On our trip to the west coast of Newfoundland this past weekend, we took a drive to see one of the best-loved sites in the area, the Tablelands.
The Tablelands, found between the towns of Trout River and Woody Point south-west of Gros Morne National Park, look more like a barren desert than traditional Newfoundland.
This is due to the ultramafic rock (high in minerals), peridotite, which makes up the Tablelands. It originated in the Earth’s mantle and was forced up from the depths during a plate collision several hundred million years ago. Peridotite lacks the usual nutrients required to sustain most plant life, hence its barren appearance. Peridotite is high in iron, which accounts for its brownish rust colour.
Norm 2.0 is a “born and raised bilingual Montrealer” who I’ve followed for the last few years here on WordPress, and more recently on Instagram.
I particularly enjoy his weekly photography feature, Thursday Doors, “allowing door lovers to come together to admire and share their favorite door photos from around the world.”
From his About page:
“Among my many interests, I like to write, travel, bake, work wood, enjoy wine, play tennis, grow vegetables and take pictures.
This blog is my creative outlet to share any of the above and so much more.”
selfishly chose the following post of Norm’s to highlight because it’s his Thursday Door post from right here in Newfoundland and Labrador. The photos are from his recent trip to Gros Morne National Park on the west coast of the province.
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Have a great weekend, everyone.