Sandbank in the context of "South Foreland"

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👉 Sandbank in the context of South Foreland

South Foreland is a chalk headland on the Kent coast of southeast England. It presents a bold cliff to the sea, and commands views over the Strait of Dover. It is centred 3 miles (4.8 km) northeast of Dover and 15 miles (24 km) south of North Foreland. It includes the closest point on the Island of Britain to the European mainland at a distance of 20.6 miles (33.2 km).

This proximity gives it military significance and during the Second World War its coastal battery was built, along with a radar station. Lying between the busy Port of Dover and the remote and hazardous Goodwin Sands sandbank, its two lighthouses were important for navigation before their disuse. Much of the area is now owned by the National Trust and is open to the public; it is traversed by the Saxon Shore Way, the Kent coastal walk.

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Sandbank in the context of Kamyana Mohyla

Kamyana Mohyla (Ukrainian: Кам'яна Могила, lit.'stone grave'; Russian: Каменная Могила, romanizedKamiennaya Mogila) is an archaeological site in the Molochna River (lit.'milky river') valley, about a mile from the village of Terpinnia, Zaporizhzhia Oblast, Ukraine. Petroglyphs of Kamyana Mohyla are dated from Upper Paleolithic (Kukrek culture) to Medieval, with Stone Age depictions subjected to most archaeological interest. The site is listed on the Tentative List of World Heritage Sites in Ukraine.

The site encompasses a group of isolated blocks of sandstone, up to twelve meters in height, scattered around an area of some 3,000 sq m. As Noghai legend has it, it resulted from a scuffle of two baghaturs who took turns throwing rocks at each other. In truth, the site had its origins in a sandbank of the Tethys Ocean. For a long time it was an island in the Molochna River, which has since been silted up and now flows a short distance to the west. It is thought to represent the only sandstone outcrop in the Azov-Kuban Depression. The shape of this sand hill is similar to that of kurgans that dot the Pontic–Caspian steppe.

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Sandbank in the context of Burrard Inlet

Burrard Inlet (Halkomelem: səl̓ilw̓ət) is a shallow-sided fjord in the northwestern Lower Mainland, British Columbia, Canada. Formed during the last Ice Age, it separates the City of Vancouver and the rest of the lowland Burrard Peninsula to the south from the coastal slopes of the North Shore Mountains, which span West Vancouver and the City and District of North Vancouver to the north.

Burrard Inlet opens west into the Strait of Georgia between Point Atkinson and Point Grey. Vancouver's Downtown Peninsula protrudes northwesterly into the inlet, separating it into the wide outer Burrard Inlet to the west and the elongated inner Burrard Inlet to the east. The southeastern portion of the outer inlet is an open bay known as English Bay, which has a narrow eastern inlet called False Creek. The 400-metre-wide (1,300 ft) strait between Prospect Point and the sandbanks just east of the Capilano River mouth, which connects the inlet's outer and inner sections, is known as the First Narrows, traversed by the Lions Gate Bridge. The inner inlet then widens into Vancouver Harbour, which hosts the Port of Vancouver, Canada's largest port.

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