Sam's Point
Ellenville, NY - June 19, 2010
Vi and I went hiking at Sam’s Point. It’s about a 40-minute drive in the village of Ellenville. Off the main road is a narrow road flanked by trees and private homes on either side until after about three miles of driving we approach the visitor center at Sam’s Point.
From there, over 10 miles of trails loop around Sam’s Point.
Sam’s Point's geological formation is characterized by its ridges -- massive bedrocks protruding along the top’s sides of the Shawangunk Mountains. The ridges were formed 270 million years ago when 470-million year-old sedimentary rocks submerged deep in the ocean were uplifted through geological events. The rocks are made of white quartz pebbles and sandstone fused together and hardened by silica for millions of years.
There are several attractions on top of the Shawangunk Mountains. On the plateau there is big lake (Lake Mataranza), a waterfall taller than Niagara Falls (Verkeerder Falls stands at 180 feet while Niagara Falls is 173 feet), and “the largest open fault in the United States with corresponding ice caves”. Because of the cool climate inside the caves, ice is present all year round.
Rising as high as 2,289 feet, with easy-to-reach rocky cliffs all along its perimeter, Sam’s Point offers a spectacular view of the valley around it below. And even if one ventured only within its perimeter to explore the many attractions inside Sam’s Point -- its lakes, caves, and waterfalls -- 10 miles may seem daunting when looking at the map but the continuous array of visual treats along the way will make the hike hardly felt at all.
Sam’s Point got its name from the story about a man called Sam being chased by Indians who jumped off a ridge and survived.
(source: wikipedia.org)
Click on a picture to enlarge.
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