Search results
Results From The WOW.Com Content Network
The River Hull tidal surge barrier is a flood control gate located on the River Hull in the city of Kingston upon Hull, in the East Riding of Yorkshire, England.The barrier impounds the river in times of tidal surges, preventing water moving upstream of the river from the Humber Estuary, and flooding the areas of the city which are near to the river, or susceptible to flooding.
The River Hull is a navigable river in the ... The tidal range of tides can be up to 7 feet (2.1 m ... The gate was initially lowered about twelve times a year, and ...
The Port of Hull is a port at the confluence of the River Hull and the Humber Estuary in Kingston upon Hull, in the East Riding of Yorkshire, England.. Seaborne trade at the port can be traced to at least the 13th century, originally conducted mainly at the outfall of the River Hull, known as The Haven, or later as the Old Harbour.
Discover the latest breaking news in the U.S. and around the world — politics, weather, entertainment, lifestyle, finance, sports and much more.
The Holderness area is drained by the River Hull and its tributaries and a number of coastal streams. The valley of the River Hull is broad and shallow and in its lower reaches the river is contained within flood banks. The River Hull Tidal Surge Barrier at the mouth of the river can be used to prevent surge tides overwhelming the flood defences.
Due to its gentle slope, at low tide, the beach extends several hundred yards in width, forming tide pools that have become a well known, picturesque characteristic of the site, renowned for their reflections of the sunsets and sunrises. The northern part of the beach is private, administered by the Town of Hull, and does not allow visitors to ...
Although Beverley was served by the Hull and Selby Railway from October 1846, the canal remained independent, and therefore competitive for trade to Hull. The competition helped to keep railway tolls lower than they might otherwise have been, and traffic on the Beck continued to grow, rising from 31,185 tons in 1838 to 51,578 tonnes in 1888 and ...
Tide tables list each day's high and low water heights and times. To calculate the actual water depth, add the charted depth to the published tide height. Depth for other times can be derived from tidal curves published for major ports. The rule of twelfths can suffice if an accurate curve is not available. This approximation presumes that the ...