In absence of @Tidgy’s Dad, I wanted to share with you all some pictures of... my fossil hunting in Canada! Adam, I was thinking of you a lot on this trip!
(It was also part of my geocaching hobby; challenges like this are called EarthCaches.)


Canadian Museum of History is probably one of the most visited museums in Canada, featuring a huge hall with totem poles, a detailed story of the First Nations and European settlement, and a giant wing for kids (always a perk!). What is also extremely interesting is that the building itself was constructed from the so-called Tyndall Stone, a type of limestone full of trace and body fossils. So, it’s history in and out!

450 million years ago (in what geologists call the Ordovician Period), what is now southern Manitoba was at the bottom of a shallow tropical sea. Abundant marine organisms lived in this tropical sea, mostly on or near the seabed. When these organisms died, they became incorporated into the mud, and the calcium carbonate in their skeletons provided lime that contributed to the transformation of the mud into limestone.
Here are some of the examples we saw:







Canadian Museum of History is probably one of the most visited museums in Canada, featuring a huge hall with totem poles, a detailed story of the First Nations and European settlement, and a giant wing for kids (always a perk!). What is also extremely interesting is that the building itself was constructed from the so-called Tyndall Stone, a type of limestone full of trace and body fossils. So, it’s history in and out!

450 million years ago (in what geologists call the Ordovician Period), what is now southern Manitoba was at the bottom of a shallow tropical sea. Abundant marine organisms lived in this tropical sea, mostly on or near the seabed. When these organisms died, they became incorporated into the mud, and the calcium carbonate in their skeletons provided lime that contributed to the transformation of the mud into limestone.
Here are some of the examples we saw:





















