Estimated Read Time: 7 minutes (but trust me, it's funny)
The Top of the World (sort of)
Thanks to a high-speed collision – and some discovery and then re-discovery (or not) – we get to introduce you to the mountain behind the ecosystem.
So, this is it – the top of the world. Well, the top of the Rocky Mountain world, at least. Well, where we’re standing isn’t the top of the world – that would be the ice dome that caps Mount Robson peak and, with apologies, I’m not conquering that for you. In fact, very few people have. Though famed as one of the most iconic mountain climbs in the world, it’s believed that only about one in ten succeed.
The reason? Well, it’s tall for starters – 3954 metres, to be exact – which makes it the tallest in the Canadian Rockies.
Though by default your eye looks to the top of the mountain, to really understand what makes Mount Robson so formidable, you need to look down.
Unlike most tall peaks, Mount Robson rises from the valley floor. As a result, you can see where it starts and where it ends – at least, when it’s not covered in cloud, which is rare – and that’s why geologists refer to it as a prominent peak (seriously, we couldn’t have come up with a more creative name?) because its, um, prominence helps us better judge the size of the peaks around it.
In fact, because this peak doesn’t start halfway up a mountain, the distance from the valley floor to its top amounts to 3128 metres – making the elevation gain of Mount Robson the largest of any peak anywhere in the Rockies.
Which is not to say it’s one of the highest peaks in Canada. Despite their, um, rocky nature, the Rockies don’t account for any peak in Canada’s top 20 (Mount Robson comes in at number 21…so close, little buddy).
But this peak is a mammoth fortress, and it’s the first massif – or sizeable block of rigid rock jutting from the Earth’s crust – that moist Pacific air crashes into on its eastward journey.
That’s the reason why Mount Robson can literally create its own weather system – it’s size, especially compared to the relatively low-lying valleys, enables it to design a regional microclimate that’s one of the most unique in the world: the inland temperate rainforest found near its base.
In case you’re a nut for rocks, this is where you’re probably keen to know it was formed 100 million years ago, according to new research. Which means Mount Robson and other Canadian Rocky Mountain peaks are super young in geology terms. Which is also why they’re so pointy. The younger the mountain, the sharper its edges; the older the mountain, the rounder it becomes (thanks erosion!). Which, when you think about it, is basically a metaphor for human aging, just over a much, much larger time scale.
According to scientists from the University of Alberta, the Rockies weren’t formed by a “gradual accumulation of matter”, but rather by a high-speed collision – again, high speed is relative to geologists (if you’re picturing two mountain-like trains colliding at 100 kilometres an hour, you’ve forgotten why geologists are rarely the toast of the party).
So, what does that mean then? I’m not even going to try to explain. Take it away U of A!
“The results suggest that an ocean basin off North America’s west coast descended beneath the ribbon-shaped microcontinent, dragging North America westward, where it collided with the microcontinent.”
Neat.
