Sunday, August 23, 2020

Travel Close to Home No. 5: Snakes and Ladders

This next episode in my southern Ontario travels is actually the "Daily Double," since it encompasses two destinations. But there's method in my madness, because the two locations are two of the many beauty spots in the province that share a single common feature: the Niagara Escarpment.  

The Escarpment of course takes its name from its single most famous and most-visited attraction, the world-renowned Niagara Falls.  By far the largest, Niagara is, all the same, only one of the hundreds of streams of all sizes that tumble over the edge of this cliff throughout its length, some falling dramatically in a straight line, others cascading over multiple tiers of rocks.  Here's another one: Webster's Falls on Spencer Creek, in Hamilton, in a photo from April 2014.

The sheer size of the Niagara Escarpment eludes many people -- and I'm not referring here to its height, but rather to its length.  Here's a map to illustrate the approximate path of the escarpment across New York, Ontario, Michigan, and Wisconsin.  The upper level above the cliff or slope is always in the part of the map below the red line

The height and shape of the Escarpment also can vary dramatically from place to place.  One of the highest points I've visited is the lookout at Ten Mile Point on the northeast corner of Manitoulin Island, with its spectacular view towards the mountainous La Cloche region on the North Shore of Lake Huron.

The vertical edge which is the most characteristic shape of the Escarpment is the result of a simple trick of the geological formation.  The rock structure is composed of multiple layers of sedimentary rocks, mostly sandstones and shales, but with a top or cap layer of notably harder dolostone.  As the forces of wind, weather, and falling water eat away at the rocks, the process of erosion happens faster in the soft under-layers.  A section of the cap layer is left protruding, eventually breaking off and falling, but leaving behind a new, sharp edge to the cliff.  This gives the Escarpment its characteristic form of a vertical drop with a sizable heap of loose rock rubble at the base, usually extending up about half the height of the cliff.

Diagram from whaton.uwaterloo.ca

The earliest long-distance hiking trail in Ontario is the Bruce Trail, which was already in existence over half a century ago.  In its final form, this trail follows the course of the Niagara Escarpment all the way from the Niagara River to Tobermory at the northern tip of the Bruce Peninsula.  The trail passes through all the hiking locations I'm discussing in this blog post.

So, let's go Escarpment hunting in the regions not too far either from Toronto, or from my home.

Our first destination is easier to spot, visually, than any of the other places I've visited on this series because it is right beside the longest freeway in Ontario, Highway 401, and in the Region of Halton, a mere 25 minutes or so driving time west of Toronto airport.  Although it shares the characteristic features of the Escarpment, this massive headland is actually not part of the main feature but a separate formation known as the Milton Outlier.  Think of it as an island.  Indeed, if this region were to be flooded beneath 30 metres or so of water (as it was at the end of the last Ice Age), the Milton Outlier would appear as a sizable, oval-shaped island a short distance offshore from the Escarpment proper.  

Word to the wise, though -- if you're planning to visit the parks on and around the Milton Outlier, you'd do well to study a map of the region in advance.  Right beside Highway 401 it may be, but there is no direct exit from the freeway to take you right there.  Also, the largest park -- Kelso Conservation Area -- has sections both above and below the Escarpment, and you certainly want to wind up in the right place in that park, depending on what sort of activity you're seeking -- hiking and mountain biking above or rock climbing, swimming, kayaking, and canoeing at the reservoir below.  On the other side of the highway is another sizable conservation park on the Escarpment proper, with multiple hiking trails, at Hilton Falls.

Most important point of all: although the park at Rattlesnake Point looks easy to get to from the QEW or Highway 407 -- a straightforward run up Appleby Line from interchanges on those freeways -- the narrow, contorted hill which carries Appleby Line up the Escarpment to the park is closed to coaches, motorhomes, and other long vehicles, and could easily give other drivers unused to such roads the heebie-jeebies, to cite an ancient medical description.  What else can be said about a road which includes a hairpin bend that's not just signposted at a 10 kilometres per hour speed limit, but also equipped with a roadside mirror to help you see if anyone is approaching said hairpin bend from the other direction?

Either the 14th Side Road or Steeles Avenue provides an easier and safer drive up the Escarpment on the eastern side from Tremaine Road (Regional Road 22). 

Next step: a critically important one.  Due to the Covid-19 outbreak, and to minimize crowding by controlling numbers of visitors, all facilities at Kelso, Rattlesnake Point, and the other major conservation parks in Halton Region, are subject to advance visitor reservations, which can be made online. Reality check: if you try at the last minute, you will likely not be able to get a reservation at all on Saturday or Sunday!  The driver who arrived ahead of me had been forced to pull over to one side at the gatehouse while searching frantically through the website for an available time.

Here's the link to make a reservation as required at any Halton Conservation Park:

Conservation Halton Parks Reserved Visits

The website displays a list showing availability day by day, and when you enter the system to make a reservation you will choose from admission times in 10-minute intervals throughout the day, where space is available. You'll also prepay your admission fees as you reserve your time.

My biggest reason for choosing to head for Rattlesnake Point:  the view does not include the six traffic-jammed lanes of Highway 401!   Before anyone panics over the name of the park, I'd just add that I doubt any rattlesnakes are ever seen there nowadays -- their habitat is generally much further north, on the Canadian Shield.  Perhaps the name dates back to some incident in the earliest days of European settlement here.  I'm sure that if snakes were likely to appear, the fact would be mentioned in the park's website and on signs in the park itself.

Once you are inside the park at Rattlesnake Point, bear right on the circular driveway.  There are two main parking areas, and from either one it's a short, easy walk over level ground through the forest towards the rim of the cliff.  I chose to start by heading for the Upper Parking area, clearly signposted inside the park.  Here's a map of the park and its trails on the signboard at the upper parking lot. 

My hike here took me right around the entire loop marked in green, with a little add-on for a few minutes along the Bruce Trail beyond the Nassagaweya Canyon Lookout, and took about 50 minutes.

The first leg is deceptively simple.  The trail here is wide and level, indeed completely suitable for people of almost any level of mobility. 

The forest is mature but fairly open and light, not deeply shaded.

As you approach the cliff, you begin to glimpse through the trees the view over the edge.  Note that the edge of the cliff in this park is in many areas unprotected by fences or walls.  Hikers with small children need to remain alert.  Up the hill to the right you can see the beginning of the old stone wall which marks the Nelson Lookout.  Climb up and enjoy the view.

It's almost shocking that such a pleasant rural landscape can exist so close to one of the continent's biggest conurbations, the eight-million-plus people of the Greater Toronto Area.  This is the success story of the Greenbelt, created back in the year 2005 by the Province of Ontario to protect environmentally sensitive lands in an arc around the Toronto urban area.  At a size of 7,284 km² or 2,812 mi², the Greenbelt is one of the largest and most successful near-urban land preservation schemes in the world. 

And what is that you see in the distance, which looks like it could be another section of the Escarpment?  It is indeed.  That is Mount Nemo, on the northwestern outskirts of Burlington, the location of yet another Halton Conservation Park.

I took a pass on the Trafalgar Lookout, which turns the view further around to the east, because some people were already up there and the scramble up the rocks at that point didn't look like providing a safe social distance.  

Close to the Nelson Lookout, though, is the Pinnacle Lookout, and here a staircase descends the cliff in a series of flights that give spectacular views of the Escarpment's underpinnings.




Plainly visible are the fracture lines running horizontally between rock layers, and cutting vertically across the layers.  It's these cracks and the resulting water penetration which erode the rocks and eventually allow the edge to crack off and recede.  The tree roots penetrating and loosening the rock from above play a role too.  Of course the undercutting process is necessarily much slower than it is at Niagara, where the tons and tons of falling water hammer incessantly at the rock face.

Proceeding west from the Nelson Lookout around the rim of the park brings you onto a wild and rugged stretch of trail.  The ground becomes in places very broken and uneven, and you descend a considerable distance during this leg of the hike as the rim of the Escarpment becomes much lower on the west side. 

I'd say it's a 50-50 tossup whether this stretch of the hike would be more strenuous if you were going clockwise or (as I was) counterclockwise.  Along the way, trail markers help to keep you on course.  The green and yellow discs correspond to the green and yellow colours marking the trails on the park map (see above).  The vertical blue paint blazes are the markers of the Bruce Trail, which shares this part of the Rattlesnake Point trail system.

Eventually you come around to the more westerly view of the Nassagaweya Canyon Lookout, although the Canyon itself (farther to your right) is not readily visible because of the way the trees have grown up around the lookout area through the years.


Cutting through the trees below you, you can trace the gap which marks the course of a small river.  This is Limestone Creek, which flows south through the Nassagaweya Canyon.  The Canyon, by the way, separates the Milton Outlier where you are standing, from the main Niagara Escarpment proper, just to the west.  Limestone Creek empties its waters into Bronte Creek, on the way south to Lake Ontario.

From this point, it's a short distance to the Lower Parking area, and from there you can follow the trail markers onto the final stretch of the Vista Adventure trail, a short walk through the woods which climbs back up to the upper level, but with a much smoother surface than the trail along the edge of the cliff.  You then follow the paved road back to the parking lot where you started.

In the areas around the parking lots there is a good deal of open space, some parts of which are dotted with picnic tables.  This open area provides a place for games and activities as part of more leisurely warm-weather visiting.  Sadly, at this time, the length of visits to the park is capped at 2 hours, again, to avoid overcrowding and give more visitors a chance to get in under the current pandemic conditions.

 

My second Escarpment expedition took me to the area just north of Orangeville, more or less half way from Lake Ontario to Georgian Bay.  In the heart of Mono Township you'll find the Mono Cliffs Provincial Park.  This is a natural environment park, with limited day use facilities only.  It preserves a particularly picturesque portion of the Niagara Escarpment, consisting of the main escarpment itself and two outliers -- a larger one at the south end of the park, and a smaller one to the north.

 Unlike some of the smaller parks I've visited earlier in this series of posts, Mono Cliffs calls for some serious hiking with a fair degree of care and attention to your surroundings.  The trails are rugged, the climbs have stiff grades, and rocks and tree roots protruding through the ground on the trails are a dime a dozen.  You need proper shoes or hiking boots for this kind of wild terrain.  Like the Vista Adventure Trail at Rattlesnake Point, this most definitely is not the place for a casual stroll in your flip-flops.

Mono Cliffs is easily reached by following provincial Highway 10 north of Orangeville to the village of Camilla, then turning right on County Road 8 and following the signs.  If you're arriving by car and you search the park on Google Maps, for instance, you'll get directed to the main, fairly sizable parking lot on Township Road 3.  There are vault toilets here.  The only fee is for the use of the parking lot, at a pay-and-display machine.  It offers two choices: a 4-hour permit, or an all-day permit.  Unless you plan to hike every single inch of every single trail in the park, the 4-hour permit should suffice.  My little hike up to the lookout point and back lasted for 1 hour 45 minutes.

The trail out of the parking lot is called the Carriage Trail, and since it is wide enough to drive a carriage or wagon along, I'd guess it was originally built to serve one or more farms.  The first sight on the right is a small forest pond, basking in the sunshine.

Along the way, you pass through a couple of overgrown clearings which were probably farms at one time.  You also pass through a substantial forest of white cedar...

...and other more assorted forest types.


The trail is firm, but has very deep ruts and washdowns which no doubt occur after heavy rains.  That's because the trail is climbing almost all the way.  

This trail is not overly steep, although you do have to watch your footing around some of the deeper ruts -- and since this route is also available for horseback riding, you definitely have to keep one eye on the ground to avoid a disagreeable encounter with certain equine byproducts.  The path keeps climbing at a steady grade for a considerable distance -- it took me about 15 minutes of uphill walking time, before I reached the centre of the park.  

I mention this fact because it was not until this trail junction, fifteen minutes in, that the park finally deigned to post a signboard with a map of the trails.  It was also the only such map that I saw.

At this point, you have to do a short zigzag, first to the right, and then, a minute later, back about the same distance to the left.  This is clearly shown on that map board, and on the slightly less clear map on the Ontario Parks website.  Just keep following the signs for the Carriage Trail.

Which is ironic, because no carriage would ever get up the next part.  All the climbing you've down till now has been just positioning.  Now, you're going to actually start up the Escarpment.  The trail gets truly steep now, and very bumpy with rocks and roots.  After a good stiff climb you come to a wooden staircase in several flights, totalling about 80 steps.  At the top of the stairs, there follows another steep and rugged incline finishing the climb up onto the more-or-less level ground at the top.  Only about one-third of that upper grade above the stairs is visible in this photo before the trail bends to the left. 

My guess is that the stairs represent about one third of the total climb up the Escarpment.

On more-or-less level ground at the top of the hill, there's a junction.  The signpost indicates trails with specific names going straight ahead and to the left.  But on the right there's a third, much narrower trail which is not indicated by name on the signpost.  This is the trail you want -- the Clifftop Trail.  It snakes through the forest, basically a single-file path all the way, with plenty of smaller ups and downs.  Just off to the right you can see the drop-off of the Escarpment falling away, but the path never gets too close to the edge.  

After about 10 minutes of this, you come to a wider path, turn right a short distance, and you reach the viewpoint over the cliff.  At the end of the short steel walkway projecting out into the free air, you enjoy this vista.  Over to the left is the North Outlier, plainly visible and appearing like a flat-topped mesa covered with trees.

Below you, among the trees, you can glimpse one of several small lakes in the park.  

 

 If you look straight ahead, you can see in the distance another high ridge closing the horizon.  That ridge marks a sizable height of land west of Lake Simcoe which slopes down into the valley of the Nottawasaga River just to the west of Simcoe Road 27 (and therefore just a few kilometres west of Highway 400).  It was easy to see on this crystal clear summer morning.  At a rough guesstimate it would be about 35 kilometres away to the east from the Mono Cliffs lookout.  

Directly below the lookout (yes, you can look straight down over the edge, and even through the walkway's steel grid), there's a curious hole in the forest and the open forest floor is littered with pieces of tree branches.  I have no idea how this might have happened. 

Continue a little further north along the clifftop trail, and you come to another staircase down the cliff.  Unlike the route you took coming up, but like the one at Rattlesnake Point, this set of stairs goes down only part way, onto a walkway which then comes to a dead end.  But this is a perfect spot to get up close and personal with some very peculiar geological features -- two large chunks of the Escarpment which have become completely separated from the main body by erosion.  The walkway passes between the isolated rock masses and the main cliff, with the hard top layer slightly overhanging the walkway.  Difficult place to photograph with a phone because of the odd lighting through the trees -- I only got one good picture.  I should have taken my regular camera.  Lesson learned for the next visit.

At this point, I'd been walking for about an hour, and time was beginning to press on me.  I therefore turned around and retraced my steps, still leaving plenty of trails to explore another time.  The hike back to the car was much easier, since it was now 80% or more downhill -- although the really steep bits before and after the staircase forced me to slow right down.  After all, you wouldn't want your intrepid blogger to tumble down the hill ass over teakettle, to quote an old British saying.  Actually, that part of the climb down became like a trip back into childhood, bringing back a memory: "You may take 487 baby steps."  Or something of that sort. 

If you want the thundering drama of the Rocky Mountains, you're not going to find it at either Mono Cliffs or Rattlesnake Point.  But you will find some eye-catching viewpoints, and get to experience some diverse and beautiful natural environments during the course or an hour or three of walking time. 

To conclude, this map shows the approximate locations of these two natural attractions.



Wednesday, August 5, 2020

Travel Close to Home No. 4: Taking the Long View

In my latest installment of intrepid travels around my region of southwest Ontario, I paid a visit this morning to Long Point on the North Shore of Lake Erie.

Long Point is one of three or four areas along the north shore of Lake Erie which share similar features and formation, and related natural environments.  What makes Long Point unique, and justifies its status as a World Biosphere Reserve, is its sheer size.  Here's an aerial view.  Even from a plane, the main shore of the lake is visible only in the distance, since it is about 40 kilometres (25 miles) away.


Indeed, if Long Point stuck straight out, perpendicular to the shoreline, instead of at an acute angle towards the east, it would stretch well over half the distance across the lake and the tip would be some miles inside United States territorial waters.

What looks at first glance like a sizable land mass dissolves on closer inspection into a bit of sand and a lot of water.  The southern edge of Long Point is a sandspit, washed up here by the wave action of Lake Erie setting from southwest to northeast along the shoreline.  The remainder of the whole formation is primarily wetlands, full of marshland vegetation.  Only near the tip are there a few parallel sand dunes inland, which likely represent older shorelines of the spit.

Similar sandspit-and-marshland formations are found across Long Point Bay at Turkey Point, and farther southwest at Rondeau, Point Pelee, and Pelee Island.

In its natural state, before the arrival of European settlers in the region, Long Point was inaccessible by ground travel and had to be reached by water.  This gave rise, in the 1850s and 1860s, to the rapid growth of illegal and unsavoury activities on the Point -- everything from smuggling and illegal stills, to gambling and prostitution in what were then called (and still are called in Canadian law) "disorderly houses."  The perpretators and customers alike hailed from both sides of the lake, and the limited law enforcement activity in the region made it easy for them to carry on business.

Also, the natural environment of the Point was being rapidly depleted by unlimited and reckless over-fishing and over-hunting.  Then as now, Long Point's huge wetland areas made it a natural home and stopover point for vast flocks of water birds, and thus it became a popular shooting area.  But by 1855 it had become far too popular with hunters trying to satisfy demand from growing cities on both sides of the border.  In 1866, a group of dedicated sport hunters banded together to purchase 16 sectioned lots, the vast majority of the total land on the Point, and immediately they sought a charter as the Long Point Company.

The shareholders in the Company included some wealthy industrialists, and sufficient funds were set aside to hire full-time patrollers.  With that transfer of the Point from Crown to private ownership, the heyday of the illegal activites ended, and the hunting-for-profit likewise dried up in just a few years.  By 1871, the Company owned the entirety of Long Point aside from the section at the very tip, reserved by the federal government for the lighthouse.

What was truly remarkable about the Long Point Company was the determination of its owners, not to plunder the land, but to guard it and restore it to vitality as a living resource with a diverse animal, bird, and vegetation environment.  The members of the Company allowed themselves only such limited amounts of hunting as would not endanger or reduce the animal and bird populations, or endanger their survival. 

In the 1860s, such a mission was all but unheard-of among the white communities of North America, although it was an approach to land stewardship that was second nature to the aboriginal peoples.  The Long Point Company was truly at the vanguard of the natural environmental movement which was just beginning to stir.  The forerunner of Banff National Park wasn't established until 1885, almost twenty years later, and Canada's oldest provincial park, Algonquin Park in central Ontario, didn't come into existence until 1893. 

While the Company has come in for a fair bit of criticism for its iron rule over the years, there's no denying the success of their environmental stewardship of Long Point.  In later years, a substantial portion was returned to the province and re-entered the Crown lands portfolio.

This map shows the distribution of land in Long Point today, in broad outline:


Road access to the Point was created in the 1920s when the province purchased the land in area 3 of the map for a park, and built the causeway from Port Rowan across the marshy area of Big Creek.  The wetlands west of that road now form the Big Creek National Wildlife Area.  The lands sold by the province to private owners for cottages actually surround an enclave of provincial land which was the original Long Point Provincial Park.  Today, it still forms part of the Park, and is called the Cottonwood Campground.  The main Park tract, in area 3, contains a sizable day use area and further campgrounds named Firefly, Monarch, and Turtle Dunes.  All of these Park facilities face the sandy beach along the south side of the Point.

The outer half of the Point, apart from the lighthouse reserve at the tip, now forms the Long Point National Wildlife Area.

Long Point Company territory is still barred to non-members, so the road onto the Point ends with the Park campgrounds.  Access to the tip is only possible by boat.  A few small tracts of land are set aside from the Wildlife Area and hold a dozen or so private cottages, also accessible by boat.

Now, with all that background, here's my photo tour of Long Point and the Park.

Begin with the causeway.  It's narrow, with no shoulders, and for most of its length there is no barrier other than the grasses, shrubs, and the odd tree to stop careless motorists from plunging into the murky swamps on either side.





With wetlands on both sides, the causeway road is a natural place for turtles to be seen as they make their slow way from one marsh to the other.  The turtle death rate here through the years has been very high, and recent work has placed a number of culverts under the road to allow turtles to pass without leaving the water.  I assume it's working, since I saw no turtles on the road at all.

At the point where you arrive at the beach front, the road makes a sharp curve to the left to follow the shore, and a warning sign advises you that water over the road is possible.  Sure enough, there's the open water of Lake Erie just to your right, and it's not much lower than the road you're driving on.

The road continues east through the cottage area, so-called, although it's obvious that many of the cottages are now year-round homes.


As you arrive at the Provincial Park, you stop at the gatehouse to pay your park fee.  You then branch immediately off to the right into the parking areas for the day use beach -- and you quickly realize that this parking lot is better shielded from lake storms than the main road back by the causeway.


The access points to the beach are over lower parts of the dunes, and mats are laid over the sand to make walking easier -- as well as to facilitate access for people of reduced mobility.


You walk, then, up and over the critical spine of Long Point and down onto the sandy beach, and take a look.  The beach stretches as far as the eye can see in both directions, off past the park and the cottage area to your right...


...and off past the campgrounds to the Long Point Company's shoreline to your left -- on and on and on.  After all, the beach does extend for virtually the entire 40-kilometre length of Long Point!


One of the striking features of this beach is the layer of reddish-purple sand which is exposed just at and above the waterline.  We had a layer just like that at our summer cottage on Lake Simcoe, north of Toronto, when I was a young 'un.  The dark layer is coloured by tannins from decayed plant matter in bygone ages, and is a natural sight at beaches which adjoin wetlands.


As with so many of the sandy beaches along the northern shore of Lake Erie, the water here is nothing if not shallow.


The people who look like only their shoulders are above the water are actually sitting down!

If you look back at the aerial view at the top of this post, you'll be able to see just how far the sandy shallows extend offshore all around Long Point -- and you'll have a better idea of just why these waters have proven treacherous to so many ships during stormy weather through the years.  Actually, many of the shipwrecks came about through the practice of "blackbirding" in the old days, whereby local residents lured ships into destruction with fake lights, and then plundered the wrecks.

On the other hand, though, the water looks so placid and non-violent on a breezy summer's day that it's fun to just sit and contemplate the rolling rhythm of the waves, and the invisible American shore of Ohio and Pennsylvania that is the next solid land directly in front of you.


Proof positive of the bigger waves that roll up on this shore during more turbulent weather is provided by the assorted driftwood and other debris flung up onto the sand some distance above the water level.  The log in this picture is one of a number lying along the beach, long since denuded of their bark, but still maintaining their shape and integrity after long immersion in the lake.


The beach was actually pleasantly uncrowded, partly because of the morning hour, and partly because of the brisk westerly breeze along the shore, and consequent cool temperature.  I enjoyed a walk along the sands, and then a sit in the sun for a while.  I took a pass on swimming, largely because I hate having to wade out hundreds of metres just to get water deep enough to float in.

On the way home after my visit to Long Point, I detoured into Port Rowan, adjacent to the landward end of the causeway, and took a couple of pictures of the boathouses in (not on) the harbour.



I'm sure most of the boats kept in those boathouses have been out to the tip of Long Point, more than once.  The tip is a popular gathering place for boaters in the summer.  Here's an internet photo to show how the tip of the point would appear to you if you were to wade out along the sandbar extension, and then turn around and look back at the lighthouse.


The road to Long Point is County Road 59 (formerly provincial highway 59), and comes off Highway 401 at Woodstock.  If you're driving by that route, a helpful hint.  When you get to County Road 13, turn right on that one.  With a couple of small jogs, well signed, it takes you straight across country, avoiding the big eastward detour of 59 to serve the town of Delhi.  Road 13 rejoins Road 59 at the point where you cross the east-west provincial highway 3. 

Here, to conclude, is a map to give you an idea of the Point's location.