Liverpool Hole is a small but significant coastal feature located in the county of Northumberland in Northeast England. Situated on the North Sea coast, it is a natural opening that connects the sea to an estuary and creek system.
The hole serves as a vital link between the North Sea and the estuary, facilitating the exchange of water and marine life. It acts as a gateway for tidal water to flow into the estuary during high tide and then recede back into the sea during low tide. This constant ebb and flow of water helps maintain a healthy ecosystem within the estuary.
The Liverpool Hole is formed by the erosion of the surrounding coastal cliffs, which have created a narrow channel leading into the estuary. The hole itself varies in width and depth, depending on the tides and the volume of water flowing through it. During high tide, the hole can be several meters deep, allowing larger vessels to navigate through it. However, during low tide, the water level drops significantly, making it impassable for most boats.
The estuary and creek system connected to Liverpool Hole are home to a diverse range of flora and fauna. The nutrient-rich waters support a variety of marine life, including fish, crustaceans, and seabirds. The surrounding salt marshes and mudflats provide important habitats for wading birds and other coastal species.
Due to its ecological significance, Liverpool Hole is a designated Site of Special Scientific Interest (SSSI) and is protected under national conservation laws. It also attracts visitors who appreciate the natural beauty of this coastal feature and the unique wildlife it supports.
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Images are sourced within 2km of 55.47734/-1.5913095 or Grid Reference NU2520. Thanks to Geograph Open Source API. All images are credited.
Liverpool Hole is located at Grid Ref: NU2520 (Lat: 55.47734, Lng: -1.5913095)
Unitary Authority: Northumberland
Police Authority: Northumbria
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