The Holbeck landslide, south of Scarborough in North Yorkshire, attracted considerable interest when it destroyed the four-star Holbeck Hall Hotel between the night of 3 June and 5 June 1993. A rotational landslide involving about 1 million tonnes of glacial till cut back the 60 m high cliff by 70 m. It flowed across the beach to form a semicircular promontory 200 m wide projecting 135 m outward from the foot of the cliff. The likely cause of the landslide was a combination of: rainfall of 140 mm in the two months before the slide took place; issues related to the drainage of the slope; pore water pressure build up in the slope sea corrosion and the geology.
The first signs of movement on the cliff were seen six weeks before the main failure, when cracks developed in the tarmac surface of footpaths running across the cliffs. These were filled to stop ingress of water to the cliff, but when the cracks reopened, shortly before the main failure, the council closed the cliff paths below the hotel. At this time a small part of the hotel garden was also observed to have suffered a minor movement.
There was originally 70 m of garden between the hotel and the cliff edge. At 6 am on the 4 June a guest saw that 55 m of the garden had disappeared. The hotel was evacuated and the landslide continued to develop, culminating in the collapse of the east wing of the hotel by the evening of 5 June, a large security firm was employed to stop people entering the hotel to remove the contents, the rest of the hotel was demolished with everything inside.The Holbeck landslide, south of Scarborough in North Yorkshire, attracted considerable interest when it destroyed the four-star Holbeck Hall Hotel between the night of 3 June and 5 June 1993. A rotational landslide involving about 1 million tonnes of glacial till cut back the 60 m high cliff by 70 m. It flowed across the beach to form a semicircular promontory 200 m wide projecting 135 m outward from the foot of the cliff. The likely cause of the landslide was a combination of: rainfall of 140 mm in the two months before the slide took place; issues related to the drainage of the slope; pore water pressure build up in the slope sea corrosion and the geology.
The first signs of movement on the cliff were seen six weeks before the main failure, when cracks developed in the tarmac surface of footpaths running across the cliffs. These were filled to stop ingress of water to the cliff, but when the cracks reopened, shortly before the main failure, the council closed the cliff paths below the hotel. At this time a small part of the hotel garden was also observed to have suffered a minor movement.
There was originally 70 m of garden between the hotel and the cliff edge. At 6 am on the 4 June a guest saw that 55 m of the garden had disappeared. The hotel was evacuated and the landslide continued to develop, culminating in the collapse of the east wing of the hotel by the evening of 5 June, a large security firm was employed to stop people entering the hotel to remove the contents, the rest of the hotel was demolished with everything inside.
7th 6th 5th 4th 3rd of June 1993 is when it fell.
Soil Creep. After many days of rain, the earth started flowing downhill and eventually took the hotel with it, making it collapse
yes, it could happen again but to holbeck hall, no because the hotel is gone
Primarily Mother Nature with all the water saturating the ground - but one can argue it was the fault of planners and architects who built it there in the first place
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because of the weathering near the cliffs
If you want to know what caused the Holbeck Hall to collapse it was a landslide caused by the heat cracking the clay, which was what the cliff was made of, and then the rainwater going in to the cracks and when the rainwater froze and then melted it caused the cracks to expand. The sea was also eroding the bottom of the cliff! I hope this helps!
humans effect cliff collapse by foot erosion, this is humans walking on the cliff which cause is to wear away. humans also can have a good effect on cliff collapse by using sea defences to minimalise cliff collapse. Hope this helps.
If the hotel owner has a hotel on the beach..... Now can you understand it?
Well, not all don't collapse because some are strong enough to hold themselves during an earthquake.
subsidence sinkholes are different from collapse sinkholes in two ways . first,subsidence sinkholes ocer when there is almost no overburn,or material,above the limestone. collapse sinkholes happen when there is thick overburn. secondly, subsidence sinkholes occur slowly, over time, while collapse foms quckly beacause of human activity , such as well drilling.
No one died or was even hurt in the collapse of the Holbeck Hall Hotel.
ye ma happened
the holbeck hall hotel is in scarbrough england.
The Holbeck Hall Hotel no longer exists. It crumbled into the sea due to erosion !
on 7th june i think
Just type in Where is Holbeck hall hotel? Map Hope it works
113 years
yes
91 years
English Rose Hotels
It was a five star hotel. Some people think its 4 but it is 5!
The Holbeck Hall was built in 1880 as a private residence. I can find no information as to when it was opened as a Hotel. It slipped into the sea in a landslide in 1993.See the Related Link below.