Jeff Munroe<p>Students in my Quaternary Geology course came at this exposure from the bottom up, and the top down -- a curious sequence of basal till overlain by silty lake sediments deformed by a later glacial readvance. <a href="https://fediscience.org/tags/geology" class="mention hashtag" rel="nofollow noopener noreferrer" target="_blank">#<span>geology</span></a> <a href="https://fediscience.org/tags/earthscience" class="mention hashtag" rel="nofollow noopener noreferrer" target="_blank">#<span>earthscience</span></a> <a href="https://fediscience.org/tags/vermont" class="mention hashtag" rel="nofollow noopener noreferrer" target="_blank">#<span>vermont</span></a> <a href="https://fediscience.org/tags/Quaternary" class="mention hashtag" rel="nofollow noopener noreferrer" target="_blank">#<span>Quaternary</span></a> <a href="https://fediscience.org/tags/outside" class="mention hashtag" rel="nofollow noopener noreferrer" target="_blank">#<span>outside</span></a></p>