Email a studentSend a postcardEmail a student
Send a postcard
Email a student
   HOME / FOR MEDIA / THE REPORTER
The University of Leeds
The Reporter
In this section
 
 
 
About
The University
Research
Studying at Leeds
Jobs
Events
Leeds & Yorkshire




Issue 480, 22 April 2002

Malham Cove yields icy secrets to diving scientist

One of the most well-known features of the Yorkshire landscape is nearly four times older than previously thought, cave diver and earth sciences technician Phillip Murphy has established.

Scientists believed that Malham Cove (pictured above) was formed during the last glaciation, which ended 14,000 years ago, but Phillip Murphy (pictured below) has collected a stalactite sample from the flooded cave system which proves the cove must be at least 50,000 years old.

"As one of the few cave-diving earth scientists in the UK, I can reach otherwise inaccessible areas," he said. "I heard that a fellow diver had come across a speleothem – as stalactites and stalagmites are collectively known – in an underwater cave. Speleothems normally form once a cave passage is no longer flooded, so to find one underwater means that some change has taken place to flood that cave system."

Malham Cove is a 'step' formed by glaciers and waterfalls. The area is criss-crossed with cave systems, created by water dissolving the limestone rock. The valley below the cove was gouged out by a glacier, draining the cave system of its water. Then a later glacier brought sediment over the lip of the cove, pooling the site with silt which caused the cave system to once again fill with water.

The speleothem provides the key to dating these events, as Phillip Murphy explains: "Speleothems don't form during glacial periods, as freezing temperatures above and below ground mean there is no moving water. So the speleothem discovered in the Malham cave system must have been formed during a warm period between the glaciation which formed the cove and another which deposited the silt. When the ice melted, the silt then caused the caves to flood."

University of Liverpool archaeologist Alf Latham helped him date the speleothem and found it to be around 26,000 years old.

This proves that the cave system was re-flooded after the last ice age when, between 23,000 and 20,000 years ago, glaciers covered the region creating the Dales landscape we know today. It also proves that the initial formation of Malham Cove must have taken place over 50,000 years ago, predating the last ice age and the warm period known to precede it.

Phillip Murphy: "Although glaciers played a major role in forming the Dales landscape, they also scoured the area clean, leaving little surviving data on the surface. The discovery of this speleothem shows that important evidence still exists underground, especially in the flooded caves where the only access is by diving."


 
  Current issue
  Back issues
  Search all online issues of the Reporter
  Search current issue
  Email the reporter
  Dates
  Small ads

See also
  Press office
  Press releases
  In the press
  News archive
  Facts and figures
  History of the University
  Send a post card

 
Quick Links A-Z staff & students Departments Administration & services Library Student Union Campus map Website map Top 10 Intranet Contact us