Cross-River Cousins
This week I climbed Sugarloaf Mountain (652 feet) and then North Sugarloaf Mountain (791 feet) and finally Mount Toby (1269 feet).
![from-sugarloaf Mount Toby, seen from Mount Sugarloaf](https://stephenhartshorne.com/wp-content/uploads/2010/08/from-sugarloaf.jpg)
![from-toby North and South Sugarloaf from Mount Toby](https://stephenhartshorne.com/wp-content/uploads/2010/08/from-toby1.jpg)
North Sugarloaf is composed of hard basalt, while South Sugarloaf is made of sandstone, and was formed by the southward moving glaciers in the ‘lee’ of North Sugarloaf, a kind of shadow. That’s why South Sugarloaf is eroding away much more quickly and a saddleback has formed between the two.
Mount Toby on the other side of the Connecticut River is composed of (what else?) Mount Toby conglomerate. Now cross-river cousins, Sugarloaf and Toby were once on different continents.
August 4, 2010 @ 1:11 pm
And what a view you get from the top! Lovely pictures.