Search results
Results from the WOW.Com Content Network
Target Lodging was number #305 on the list of 5,000, with three-year growth of 1,225 percent. Its revenue increased from $3.5 million in 2008 to $45.8 million in 2011. Inc. Magazine also ranked Target Lodging number #19 on the list of top 100 business products and services companies. [26]
Saddleback Maine is a ski resort located in Sandy River Plantation, near Rangeley, Maine, on the northwestern slopes of Saddleback Mountain. It is the largest independent ski area on the east coast, in terms of number of skiable acres (600). It has (6) lifts, (85%) snowmaking percentage, vertical drop (2,000 feet [610 m]), and skier days.
Saddleback Mountain (Lewis, Essex County, New York), 963211 Saddleback Mountain (Keene, New York) , 970556 Saddleback Mountain (Bandera County, Texas) , 1345828
Get AOL Mail for FREE! Manage your email like never before with travel, photo & document views. Personalize your inbox with themes & tabs. You've Got Mail!
The State Range Trail begins at the lodge and continues 3.1 miles (5.0 km) to the col between Gothics and Saddleback, then turns up Saddleback for the final 0.6 miles (0.97 km) to the top. The saddle-shaped ridge between the two peaks is 0.2 miles (0.32 km). [5] Saddleback can also be hiked as part of a complete hike of the Great Range. [6]
Discover the latest breaking news in the U.S. and around the world — politics, weather, entertainment, lifestyle, finance, sports and much more.
The Appalachian Trail, a 2,170 mi (3,490 km) National Scenic Trail from Georgia to Maine, runs along the ridge of Saddleback, crossing the summit. Saddleback Maine, a ski area, is located on the north face of the mountain. Ranging from beginner trails to advanced and expert trails, the mountain contains 66 ski trails along with 5 ski lifts.
Packsaddle Mountain is a laccolith set in the Chihuahuan Desert where it is a landmark along Highway 118 which skirts the eastern base of the mountain. The mountain is composed of a core of intrusive igneous rock that forced up and breached the roof of light-colored Late Cretaceous sedimentary rock of the Boquillas Formation and the Pen Formation, leaving the strata tilted around the ...