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Mount Toby information


Mount Toby
Mount Toby as seen from South Sugarloaf
Highest point
Elevation1,269 ft (387 m)
Prominence856 ft (261 m)
Coordinates42°29′16″N 72°32′15″W / 42.48778°N 72.53750°W / 42.48778; -72.53750
Geography
LocationSunderland and Leverett, Massachusetts Massachusetts, U.S.
Parent rangeAssociated with the Metacomet Ridge
Geology
Age of rock190 million years
Mountain typeFault-block; sedimentary
Climbing
First ascentElnathan Toby (first reported)
Easiest routeTelephone Line Trail

Mount Toby, 1,269 feet (387 m), is the highest summit of a sprawling collection of mostly wooded hills and knolls that rise from a distinct plateau-like upland in the towns of Sunderland and Leverett, Massachusetts, just east of the Connecticut River. This mountain mass, part of the Metacomet Ridge geology, is oval shaped and roughly three miles by two miles wide. Although three of the subordinate peaks have names of their own (Roaring Mountain, Ox Hill, Bull Hill), none of them are noteworthy on their own, and the designation “Mount Toby” is most often used (locally and formally) to describe the entire geologic mass.[1][2] This article, therefore, describes the entire Mount Toby upland.

Mount Toby is notable for its high biodiversity, attractive woodlands, waterfalls, and its glacial kettle ponds (most notably Cranberry Pond). Although the summit is wooded, there is a fire tower, open to the public, which provides 360-degree views of Amherst and the Holyoke Range in the south; the Connecticut River and Mount Sugarloaf to the west; Mount Snow, Mount Ascutney, and Mount Monadnock in the north; and the nearby Peace Pagoda in Leverett to the east. Additionally, there are several cliffs located on the lower south and southwest facing slopes overlooking the Connecticut River Valley and the town of Sunderland.[3]

  1. ^ "Mount Toby Ecosystem.” Archived 2009-02-25 at the Wayback Machine The Mount Toby Partnership. University of Massachusetts Amherst. PDF webfile, cited November 30, 2007.
  2. ^ "Stratigraphy and Paleocology of the Deerfield Rift Basin (Triassic-Jurassic, Newark Supergroup), Massachusetts". Guidebook for Field Trips in the Connecticut Valley Region of Massachusetts and Adjacent States. vol. 2, 84th annual meeting, New England Intergollegiate Geological Conference, The Five Colleges. Amherst, Massachusetts. October 9–10-11, 1992: 488–535. Cited from the web, Dec. 1, 2007.
  3. ^ Christopher J. Ryan. Mount Toby Trail Map. Fourth edition. Newall Printing, Amherst, Massachusetts, 1999.

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