Question: In which municipality in the country where Blomidon formation can be found is Kinsac located?

full_context: Document 1: Mineville, Nova Scotia: Mineville, Nova Scotia is a suburban community within the Eastern Halifax Regional Municipality, Nova Scotia, Canada, between Lake Echo on Trunk 7, Highway 107 and Upper Lawrencetown on Route 207. The main road is called the Mineville Rd. The other road is called Candy Mountain Road. The community has two lakes: Lawrencetown Lake and Lake Echo.
Document 2: Upper Lakeville: Upper Lakeville is a small cottage community on the Eastern Shore of the Halifax Regional Municipality, in the Musquodoboit/Sheet Harbour region of the Marine Drive, in Nova Scotia. Upper Lakeville road is located on the junction of Trunk 7, 55.3 km from Dartmouth, and 58.9 km from Halifax.
Document 3: Candiac, Saskatchewan: Candiac is an organized hamlet located at the intersection of Highway 48 and Highway 617 in the southeast quadrant of Saskatchewan, Canada. It is directly south of Wolseley, and between Montmartre and Glenavon, approximately one hour's drive southeast of the provincial capital Regina. It is no longer listed as a separate community by Statistics Canada, and is considered part of the Rural Municipality of Montmartre #126. The population within the community's boundary is less than 50. Besides some bush on the northern end of the town, it is surrounded by open fields and pasture.
Document 4: Geological history of Earth: To the north of Africa the Tethys Sea continued to narrow. Broad shallow seas advanced across central North America (the Western Interior Seaway) and Europe, then receded late in the period, leaving thick marine deposits sandwiched between coal beds. At the peak of the Cretaceous transgression, one-third of Earth's present land area was submerged. The Cretaceous is justly famous for its chalk; indeed, more chalk formed in the Cretaceous than in any other period in the Phanerozoic. Mid-ocean ridge activity—or rather, the circulation of seawater through the enlarged ridges—enriched the oceans in calcium; this made the oceans more saturated, as well as increased the bioavailability of the element for calcareous nanoplankton. These widespread carbonates and other sedimentary deposits make the Cretaceous rock record especially fine. Famous formations from North America include the rich marine fossils of Kansas's Smoky Hill Chalk Member and the terrestrial fauna of the late Cretaceous Hell Creek Formation. Other important Cretaceous exposures occur in Europe and China. In the area that is now India, massive lava beds called the Deccan Traps were laid down in the very late Cretaceous and early Paleocene.
Document 5: Halifax County, Nova Scotia: Halifax County is a county in the Canadian province of Nova Scotia. The Municipality of the County of Halifax was the municipal government of Halifax County, apart from the separately incorporated towns and cities therein. The Municipality was dissolved in 1996, together with those town and city governments, in their amalgamation into Halifax Regional Municipality.
Document 6: Beaver Bank, Nova Scotia: Beaver Bank (2011 population: 7,119) is a suburban community northeast of Lower Sackville on the Beaver Bank Road (Route 354) within the Halifax Regional Municipality, Nova Scotia, Canada. It is about 35 kilometres from the City of Halifax.
Document 7: Kinsac, Nova Scotia: Kinsac is a suburban community in District 2 of the Halifax Regional Municipality, in Nova Scotia, Canada on Nova Scotia Route 354.
Document 8: Bayan Mandahu Formation: The Bayan Mandahu Formation (or Wulansuhai Formation) is a geological unit of "redbeds" located near the village of Bayan Mandahu in Inner Mongolia, China Asia (Gobi Desert) and dates from the late Cretaceous Period. Laid down in the Campanian, it is dated somewhat uncertainly to between 75-71 mya (million years ago).
Document 9: Marine Drive (Nova Scotia): The Marine Drive is a designated scenic route along Nova Scotia's Eastern Shore. It closely follows the coast of the Atlantic Ocean and the Strait of Canso from the Canso Causeway to the junction of Route 322 and Highway 111 in Dartmouth.
Document 10: Dean, Nova Scotia: Dean is a small farming & forestry community in the North Branch Musquodoboit in the Musquodoboit Valley along the Halifax Regional Municipality/Colchester County county line, in the Canadian province of Nova Scotia, along Route 336. Other communities in the North Branch include Elmsvale, Greenwood, Upper Musquodoboit, and Moose River Gold Mines, among others.
Document 11: Arthur's Seat: Like the rock on which Edinburgh Castle is built, it was formed by an extinct volcano system of Carboniferous age (lava samples have been dated at 341 to 335 million years old), which was eroded by a glacier moving from west to east during the Quaternary (approximately the last two million years), exposing rocky crags to the west and leaving a tail of material swept to the east. This is how the Salisbury Crags formed and became basalt cliffs between Arthur's Seat and the city centre. From some angles, Arthur's Seat resembles a lion couchant. Two of the several extinct vents make up the 'Lion's Head' and the 'Lion's Haunch'.
Document 12: Shelburne dike: The Shelburne dike, also known as the Great Dike, is a large northeast trending Mesozoic diabase dike in southeastern Nova Scotia, Canada. It is long, although some evidence suggests it extends a further to the northeast to Sambro Island. The dike might have fed volcanoes in the Triassic period when the landscape was rifting apart during the breakup of supercontinent Pangaea.
Document 13: Blomidon Formation: The Blomidon Formation is a unit of Upper Triassic (Norian–Rhaetian) sedimentary rocks, which outcrops in Nova Scotia. At outcrop they reach a maximum thickness of , but up to has been proven from well data and a thickness of up to has been inferred from seismic reflection data. It overlies the mainly Carnian Wolfville Formation and underlies the North Mountain Basalt. The type section is exposed between Cape Blomidon () and Paddy Island ().
Document 14: Fremouw Formation: The Fremouw Formation is a Triassic-age rock formation in the Transantarctic Mountains of Antarctica. Fossils of prehistoric reptiles and amphibians have been found in the formation. Fossilized trees have also been found. The formation's beds were deposited along the banks of rivers and on floodplains. During the Triassic, the area would have been a riparian forest at 70–75°S latitude.
Document 15: Goat Rock Beach: The sea stacks along the coast at Goat Rock Beach consist of rocks from the Franciscan Complex, formed within an era of plate collision along the western coast of North America. From about 200 to 30 million years ago, the North American Plate was in continual collision with the Farallon Plate. A variety of rock types resulted from this collision, including pillow basalt, chert, and marine sandstone. During the plate collisions, these rocks were considerably faulted and crushed into melange, which is a mixture of ground-up matrix and resistant pockets of rock floating within. When melange is eroded by wave action, the softer part of the matrix is washed away, leaving the more resistant blocks exposed in the ocean as sea stacks. Goat Rock is such a flat topped sea stack comprised by a block of resistant greywacke.
ground_truth: Halifax Regional Municipality
sub_queries: Blomidon Formation >> located in the administrative territorial entity Answer: Nova Scotia
Kinsac, Nova Scotia >> located in the administrative territorial entity Answer: Halifax Regional Municipality