Crater Lake National Park is one of those places like the Grand Canyon I’ve seen hundreds of photos of, and just like the Grand Canyon, it was one of those iconic, majestic, awe-inspiring, huge natural places I told myself I would go see someday. This summer, after cancelling a trip to go in 2020, I made it.
The first view I glimpsed after a long morning of driving was just like the pictures I’d seen. But, well, better, bigger and bluer. Much like the immensity of the Grand Canyon, the deep blue hue of the water and the sheer size of it, the steep gradient of the inner slopes, just cannot be quite captured in photographs or words. Seeing something like this in person is truly incredible.
Partway up the island, northwest of Qualicum Beach (well-known for its beaches and ban on national chain stores) are the Horne Lake Caves. The four official caves are part of the Horne Lake Caves Provincial Park along the Qualicum River. The caves are part of a karst topography, which typically forms where acidic water (commonly rainwater) dissolves rock. Generally, most caves form in limestone because it is especially susceptible to anything acidic. Limestone is a sedimentary rock made of marine fossils (often micro-fossils). This tell us that millions of years ago, there was once a sea or ocean where there is now limestone rock.
Since hearing about the big earthquake on the weekend, my thoughts have been drifting to New Zealand more frequently than usual. I was lucky enough to live there for a number of years, and I am so in love with the place – it has to be my favourite and most beautiful place on earth.
On a search to find the hike to Benson Creek Falls and Ammonite Falls near Nanaimo, my partner and I walked through the forest listening for the sound of flowing water. After a summer of drought, the creek was running pretty low and the falls turned out to be only a mere trickle. We weren’t even sure we found the right waterfall. Unfortunately, the trail signs at Benson Creek Falls Regional Park are not all that well marked and there is no signed map at the parking lot.
However, we still managed to have a nice walk and found some other surprising things instead. Its not the first time one of our hike hasn’t gone to plan for whatever reason, and for the most part, we tend to look on the bright side. Even if we miss what we came to see, its usually still an enjoyable walk and time spent outside.
Everywhere, the Canadian Rockies are scoured and marked by the power of ice. We have these powerful glaciers to thank for much of the beauty we now enjoy. Banff NP’s Lake Louise at 1,731m elevation is one example of one such famous site created by glacial erosion.
Above the head of the lake lies Victoria Glacier, a valley glacier, which feeds Lake Louise with beautiful blue-green meltwater (Britannica). Years ago, the Victoria glacier probably once extended much further into the valley while only a fraction of it remains today.
The Bow Valley of Banff NP, which today provides a rich habitat we are familiar with, was once covered by glaciers and ice 20,000 years ago during a period of time known as the Last Glacial Maximum. Glaciers carved through the mountains, creating a U-shaped valley with a flat bottom and steep sides. These glaciers disappeared from the Bow Valley by about 13,000 years ago, beginning the development of today’s modern montane valley (Reasoner and Huber, 1999).