News   GLOBAL  |  Apr 02, 2020
 10K     0 
News   GLOBAL  |  Apr 01, 2020
 42K     0 
News   GLOBAL  |  Apr 01, 2020
 5.9K     0 

Nothing happens to streetcars in the snow. It is not at all unusual to see rubber tired vehicles stranded, while rail vehicles sail right on through. The biggest concerns are idiot snowploughs blocking the trackage (not much of a concern on private rights-of-way), or cars parking closer to the tracks because of snowbanks (also not a concern on private rights-of-way). Ice storms are also a concern, but that's a different thing entirely.
 
Uhh... Say what you will about P3s, but the arrangement is specifically designed to pass the maintenance cost onto the contractor. The TTC as operator will not be responsible for maintenance costs. The line is owned by Metrolinx and Crosslinx will continue to maintain the line for 30(?) years.

That's actually the point, because at this late date any work going on (and holding up commissioning) is not maintenance but rather correction of deficiencies in the construction...., which the builder and ML will claim is the other guy's fault. Or unnecessary.
And while they argue, TTC will be unable to commence operation.

- Paul
 
Nothing happens to streetcars in the snow. It is not at all unusual to see rubber tired vehicles stranded, while rail vehicles sail right on through. The biggest concerns are idiot snowploughs blocking the trackage (not much of a concern on private rights-of-way), or cars parking closer to the tracks because of snowbanks (also not a concern on private rights-of-way). Ice storms are also a concern, but that's a different thing entirely.

With all due respect, in my area of TO snow and ice (freezing rain) tend to come either in the same storm or the snow quickly becomes icy.

Not sure they are different things entirely.

How do the streetcars deal with icing over?
 
Last edited:
With all due respect, in my area of TO snow and ice tend to come either in the same storm or the snow quickly becomes icy.

Not sure they are different things entirely.
They are totally different things. An ice storm doesn't really involve snow, at least through most of its cycle.
A simplified explanation is that it's a rare phenomenon where the ground temperature is actually colder than the temperature higher in the atmosphere, so rain falls and when it gets down to something on or near the ground that water freezes and the ice accumulates more and more with each rain drop. There doesn't have to be any snow for this to happen, though snow can come later after the ice is already there. They are rare. There was an infamous one here in 2013. There was a disastrous one in Quebec in 1998.

A snow storm has none of the above happen. It's just snow, no rain.
 
Last edited:
Bayview-Eglinton is one of those places where even before Crosstown I wished I had had a Sim City-esque landscape tool to raise all four corners a few meters. Could have the LRT cross at current road level and not have such a climb up to Mount Pleasant, but also take a chunk out of the sharp down grade on 3 sides.
There's a over a kilometer of distance between Bayview and Mount Pleasant. Even if the tunnel was built at the same depth from ground level between the two, the slope between the two is insignificant to non-existant.

Precisely. Absolutely nothing. The only issue I've seen, about once or twice a decade, is the occasional ice storm.
And to be honest, there's a very, very good chance that the LRTs on Eglinton will be less affected by ice than the streetcars on the rest of the system.

Dan
 
There are rumours of possible tracks sinking near the Bayview station due to quick sand.

I’m not sure about that but there are hidden rivers in that part of town.

You guys were all getting sick of me joking about "Cracked foundation slab at Eglinton" but this is ever better.

I didn't even know you could have quick sand in non tropical regions.

Hahaha.

😄 :eek:

It's different geology at Laird. The issue is was at Bayview - Leaside station, not at Laird station.

You can see a typical Leaside borehole log at https://files.ontario.ca/moe_mapping/downloads/2Water/Wells_pdfs/727/7278792.pdf - as you can see from 30 feet to 60 feet is sand, with sandy clay/silt on top, and clay underneath.

But at Laird (https://files.ontario.ca/moe_mapping/downloads/2Water/Wells_pdfs/726/7263118.pdf) there's silt in the matrix all the way to the bottom, at 80 feet.

I think the log I did in the 1990s said "flowing sands" - but it was a long time ago - and before drillers had to submit their own (typically under-described) logs to the Ministry.
Laird Station
View attachment 667333


Leaside Station
View attachment 667334

Bayview / Eg is the site of the former path of Walmsley Brook. It survives south of the CPKC tracks near the future Ontario Line MSF, and its headwaters are historically by Duplex and Montgomery. I traced its route in 2018.

Untitled.png


I should also quote back to this:

At City Council, Mike Colle was blasting the Premier on Bill 212. During the rant, he makes a comment that "He should complete the f-ing Eglinton Crosstown. After 13 years, you'd think he would focus in on finding out why the Eglinton Crosstown tunnel is sinking."

I know folks here are adamant that there's no crack in the Eglinton - Yonge station box. But I'm very curious if there's basis for Colle's comment.
 
The exact same thing will happen as does with the streetcars that operate on private rights-of-way.
The vehicles would be able to perform better than the streetcars since they are paired together and will use both car pantographs. You can fit one or both cars on a few trains with ice scraper contact strips for when freezing rain gets bad enough. The one benefit of having couple vehicles from the get go is the distributed power between cars.
 
It's different geology at Laird. The issue is was at Bayview - Leaside station, not at Laird station.

You can see a typical Leaside borehole log at https://files.ontario.ca/moe_mapping/downloads/2Water/Wells_pdfs/727/7278792.pdf - as you can see from 30 feet to 60 feet is sand, with sandy clay/silt on top, and clay underneath.

But at Laird (https://files.ontario.ca/moe_mapping/downloads/2Water/Wells_pdfs/726/7263118.pdf) there's silt in the matrix all the way to the bottom, at 80 feet.

I think the log I did in the 1990s said "flowing sands" - but it was a long time ago - and before drillers had to submit their own (typically under-described) logs to the Ministry.
Laird Station
View attachment 667333


Leaside Station
View attachment 667334
I found an article about Leaside's construction here
Leaside station box was dug down to 22 metres or 72 feet. The pilings for the station are even deeper. Some down to 27 metres and others down to as much as 50 metres. So I highly doubt anything in the area is sinking
 
Same problems happened with Keele Station and High Park Station of Line 2. There are underground creeks in the neighbourhood of those stations. Keele School had to be rebuilt because of the rather loose soil

1753123796115.png

(High Park should have continued north of Bloor Street following those now buried ravines.)
 
Last edited:
Bayview / Eg is the site of the former path of Walmsley Brook. It survives south of the CPKC tracks near the future Ontario Line MSF, and its headwaters are historically by Duplex and Montgomery.
Excellent work!

I've always wondered what happened if you managed to inadvertently dam across the more conductive sands and gravels where an old creek was, with foundations and caisson walls.

It wouldn't be the soils themselves that are the issue, but the groundwater rising higher than it used to in places, trying to find a new path. It shouldn't really be a problem other than leakage, unless they were somehow washing away all the fines - and that would take years. I've got a story to tell one day of a building on a different Toronto former creek, but it will have to wait a decade or two for the legal stuff to stop flying.

Leaside station box was dug down to 22 metres or 72 feet. The pilings for the station are even deeper. Some down to 27 metres and others down to as much as 50 metres. So I highly doubt anything in the area is sinking
Gosh, that is deep! And presumably designed that way because of the unusual sands we've been discussing.
 
Bayview / Eg is the site of the former path of Walmsley Brook. It survives south of the CPKC tracks near the future Ontario Line MSF, and its headwaters are historically by Duplex and Montgomery. I traced its route in 2018.

View attachment 667702

I should also quote back to this:
Thanks for this excellent work, I've always wondered where the creek ran, as I presumed it would be north to south. Since it does come out as a creek past the railroad tracks, I have to presume there is still running water underground. In the 1970s, when construction projects were probably not as well researched before they started, building sites downtown kept "rediscovering" Taddle Creek, forcing a change in plans after holes had already been dug!
 

Back
Top