this post was submitted on 06 Dec 2024
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Because the world seemed so different in the past, it’s very easy to forget that the planet has almost always been subjected to the same processes we can observe in the modern day!
Think modern day examples– like windblown dust from the Sahara traveling with the winds of the intertropical convergence zone to end up as a primary nucleation point and fertilizer for the Central and South American Rainforests!