: Natural History

Earthquakes in Wales

27 March 2008

Although not competing with areas famous for their instability such as western California, Japan or Sumatra, Wales is a region of regular active Earth movements. You might be surprised to learn that at least sixteen significant earthquakes have occurred in Wales during the last century.

Seismograph showing an earthquake in north Wales in 1994

Seismograph showing an earthquake in north Wales in 1994

Why do earthquakes occur in Wales?

The British Geological Survey (BGS) records around 300-400 earthquakes each year in Britain. Wales, along with the rest of the UK, sits on the European plate, and stress builds up as it is pushed slowly north-eastwards from the Mid-Atlantic Ridge. The stress is released by movement along pre-existing fault planes, causing an earthquake.

Where do earthquakes occur in Wales?

There are several long-active fault systems in Wales. Once faults form, they create weak zones in the crust that can be reactivated time and time again. For example, the fault system running parallel to the Menai Strait between Anglesey and Bangor in north Wales are known to have been active over 500 million years ago and have also been the sites of more recent earthquakes.

The Menai Strait area is the most seismically active area in Wales and one of the most active in the UK. The last major earthquake occurred here in 1984, but many others are known from historical records (including 1827, 1842, 1852, 1874, 1879, 1903). Although many events have been recorded in south Wales, from Pembroke to Newport, only the Swansea area shows consistent activity, with significant earthquakes occurring in 1727, 1775, 1832, 1868 and 1906.

 

Largest earthquake in Wales for 100 years

The 1984, magnitude 5.4, Menai Strait earthquake was the largest onshore UK event for over 100 years. The epicentre was located in northern Llŷn, north Wales and the quake originated at a depth of approximately 22 km in the Earth's crust.

Another major UK earthquake occurred on 2 April 1990 in the Welsh Borders. This magnitude 5.1 event was felt over an area of approximately 140,000 square kilometres and was followed by six aftershocks. The epicentre was initially identified as being at Bishop's Castle in Shropshire, but this was later revised to a location just inside the Welsh border (latitude 52.43°' N, longitude 3.03° W).

Local damage

In both earthquakes the damage was relatively minor, including cracks in plaster and masonry and collapse of chimneys. In the Bishop's Castle event this was limited to the area immediately around the epicentre.

The only fatality known from any seismic activity in Wales is from a woman falling down the stairs and being killed during the Porthmadog earthquake of 1940.

Recent activity

An earthquake with a magnitude of 4.6 occurred in south Wales on February 17, 2018. According to the British Geological Survey (BGS), its epicentre was between Ystradgynlais and Ystalafera. A Welsh earthquake also occurred in the Bristol Channel on 20th February 2014, and was widely felt across South Wales, Devon, Somerset and western Gloucestershire. The BGS received several reports from the media and local residents describing “felt like the vibration of a large vehicle passing the building”, “the whole house seemed to move/wobble back and forth a few times”..

The magnitude 4.1 earthquake is the largest to hit South Wales since 2013.

Other recent earthquake activity from Wales include:

  • A magnitude 3.8 earthquake on the Lleyn Peninsula on 29th May 2013.
  • Magnitude 2.9 earthquake near Nantyffyllon on 5th June 2009.
  • Magnitude 2.9 earthquake near Llangollen on 30th November 2007
  • A magnitude 2.9 quake in Cardiff on 20th June 2002.

In general, humans cannot feel events of less than magnitude 2.

Recording earthqake activity at Amgueddfa Cymru.

A seismograph at National Museum Cardiff displays output from a local seismometer and allows observation of data from seismic events.

As seismometers are very sensitive to all types of ground vibrations, not only earthquakes but local traffic, trains and even roadworks, it was not possible to locate a seismometer in Cardiff city centre. Instead, data is obtained by a radio link from the nearest BGS seismometer near Newport, Gwent.

Glossary

  • Aftershocks are earthquakes that follow the largest shock of an earthquake sequence; they are smaller than the main event and can continue for years afterwards. The length of the aftershock period relates to the magnitude of the main shock, with large events having more numerous and larger aftershocks for the longer periods.
  • Epicentre this is the point on the Earth's surface above the earthquake hypocentre.
  • Hypocentre this is the place deep in the Earth where the earthquake rupture starts.
  • Intensity is a measure of an earthquake's effect on people and the environment. It is controlled by: the distance from the epicentre, the magnitude of the earthquake and the local geology. In Europe the 12 division EMS 98 (European Macroseismic Scale) is used and in the USA the Modified Mercalli Intensity Scale. For details of the EMS 98 see www.earthquakes.bgs.ac.uk/macroseismics/ems_synopsis.htm.
  • Magnitude is a measure of the strength of an earthquake. This is a logarithmic scale, which means that for each whole number increase there is a ten-fold increase in ground movement. There are several types of magnitude scale, but the 'Richter Scale'(ML — magnitude local) is the one used most commonly in the UK for 'local' earthquakes.
  • Plate. The outer layers of the Earth's crust and mantle are divided into segments known as plates, which are in constant motion. The process by which plates move is know as plate tectonics.
  • Seismometers work by measuring the position of a weight, to which a coil is attached, relative to a magnet in a frame. Vibrations cause movement of the coil and the generation of an electrical current which is then recorded by a seismograph. Seismometers, are highly sensitive, and can record the slightest of movements that are totally unfelt by humans.
  • Seismographs record the motion detected by the seismometer. This is either on a paper trace or as electronic data. Time markers record the precise time a seismic event reaches the seismometer. By using data from at least three seismographs the position of an earthquake can be calculated.

For current earthquake data see: http://earthquake.usgs.gov/earthquakes/ & http://www.earthquakes.bgs.ac.uk/ & http://www.emsc-csem.org/

Museum records largest earthquake in UK for 25 years

28 February 2008

A scan from the seismograph at National Museum Cardiff.

A scan from the seismograph at National Museum Cardiff showing the Market Rasen earthquake on 27 February 2008 at 00:57.14 GMT. The shock waves were recorded by a seismometer located near Newport, south Wales, and transmitted to the seismograph at the Museum.

The seismograph at National Museum Cardiff has recorded the largest onshore seismic event in the UK since 1990.

The earthquake was recorded by the Museum's seismograph at 00:57.14 GMT 27 February. This has been identified as the Magnitude 5.2 earthquake detected by the British Geological Survey. The epicentre was initially reported as located just north of Market Rasen, Lincolnshire, at 00:56.47 GMT.

The earthquake waves took just 27 seconds to travel the 158 miles between Market Rasen and the Museum's seismometer near Newport, south Wales. This means that the earthquake's waves were travelling at approximately 5.85 miles per second.

This is the largest onshore event in the UK since the Magnitude 5.1 earthquake at Bishops Castle in the Welsh Borderland on 2 April 1990.

The Market Rasen event was felt by people as far afield as Newcastle, Yorkshire, London, Cumbria, the Midlands, Norfolk and parts of Wales. Damage to roofs, walls and chimneys around the epicentre area were reported and one person was injured in Wombwell near Barnsley, South Yorkshire as a result of falling masonry.

Aftershock

Earthquakes of this size are typically followed by smaller earthquakes or 'aftershocks'. A magnitude 1.8 earthquake was recorded in the region just a few hours after the main event.

A detailed investigation is required to establish the geological structure responsible for the main earthquake. The Geological Survey has already calculated that the quake occurred at a depth of around 18km. This suggests it most likely occurred along an ancient fault in Precambrian rocks, such as those that underlie much of Wales.

The exact fault along which the quake occurred is unlikely to be exposed at the surface as younger Palaeozoic and Mesozoic rocks (Carboniferous, Permian, Triassic and Jurassic, for example) overlie the Precambrian rocks in the Market Rasen area.

The magnitude 5.4 Lleyn Peninsula earthquake of 19 July 1984 remains the largest recorded onshore earthquake in the UK.

Information from:

Drawn from nature: Botanical illustrations

20 August 2007

Old herbal

Throughout the Dark Ages, disease and poor hygiene were rife and people relied on herbalists and their remedies. Cure for deafness: take rat's urine, the oil of eels, the house leek, the juice of travellers' joy and a boiled egg.

Magnolia

Plant collectors travelled to remote parts of the world. Finding new plants meant exploring new lands - often without accurate maps, through country without roads, and with few settlements.

Tulips

In the 17th century, travel and trade brought many new exotic plants to Europe. So-called 'Tulipomania' rose from the passionate desire of the wealthy to own the rarest plants. In Holland, a single tulip bulb was bought for 4,600 florins, plus a coach and a pair of dappled greys.

Papaya

Many of the exotic fruits such as the Paw-paw and Pineapple discovered on the voyages of discovery quickly became fashionable in Europe. The Paw-paw (papaya) is a native of tropical America.

Mankind has always been fascinated by flowers, by their beauty, and by their possibilities for healing and knowledge. Amgueddfa Cymru holds a unique collection of more than 9,000 botanical illustrations spanning five centuries.

After a small exhibition at National Museum, Cardiff in 1942, the illustrations were put into store. Fifty years later the breadth and significance of the collection was rediscovered and their exquisite draughtsmanship fully appreciated.

The collection comprises work ranging from professional engravings to amateur watercolours, and includes several items by acknowledged masters such as Georg Dionysius Ehret and Pierre Joseph Redouté.

500 years of botanical illustrations

The collection traces the development of botanical illustration and its relationship between art and science from the medieval herbals of the Dark Ages, when man feared nature, through the Enlightenment and the great voyages of discovery to the contemporary illustrations of the 21st century.

Floras

By 1600, after the early woodblocked herbals, the process of engraving on metal allowed a finer delineation of every minute detail, revolutionising botanical illustration. Flora Londinensis (1777-87) by William Curtis is one of the most famous British floras listing all the plants within a ten-mile radius of London. An important early 19th century European flora is the Flora Danica (1763-1885), which took almost a hundred years to complete.

In the 17th century, plants were grown for their beauty as well as practical and scientific use. The wealthy produced 'florilegias' illustrating the rare and beautiful plants on their estates, while scientific guides were full of precise illustrations from a whole range of plants.

The collection contains many original prints from the 17th century, including work by Redoute, Sowerby, Fitch and the Welsh-born Sydenham Edwards.

The introduction of taxonomy

In 1753 the Swedish naturalist Carl Linnaeus developed a new system of naming and classifying all living things. Everything was given two names in Latin: a genus name and a species name. This had a profound impact on the style of botanical illustration. Emphasis was now on the plant's sexual organs — much to the alarm of polite society.

The acceptance of the new Linnaean system was helped, in part, by the high quality of illustrations produced by G. D. Ehret at that time. The Museum holds illustrations by Ehret from Plantae Selectae (1750-73) and also a collection by J. S. Miller from Bute's Botanical Tables (1785), commissioned by John Stuart, 3rd Earl of Bute.

The collection also includes works by Redouté, Kirchner and Elizabeth Blackwell. Backwell illustrated a herbal entitled A Curious Herbal to free her husband from incarceration in a debtor's prison.

Voyages of discovery

Botanists accompanying the epic voyages of discovery in the 18th and 19th centuries were the first to record and collect the exotic plants encountered in the remote uncharted lands. For the first time Europeans saw pictures of exotic fruits such as pineapples, paw-paws and pomegranates. Examples in the collections include Banks' Florilegium and works from Curtis's Botanical Magazine.

Victorian enthusiasm

The Victorians brought about an immense enthusiasm for science. Engravings of newly introduced plants became widely available through journals and popular magazines, such as Carter's Floral Illustrations and Paxton's Floral Garden.

With the discovery of Victoria regia, the giant water lily from the Amazon, there was much rivalry between the gardeners of the stately houses of England as to who would be first to induce it to flower in Britain. Joseph Paxton, the gardener at Chatsworth, won the race. It is said that the structure of the huge leaf inspired his design for the Crystal Palace.

The largest turtle in the world

15 August 2007

The leatherback turtle on display at National Museum Cardiff was washed ashore on Harlech beach, Gwynedd in September 1988. Sadly, the turtle had drowned after being trapped by fishing lines. It was approximately 100 years old when it died. The turtle attracted worldwide attention as it was the largest and heaviest turtle ever recorded, measuring almost 3m (9ft) in length and weighing 914 kilos (2,016 pounds).

The turtle's arrival on the beach saw a flurry of activity by Museum staff who were keen to exhibit the turtle. However, preparing such a specimen for display was not straightforward.

Leatherback turtle

The turtle had to be flipped upside down before repairing cracks on the underside.

Displaying the world's largest turtle

After undergoing an autopsy for scientific information, the skin was removed and preserved and a mould of the body shape was made. The preserved skin was stretched over the mould to produce a lifelike pose.

The skeleton was also removed and prepared for display alongside the body. The taxidermy mount and associated skeleton were then put on display in their own gallery, with linking displays on the leatherback's history, threats, ecology and conservation.

Leatherback turtle

The Leatherback being cleaned and repaired

Sixteen years on

After 16 years on display, significant cracks had started to appear on the specimen. There had long been problems with cracking, and it had been patched up over the years. Low humidity was identified as a cause, so there was no choice but to close the gallery and conserve this popular specimen properly.

The first stage was to clean the turtle of its layer of dust and oily grime. A non-ionic detergent removed the worst of the dirt.

Once reasonably clean the next stage was to return the distorted parts of the specimen back to the correct shape. This involved soaking the exterior with a solution of deionised water, salt and detergent, enabling it to be moved back into position.

Removing old repairs

Once the specimen was dry, the old repairs were removed. This was a long and slow process requiring care so as not to damage the turtle's skin any further. A large amount of the skin had been painted black some years before, so this also had to be removed. This was achieved with acetone and a mobile fume extraction system.

Once the previous repairs and paint were removed, the turtle's original patterns and skin texture could be seen once more. Gaps and splits in the specimen were then filled in and painted over to blend with the turtle's original skin colour and texture.

Letherback turtle

The Turtle after conservation

Leatherback Turtle

The leatherback turtle in its new display at the National Museum, Cardiff

Redisplaying

The skeleton was also carefully cleaned before the finished turtle was re-hung as before. After 4 months of work, the turtle gallery could finally be re-opened to the public.

Another journey for the turtle

Conditions in the turtle gallery were continuing to cause conservation problems. As a result, during 2006 the turtle was moved to a new location in the adjoining 'Man and the Environment' gallery, next to the humpbacked whale. The new space has better environmental conditions, allowing the turtle to remain on open display. In addition, the information panels have been renewed with up-to-date information. The turtle now sits as a fine addition to this gallery space.

Up close with nature

3 August 2007

Witness the bizarre structures and patterns of nature close up. These amazing images have been created by the scientists at Amgueddfa Cymru using highly magnified photography. From butterflies to microscopic plankton - remarkable details are revealed in a whole new light in these breathtaking pictures, which are to be admired for their striking beauty as well as the scientific value they hold.

At this level of magnification, reality becomes quite surprising, click on the images below to discover more...