ⓘ Penitentiary Member. The Stony Mountain Formation is a stratigraphical unit of Ashgill age in the Western Canadian Sedimentary Basin. It takes the name from the ..


ⓘ Penitentiary Member

The Stony Mountain Formation is a stratigraphical unit of Ashgill age in the Western Canadian Sedimentary Basin.

It takes the name from the community Stony Mountain, Manitoba, and was first described in the town quarry by D.B. Dowling in 1900.


1. Lithology


The Stony Mountain Formation is divided in the following sub-units:

South Williston Basin
  • Penitentiary Member: argillaceous dolomite
  • Gunn Member: interbedded calcareous shale and fossiliferous limestone
  • Lower Stony Mountain: argillaceous dolomite
  • Gunton Member: crystalline dolomite

2. Distribution

The Stony Mountain Formation occurs throughout the Williston Basin. It reaches a maximum thickness of 45 metres 150 ft in the sub-surface at the Canada/United States border, and thins out towards the east, north and west. In Manitoba, where it is exposed at the surface in the erosion belt, it has a thickness of 30 metres 100 ft.


3. Relationship to other units

The Stony Mountain Formation is slightly unconformably overlain by the Stonewall Formation and sharply overlays the Red River Formation or the Herald Formation.

  • Stonewall Formation is overlain by the Interlake Group conformably in the south, disconformably in the north and sharply overlays the Stony Mountain Formation
  • Herald Formation reaches a maximum thickness of 38 metres 120 ft in the Lake Alma area. The Herald Formation is disconformably overlain by the Stony Mountain
  • The Red River Formation is slightly unconformably overlain by the Stony Mountain Formation and sharply overlays the Winnipeg Formation in Manitoba, the
  • Stony Man Mountain also known as Stony Man, is a mountain in Shenandoah National Park, Virginia and is the most northerly 4, 000 foot peak in the Blue
  • soil and the Hazleton soil. No fish inhabit the stream. Stony Run begins on Little Mountain in Union Township. It flows east for several tenths of a
  • Bloomsburg Water Company. Stony Brook starts in northwestern North Centre Township, on the southern edge of Knob Mountain It begins flowing southwest
  • ocean - going runs of steelhead. Stony Creek was named for the large amount of rocks and sediments it once washed down from the mountains during floods. Today, most
  • A rock formation is an isolated, scenic, or spectacular surface rock outcrop. Rock formations are usually the result of weathering and erosion sculpting
  • Carolina. The mountains are typical of the rolling terrain of the piedmont region of North Carolina, and are somewhat similar in formation to the nearby
  • It lies just above Jones Point, New York, within Bear Mountain State Park and the town of Stony Point in Rockland County, New York. Dunderberg also historically
  • Spetchy Kopf Formation and Huntley Mountain Formation In South - central Pennsylvania, the Pocono often interfingers with the Rockwell Formation Paleozoic

  • Vineyards and Winery Smith - Madrone Vineyards and Winery Spring Mountain Vineyard Stony Hill Vineyard Sherwin Family Vineyards Vineyard 7 8 York Creek
  • top to base: Heath Formation black shale with sandstone lenses. Otter Formation limestone and grey to green shale Kibbey Formation shaly sandstone The
  • pipeline runs from the Hudson River into Stony Point. Much of the Tomkins Cove perimeter borders Bear Mountain State Park. Tomkins Cove prides itself on
  • The Bakken Formation ˈbɑːkən is a rock unit from the Late Devonian to Early Mississippian age occupying about 200, 000 square miles 520, 000 km2 of
  • Hamilton Group, along with the underlying the Marcellus Formation Shale. South of Tuscarora Mountain in south central Pennsylvania, the lower members of this
  • have weathered unevenly, bizarre formations have been created in the Lattengebirge these include Steinerne Agnes Stony Agnes ca. 1, 400 m the rugged
  • most complete exposures of the Tuscarora Formation are in two quarries at the crest and south end of Canoe Mountain Spruce Creek Quadrangle The Tuscarora
  • Binghamton. Retrieved 2008 - 05 - 23. Marcellus Formation Group The Paleobiology Database. Retrieved 2008 - 04 - 03. Stony Hollow Member The Paleobiology Database
  • Branch of the Ashuelot. To the southeast of the mountain Mead Brook and Stony Brook flow to Mountain Brook, a tributary of the Contoocook River, which
  • find reputed to come from a large unconfirmed iron mountain in Africa. The existence of a huge stony - iron mesosiderite approximately 45 kilometers from
  • north of the Roanoke River: Stony Man 4, 031 ft 1, 229 m Hawksbill Mountain 4, 066 ft 1, 239 m Apple Orchard Mountain 4, 225 ft 1, 288 m and Peaks
  • The Bearpaw Formation also called the Bearpaw Shale, is a geologic formation of Late Cretaceous Campanian age. It outcrops in the U.S. state of Montana
  • as the international boundary west from Lake of the Woods to the Stony Mountains the UK and the USA agreed to what has since been described as joint
  • of Salt Pond Mountain crossed Potts Mountain dropping down into the Big Stony Creek watershed, continued to cross over Peters Mountain passed by Salt
  • River in the Gates of the Mountains Montana are formed by Madison Limestone. Montana - Wyoming - Manitoba The following formations are recognized in Montana
  • calcareous material or a deeper soil that is extremely gravelly and or stony Leptosols cover approximately 1.7 billion hectares of the Earth s surface
  • tip of the Black Mountains an extensive upland massif which straddles the border between south - east Wales and England. The mountain sits at the point
  • from surrounding mountains or by weathered debris from the formation itself, making finding outcrops for study difficult. The formation is thought to represent
  • Skeletic Cambisol, Leptic Cambisol, Skeletic Regosol moderately deep dark stony clays with good natural fertility Vertic Cambisol deep, dark cracking

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