Saddle Ball Mountain
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Located in
Berkshire County Berkshire County (pronounced ) is the westernmost county in the U.S. state of Massachusetts. As of the 2020 census, the population was 129,026. Its largest city and traditional county seat is Pittsfield. The county was founded in 17 ...
, Saddle Ball Mountain is the 2nd highest peak in the
Commonwealth of Massachusetts Massachusetts ( ; ), officially the Commonwealth of Massachusetts, is a U.S. state, state in the New England region of the Northeastern United States. It borders the Atlantic Ocean and the Gulf of Maine to its east, Connecticut and Rhode ...
. List of mountains in Massachusetts Other than the
Mount Greylock Mount Greylock is the highest point in Massachusetts at 3,489 feet (1,063 meters). Located in the northwest region of the state, it is part of the Taconic Mountains, a geologically distinct range from the nearby Berkshire Mountains, Berkshire ...
summit itself, Saddle Ball is the highest in a series of four outcroppings or lobes along the southern ridge of the Mount Greylock Range. The
Appalachian Trail The Appalachian Trail, also called the A.T., is a hiking trail in the Eastern United States, extending almost between Springer Mountain in Georgia and Mount Katahdin in Maine, and passing through 14 states.Gailey, Chris (2006)"Appalachian Tra ...
(AT) intersects and parallels this ridge as it heads north toward the summit of Mount Greylock. The Albany 30 x 60 Quadrangle map locates the highest outcropping of Saddle Ball on the Appalachian Trail, about 0.2 to 0.3 miles north of its junction with the Jones Nose Trail.


History / name

Mount Greylock was known to 18th century English settlers as Grand Hoosuc(k). In the early 19th century, Greylock was called Saddleback Mountain because of its appearance when viewed from the south. From this view, Saddle Ball Mountain is the cantle of the
saddle A saddle is a supportive structure for a rider of an animal, fastened to an animal's back by a girth. The most common type is equestrian. However, specialized saddles have been created for oxen, camels and other animals. It is not know ...
and Mount Greylock the pommel. Saddle Ball Mountain itself was formerly known as Mt. Griffin during the early 1800s. By the mid-eighteen hundreds, the name controversy between Greylock versus Saddleback was resolved, leaving Saddle Ball Mountain as a remnant of Greylock’s earlier name.Deborah E. Burns and Lauren R. Stevens, Most Excellent Majesty: A History of Mount Greylock, Berkshire County Land Trust and Conservation Fund, 1988. John Bascom’s 1907 monograph suggests its location along the ridge: “Mount Griffin still another two miles to the south and 220 feet lower than Greylock, which is 3,505 ic. There remains some controversy about the exact location of the highest peak. *The 1988 Cheshire USGS 7.5 x 15 minute – 1:25,000 scale map locates Saddle Ball Mountain at #3 at 986 meters (3,235 feet) on the photo above. *The 1989 Albany USGS 30 x 60 Quadrangle - 1:100,000 scale locates Saddle Ball Mountain at #1 at 987 meters (3,238 feet) on the photo above. *The Mass. DCR Trail Map dated 2012 shows Saddle Ball Mountain at #1 at 3247 feet. * In June and July 2013, two independent parties collected data using GPS and altimeter readings from all four Saddle Ball outcroppings. That information and historical data indicate that the southernmost Saddleball outcropping is the highest. The cairn on the west side of the Appalachian Trail is close to, if not the actual highpoint on Saddle Ball Mountain.


Geology

Mount Greylock and the neighboring Taconic Mountains are composed predominantly of
Ordovician The Ordovician ( ) is a geologic period and System (geology), system, the second of six periods of the Paleozoic Era (geology), Era, and the second of twelve periods of the Phanerozoic Eon (geology), Eon. The Ordovician spans 41.6 million years f ...
phyllite Phyllite ( ) is a type of foliation (geology), foliated metamorphic rock formed from slate that is further metamorphosed so that very fine grained white mica achieves a preferred orientation.Stephen Marshak ''Essentials of Geology'', 3rd ed. I ...
, a
metamorphic rock Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock ( protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, caus ...
, overlain on younger layers of metamorphosed
sedimentary rock Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or de ...
, especially
marble Marble is a metamorphic rock consisting of carbonate minerals (most commonly calcite (CaCO3) or Dolomite (mineral), dolomite (CaMg(CO3)2) that have recrystallized under the influence of heat and pressure. It has a crystalline texture, and is ty ...
. Mount Greylock is the product of thrust-faulting, a
tectonic Tectonics ( via Latin ) are the processes that result in the structure and properties of the Earth's crust and its evolution through time. The field of ''planetary tectonics'' extends the concept to other planets and moons. These processes ...
process by which older rock is thrust up and above younger rock during periods of intense
mountain building Mountain formation occurs due to a variety of geological processes associated with large-scale movements of the Earth's crust (List of tectonic plates, tectonic plates). Fold (geology), Folding, Fault (geology), faulting, Volcano, volcanic acti ...
.


Geography

Saddle Ball Mountain and Mount Greylock are part of an 11-mile-long by 4.5-mile-wide island-like range that runs in a north-south direction bordered by the
Hoosac Range The Hoosac Range is a mountain range that forms the western edge of the northwest Berkshire Plateau of western Massachusetts, an extension of the southern Green Mountains of Vermont Vermont () is a U.S. state, state in the New England reg ...
to the east, the
Green Mountains The Green Mountains are a mountain range in the U.S. state of Vermont and are a subrange of the Appalachian Mountains. The range runs primarily south to north and extends approximately from the border with Massachusetts to the border with Que ...
to the north and the Taconic Mountains to the west. During the
Pleistocene The Pleistocene ( ; referred to colloquially as the ''ice age, Ice Age'') is the geological epoch (geology), epoch that lasted from to 11,700 years ago, spanning the Earth's most recent period of repeated glaciations. Before a change was fin ...
, 18,000 years ago, Mount Greylock and adjacent peaks were covered by
ice sheets In glaciology, an ice sheet, also known as a continental glacier, is a mass of glacial ice that covers surrounding terrain and is greater than . The only current ice sheets are the Antarctic ice sheet and the Greenland ice sheet. Ice sheets ...
up to 1-kilometer in thickness. As the most recent ice cap receded, the Greylock Range was an island in the midst of Lake Bascom.Natural History of the Berkshires
. Williams College. Retrieved 2008-03-09.


Forests and ecology

Along the ridgeline of Greylock above 3000 feet between Mount Fitch on the north and the Saddle Ball series on the south is the only place in Massachusetts where a taiga-boreal or subalpine forest flourishes. The Mount Greylock range is designated as an
important bird area An Important Bird and Biodiversity Area (IBA) is an area identified using an internationally agreed set of criteria as being globally important for the conservation of bird populations. IBA was developed and sites are identified by BirdLife Int ...
. There are a number of species of birds which breed in the taiga or boreal forests at the higher altitudes of the mountain, which are not normally found breeding in Massachusetts. These species include the blackpoll warbler and Bicknell's thrush.


Recreation

Northbound hikers on either the
Appalachian Trail The Appalachian Trail, also called the A.T., is a hiking trail in the Eastern United States, extending almost between Springer Mountain in Georgia and Mount Katahdin in Maine, and passing through 14 states.Gailey, Chris (2006)"Appalachian Tra ...
or the Jones Nose Trail will pass over the southernmost and highest Saddle Ball about 0.2 to 0.3 miles north of the AT/Jones Nose junction. The high point is in the vicinity of a small
cairn A cairn is a human-made pile (or stack) of stones raised for a purpose, usually as a marker or as a burial mound. The word ''cairn'' comes from the (plural ). Cairns have been and are used for a broad variety of purposes. In prehistory, t ...
on the west side of the AT. The two most northerly Saddle Balls require a short but strenuous easterly bushwhack from the AT to reach the non-descript, forested high points.


References

{{Mountains of Massachusetts Taconic Mountains Mountains of Berkshire County, Massachusetts Mountains on the Appalachian Trail