Yearly Archives: 2015

Adam Alexander Homestead – Halton Region Museum

Saturday, Nov. 7, 2015

Four different men, all named Adam Alexander, owned and operated this innovative family farm between 1836 and 1961.  Today it has been converted to house the Halton Region Museum.  Having visited Kelso’s Kilns we made our way through the conservation area toward where we had parked on Kelso Road.  Light rain was falling but we took the time to look around the outside of the buildings.

In 1826 Aberdeen in Scotland experienced a severe drought that led to some of the worst crops in the previous sixty years.  Potatoes and turnips didn’t form at all and many people left for greener places.  Among them were Adam and Margaret Alexander who decided to move to Upper Canada.  They brought their four children, including Adam Alexander II,  with them on the voyage to Montreal which typically would have lasted about 44 days.  From Montreal, it was on to Ancaster which had become Upper Canada’s second largest town, next to Kingston.  The Alexanders lived in Ancaster for ten years and Adam was able to ply his trade as a stone mason. One significant project that he worked on was Dunburn Castle built for Allan McNabb between 1832 and 1835.  The old postcard below shows the castle around the turn of the century.

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In 1836 Adam purchased this 200-acre lot of land at near the foot of the escarpment just west of Milton.  The land was covered in a forest of trees that were up to 200 feet tall and four feet across at the base.  The trees that were cut down to make the first clearing were used to build a log cabin for the family.  The original log house has been removed.  A different log house has been moved to the approximate location of the original one.  This cabin was found in a forest tract north of Campbellville and the details of its construction are not known.  It has two rooms inside and is typical of first homes built by Scottish and Irish settlers.

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Clearing the land was a major chore and it took over 25 years for the Alexanders to slowly cut down all the original forest cover.  Trees were normally cut during the winter when other farm work was greatly reduced.  As soon as the frost was out of the ground the work of grubbing the stumps would begin.  A grubbing axe was used to dig around the stump and cut off the smaller roots.  Pulling oak tree stumps was hard work and would often take a whole day to remove a single stump.  It was normal to leave the stumps in the ground for a few years to let the roots rot and crops were grown around the stumps while they waited. The Alexanders saved and bought a stump puller to ease the work.  The walnut tree in the picture below was planted in 1893 to celebrate the birth of Adam Alexander IV.

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When the family had been settled long enough to have a productive farm they turned their attention to a more comfortable dwelling.  Adam Alexander used his skills as a stone mason to build a home out of local limestone.  The style was Gothic Revival which was popular from 1830 until about 1900.  One of the most common elements of the style is the pointed arch, often used in windows.  The original home is seen in the cover photo and these pointed window arches are seen on all the second story windows.  The house was damaged by fire and rebuilt in 1918 at which time the windows were changed to the more vernacular ones seen today.  Steeply pitched roof lines with front facing gables are also common to the Gothic Revival style.  This element used to adorn the centre of the original house but was removed after the home was rebuilt.

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The family prospered selling cash crops like wheat, butter, potatoes, timber and wool.  They also raised cattle sheep and pigs.  The family was self-sufficient and built their own blacksmith shop for shoeing the horses and making repairs to equipment.

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By the 1880’s they family had built a large Pennsylvania style barn.  The barn was renovated in 2001 and a third story was added.  The barn can be seen in the photo above of the walnut tree. In 1898 Adam Alexander III tapped into a stream flowing in the escarpment above the property. He piped the water to the barn and house where he installed water motors.  These motors created electricity to power farm and household equipment.  In the barn a fanning mill, circular saw and grain crusher were a few of the automated devices Alexander ran.  In the house, the chores were simplified with an electric washing machine, cream separator, butter churn and meat chopper.  While other local farms were lit with kerosene and run by manual labour the Alexanders had comparative luxury.  The water was also used for a small fountain in the yard of the house.

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Parts of the farm were sold off over the years including a small piece for the erection of a one-room school.  When the Credit Valley Railroad was being constructed the Alexanders sold a strip of land for its construction.  Finally, in 1961 Adam Alexander IV retired and sold the farm to the Sixteen Mile Creek Conservation Authority for use as a park and flood control facility. Starting the following year the farm buildings were slowly converted to house the Halton Region Museum.  The pond was created in 1967 to feed the snow making machines but it was soon discovered that it was far too small and now has been left to develop a more natural condition.

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Travellers have always needed service centres to keep the fluid topped up in their vehicles.  The stone trough pictured below was supplied by Halton County and carved out of local limestone. Originally located on Steeles Avenue west of Hornby it was provided for horses to get a drink along the road.  It has been moved to the Alexander farm as part of the museum display.

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Old millstones were sometimes converted into tire setting stones.  They would be used to hold a wooden wagon wheel while an iron tire, shaped like a loop, was slipped around the outside. The heated metal was allowed to cool on the wheel leaving it set in place.

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There are plenty of other trails remaining in the area for possible future exploration.

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Kelso’s Kilns

Saturday, Nov. 7, 2015

Near Kelso are several abandoned lime production facilities that preserve part of our industrial heritage regarding the extraction and processing of construction materials.  We decided to look for evidence of two of these plants that operated between the south side of the Credit Valley Railway (CVR) and the edge of the escarpment.  We parked on Kelso Road and set off to make our way to the foot of the escarpment with our eyes set on the vertical cliff face that shows up in archive photos of the kilns.

The area around Milton has always been known for aggregate extraction and the production of lime, limestone and bricks.  It was settled beginning in 1819 by Scottish immigrants to the extent that the area became known as the Scotch Block.  In 1844 Alexander Robertson settled in the area of Milton and began raising his 8 children.  His son, David, started Milton Pressed Brick and Sewer Company as seen in Pine Point Park.  Another son, Duncan started the Robertson Lime Company in the 1880’s on a strip of land between Kelso Road and the escarpment.  The company was operated by him and then his son Donald until 1929 when they sold the business to Gypsum Lime and Alabaster Limited.  Robertson built his company on the embankment along side the CVR (now CPR).  Original stone construction and later concrete additions and repairs remain near track level while the remains of kilns stand slightly uphill.

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Gypsum Lime and Alabaster Limited sold to Dominion Tar (Domtar) in 1959 and they closed the facility a few years later.  Two concrete silos stood on the west end of the structure joined by a bridge across the top.  Birch trees are growing in and around the structures, which look like a giant pair of sunglasses.  These were possibly used in the production of quick lime by adding water to the burnt lime from the kilns.

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The picture below is credited to Robert Sandusky and is from 1957.  It shows the Gypsum Lime and Alabaster Limited facility in the background.  The three lime kilns are in operation and one of the two silos can be seen on the right.  The location of this bridge on Sixteen Mile Creek is now lost under Lake Kelso.

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The view from near the foundations of the Robertson Lime Company.  Lake Kelso can be seen between here and the 401.  A dam and flood control facility for Sixteen Mile Creek created this lake in 1962.  It was a mostly cloudy day which gave way to light rain toward the end of our hike. There is still some colour left in the trees but mostly in the willows and oak trees.

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We ended up on the wrong side of the fence and had to walk down the tracks to Appleby Line. This isn’t recommended.  From here we made our way south and found an entrance behind the site of the Christie lime kilns.  David Christie built two draw kilns each 55 feet tall on the site. The first was completed in 1883 and the second in 1886.  The cover photo shows the view up inside one of these kilns.

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The picture below shows the furnace where the wood was burnt to provide heat to break down the limestone.  Temperatures in the oven could reach as high as 1800 degrees F.  The person who filled the furnace was known as a fireman and he made $1.00 per day.  He had to load about 8 cord of wood into the two kilns each day.  The four quarry workers each made $1.25 daily.  The foreman was paid $400 per year.  Workers got Sunday off and many of them attended the church building on the corner of the Christie Homestead.  It has since been converted into a house.

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Chunks of limestone were moved from the quarry behind the kilns to the kiln site.  From here they were dumped into the top of the kiln to be burnt into lime.  The picture below shows the top abutment for the bridge that carried the limestone to the kiln.  There are still pieces of the log supports in the holes in the side of the abutment.

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The archive photo below shows the Christie Kilns in 1911.  Notice the bridge running from the top of the kiln to the embankment behind. The supports and trusses for the bridge can be seen behind the kiln.

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A small tramway was installed to bring limestone to the kilns and it was opened in July 1922.  Rock could be brought from the quarry to the kiln in under 2 minutes via a steel rope half the size of the one we found on The Cox Property.  This was a marked improvement over the previous method using horses to haul the stone to the kiln.  The horses were suitably impressed too!

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Between the two draw kilns and slightly to the rear are the remains of a third kiln.  This kiln is shorter and of a different construction.  This set kiln was used by loading limestone in and packing firewood around it.  The method was slow and required a cool down period before the product could be removed.  This kiln was likely abandoned when the draw kilns were installed.

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There is a footbridge to get across the CPR tracks and so we took it back into the park.  From here we could see the vertical cliff face that we had been close to after exploring the Robertson Lime Company foundations.

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Growing along the side of Kelso Road are some wild grapes.  Care should be taken to ensure that you are in fact looking at wild grapes and not moonseed, which is poisonous.  One way to tell is to look at the seed shape which predictably looks like a moon in the moonseed plant.

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Google Maps Link: Kelso

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Hilton Falls

Sunday November 1, 2015

Hilton Falls makes a scenic 10 metre drop over the escarpment beside the ruins of a thrice abandoned saw mill. We decided to visit the falls and investigate a section of the escarpment we had never been through before. We parked on the sixth line at the parking lot for the Halton Regional Forest Britton Tract and set off on an extended hike to the falls.

The Britton Tract has been managed by Halton Region since 1952 and contains the Bruce Trail as well as several side trails.  The escarpment here is dolomite which can hold water in pools close to the surface providing a large amount of water in streams and wetlands.  It also leads to the growth of extensive amounts of moss on the rocks.  The trees don’t tolerate the wet conditions and many fall before they reach their full size giving the forest a youthful appearance.

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The autumn meadowhawk, as implied by it’s name, is seen in late summer or fall.   However, the name may suggest a bird rather than a dragonfly.  This dragonfly has relatively large eyes as compared to most members of the genus.  They feed on insects including the beloved mosquito and they themselves are eaten by fish.  Large Mouth Bass are known to catch them as they touch the water when the male and female are locked  in the process of mating.  It’s Latin name means “with rock” and refers to their habit of sunning themselves on the rocks along the shoreline of lakes and steams.

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Along the side of the blue trail we found a glacial pothole. These potholes generally are wider in the middle than either the top or bottom. Early concepts of their creation suggested that aboriginal people had carved them. Smaller ones supposedly being used for cooking. They are also called “Moulin Potholes” and are now believed to have been formed when water poured through a hole in a melting glacier and eroded the stone beneath. They range in diameter to over 25 feet and the one pictured below is about 15 feet deep.

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As we made our way through the woods we saw an old stone wall on the left of the path.  Stone fences were the easiest solution for disposing of rocks during the annual clearing of farmland. This particular tract of land was difficult to farm and the fields have been left to go wild again. Now the stone walls are running through the forest where once they would have divided fields.  Like other surfaces in the area the stone fence is covered with a thick layer of moss.

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The water in the wetlands is controlled by means of a modern sluice gate.  The pipe on the top houses the cylinder that presses a metal plate down to seal the flow of water.

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Following Sixteen Mile Creek we came to a place where the sunlight sparkled on the water as it vanished over the crest of a waterfall.

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In 1830 Henry Young gained title to lot 8 in the fifth concession.  He allowed Edward Hilton to build a saw mill in 1835 which Hilton operated until 1837.  This was when he decided to leave to fight in what came to be known as the Upper Canada Rebellion of 1837.  The mill was left to rot and it appears Hilton didn’t return for about twenty years.  Hilton gave his name to the falls although he only operated a mill here for a short time.  Hilton Falls plunges over the escarpment and provided the power to turn the water wheel for the saw mill.

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In 1856 the site was purchased by Dr. George Hamilton Park who had the mill rebuilt.  He likely bought it under speculation and it was operated under several names until 1863 when it burned down.  At the foot of the falls stand the remains of the water wheel housing from Dr. Park’s mill.  This cut stone structure supported a wood and iron wheel that was reported to be 40 feet in diameter.  Estimations of the site suggest that 26 feet was more likely the size.  The water was brought from a mill pond above the falls through a flume to the top of the wheel.  The stone arch provided an exit for the water after it turned the wheel.  The wheel housing and the mill were solid construction.  The saw mill was 30 feet wide, 50 feet long and stood 18 feet tall.  The wheel housing can be seen below as well as in relation to the falls in the cover photo.

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Along the way back we decided to take a brief trek along a side trail near the sluice gates. Here we discovered this small pond.  The white rock along the far shore of the pond is another large glacial pothole.

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Ontario’s crown forests cover almost two thirds of the province.  When almost all of the original tree cover was harvested in the first century of settlement the government set out a program to encourage reforestation.  Tax grants were made available to people who planted a portion of their land with forests.  The land in the escarpment was poor for farming and was often reforested with trees planted in straight rows as seen below.

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This small red oak tree has it’s bright red leaves shining in the fall sunlight.  This tree can grow very fast and in 10 years can reach up to 20 feet tall.  As noted earlier, the growing conditions here will likely cause it to die before it reaches it’s potential of 500 years old.

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The Niagara Escarpment was named a World Biosphere Reserve by UNESCO in 1990. Development and land use are strictly controlled along the escarpment.  Mineral extraction is one of the permitted uses of the escarpment under tightly controlled conditions.  The Milton Quarry is across the street from where we parked and has filled up with water.  On the far side of this photograph is a white building.  Behind it a foot bridge carries the Bruce Trail across “The Gap” in the escarpment.  This gap can be seen from the 401 and was created in 1962 when the quarry was opened.  The trail over The Gap makes for a fun hike that I hope to repeat soon.

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Taking the scenic route it was 5.9 km to the falls but the more direct route back was only 4.26 km for a total hike of 10.25 km.  This is a lengthy hike but there is a shorter means to access the falls from Hilton Falls Conservation Area.

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Ontario’s First Rehab Hospital – St. John’s Rehab

Sunday October 25, 2015

The story of The Road To Recovery starts on October 28th 1837.  For me personally it started on October 23rd when my wife was transferred to St. John’s Rehab Hospital.  It was then that I discovered that the hospital hidden in the gardens on Cummer Avenue was the very first rehab hospital in Ontario.  Sunday afternoon I decided to park a short distance from the hospital and walk through Newtonbrook Ravine on my way to visit her.  It was a sunny afternoon and the fall air was fresh with a crisp breeze.

I parked on Manorcrest Drive near Bayview and Finch and entered Newtonbrook Park.  It was a windy day and the milkweed plants were shedding their seeds.  Milkweed is essential in the life cycle of the monarch butterfly and it is recommended that everyone grow milkweed in their garden.  Collecting local seeds and starting your own plants will bring these beautiful butterflies into your yard.

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This little park does not connect with the paved path unless you cross Newtonbrook Creek.  The water level was low and people have made a stone path through the water.  The park itself has some wild stretches along the creek.  The sunlight was working on the late leaves bringing the yellow and orange into a bright collage of colour.

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Along the side of Newtonbrook Creek there are extensive sand deposits.  The creek has cut through these indicating that it had a much stronger flow at times in the past.  The sandbank below had several small holes and one large one cut into it.  Suspecting a large animal, perhaps a coyote, had made that large hole I decided to work my way around for a closer view.  It is simply a spot where a large chunk of sand fell out due to erosion.

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Hannah Greir Coome was born in October 1837 at The Carrying Place, Upper Canada.  When Hannah’s husband died in 1878 she decided to dedicate her widowhood to the service of God and was on her way to England to join a convent.  Having stopped in Toronto on route she met a small group of people who convinced her to start a religious order in Canada.  She agreed and joined an Episcopalian-Anglican order in New York state for training.  She took her vows on Sep. 8, 1884 and this is the founding date for the Canadian Order of the Sisterhood of Saint John The Divine.  The archive picture below shows Mother Hannah in 1918.

Mother Hannah

On Dec. 27, 1884, the feast day of St. John The Divine, the Order formally opened it’s first convent called St. John’s House.  It was located at 71-73 Robinson Street, now renumbered 81-83, and included a dispensary to provide free medication to the poor.  In 1885 the adjacent property on Euclid Avenue was acquired and converted into an infirmary which was named St. John’s Surgical Hospital for Women.  Hannah had been born in the year of the Upper Canada Rebellion and delayed the opening of the hospital to participate in the 1885 Riel Rebellion. Hannah, along with nurses and a doctor, traveled to Moose Jaw to create a hospital for the Canadian Army.  By 1890 a larger hospital was required in Toronto and using this experience several lots were purchased on Major Street for a new facility.

This hospital featured large verandas which connected to, or over looked, the gardens.  From the beginning open air and access to nature were combined with scientific medicine and the Sister’s prayers and spiritual attention.  The hospital always operated independent of government funding and when 1930’s medical advances required excessive investment the Sisters decided to take advantage of their unique approach to convalescence.  In 1933 they had the idea to create a centre for rehab treatment for patients from all seven Toronto public hospitals.  This would free up beds in the hospitals for patients needing active treatment.  They laid the corner stone for their new building on Cummer Avenue on October 8, 1935.

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The Governor General of Canada officially opened the facility on May 22, 1937.  The original hospital had the same number of beds as the Major street facility and contained three floors of rooms with a four story bell tower.

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The Sisters owned 31.5 acres of land with the southern border being the Newtonbrook Ravine which features the type of natural beauty displayed above.  The property was flat farmland but they transformed it into a series of gardens so the patients could experience the calming effect of nature.

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The hospital was founded by an Anglican order on their spiritual principles to specialize in women’s care, especially for the poor.  However, they never turned people away based on their gender, race or social status.  They asked those who could pay to do so to offset the cost of tending  to the needy.  They have always included prayer and an open spiritual atmosphere as an essential element of their care.  Today they have an open policy that is accepting of all faiths. The chapel was consecrated on June 4, 1953 and is designed to accommodate those in all stages of recovery from beds to wheel chairs then to regular seating.  The chapel is beautiful inside and my wife and I spent a few quiet moments there.  On the east wall is a stained glass mural depicting the sisterhood’s contribution to nursing.  Notice the nun in the lower right hand corner.

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The hospital operated on the Sister’s experience that rehabilitation needed to look after more than just the body, it included the mind and spirit as well.  This led to the North American College of Physicians designating them as the standard for rehabilitation.  It occurs to me that hiking also challenges the body, stimulates the mind and soothes the spirit.  As I left the hospital I stopped to look back down the Road to Recovery at the bell tower and wondered how many people have traveled that road.  Going in via hospital vehicle and leaving to go home.

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I slowly made my way back through the ravine to the car enjoying the restorative wonder and beauty of creation.

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The Caledon Aerial Tramway – The Cox Property

Saturday Oct. 24, 2015

For over 100 years a steam powered aerial tramway has been hidden away in the Caledon hills. It was 8 degrees when we set out and it started lightly raining almost as soon as we found the west end of the tramway.  Having parked on The Forks Road near Dominion Street we walked up the hill to the hairpin turn.  This is where the Credit Valley Railroad (CVR) built their station.  The CVR was absorbed into the Canadian Pacific Railroad (CPR) who took over transportation for the mineral extraction activities in the area.  The embankment on the side of the railway has been reinforced by driving steel rails into the ground to support boards.

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The medina sandstone in the Caledon hills had not been exploited with much success until the coming of the CVR.  McLaren’s Castle was built in 1864 and is a rare example of local stone prior to the arrival of the railway in 1879.  For the next thirty years quarries mined all the easily accessed deposits until one by one they were closed.  In 1900 an aerial tramway was built to bring stone from the eastern embankment of the Credit River to the railway line.  This avoided bringing it down to Dominion Street and then back up the hill on the Forks of the Credit Road. McLaren’s castle is shown in the archive photo below but it was destroyed in a series of fires in the 1960’s.

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The Cox Property is the east half of lot 9 concession 4 while the west half of lot 9 is the Willoughby Property which features the Stonecutter’s Dam.  Both properties are owned by the Credit Valley Conservation Authority.  The CVC has taken a “hands off” approach to managing the Cox property.  No formal trails have been established and the area is being allowed to return to it’s naturally vegetated condition.  Almost immediately we found an area of disturbed rocks where steel rails could be seen underneath.  After a brief investigation we located the two inch steel cable from the tramway running through a chamber below ground.

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A little farther along several steel railway rails have been exposed.  These rails support chunks of stone that hide the chamber below where the cable runs.  Inside, the curving end of the tramway cable can be seen.

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I climbed into the chamber that the cable ran through.  After cleaning a bit of debris away I still couldn’t see where the cable went as it curved around a large block of cut stone and down deeper into the underground chamber.  Without preparations, or permission, it wasn’t possible to dig all the stone fill out of the chamber and discover if the cable turns on a hidden drive below.  The cover photo shows the cable from inside the chamber looking to the east where it entered this end of it’s route.  The walls are lined with cut stone and the roof is supported on a series of steel rails.  Above ground the rails are covered with a layer of stone that has been spread over the top.

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The steel wire rope used on the tramway had a two inch diameter as can be seen relative to the 28mm (1.1 inch) coin in the picture below.  The rope appears to have a 6 X 7 construction which means that it has 6 strands made of 7 wires each.  The six strands are wrapped around a central core. Without seeing a cross section it isn’t possible to determine of there is a 7th strand in the core making it a 7 X 7 rope.  Using 7 wires per strand allows for larger outer wire diameter which greatly improves abrasion resistance but reduces flexibility.  The wires in the strands of this rope run in the same direction as the stands and this is known as a “lang lay”. Depending on the exact construction this wire rope should have a breaking strength somewhere between 175 and 200 tons.

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Other evidence of past industrial use of the land is seen in the remains of a steel ladder.

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There is a small patch of horsetail growing on the side of the hill and most of it has been chewed off.  White tail deer will sometimes eat horsetail and we saw the departing end of a deer as we came through this part of the woods.

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Stone was brought from the quarry on the other end of the tramway and unloaded to waiting train cars on the CPR.  A large steel spike is seen protruding out of the side of the hill near where the tramway ended. This spike is similar to the ones I saw on the 1855 Gore and Vaughn Plank Road I reported in Dufferin Creek.

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The Cox Property was the site of quarry number two as well as several smaller quarries.  The picture below shows the face of one of the smaller quarries.  We found various metal and wire scraps in this overgrown quarry.

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Turkey tail fungus is known by the scientific name Trametes Versicolor and it grows on fallen hardwood and stumps.  This fungus contains a protein called PSK which has been shown to have anti-cancer properties.  It inhibits growth of breast and lung cancers as well various ones in the digestive system.  Treatment with turkey tail proteins has shown very little negative side effects.

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The eastern end of the tramway was at a much higher elevation than the western end and I could see that cable making an excellent zip-line across the Credit River valley.  This picture looks from near the terminus on the Cox Property across the valley to where the steam boiler that powered it hides at the other end.

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The Caledon aerial tramway has given up some of the secrets it guarded for the past century but I suspect that there is even more buried in that underground chamber.  The Cox property also contains a couple more quarries and access roads but after a couple of hours of non-stop rain, we decided to call it a day, leaving the rest for another time.

Please note that the Credit Valley Conservation considers this property to be private and as noted above, no trails are maintained on it.  Access to the property is by permission only.

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Abandoned Passmore Avenue

Sunday October 11, 2015

Passmore Avenue was never completed as a continuous road but today it has become even more fragmented.  I set out on Sunday afternoon to hike through the sections which had once been opened and are now closed (marked in green on the map below).  Passmore Avenue , also known as the 5th Concession, ran from The Scarborough – Pickering Townline to where the 404 now lies. Parts of it are still open under other names, including Gordon Baker Drive which lies on the old roadway. From Kennedy Road to Midland it still bears the name of Passmore Avenue. At Markham Road there are still sections running both east and west known as Passmore Avenue.

Steeles Avenue runs across the top of the 1877 historical atlas pictured below.  Passmore Avenue runs one lot below except where the line is dotted indicating that the road allowance was never opened.  The Rouge River cuts through the centre of the map between lots 12 and 13 (numbered along the top).  Between lots 10 and 11 runs Littles Road (yellow) which has also been recently closed.  It is shown extending one lot beyond Passmore Avenue but the southern portion has been closed so long the farmer has taken it back as part of the field.  The area east between here and the Rouge River is now Cedar Brae Golf and Country Club.

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This picture looks from the end of Littles Road along Passmore Avenue toward the golf course.

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In the field just before the golf club are the remains of a race track for horses.  It was built in 1966 and within 20 years it was gone.  From the ground little can be seen except the remains of the barn and the foundations of some out buildings.  The last three structures on the property were removed in 2002.  This picture is taken from standing on the racetrack looking north to where it curves left just before the trees at the horizon.  The outline of the oval track is still clearly visible from Google Earth.

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Passmore Avenue used to run east from Littles road.  On the county atlas there is a road which runs between lots 8 and 9 and divides John Sewells properties.  Today we call this Sewells Road (orange) and where it crosses the Rouge River on the map is the site of Toronto’s only suspension bridge.  The section of abandoned  Passmore Avenue (green) between Littles and Sewells roads has become fully overgrown.  It is little more than a strip of trees one chain wide (66 feet) along the end of the farmer’s field.

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I have walked through this section several times over the years and always find old pop bottles along here.  Today I found a 1962 Pepsi bottle but the condition was poor and I already have a better example.  Like all closed roads they seem to attract people with garbage.  There are the parts of an old truck scattered along the old road allowance.  The steering wheel is seen in the picture below.

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White asters bloom in places along the roadway.  These examples are smaller in size than their purple cousins that are common at this time of year.

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Motorists driving down Sewells Road would never see where Passmore Avenue emerges from the woods.  Two large trees stand guard over either corner of the former roadway and it’s intersection with Sewells Road.  The tree featured below is the southern of the two and has seen the transition from horses to model T’s and now to only the occasional hiker.

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The section of road along lots 7 and 8 was never opened but lot 7 was one of several owned by the Reesor family who lend their name to Reesor Road (pink).  I returned to the car and moved it to Gordon Murison Lane (red) which runs between lots 4 and 5 and leads to William Murison’s farm on the county atlas.  At the curve it joins Passmore Avenue and I parked where the maintained road ended.  I spoke briefly with the people who live in the old Murison home and they feel that the old roadway is now private property but have not posted it as such.  I walked from here through to the town line which is on the right side of the atlas pictured above.  The road allowance from the Murison’s through to Beare Road (brown) is a regularly used trail with the eastern section servicing a few houses.

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The final section between Beare Road and Town Line (grey) is almost impassible.  Dog Strangling Vine has taken over the most of the old road allowance.  This invasive weed wasn’t here when I last hiked this section in 2011.  I decided to make my way along the edge of the roadway because walking through the vines at this time of year helps spread the seeds.  Soybeans are being grown in the adjacent field.  Per acre, soybean produces more protein than most other land uses.  Some studies suggest that men who eat a lot of soy products may have a lower sperm count and it is not recommended for those hoping to conceive.

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Orange Crush was sold in small brown bottles following World War two until 1958 when the new clear Marilyn Monroe bottles were introduced.  These brown bottles were described as able to “protect the fresh fruit flavor from the harmful effects of light.”  I found a bottle that was, unfortunately, missing the bottom.  The applied colour label was badly faded on the side that was facing down (shown) and completely missing on the exposed side.

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When it was new the Orange Crush bottle would have  looked like the one I have on my desk at work. From left to right a 1970 no return 7-Up, 1860’s Minard’s Linament, 1906 Milk of Magnesia, 1949 Orange Crush, 1953 Pepsi, 1880’s perfume sampler, 1956 Coke, 1860’s Pitcher’s Castoria and a 1984 Labbatt Blue bottle complete this picture.

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A pair of abutments is all that remains where Passmore Avenue crossed Petticoat Creek.  There isn’t much water in here at the moment but at times there must be a fair bit.  The short span of the bridge can be seen in the cover photo.

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Passmore Avenue never ran the full length of Scarborough Township and several sections have since been closed.  Those sections make for an interesting hike where I always see something new each time I explore.

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Toronto’s Only Suspension Bridge

Sunday Oct. 5, 2015

The Rouge River flows between two historically significant bridges in Scarborough.  I decided to try to hike the river from one to the other.  I parked on Sewells Road a little north of the suspension bridge.  It was a nice fall day with temperatures in the “no bug” zone of 12 degrees.

Frank Barber (1878-1945) was a civil engineer who designed several bridges in Toronto including the Middle Road Bridge (1909) and the bridge at the Old Mill (1916) both of which were visited in previous posts.  In 1912 he designed the suspension bridge across the Rouge River on Sewells Road.  At the time, Toronto was expanding and access to new parts of the city was restricted by the deep ravines of the Humber, Don and Rouge Rivers.  This was one of the early bridges to provide a permanent crossing to the river in this area.

Suspension bridges are normally a solution for major waterways or wide valleys but this one is just 160 feet long. The bridge deck is concrete suspended 13 feet above the river by two cables securely anchored into the ground on either end. The cables are seen in detail in the cover photo.  These cables bear the load of the bridge which is suspended on hangers or vertical rods.  Barber completed the bridge in 1912 and it was restored in 1981.  It is one of only a few suspension bridges in Ontario and the only one in Toronto.  It is also one of 15 bridges listed as heritage properties by the city.

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Under the bridge is the distinctive nest of  the organ pipe mud dauber wasp.  This is an unusual wasp in that the male stands guard at the nest while the female gathers food.  One of the main food sources is spiders.  The wasps are about an inch long and as such are the largest of their species.

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Also under the bridge is the Google logo which is a rare example of graffiti that can actually be read.

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Rough Cockleburs grow along the side of the Rouge River.  This member of the aster family doesn’t have the usual wind blown seeds.  Instead, it spreads through seeds that grow inside of oval heads that are covered with spines.  They get caught in animal fur and clothing and can be carried long distances.  The cocklebur is also related to the sunflower and daisy and has been used for it’s anti-inflammatory and antimicrobial properties.

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I had chosen to try to follow the west side of the Rouge because a thirty foot sand bank on the east side of the river can be seen from the road.  As you get closer you can see that there are hundreds of Sand Martin holes along the edge of the cliff.  These birds dig winding holes into the side of the sandbank where they are difficult for predators to reach.  There is a large breeding colony living in this embankment.

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After disturbing a Great Blue Heron and traversing a mess of poisonous wild parsnips I discovered that there is an even taller sand bank on the west side.  It may be possible to pass on the edge of the river, but not when hiking alone.  The strip along the water’s edge is made of material that has fallen down the face of the sand bank and may not be very stable in spite of the thin vegetation growing on it.

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My attempt to make my way downstream to the second local bridge of interest wasn’t successful and so I moved my car to the Rouge Park Finch Meander Area parking lot.  Near the parking on Old Finch Avenue is a tree with a large number of artist conks growing on it.  They can be picked and the white underside scratched to produce pictures or writing which turns brown as the conk dries.  The surface then becomes hard and the artwork is permanent.

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On October 15, 1954 Hurricane Hazel landed in Ontario bringing heavy rain and strong winds and taking 81 lives in it’s wake. Rivers across the GTA flooded and bridges were destroyed or damaged on every major waterway.  Sections of the city were isolated and traffic flow was severely affected.  To get people moving again the army was called in to help build temporary bailey bridges.  Only one of these remains in service in Scarborough and it is the one on Old Finch Avenue.  It is 130 feet long and, along with the wood piers in the middle, was constructed by the 2nd Field Engineer Regiment in just 3 days.

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The Strawberry Fields Weren’t Forever

Saturday October 3, 2015

The Trafalgar, Esquesing and Erin Road Company established a toll gate on Trafalgar Road in Oakville near the present site of Inglehart Street.  Tolls were collected to pay for the maintenance of the plank road that was to be built from Oakville to Fergus.  We decided to return to Sixteen Mile Creek and continue north from Kerosene Castle, hiking on the east side of the creek.  We parked on Inglehart street near Trafalgar.  It was cloudy and windy with a temperature of only 7 degrees.

The Hamilton Radial Electric Railway Company was chartered in 1893.  In 1905 it was extended to Oakville and a large steel bridge was constructed across Sixteen Mile Creek.  The Oakville station is seen in this archive photo as it appeared in 1908 with one of the electric cars in front.

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The Oakville station is the only remaining one on the line but the building is abandoned today and has some broken windows on the front.  We took a short trip down to the site of the old station before starting our hike.  Some windows have been added to the rear portion of the building but otherwise it retains it’s original charm.

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Directly across the street from the train station is the Scout Hut built in 1926.  The location is perfect since Scouts were expected to be well trained.

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John Cross introduced the growing of strawberries to Oakville.  He found that the fruit grew wild in the area and was easily cultivated.  Soon others were following suit and by the mid 1870’s Oakville was the primary strawberry production area in the Dominion of Canada.  The delicate fruit was easily damaged and so to support it’s storage and transportation a local basket industry developed.  Cross designed a wood veneer basket that he produced.  Soon John A. Chisholm opened his own basket factory and expanded operations in 1874.  His son, Charles, invented a machine to slice wood veneer for the baskets.  By 1877 there were almost 750,000 fruit baskets being produced each year in Oakville.  In 1889 he sold the business which was re-named the Oakville Basket Company  three years later.  Although it was destroyed by fire twice it was rebuilt each time.  It operated until 1984 when it was finally shut down.  In it’s later years all the local strawberry fields had been subdivided for housing and so the factory produced Popsicle sticks and tongue depressors.  The drive wheel from the steam generator has been preserved and is located in Old Mill Parkette.

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We descended to the level of the creek soon after we crossed Trafalgar and began to make our way upstream. It was a windy morning and we were watching the wind burst in sudden swirls on the surface of the water.  Suddenly we heard a loud crack from directly across the creek and looked in time to see three quarters of a large tree collapse to the right.  As it came to rest the remaining section topped in slow motion to the left.  In all my time spent hiking in the woods this is the only time I’ve witnessed a tree fall and it most certainly does make a noise.  The broken and twisted remains of the tree stump can be seen in the picture below.

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Cormorants were fishing in the Sixteen Mile Creek.  The rock on the right in this picture had three of them standing on it at one point.  As they flew away they almost skipped across the top of the water like a flat stone.  The bird on the wing below slapped the water fast enough that the spray from the previous two impacts hasn’t settled back into the creek yet as it reaches for the next wing flap.

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The fall colours are still not at their prime but there are places where the display is beginning. The trigger for change is the shorter hours of daylight which causes the change to happen at nearly the same time each year, regardless of the temperature.

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The yellow iris has seed pods that contain rows of brown seeds.   These seeds react to the freezing and thawing cycle in the spring to wake them from their dormant state.

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We made our way along the shale embankment on the east side of the creek.  There were many places where we had to go part way up the embankment to get around a fallen tree or a place where there was no footing at the water’s edge.

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It’s quite common to find the remnants of some person’s temporary shelter in the woods. Seldom do they take the time to build from shale and have a more durable home complete with a fire place.

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A little past the shale home in the woods we decided to climb the hill where we found the Oakville St. Mary Pioneer Cemetery.  This cemetery contains Oakville’s founder William Chisholm and the first mayor George King Chisholm in a separate family plot surrounded by a wrought iron fence.  Like most pioneer cemeteries there is a tale of premature death and the loss of infants.  There are several stones here that record the tragic loss of multiple children within a family.  Weather has eroded some of the earliest stones until they’re almost illegible but the bold and deep carving of this one will last for many more centuries.

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We walked along the historical trail on the way back to the car.  It follows the street and is far less challenging than the arduous journey along the edge of the creek. Looking down at the curve in the creek where we had been climbing it was obvious that this is not a hike to be undertaken alone or by those just starting out.

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Much of the industry in Oakville was located on the west side of the creek and so a future journey may undertake to see what remains from this period.

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The Royal Oak Of Speyside

Saturday Sept. 26, 2015

Speyside is a ghost town.  Of the once thriving village only the corner store remains, and the closed building is starting to decay.  Many such communities dot rural Ontario but what makes Speyside different is it’s Royal Oak tree.  Fall started in a glorious way with sunshine and the early morning temperature of 12 degrees rising quickly.  It made for a perfect morning to go and check it out.

There were five one room schools in the area of Speyside.   These School Sections (SS) were SS #5 Waterloo, SS #8 Dublin, SS #10 Dufferin, SS #12 Lorne and SS #16 Stone.  In 1960 these 5 schools were replaced with the Speyside Public School.  This served until 1986 when it was closed and the students were dispersed between four other local schools.  The building now sits abandoned and is for sale.  The picture below from 1967 was supplied by Marion Frank-Rice who attended the school and can be found along with other memorabilia at   http://www.facebook.com/groups/SpeysidePS

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The school as it stands today with the addition of extra rooms and wire mesh on the windows.

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The story of the Royal Oak of Speyside actually starts in England in 1651.  England was near the end of their civil war and King Charles II was trying to escape with his life after the battle of Worcester.  He later reported that he had hid in an English Oak tree all day while parliamentarian patrols searched for him.  This tree became known as the Royal Oak tree and the English Oak got a new nick name.  May 29th was celebrated as Royal Oak Day for centuries in England to mark the restoration of the monarchy.  In 1937, to celebrate the coronation of King George VI on May 12th, acorns from Windsor Park in England were sent all across the commonwealth.  A one room school stood on 22 side road north of Speyside and a 1944 picture of the school is seen in the cover photo.  Students at SS #8 Dublin planted their acorn in a special evening ceremony in that year.  Marion’s father was among the group of students involved. When the school closed in 1960 they raised the money to have tree surgeons move the 20 foot high oak tree.  They planted it beside the gym at the new school where it continues to grow.  When the school closed in 1986 acorns were brought from England to plant “cousin” oak trees at Brookville, Limehouse, Pineview and Stewarttown where the Speyside students were transferred.  The Royal Oak of Speyside received an heritage designation in 2007 for it’s cultural significance.  The tree is expected to live for up to 500 years and the owner of this property is required to maintain it during it’s lifetime.

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Speyside grew into a considerable community as the street plan in the 1877 Halton County Atlas shows.

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The village had two hotels, two general stores, a tannery, a large stone quarry and a village hall. The picture below shows the only remaining building from the original Speyside.  Newer homes have been added over the years.  This structure operated as a store under many names and was even moved back from the road 17 feet in 1942 when the highway was paved.  Today it is closed and a few modern homes provide the only hint of the former life of Speyside.  Directly across the street from the store stood the original log cabin that served as a post office from 1873 until 1914.  The first postmaster is rumored to have been illiterate and relied on the school children from SS #10 to help him sort the mail.The post office closed in 1914 when rural mail delivery made it obsolete.

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We parked off 15 Sideroad in the Bruce Trail parking lot and went for a walk in the Speyside Resource Management Area.  Not far from the parking lot stand the remains of two kilns. These were used by Alexander Livingstone to dry the hops he grew when this was a farm.

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There is a pond along the trail which has a small sluice gate maintaining the water level.  It has been created by damming the tributary of the Sixteen Mile Creek that passes through town.

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Puff balls are one of several genera of fungi that do not have open caps or external gills to distribute their spores.  They form their spores in the centre of the fruit body.  When the fruit dries out it turns brown and the skin ruptures releasing a puff of spores from the ball.  When harvested around this time of year then sliced thinly and fried in butter and garlic they become quite tasty.  This one was too small to be bothered with but they can get to be nearly the size of a soccer ball.

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Along the side of the trail a series of hoses run between trees and end in this shed where maple sap is collected and boiled down to make maple syrup.

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Butter and Eggs flowers, also known as yellow toadflax, are related to the snapdragon. The flowers are often added to arrangements because they last for a long time after cutting. This plant has been used for an herbal remedy in teas for both diuretic and laxative effects.  This little flower has the power to make you go.

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The Glencairn Golf Club is just south of Speyside near the old school.  The concrete remains of a kiln can be seen from the roadside.

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Near the 1873 school was a quarry which came to be known as Scotch Block.  Stone from this quarry was used in several local bridges for piers and abutments.  In 1868 the Presbyterians used this stone to build their Boston Church on the 3rd line.

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There are plenty of nice weekend days left this year to get out and enjoy.  Fifteen of the top hikes are listed here.

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Rattray Marsh

Saturday, Sept. 19, 2015, and Monday, Sept. 11, 2017

Rattray Marsh contains fossils that help form it, abundant wildlife and 100-year-old abandoned structures. And that’s just in the corner we explored.  We set out to enjoy the last Saturday of summer and decided to visit the Rattray Marsh.  There is very little parking at the marsh and so we parked at the Bradley Museum.

James Rattray was born in 1887 and after having served in WW1 he made a fortune in the mining industry.  He was friends with Percy and Ida Parker who owned the Riverwood Estate.  In 1945 he bought the Fudger mansion along with 148 acres including the mouth of Sheridan Creek.  The historical atlas shows that the creeks emptying into Lake Ontario along this stretch all had a marsh where they emptied into the lake.  Today, the marsh on Sheridan Creek is the only one left between Toronto and Burlington.  The rest of them have been filled in and when James Rattray died in 1959 developers started making plans to build homes on this one too. The Credit Valley Conservation bought the property in 1972 after local residents petitioned to have the marsh saved.  It was opened as Rattray Marsh Conservation Area in 1975.

The shoreline along this part of the lake is made up of flat stones that have been rounded through years of wave action.  They have been washed up on the beach in a wall known as a shingle bar.  This rock barrier slowed and sometimes stopped, the flow of Sheridan Creek into the lake.  The waters pooled behind this wall and silt settled on the bottom where aquatic plants took root forming the marsh over time.  The picture below shows the mouth of Sheridan Creek and the rock barrier, or shingles bar, that maintains the marsh.

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The threat to the marsh actually started long before the developers made specific plans to fill it in. Without realizing it they had already initiated a slow process that would do so.  As development occurred on properties upstream the amount of sediment in the marsh increased.  Buildings, roads, and parking lots don’t absorb water like fields and forests do. Water runs off quickly and carries soil and other dirt into the creek.  The water slows down in the marsh where this silt settles and quickly buries the natural ecosystem.  To restore the marsh some of this sediment was removed to expose the native soil and allow the seeds trapped inside to germinate.  White carp have also invaded the marsh and are disturbing the sediment on the bottom through their feeding.  This has destroyed plant life and the habitat it provided. The carp have been isolated and are now kept out by fences in the marsh like the one pictured below.

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We did a little beach combing looking for interesting rocks and fossils.  The wall of shingle stones along the shoreline is full of fossils.  The remains of these long-gone creatures now serve to keep the creek out of the lake and helped the marsh to form.  There were many small stones with multiple fossils of worms in them.

Along the lake shore at the creek mouth, there is a deteriorating break wall that was installed to help preserve the marsh from erosion.  A little east of here a large concrete chamber stands looking out over Lake Ontario.  The top is broken off and several small trees are taking root inside.  This was likely built in 1918 when Fudger had the house built on the property,  He was obsessed with fire protection and built his house out of concrete.  This appears to be an old pump house, perhaps part of a fire suppression system.

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Turtlehead flowers grow in moist soil and bloom from late in August through to October. They get their name from the shape of their white, red or pink flowers which look like a turtle with its mouth open.  Turtlehead flowers have been used in traditional medicines for centuries.  They make an excellent remedy for skin sores as well as reportedly being used for birth control by some native tribes.  They are a favourite food for white tailed deer like the young male featured in the cover photo.

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Aside from carp, Rattray Marsh has also been invaded by the emerald ash borer.  This little green insect kills 99.9% of all ash trees it comes into contact with.  Unfortunately, most of the tree cover in the marsh and surrounding area is ash.  The picture below shows trees with an orange mark on them.  These are infested with the ash borer and will be cut down and replaced with new plantings.  Trees that are not infected can be protected against the insect at a cost of about $200 per tree for an injection that must be repeated every two years.  Injected trees have a little metal tag on them.

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On Monday, September 11, 2017, we returned to the marsh to explore the boardwalks and see what the back half of the park holds.

The Trans Canada Trail and the Waterfront Trail pass through the 90-acre park on a common boardwalk. There is a secondary trail which is 1.8 km long and a small 0.3 km loop known as the Knoll Trail.  Credit Valley Conservation has recently completed upgrades and replacements to much of the boardwalk around Sheridan Creek and they reopened on September 2, 2017.

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Rattray Marsh was rather low on water and we could see where it had been several feet deeper recently.

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Google Maps Link: Rattray Marsh

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