Welcome to On Verticality. This blog explores the innate human need to escape the surface of the earth, and our struggles to do so throughout history. If you’re new here, a good place to start is the Theory of Verticality section or the Introduction to Verticality. If you want to receive updates on what’s new with the blog, you can use the Subscribe page to sign up. Thanks for visiting!
Click to filter posts by the three main subjects for the blog : Architecture, Flight and Mountains.
Mountains and Glaciers
The relationship between mountains and glaciers is a fascinating one. Where glaciers exist, the morphology of a mountain created the conditions necessary for a glacier to form. Once formed, a glacier’s growth and movement will slowly erode away the very mountain that created it. Over time, this movement carves and changes the landscape, resulting in moraines, cirques, fjords, and various other landforms.
Altitudinal Zonation : Mountains and Verticality
The earth’s atmosphere is defined by vertical gradients. As one rises, the air thins out, humidity decreases, and temperatures drop. It’s why we get altitude sickness when we travel to high places, and it’s why the tops of very high mountains are snow-capped. These vertical gradients are defined by altitudinal zonation.