Another interesting observation is the increasing annoyance of drivers. In summer they seemed to just accept the invasive cyclists and clinch fists in silent rage inside their AC-ed vehicles. In winter drivers are the nicest - take up the whole street and nobody will honk. My theory on that is that they just don't want to mess with "crazy" people; oh well, their loss. The fall time, at least this year, seems to be the polar opposite - our sworn enemies seem to be vexed by us not being in a rush to hang those Raleighs and Giants on the garage wall, especially when the weather is absolutely summery. Honking and overtaking with revving engines seem to be the new... well, new honking and revving, just the number of the incidents has increased recently. Or may be I just ride less carefully.
It seems, however, that a number of cyclists take the dangers of commuting rather seriously. Lots of pedal-propelled commuters live with the USSR Pioneer motto on their lips - "Always prepared!" Thus the observed increase in the aggressive driving behavior is supported by the surging preparedness of the cyclists:
Once out of the streets, end of October is probably the best time to ride. The "urban mountain" that us Montrealers are so proud of, but that we so rarely visit, is something worth having a one-day pilgrimage to. Once out of the wide gravel road and a hundred meters into the "woods" you can actually forget, only for a couple of minutes, about the civilization that is about to jump on you from around the corner:
Here's an igneous rock, formed by magma solidifying underground, with a xenolith (from Greek: xeno: alien, lith - rock) - the white spot in the middle. When magma was moving under ground, a piece of the vent broke off and entered the flow, but did not melt. When magma solidified, the rock remained imprisoned in it:
On the picture below, in the left top corner, the coarse-grained igneous rock that cooled from magma underground, is neighboring the preexisting sedimentary rock (bottom right). Along the border traces of contact metamorphism can be seen. There the hot molten magma came in contact with sedimentary rock and changed its mineral structure.
The cemetery is also a great place to visit. The background is rather peaceful than grim, so you don't have to be an adept of black humor to enjoy the tour. For the sake of style however, here is a color-accented depiction:
That, amici, is all. Now get out there and see what can you find yourselves!
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