep impression in the ground to our left. The impression is a remnant of the Patterson Mine. The Patterson Mine last saw operation at the end of the 1800’s. Ore from the Patterson Mine was sold to the local market or supplied ironworks found in the area.
Check out the abandoned motorcycle to our right! It’s pretty old but it is still standing.
Off to the left of the woods road is a vernal pond. Vernal ponds are temporary pools of water that are free of fish and provide valuable areas for amphibians such as Wood Frogs to lay eggs. Wood Frogs are found further north than any other species of frog. Ross explains that the theory is this: water found in cells will expand to the point of explosion when frozen. Wood frogs have found a way to move water molecules outside their cells when they get frozen to prevent this from happening.
We’ve just turned right on another unmarked trail following Beech Brook to our right. Ross suddenly stops. He’s found a Red Velvet Mite! Red Velvet Mites live in the soil and eat fungi and bacteria. Red Velvet Mites are harmless to humans and are part of the arachnid family (the same family spiders belong to).
Well, we’ve arrived back at the gate and back at our cars! What a great hike!
Want to check out this hike for yourself? Here are the directions to the parking lot where the hike begins!
Take exit 57 on Rt. 287 to Skyline Drive. Follow Skyline 5 miles north to Greenwood Lake Turnpike. Make a right there onto Greenwood Lake Turnpike and follow it about 4 miles to a right on Beech Road. Look for a gravel parking area at the reservoir on the left.
Check out Plant Communities of New Jersey.
NJ’s geology, topography and soil, climate, plant-plant and plant-animal relationships, and the human impact on the environment are all discussed in great detail. Twelve plant habitats are described and the authors were good enough to put in examples of where to visit!
Click here for more information!
Don’t miss The Highlands: Critical Resources, Treasured Landscapes! The Highlands exemplifies why protection of New Jersey’s Highlands is so important for the future of the state. It is an essential read on the multiple resources of the region.
Click here for more information!
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
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 classified Pequannock 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.
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.
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.
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.
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.
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.
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!
The western view is continuous as we continue south and pass an interesting balanced boulder with the White Trail Blaze painted on it.
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!
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!
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.
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.
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).
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!
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.
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 e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
HELP SPREAD THE WORD ABOUT SILAS CONDICT COUNTY PARK ON FACEBOOK, TWITTER AND OTHER SOCIAL MEDIA BY CLICKING A BUTTON BELOW!!
The Great Swamp Outdoor Education Center (GSOEC) consists of a 44 acre portion of the Great Swamp managed since 1963 by the Morris County Parks Department. The GSOEC hosts guided nature walks, school, scout and public educational programs.
The GSOEC hosts periodic studies of the flora and fauna to determine the overall health of the Great Swamp.
The estimated 7,768 acre Great Swamp National Wildlife Refuge (GSNWR) abuts the GSOEC to the west. The GSNWR is one of 553 refuges administered by the Department of the Interior’s U.S. Fish and Wildlife Service. Lands comprising a National Wildlife Refuge are managed for the protection of wildlife and its habitat.
History of the Great Swamp
The origin of the Great Swamp begins with the melting and subsequent retreat of the Wisconsin Glacier around 25,000 years ago. Debris from the glacier blocked the passage of an ancient river creating an enormous lake known as Lake Passaic. Lake Passaic is thought to have been 30 miles long and 10 miles wide. Over time, an outlet was formed near Little Falls NJ draining the lake via the Passaic River. This drainage is still occurring today. Today the Great Swamp forms a remnant component of the once great Lake Passaic.
In the late 1950’s the area now known as the Great Swamp was identified by the NYNJ Port Authority as an ideal location for a new jetport. The Great Swamp Conservation Foundation mobilized volunteers to protect the Great Swamp. The result was the establishment of the Great Swamp National Wildlife Refuge. The Great Swamp Conservation Foundation later became the North Jersey Conservation Foundation and then finally known as New Jersey Conservation Foundation.
GSOEC features four short loop trails. Two of the four trails (Orange & Red) are interpretive and follow 16 markers listed in a self guided trail booklet available at the education center. Click here for a trail map!
The total length of the trails is 1.4 miles.
Ready to take a virtual tour of the Great Swamp Outdoor Education Center? Let’s Go!
Stop by the kiosk near the parking lot to pick up a trail map. From the kiosk, head to the education center to view the exhibits on the flora and fauna of the Great Swamp.
After checking out the exhibits inside, it’s time to start our hike.
Let’s begin our virtual hike by taking the Orange Blazed trail located to the south of the education center. The Orange Trail at .61 Miles is the longest trail present in the GSOEC. It contains Markers 1-10 from the self guided trail.
The first marker, regarding the Red Maple tree, appears shortly after the beginning of the orange trail. Red Maple is the most common tree in the Great Swamp as well as the eastern deciduous forest.
Red Maple’s flowers are red in the spring and the leaves turn a brilliant red in the fall. Though the Sugar Maple may come to mind when it comes to maple syrup, Red Maple can be tapped for syrup as well. Red Maple should be tapped before budding occurs as the buds change the chemical makeup of the syrup.
Continuing on the orange trail, marker #2 comes into view on the right where a large depression may be found.
The large depression is known as a vernal pond. Vernal ponds do not support fish and may be dry or filled with water. Due to the lack of predators (i.e. fish) the vernal pond provides a safe haven for amphibians such as Wood Frogs, Spring Peepers and Blue-Spotted Salamanders among other species to breed and lay eggs. Continuing past the vernal pond, two fenced areas appear shortly after on the left.
Marker # 3 explains that these sections of the GSOEC were fenced in 2009 to study how plant communities recover from the damage caused by an overpopulation of white tail deer.
Marker #4 describes an Ecotone. An Ecotone is anywhere two habitats meet and create an edge. The Ecotone present here was created by the Power line right of way. The positive aspects of this man-made Ecotone is the creation of suitable nesting habitat for the local turtle population in addition to providing a valuable hunting ground for birds of prey. On the flipside, the disturbed ground caused by the creation of the power lines have provided ideal habitat for invasive plants as Autumn Olive, Multiflora Rose, Garlic Mustard, Wineberry & Japanese Barberry.
Continuing in a southwest direction, the dirt path changes to a boardwalk as the trail traverses the wetland area.
A short boardwalk appears to the right of the main boardwalk which leads to the Pond which is marker #5.
Ponds are usually less than 18 feet deep. Eventually as plant matter and other organic material decays, the pond will begin to become a marsh, progress to a forested wetland and finally upland habitat after many years.
The Pond at GSOEC is manmade and provides habitat for Eastern Painted Turtles, Snapping Turtles, Wood Ducks, Mallards, Belted Kingfisher and River Otters among others. Flora of the Pond includes Yellow Flowered Spatterdock & Duckweed.
Continuing on the trail leads to Marker #6 which describes Poison Ivy which is seen here growing as a hairy vine. Poison ivy contains a clear liquid known as urushiol which causing a burning itching rash in many people. In addition to a hairy vine Poison Ivy can be found as a shrub reaching over three feet tall or as a trailing vine on the ground.
Several rhymes exist warning of the dangers of Poison Ivy:
“Leaves of three, let them be”
“Hairy rope, don’t be a dope”
“Hairy vine, no friend of mine”
Despite the negative publicity this native plant receives, Poison Ivy has tremendous value for wildlife. Native birds such as Eastern Bluebird, Gray Catbird, Dark Eyed Junco and Northern Flicker eat Poison Ivy’s white berries. Mammals such as White-Tail Deer and Eastern Cottontail consume Poison Ivy’s leaves.
At this point of the hike you may notice abundant Mountain Laurel. Marker # 7 appears here.
Its purpose is to briefly touch upon “the browse line”. The over abundant white- tail deer have stripped all leaves of vegetation from six feet down. If the current trend continues, there may not be a forest here in the future.
From this area, the trail head of the .23 of a mile Blue trail loop appears.
Let’s take a brief break from the interpretive trail to explore this short trail.
The Blue Trail Loop goes through an upland area consisting of mostly Mountain Laurel and Swamp Chestnut Oak.
The trail encircles a small vernal pond (the vernal pond, seen here at the end of September 2012 was dry).
Completing the Blue Trail Loop, head back to the Orange Trail and to Marker # 8 which describes the function of a rotting log in the forest.
Standing dead trees or snags play an important role in the eastern deciduous forest. Woodpeckers including Pileated, Downy and Red-Bellied among others excavate holes in the dead trees searching for tasty insects. These excavated holes in turn create habitat for birds including Black-Capped Chickadee. Fungus will usually invade the dead wood further softening it. Eventually, the tree will fall to the forest floor where it will continue to decay creating a rich organic soil which will support future species of trees.
Proceed east to Marker # 9 The Phragmites Marsh. Phragmites (aka Giant Reed) is a giant species of grass which can grow from 10-20 feet. Phragmites thrives in disturbed areas. Phragmites found in the Great Swamp are native to the eastern deciduous forest. Phragmites are considered invasive because of its aggressive growth and tendency to overwhelm all other vegetation.
From here the trail leaves the boardwalk and heads south to marker # 10 which passes an outdoor study area and leads to a Wigwam replica.
The Lenape Native Americans (the original people) created Wigwams as shelter from saplings, tree bark and Cattail Mats among others. This replica would have been big enough for two people. Marker #10 is the last marker for the orange trail.
After heading back from the Wigwam, turn right on the Orange Trail and follow the trail a brief distance to its terminus.
The “Prayer of the Woods” sign is found right before the start of the Red Trail. After reading the Prayer and taking in its message, turn right to start hiking the .39 mile Red Trail to continue the interpretive trail.
The first marker on the Red Trail is #11 which identifies trees found in the Eastern Deciduous Forest.
Trees found in the Eastern Deciduous Forest include the below among others:
The term “deciduous” indicates that the trees comprising this type of forest lose their leaves each fall and grow new leaves in the spring.
Continuing on the red trail leads Marker #12 “Transmission Lines and Marsh”.
Here, vegetation is periodically removed or trimmed back so as to not interfere with the power lines. This wet marsh provides habitat to Wood Ducks, Mallards, Muskrats and Red-Wing Blackbirds among others.
From here turn left at the sign leading to the education center to go to Marker # 13.
The Red Trail approaches Marker #13 as it crosses a stream.
Sediments and rocks on the stream bottom provides habitat for a variety of Crayfish and Macro-invertebrates. Marco-invertebrates lack backbones and can be seen without the aid of a microscope. Certain macro-invertebrates such as Caddisflies are pollutant intolerant. Presence of pollutant intolerant macro-invertebrates are one way to indicate the health of a stream. Macro- invertebrates eat many different things depending on the species-there are predators, scavengers, and herbivores among them. In turn, macro-invertebrates are a source of food for various turtles, fish and frogs.
Continuing on the red trail leads to Marker #14 which discusses“The Wet Meadow”. The Wet Meadow is a man-made habitat created by a power-line cut and is home to field mice, star-nosed moles and various hawks & owls among others.
Marker #15 leads to an American Beech Tree. The smooth gray bark of the American Beech Tree usually invites individuals to carve their names and other messages into the trunks. Carving in a tree trunk is similar to a cut on your finger. However, unlike your injured finger, a tree cannot put a band-aid on its wound. The carved bark is an open door for disease.
Beechdrops, seen here in this picture, lack both leaves and chlorophyll and is a parasitic plant of the American Beech Tree.
#16 The Swamp
The final marker on the red trail briefly discusses the importance of the Great Swamp. The land comprising the Great Swamp is a mix of meadows, upland woods, marsh and brush covered swamps. Only 40% of the Great Swamp is wet either part of the year or all year long whereas 60% of the Great Swamp consists of upland forest & meadows.
You are now at the end of the Red Trail.
At the end of the red trail head north to catch the beginning of the short .20 of a mile Green Trail near the parking area. The Green trail traverses in a short loop in an upland portion of the GSOEC.
Check out these mushrooms found growing in September 2012!
In the parking area near the end of the Green Trail you may notice a black box hanging from a tree. The Black boxes are used to detect for the presence of the Asian Long-Horn Beetle, an invasive species from Asia.
After the Green Trail is complete, it’s time to visit the Observation Blind located off the parking lot which views the Pond looking west.
This concludes our virtual hike! I hope you enjoyed it and it inspired you to take a trip to see the GSOEC for yourself!
Click here for directions!
Feel free to e-mail NJUrbanForest at NJUrbanForest@gmail.com with any comments, memories or suggestion! Thank you and have fun exploring!
HELP SPREAD THE WORD ON THE MORRIS COUNTY GREAT SWAMP OUTDOOR EDUCATION CENTER ON FACEBOOK, TWITTER AND OTHER SOCIAL MEDIA BY CLICKING ONE OF THE BUTTONS BELOW!!
The 2011 Pequannock River Coalition Fall Hike took place in West Milford’s Kanouse Mountain located in the Newark Watershed lands. The mountain is part of West Milford’s baker’s dozen-a series of mountains you can hike in West Milford.
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 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.
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 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 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.
Other flora found includes these among others:
- Quaking Aspen
- White Oak
- American Beech
Ross explained that Black Bears love the fruits of Shadbush. He once tasted the berries and compared them to wet cardboard. White Oak Ross said was cherished by wildlife for its sweet acorns.
The hike was an estimated six miles and went in a loop fashion so that attendees came out the same way the came in. What a great fall hike!
The Pequannock River Coalition holds three hikes a year (Fall, Winter and Spring). They are worth checking out!
Remember, to hike in the Newark Watershed land a permit is required. For more information on obtaining a Newark watershed permit click here.