The 22 acre Swan Lake was created by impounding a tributary of the Pocantico River (a tributary of the Hudson River).
Carriage Road Rockefeller State Park Preserve
The carriage roads we will be walking on were developed by John D Rockefeller Sr & John D Rockefeller Jr between the years 1910-1950. Every winter the Friends of the Rockefeller State Park Preserve evaluates which trails need fresh surface material added. Drainage of trails is completed every spring to ensure carriage roads stay dry. Trail maintenance is a 12 month process!
After paying the minimal parking fee ($6 at the time of this writing in 2013) let’s walk over to the visitor center.
After picking up a trail map let’s check out the interesting flowering plants blooming nearby. These flowers are Japanese Peony and are known as the “King of Flowers” in Japan.
Just past the flowers and the visitor center there is a kiosk chock full of information about the Rockefeller State Park preserve.
Birds and Wildflowers of the Preserve
Here we can find excellent information regarding common flora and fauna of the preserve. All set? Let’s head towards Swan lake!
Leaving the Fern Garden we follow a brief trail through a forest to get to Brother’s Path.
We are going to be following the 1.1 mile Brother’s Path which encircles Swan Lake. As we start out heading south on the Brother’s Path, the trailhead of the .7 mile Overlook Trail appears to our right.
Let’s take a quick detour from Brother’s Path to walk a section of the Overlook Path for a few minutes. According to the Hudson River Audubon Society website this area is one of the best spots to view Eastern Bluebirds. Eastern Bluebirds, New York’s state bird, are a small thrush whose habitats include open woodlands and meadows such as where we are right now. Eastern Bluebird populations have experienced a decline due to strong competition from aggressive non-native birds like the House Sparrow and European Starlings.
Eastern Blue Bird (NY’s State Bird!)
As we ponder the future fate of these birds a blue blur flies by and lands on a nesting box which has been placed in the meadow by a member of the Rockefeller State Park Preserve staff. Ready to head back to the Brother’s Path? Let’s head back to continue our journey around Swan Lake. Heading south on Brother’s Path we see continuous views of Swan Lake mixed with occasional Flowering Dogwood to our left.
Flowering Dogwood, native to the eastern United States, is a common understory tree found in forest edges.
Rockefeller State Park Preserve Meadow
Continuing south an opening has appeared to our right providing a view of the sweeping meadows we sampled on the Overlook Trail. As we walk Swan Lake is becoming narrower. Turning east we cross over two Pocantico River tributaries draining Swan Lake.
I’m not sure if the chipmunk is sounding the alarm over us or this Northern Black Racer lurking nearby. Maybe both?
As we leave the chipmunk and snake we hear a sudden “meow” sound and realize that the sound is not coming from a cat but a bird! The bird is a Gray Catbird. Gray Catbirds are migratory and fly to the southeaster US, Mexico and Central America for the winter months.
Continuing north and passing the trailhead to the Ridge Trail, we spot some Striped Wintergreen, a species which is considered vulnerable in New York.
Mallards near Swan Lake
We cross over a Swan Lake feeder stream and pass a couple of Mallards and a turtle as we head west on the Brothers Path back to the parking lot to complete our hike. I hope you enjoyed this virtual tour of Swan Lake and that it inspired you to visit it for yourself!
2) The Nature of New York – This work offers a sweeping environmental history of New York State. Author David Stradling shows how New York’s varied landscape and abundant natural resources have played a fundamental role in shaping the state’s culture and economy.
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. 2019 Update: Pequannock River Coalition has dissolved.
Ross Kushner Executive Director Pequannock River Coalition
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.
Pileated Woodpecker Holes
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. The 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!
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.
Yellow Birch Wolf Tree
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.
On Hasenclever Iron Trail
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.
Beech Brook Tributary
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.
Beech Farm Information
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.
Wild Turkey Sign
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 Kushner with Turkey Call
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 Kushner Squirrel Markings
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.
Edward Hewitt Interpretive Signage
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.
Ross Kushner discussing invasive plants
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.
Limestone Interpretive Signage
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 Kushner Black Birch
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.
Shagbark Hickory Grape Vine
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.
Hasenclever Iron Trail #1 Interpretive Signage
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 rebuilt the bridge in 2013.
Sterling Ridge Trail Blaze
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.
Highlands Trail Blaze
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!
Ross Kushner Iron Slag
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.
Tributary Stream Crossing
Crossing the tributary on rocks we pass the Yellow Blazed Jennings Hollow Trailhead to our left and are now stopped at the base of a Tulip Tree.
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.
Red Velvet Mite
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!
Monksville Reservoir Near the Parking Lot
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.
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 the Hart’s Brook Nature Preserve! The preserve features woodlands and wetlands, a master garden and hiking trails. Prior to becoming a preserve the property was known as the Gaisman Estate and was owned by the inventor of the famous Gillette safety razor blade Henry Gaisman. In 1957, Gaisman passed the title of the estate to the New York Archdiocese. In later years, Marion Woods Convent took ownership of 11.5 acres of the estate. The remaining acreage was purchased by the State of New York (who retains 50% ownership of the property) Westchester County and the Town of Greenburgh in 1999.
Hart’s Brook Nature Preserve
Harts Brook Nature Preserve Trail Map
Welcome to our virtual hike! Today we are going to cross brooks, pass interesting rock outcroppings and walk around 2 miles on 5 different trails! Our guide will be the trail map shown above.
Red Trail Meadow
Ready to start? From the parking area, let’s head west briefly entering the forest on the red trail. Paralleling Ridge Road, the Red Trail leaves the forest and walks through an open meadow flanked by enormous Norway Spruce trees.
Norway Spruce Red Trail
As we walk past the Norway Spruce trees we pass a spur of the red trail to our left which leads back to the parking lot. Deciduous wooded wetlands are appearing to our right as we leave the meadow and re-enter the woods. Wait! What’s that sound? Spring Peepers! Spring Peepers are a small frog common in wetlands and are among the first frogs to call out in early spring. Thus, Spring Peepers are a true harbinger of spring! Their Latin name (Pseudacris Crucifer) is named because of a dark cross which forms an “x” on the frog’s dorsa. Because of their size, Spring Peepers are difficult to locate and we do not see any today.
Green Trail Blaze
Continuing south we have come to the end of the red trail and are at an intersection with the green trail. According to our trail map we will come to a pond if we head east on the Green Trail.
Going to the Pond
Let’s go east on the green trail and check it out. After only a few minutes of walking we’ve found that we have left the green trail and are now on the yellow trail. The flora is quickly changing from deciduous forest to evergreens consisting of stately Eastern Hemlocks and Rosebay Rhododendron the closer we get to the pond.
The Hemlocks have an overall healthy appearance with very little die-back from the Hemlock Wooly Adelgid. The Hemlock Wooly Adelgid is an exotic pest from Asia 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.
Yellow Trail Bridge
Crossing a wooden bridge over Harts Brook we come to a bench overlooking the pond and its outflow dam.
Yellow Trail Bench with view of Pond
Let’s pause for a few moments and take in the beauty of our surroundings.
Hart’s Brook Park Pond
After taking in the view of the pond we’re going to continue northeast on the yellow trail following the shore of the pond. As we walk we pass several Wood Duck nesting boxes.
As we continue walking on the yellow trial we pass an old stone warming house which was part of the original Gaisman Estate. Leaving the stone warming house, the yellow trail is taking us east back to a branch of the green trail.
Heading south on the green trail we find ourselves on an orange blaze trail heading east.
Rock Outcrop Orange Trail
An interesting large rock outcrop appears to our left as we slightly climb on the orange trail.
We are now at an intersection with the blue blazed trail and it sounds like we are hearing more music of spring!
American Robins are searching for lunch and making sure we know they are present.
Blue Trail Stream Crossing
Heading east on the blue trail we find ourselves crossing a brook.
Pine Grove Blue Trail
Passing close to private residences the blue trail turns northeast and slightly climbs through a grove of White Pine trees.
As we pass a spur of the blue trail on the left the trail now becomes an asphalt path as we come close to the Maple Avenue entrance to the preserve. From here we follow the blue trail west back to the orange trail.
Blue Trail Stream Crossing as seen from Orange Trail
The stream crossing we did earlier on the blue trail is visible to our left.
We are now back at the Green Trail we left a while back. Let’s head north which will take us back to the yellow trail.
After only a short distance on the yellow trail we have just stepped out of the woods and are by the master garden area of the preserve. We are now back at the parking lot where we began. Thank you for joining me today on this virtual hike! I hope it has inspired you to check out Hartsbrook Nature Preserve for yourself!
The preserve is located at 156 Ridge Road, Hartsdale, NY.
Silas Condict Park was dedicated at 200 acres in 1964. In 2005, additional purchases of adjacent land brought the total acreage to 1,581. The centerpiece of the park is Canty’s Lake which is formed from an impoundment of a Stone House Brook tributary (which itself is a tributary of the C1 classifiedPequannock River, one of the cleanest rivers in New Jersey)
Silas Condict Park White Trail Virtual Tour
Today we are going to explore the Bear Mountain area in the southern section of Silas Condict Park via the estimated 3 mile White Blazed Trail (aka “the Bear Trail”) following the below trail map (taken from the NYNJ Trail Conference).
Ready? We’ll begin our hike by following Canty’s Lake which will be to our left as we walk north from the parking area. Before we go any further let’s see what’s hanging around Canty’s Lake.
We got company! Ring-Necked Ducks! You would think this duck would be called the Ring-Billed Duck due to a white band around its beak but the duck actually has a chestnut colored ring around its neck which is only visible at close range.
While we are chatting about Ring-Necked Ducks a bird just flew by with white tail feathers. It’s a Dark-Eyed Junco! Dark-Eyed Junco belongs to the Sparrow family and prefers forest and shrub lands. The Dark-Eyed Junco stays in New Jersey for the winter and migrates further north during the growing season.
White Trail Trailhead (Near Canty Lake)
Leaving the shore of Canty’s Lake we walk a bit north and find ourselves in front of the White Trail trail-head. We are going to be following the white trail in a loop fashion. Nice! Loop trails are always my favorite.
Silas Condict County Park Forest
Let’s enter the forest and leave civilization behind for a bit.
Mountain Laurel greets us as soon as we enter. The deciduous forest of winter is primarily colorless other than evergreen shrubs such as Mountain Laurel and the American Beech tree. American Beech (particularly young American Beech) hold onto their leaves until spring when new leaves emerge. As we walk we hear the paper like leaves blowing in the wind.
We are proceeding in a southwest direction and climbing in a zig-zag fashion on the White Trail. American Crows are sounding the alarm that we are in their forest. White-Breasted Nuthatches and Tufted Titmouse are having their own conversations as we start to climb on the trail.
East Facing View
We’ve come to the first viewpoint! Here, we are looking east. Though it’s covered with snow, we can take a seat if we want to rest after our brief climb to this view. After taking in the views we descent passing interesting rock formations.
Numerous fresh blow-downs are present throughout the forest which most likely fell during Hurricane Sandy.
Newly Created Vernal Pond Habitat
We may feel sad seeing big trees toppled over but the good news is the hollowed out area where the root structure was now becomes prime vernal pond habitat. Vernal ponds are temporary pools of water that are free of fish and provide valuable areas for amphibians such as Wood Frog to lay eggs.
As we walk Mountain Laurel becomes abundant with adjacent Chestnut Oak.
Chestnut Oak Mountain Laurel
Proceeding through the Mountain Laurel, we have entered a Chestnut Oak forest punctured here and there with Pitch Pine, a tree normally associated with the NJ Pine Barrens.
Pitch Pine grows here on thin, dry and generally infertile soil. These Pitch Pines found on this mountain are exposed to frequent ice storms in winter and strong winds year round.
Chestnut Oak is usually found on dry slopes at high elevations such as where we are right now. Shrubs such as lowbush blueberry and black huckleberry are common in Chestnut Oak forests. However, given we are in late winter, the only shrub we are encountering today is the abundant evergreen Mountain Laurel.
We’ve now started our second climb up a snow covered path.
Our efforts are rewarded with a wonderful western view of the NJ Highlands!
Pitch Pine Western View
The western view is continuous as we continue south and pass an interesting balanced boulder with the White Trail Blaze painted on it.
Balanced Rock with White Trail Blaze
We now start to descend as the trail turns east. It’s a bit tricky going down the snowy trail so be sure to watch your step!
White Trail Blaze leading to Rock Tunnel
As we continue to follow the White Trail we find it is leading us to a rock tunnel.
Let’s squeeze through to the other side!
Looking back at Rock Tunnel
Whew! We made it out! But now we have to watch our footing. We have a snow covered boulder field to walk through!
As we carefully meander through the boulder field we find ourselves following the White Trail on a slippery rock outcrop.
Whoops! We slipped!
Thankfully we’re ok.
Let’s brush ourselves off and keep moving-that Turkey Vulture flying over us seems to have ideas about us.
Trout Brook Stream Crossing
We’ve now arrived at Trout Brook and its surrounding wetlands. Trout Brook drains Canty’s Lake and is a tributary to Stone House Brook. Let’s carefully cross the stream by jumping on rocks.
Bridge over Trout Brook
As we continue on the White Trail we have yet another crossing of Trout Brook-but this time there’s a brand new wooden bridge present which makes for easy walking.
As we leave the bridge we see a massive rock outcrop before us and see the White Trail Blaze lead straight up the outcrop! Let’s watch our step and climb.
At the top we find we have left the footpath and are now following a gravel road (steep in places).
Albino White-Tailed Deer
As we walk we are suddenly surprised by a blur of white! An Albino White-Tailed Deer! The deer is so white it matches the snow around. Amazing!
Bear Mountain Silas Condict County Park
Leaving the deer and the gravel road we are back on a foot path where we see views of Bear Mountain, which we just finished climbing.
Canty’s Lake View from the White Trail
Continuing on a little further we now find a bench with a wonderful view of Canty’s Lake. We are almost at the end!
We did it! We are now at the end of the White Trail back at the parking lot near where we started!
I hope you enjoyed this virtual hike and that it inspired you to check out the hike in person!
Silas Condict Park is located at 100 Kinnelon Road, Kinnelon, NJ.
Check out some great books below to learn more about NJ’s plants and wetlands!
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.
The Great Swamp Outdoor Education Center (GSOEC) consists of a 44 acre portion of the Great Swamp managed since 1963 by the Morris County Parks Department. The GSOEC hosts guided nature walks, school, scout and public educational programs.
Herp Study in Progress
The GSOEC hosts periodic studies of the flora and fauna to determine the overall health of the Great Swamp.
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.
Outdoor Education Nature Center with Kiosk
Mammals of The Great Swamp
Endangered in New Jersey
After checking out the exhibits inside, it’s time to start our hike.
Orange Trail Trailhead
Let’s begin our virtual hike by taking the Orange Blazed trail located to the south of the education center. The Orange Trail at .61 Miles is the longest trail present in the GSOEC. It contains Markers 1-10 from the self guided trail.
The first marker, regarding the Red Maple tree, appears shortly after the beginning of the orange trail. Red Maple is the most common tree in the Great Swamp as well as the eastern deciduous forest.
Red Maple Leaves
Red Maple’s flowers are red in the spring and the leaves turn a brilliant red in the fall. Though the Sugar Maple may come to mind when it comes to maple syrup, Red Maple can be tapped for syrup as well. Red Maple should be tapped before budding occurs as the buds change the chemical makeup of the syrup.
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 with Deer Enclosure in background
Marker # 3 explains that these sections of the GSOEC were fenced in 2009 to study how plant communities recover from the damage caused by an overpopulation of white tail deer.
Marker 4 EcoTone
Marker #4 describes an Ecotone. An Ecotone is anywhere two habitats meet and create an edge. The Ecotone present here was created by the Power line right of way. The positive aspects of this man-made Ecotone is the creation of suitable nesting habitat for the local turtle population in addition to providing a valuable hunting ground for birds of prey. On the flipside, the disturbed ground caused by the creation of the power lines have provided ideal habitat for invasive plants as Autumn Olive, Multiflora Rose, Garlic Mustard, Wineberry & Japanese Barberry.
Marker 5 The Pond
Continuing in a southwest direction, the dirt path changes to a boardwalk as the trail traverses the wetland area.
Orange Trail Boardwalk
A short boardwalk appears to the right of the main boardwalk which leads to the Pond which is marker #5.
Ponds are usually less than 18 feet deep. Eventually as plant matter and other organic material decays, the pond will begin to become a marsh, progress to a forested wetland and finally upland habitat after many years.
Continuing on the trail leads to Marker #6 which describes Poison Ivy which is seen here growing as a hairy vine. Poison ivy contains a clear liquid known as urushiol which causing a burning itching rash in many people. In addition to a hairy vine Poison Ivy can be found as a shrub reaching over three feet tall or as a trailing vine on the ground.
Several rhymes exist warning of the dangers of Poison Ivy:
At this point of the hike you may notice abundant Mountain Laurel. Marker # 7 appears here.
Marker 7 The Browse Line
Its purpose is to briefly touch upon “the browse line”. The over abundant white- tail deer have stripped all leaves of vegetation from six feet down. If the current trend continues, there may not be a forest here in the future.
From this area, the trail head of the .23 of a mile Blue trail loop appears.
Blue Trail Trailhead
Let’s take a brief break from the interpretive trail to explore this short trail.
Blue Blaze Swamp Chestnut Oak
The Blue Trail Loop goes through an upland area consisting of mostly Mountain Laurel and Swamp Chestnut Oak.
Dried Vernal Pond Blue Trail
The trail encircles a small vernal pond (the vernal pond, seen here at the end of September 2012 was dry).
Blue Trail trailend
Completing the Blue Trail Loop, head back to the Orange Trail and to Marker # 8 which describes the function of a rotting log in the forest.
Standing dead trees or snags play an important role in the eastern deciduous forest. Woodpeckers including Pileated, Downy and Red-Bellied among others excavate holes in the dead trees searching for tasty insects. These excavated holes in turn create habitat for birds including Black-Capped Chickadee. Fungus will usually invade the dead wood further softening it. Eventually, the tree will fall to the forest floor where it will continue to decay creating a rich organic soil which will support future species of trees.
Marker 9 Phragmites Marsh
Proceed east to Marker # 9 The Phragmites Marsh. Phragmites (aka Giant Reed) is a giant species of grass which can grow from 10-20 feet. Phragmites thrives in disturbed areas. Phragmites found in the Great Swamp are native to the eastern deciduous forest. Phragmites are considered invasive because of its aggressive growth and tendency to overwhelm all other vegetation.
Outdoor Study Area
From here the trail leaves the boardwalk and heads south to marker # 10 which passes an outdoor study area and leads to a Wigwam replica.
The Lenape Native Americans (the original people) created Wigwams as shelter from saplings, tree bark and Cattail Mats among others. This replica would have been big enough for two people. Marker #10 is the last marker for the orange trail.
Orange Trail Trailend
After heading back from the Wigwam, turn right on the Orange Trail and follow the trail a brief distance to its terminus.
Prayer of the Woods
The “Prayer of the Woods” sign is found right before the start of the Red Trail. After reading the Prayer and taking in its message, turn right to start hiking the .39 mile Red Trail to continue the interpretive trail.
Red Trail Trailhead
The first marker on the Red Trail is #11 which identifies trees found in the Eastern Deciduous Forest.
Marker 11 Deciduous Forest
Trees found in the Eastern Deciduous Forest include the below among others:
From here turn left at the sign leading to the education center to go to Marker # 13.
Marker 13 Stream
The Red Trail approaches Marker #13 as it crosses a stream.
Red Trail Stream Crossing
Sediments and rocks on the stream bottom provides habitat for a variety of Crayfish and Macro-invertebrates. Marco-invertebrates lack backbones and can be seen without the aid of a microscope. Certain macro-invertebrates such as Caddisflies are pollutant intolerant. Presence of pollutant intolerant macro-invertebrates are one way to indicate the health of a stream. Macro- invertebrates eat many different things depending on the species-there are predators, scavengers, and herbivores among them. In turn, macro-invertebrates are a source of food for various turtles, fish and frogs.
Marker #14 The Wet Meadow
Continuing on the red trail leads to Marker #14 which discusses“The Wet Meadow”. The Wet Meadow is a man-made habitat created by a power-line cut and is home to field mice, star-nosed moles and various hawks & owls among others.
Marker #15 American Beech
Marker #15 leads to an American Beech Tree. The smooth gray bark of the American Beech Tree usually invites individuals to carve their names and other messages into the trunks. Carving in a tree trunk is similar to a cut on your finger. However, unlike your injured finger, a tree cannot put a band-aid on its wound. The carved bark is an open door for disease.
Beechdrops, seen here in this picture, lack both leaves and chlorophyll and is a parasitic plant of the American Beech Tree.
#16 The Swamp
Marker #16 The Swamp
The final marker on the red trail briefly discusses the importance of the Great Swamp. The land comprising the Great Swamp is a mix of meadows, upland woods, marsh and brush covered swamps. Only 40% of the Great Swamp is wet either part of the year or all year long whereas 60% of the Great Swamp consists of upland forest & meadows.
Red Trail End
You are now at the end of the Red Trail.
Green Trail Blaze
At the end of the red trail head north to catch the beginning of the short .20 of a mile Green Trail near the parking area. The Green trail traverses in a short loop in an upland portion of the GSOEC.
Mushrooms Green Trail
Check out these mushrooms found growing in September 2012!
Asian Long Horn Beetle Detector
In the parking area near the end of the Green Trail you may notice a black box hanging from a tree. The Black boxes are used to detect for the presence of the Asian Long-Horn Beetle, an invasive species from Asia.
After the Green Trail is complete, it’s time to visit the Observation Blind located off the parking lot which views the Pond looking west.
Turtles on the Pond from Wildlife Blind
This concludes our virtual hike! I hope you enjoyed it and it inspired you to take a trip to see the GSOEC for yourself!
Torne Mountain, standing at 1,120 feet and located in Passaic County NJ, is situated in the southern section of the estimated 4,982 acre Norvin Green State Forest. The land comprising the forest was donated to the State of New Jersey by the nephew of Ringwood Manor’s Abram S. Hewitt in 1946.
Torne Mountain Norvin Green State Forest
Norvin Green State Forest has the largest concentrations of trails in the state of NJ. Most of the trails date back to the 1920’s when members of a local organization known as the Green Mountain Club constructed them.
NJ Highlands Geology
Many of the rocks that are encountered during this hike have a rounded appearance due to the Wisconsin Glacier which came through the area around 10,000 years ago. This event is relatively recent as the Highlands rocks were formed over four billion years ago.
The rocks are “basement rocks” as the younger rocks which originally had covered them eroded away over time. Most of the rocks are thought to be comprised of ancient granite-gneiss.
Below is a brief virtual tour of a section of the 0.4 of a mile Torne Trail and a portion of the 6.4 mile Blue Blazed Hewitt-Butler Trail. Stops include outstanding views and an interesting man-made Stone Living Room. Ready? Let’s do it!
The hike is an estimated 1.5 miles from Otter Hole Road.
Entrance to Torne Trail
Starting from near the Otter Hole Road Parking area, head south to the trailhead of the red blazed Torne Mountain Trail.
To the Blue Trail (Hewitt-Butler Trail)
Once on the Torne trail, signs advertising the blue-blazed Hewitt-Butler Trail will appear.
Hewitt Butler Trail Blaze
Head southwest then south on the blue blazed Hewitt-Butler Trail to Climb Torne Mountain.
Near the western viewpoint, a short unmarked trail appears to the left leading to a man-made Stone Living Room. “Chairs” & “Sofas” have been constructed from surrounding rocks. The Stone Living Room is an excellent place to stop for lunch and rest while taking in views.
View from Stone Living Room
From the Stone Living Room, head back to the Hewitt Butler Trail. Continuing south, descend Torne Mountain passing a stand-alone Stone chair.
Here you will reach a ravine at the bottom of Torne mountain and the southern trailhead of the red blazed Torne Trail which will be your return back to Otterhole Road.
Rocky Ravine Torne Trailhead
For now, pass the southern trail-head of the Torne Trail and continue southeast on the blue blazed Hewitt-Butler trail climbing to Osio Rock.
From here, views of the Wanaque Reservoir, the NYC Skyline (on a clear day) and High Mountain of the 2nd Watchung Mountain range may be viewed to the east.
Distant Wanaque Reservoir View from Osio Rock
After taking in the views, turn around and head north west to retrace your steps back to the ravine to the red blazed Torne trail trailhead.
Here you will take the Torne trail north back to Otterhole Road where the trail began.
Flora found along the trail includes the below among others:
NJ’s geology, topography and soil, climate, plant-plant and plant-animal relationships, and the human impact on the environment are all discussed in great detail. Twelve plant habitats are described and the authors were good enough to put in examples of where to visit!
Hamburg Turnpike to Glenwild Ave. Parking area is next to Bloomingdale/West Milford border (look for Welcome to West Milford sign, or Welcome to Bloomingdale sign depending on which direction you are traveling.
In the early 1900’s the land that was to become CLP was an active quarry utilized for the construction of the nearby Kensico Dam which holds NYC drinking water.
Cranberry Lake Preserve Trail
Trails are open dawn to dusk. Trail maps are available at a kiosk outside or you can click here for a digital version.
CLP features four blazed loop trails. All trails begin and end with blazes featuring the Westchester County Parks logo. Periodic numbers appear on blazes occasionally which correspond to your current location on the trail map. These numbers are found on wooden posts. (Please note the numbers do not appear on the online version of the trail map)
All trails are accessible by either orange or white blaze connector trails.
To Nature Lodge
Many sections of CLP trails display signs which lead back to the Nature Lodge. Click here for a trail map!
At 2.4 miles the red trail is the longest trail featured in CLP. The red trail follows CLP boundaries with the exception of the quarry.
The Blue Trail loops around both Cranberry Lake and South Pond for a total distance of 1 mile.
Cranberry Lake is a natural body of water formed around 18,000 years ago by glacier activity. The lake is fed by an underground spring.
The Yellow trail traverses rocky upland and a section of Cranberry Lake.
Purple (History) Trail
Purple Trail Trailhead
The Purple Blazed History trail is a self guided trail which explores most of the preserve including the quarry. The self guided trailmap can be found by clicking here.
While CLP’s trails are open dusk to dawn, the nature lodge and its parking area are closed most days by 5PM. It is strongly recommended that you park in the designated parking area near Old Orchard Street if you plan on hiking past 5PM.
It is from the Old Orchard Street parking entrance that the below description starts out from on the way to explore CLP. Let’s go!
Eastern Chipmunk Cranberry Lake Preserve
From the parking area, walk up the road to the nature lodge.
Cranberry Lake Preserve Nature Lodge
Just to the west of the nature lodge is an interesting wetland with a dock.
Wetlands Near Nature Lodge
It was here that I saw this snake.
Head inside the nature lodge to check out the exhibits and pick up a trail map.
Inside Cranberry Lake Nature Lodge
From the nature lodge, head south to take the yellow trail down to an Orange connecting trail.
Here there is a sign advertising Cranberry Lake. The orange blazed connector trail leads to a jointly blazed yellow/blue trail with Cranberry Lake straight ahead.
Yellow Blue Blazed Trail near Cranberry Lake
Follow the Yellow/Blue blazed trail south with Cranberry Lake to your left.
Continuing south, take the Orange Blazed Connector trail which will appear to your left near a wooden boardwalk known as Bent Bridge.
View of fen from Bent Bridge
Bent Bridge provides a good opportunity to check out the fen located to the south of Cranberry Lake. In the summer, white water lilies appear on the water.
Leaving Bent Bridge, the Orange blazed connector trail leads to a man-made “cave” known as the Stone Chamber.
Looking outside from inside Stone Chamber
The ruins surrounding the stone chamber were the property of a farmer named Thomas Cunningham. The Stone Chamber is a very neat little man-made “cave” of sorts that is fun to explore.
Ruins outside Stone Chamber
From here, the orange blaze connector trail leads past more stone ruins to the Purple Trail (aka History Trail). The path here follows an old railroad which separates the fen from South Pond.
You are sure to hear splashes in the warmer months of frogs jumping in the water as you walk by.
Head east on the Purple Trail to a bench strategically placed in front of a beautiful cascade.
It’s a good spot to rest and relax in a peaceful setting.
From the cascade, continue east on the Purple Trail following signs for the quarry.
Abandoned Tennis Court
An abandoned tennis court will appear to your right.
The tennis court was part of the Birchwood Swim club which used the Quarry Pond for Swimming.
Tulip Poplar & Milkweed Abandoned Tennis Court
Nature is slowly reclaiming the tennis court. Birchwood Swim Club was discontinued in 1997.
Fish Quarry Pond
Once past the quarry pond the purple trail heads past old railroad car wheels which were used to haul granite during the quarry operation.
The Purple Trail continues heading north climbing over the rocky quarry.
The height here is an estimated 450 feet above sea level.
Derrick anchors which once held heavy quarry machinery are still fastened in the rocks along the trail.
Old Automobile on Purple Trail
From here, the trail starts to descend the quarry and heads west passing an old abandoned car.
Continuing north the Purple Trail comes across the remains of a stone cutting shed.
Stone Cutting Shed Ruins
After exploring this area, follow the Purple Trail south until it meets with the red trail. From here, take the red trail southwest with Cranberry Lake to your right. Continuing south, retrace your steps until you pass the cascade with the bench at an intersection with the Purple Trail that you previously took into the Quarry territory. Continuing south, the red trail passes South Pond to the West.
South Pond is man-made and was created during quarry activities.
Bird Tower on South Pond
A Bird Observation tower appears to your left. This tower provides great views of South Pond.
Remains of Stone Crusher
The red trail passes near the remains of a stone crusher foundation. The stone crusher was capable of crushing up to 1000 cubic yards of gravel per day when the quarry was active.
Signs for NYC Watershed appear to east of the trail.
From here, the red trail turns west and temporarily leaves CLP & enters White Plains watershed land and passes Hush Pond to the south.
Stone Wall by Red Trail
From Hush Pond, the red trail passes a couple of connector trails and turns north following an old stone wall delineating NYC watershed property from CLP. According to David Steinberg who wrote a description of Cranberry Lake Preserve in his book “Hiking the Road to Ruins” the lower, crude, sharper-tipped walls are of colonial origin and the larger, cut-stone flat-topped walls are NY DEP watershed boundaries dating from the 1960s.
It was here that I found Indian Pipe growing when I visited in June of 2012. Continue following the red trail north with the wall to your left until you reach your car.
Black Capped Chickadee at Cranberry Lake Preserve
Cranberry Lake Preserve contains diverse habitats within its 190 acres. It is worth checking out yourself!
1609 Old Orchard Street, North White Plains, NY
Park hours: Park open dawn to dusk. Nature Lodge and front gate are open Wednesday-Sunday. 10 a.m. to 5 p.m.
Welcome to the 20.68 acre Alonzo F. Bonsal Wildlife Preserve! The preserve is located and owned by the Township of Montclair, New Jersey and was purchased with NJ DEP Green Acres funds. The City of Clifton is located to the north, and residential development surrounds the preserve to the south, east and west. There are 9.12 acres of adjacent lands located to the north of the preserve which are controlled by the North Jersey District Water Commission for its Wanaque Reservoir Balancing Tank which provide additional habitat for wildlife. A citizens group lobbied to save the woodland from development in the 1970’s. The Bonsal Preserve was named after a local resident whose family’s contribution augmented Green Acres funding of the site.
Alonzo F. Bonsal Wildlife Preserve
The preserve consists of remnant wetlands and uplands surrounding the Third River, a major tributary of the lower Passaic River watershed. The Third River headwaters are located in Rifle Camp Park in Woodland Park.
The headwaters were impounded in 1899 to form the Great Notch Reservoir which greatly reduced the river’s flow. The Third River’s current name was derived from the fact that it lies north of two other Passaic River tributaries (1st & 2nd Rivers).
Years ago, the river was known as Pearl River due to the discovery of the Queen Pearl aka Paterson Pearl . Freshwater pearls are found in a river’s mussel population. The Paterson Pearl, a 93 grain pink pearl, was one of the first freshwater pearl to be discovered in the United States. Other pearls were found in the Third River but none matched the Paterson Pearl.
Today, the mussels are long gone and the name Pearl River has been replaced by Third River as designated by cartographers.
The preserve has been left in its natural state with the exception of an old sewer line built in the early 1900’s. The sewer is owned by the City of Clifton. In 2008, around 10 trees in the preserve and a 12 foot wide woods road was constructed near Daniels Road, a dead end street in Clifton, to access a ruptured section of the pipe. Plans are being made to remove and reroute the sewer as of January 2014.
Bridge over Third River
The main entrance to the Bonsal Preserve is located in a right of way off of Riverview Drive in Montclair. After crossing the bridge over the Third River, you can continue north to Daniels Drive in Clifton or head east or west to explore the wetlands near the Third River. The trails are not blazed but due to the size of the preserve, you can’t get lost physically without soon discovering a spot you previously traveled.
Small preserves in urban settings really provide a great opportunity to take your time and enjoy nature right in your own backyard.
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 preserve, known locally as Montclair’s paradise, is a great place to take a walk, birdwatch and just kick back and enjoy. Click here for directions!
For more information on this fantastic preserve be sure to contact Friends of the Bonsal Preserve at the email address BonsalPreserve@verizon.net.
Great Ecology/Birding Books!
1. Pocket Guide to Eastern Streams – This book is perfect for nature-lovers, hikers, anglers, naturalists, and wildlife professionals
* Includes information on restoring and preserving threatened or damaged stream ecosystems!
Welcome to a virtual tour of the Franklin Lakes Nature Preserve!
Franklin Lakes Nature Preserve
The 147 acre preserve consists of three bodies of water (lagoon, upper lake and lower pond) deciduous wooded wetlands and wooded upland habitat. The Borough of Franklin Lakes purchased the land in 2006 from the Borough of Haledon for $6.5 million using funding from Green Acres and the Bergen County Open Space Fund. The preserve was open to the public in June of 2011.
The Franklin Lakes Nature Preserve features 2 primary hiking trails. Access is available from Ewing Avenue, a small parking lot off of High Mountain Road and from nearby High Mountain Park Preserve’s Red Trail via Reservoir Drive and crossing High Mountain Road.
Shoreline Loop Trail
The main trail is the 1.5 mile white blazed Shoreline Loop Trail which encircles the entire Upper Lake and Lagoon.
Preserve Shoreline Trailhead on Upper Lake Dam
Starting from the parking area, the trail heads over the dam separating the Upper Lake from the small pond to the south. The trail follows alongside the Upper Lake and near High Mountain Road and Ewing Avenue.
Island Bridges Trail
The western portion of the Island Bridges Trail is accessible near where the Shoreline Loop Trail passes by Waterview Drive.
High Mountain as seen from the Franklin Lakes Nature Preserve
Beautiful views of the Upper Lake with High Mountain visible can be seen from this area. After exploring the western section of the Island Bridges Trail (the Island Bridges Trail is about a half a mile in length) head back to the Shoreline Loop trail which will briefly exit the Franklin Lakes Nature Preserve near an outflow from a neighboring swamp (you can also continue via two floating bridges on the Island Bridges Trail to continue to the eastern side of the Shoreline Loop Trail skipping the entire northern section).
Backwater Lagoon crossing
Once the Shoreline Loop Trail enters back into the preserve, the trail crosses backwater of the lagoon.
Molly Ann Brook Crossing
Continuing on the trail you will cross the Molly Ann Brook over a wooden bridge. Frogs can be heard (and sometimes seen) splashing into the water here during the warmer months.
From here, the Shoreline Loop Trail heads east near a church and near a new housing development. Along the way, the trail comes across a basalt beach.
Basalt was formed when molten lava extruded out of the earth’s surface and cooled rapidly. Basalt is found in nearby High Mountain Park Preserve which is situated on the 2nd Watchung Mountain. Once past the basalt beach, the trail turns south. The eastern section of the Island Bridges Trail is accessible from this point.
Island Bridges Trail
Reservoir Trail (East)
After exploring the eastern section of the Island Bridges Trail, head back to the Shoreline Loop trail and continue south until the trail terminates near a picnic area in a pine grove near where the trail began. Accessible Trails have been constructed in this area and intersect with Shoreline Loop Trail. The Accessible Trails will remain unblazed and are not currently maintained by the NYNJ Trail Conference.
Flora found at the Franklin Lakes Nature Preserve includes the below among others:
Fauna that I’ve spotted at the Franklin Lakes Nature Preserve includes:
Canada Geese Eggs
This preserve is a great place to explore and just relax. Directions are listed below (as taken from the NYNJ Trail Conference Website)
Take N.J. Route 208 to the Ewing Avenue exit in Franklin Lakes. Turn left at the end of the ramp (if coming from the west, turn right) and continue for about two miles until Ewing Avenue ends at High Mountain Road. Turn left onto High Mountain Road and continue past a lake and a smaller pond on the left. In 0.5 mile, at the end of the smaller pond, you will see a small brown sign for the Franklin Lakes Nature Preserve on the left. Turn left into a driveway, passing old reservoir buildings on the right, then turn left again at a sign for parking and continue to a parking area just below the dam.
Note: Part of the preserve, including the entrance and parking, is in North Haledon (Passaic County).
The address for the preserve is 1196 High Mountain Road, North Haledon, N.J. 07508