Showing posts with label Lancashire. Show all posts
Showing posts with label Lancashire. Show all posts

Wednesday, 20 June 2018

Warning issued after bloom of Lion's Mane Jellyfish wash up on Lancashire coast.

A warning has been issued by the Lytham and Blackpool Coastguard after dozens of Lion's Mane Jellyfish, Cyanea capillata, washed up on the coast between Fylde and Lytham St Annes this week. The Jellyfish are potentially dangerous if touched, as they can still sting when dead, though the stings are no worse than those of Bees or Wasps, and not generally dangerous unless people have an allergic reaction. The Jellyfish are far more dangerous when encountered in the water, as their tentacles can entangle swimmers, resulting in large numbers of stings, which can cause the swimmer to go into shock and drown.

A Lion's Mane Jellyfish, Cyaneae capillata, off the coast of Sweden in 2016. Wikimedia Commons.

The Lion's Mane Jellyfish is the largest known species of Jellyfish, reaching over 2 m in diameter and with tentacles that can be more than 30 m in length. They are exclusively found in cooler temperate waters around the North Atlantic, North Pacific, Arctic Ocean and Baltic Sea. They are pelagic, able to swim against currents under their own energy, rather than drifting as many Jellyfish do, and spend most of their lives in open water, but they move into coastal waters towards the end of their annual life-cycle, when the (sexual) medusae produce eggs, which in turn hatch into a polyp which attaches to the seafloor in shallow waters, from which new medusae bud off asexually.

See also,,,

http://sciencythoughts.blogspot.com/2018/06/aurelia-sp-over-800-bathers-stung-by.htmlhttp://sciencythoughts.blogspot.com/2018/04/western-australian-beach-closed-after.html
http://sciencythoughts.blogspot.co.uk/2018/04/western-australian-teenager-released.htmlhttp://sciencythoughts.blogspot.co.uk/2018/03/warning-issued-to-tourists-after-box.html
http://sciencythoughts.blogspot.co.uk/2016/07/jellyfish-damage-to-farmed-salmon-on.htmlhttp://sciencythoughts.blogspot.co.uk/2014/11/scavengers-on-jellyfish-carcasses-on.html
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Saturday, 29 August 2015

Cryptosporidium discovery at water treatment plant leaves around 300 000 without drinkable water in Lancashire, England.

Around 300 000 homes were left without drinkable water after the parasitic microorganism Cryptosporidium was discovered at the United Utilities operated Franklaw Water Treatment Plant near Preston in Lancashire, northwest England, on Thursday 6 August 2015. The parasite, which causes stomach cramps and diarrhea and which can cause severe and persistent infections in small children and people with immunological disorders, is notoriously hard to remove by the use of disinfectants and is best eradicated from water supplies with exposure to ultraviolet radiation. For this reason around 300 000 customers in the Blackpool, Chorley, Fylde, Preston, South Ribble and Wyre areas were advised to boil all water prior to use for consumption or cleaning from 7 August onwards. On Thursday 27 August United Utilities lifted the boil water on about 80 000 homes in the Preston, Blackpool and Chorley areas, and the company hopes to restore normal water supplies to all of its customers within a week.

Cryptosporidium: Mature schizont releasing merozoites. The spherical organisms releasing the crescent-shaped merozoites are seen attached to the microvillus brush border. RE Pugh/Deb Stenzel/Laurine Moreau.

Cryptosporidium is an Apicomplexan Protist (single celled Eukaryote, an organism having a cell nucleus) related to the pathogenic Toxoplasma and Malaria causing Plasmodium, though unlike these organisms it causes infections in Mammals and Birds without an intermediate invertebrate host. The organisms live and reproduce inside the small intestines of their hosts, producing large numbers of hardy cysts which are expelled in feces, and which can survive outside a host for long periods of time. It is these cysts which are resistant to disinfectants, making them problematic if they reach water treatment plants, swimming pools or similar man-made environments. Eventually the cysts reach a new host, typically via consumption of water, and mature to become reproductive schizonts, causing a new infection and repeating the infection cycle.

See also...

Water quality is a major issue in South Africa, where efforts to expand clean water supplies to the whole population in the post-Apartheid era have faced severe challenges due to a limited supply of potable...


Free-living Amoebae are unicellular protozoan’s common in aquatic ecosystems, which are also known to colonize Human created water systems such as water supply systems and swimming pools. Whilst in some ways these organisms can be helpful, consuming a range of Bacterial, Viral and Fungal pathogens...


Toxoplasma gondii is a protozoan parasite that affects humans, and many other animals, across the globe. While it causes disease in many organisms, it reproduces only in Felids, particularly in Domestic Cats, with oocysts (egg-like cysts) being shed in Cat faeces spreading the disease to many other organisms...


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Monday, 2 September 2013

Magnitude 2.6 Earthquake of the Lancashire coast.

The British Geological Survey recorded a Magnitude 2.6 Earthquake at a depth of 10 km, beneath the Irish Sea roughly 30 km off the coast of Lancashire, slightly after 7.35 am British Summertime on Friday 31 August 2013. This is a moderately large quake by British standards, though there was no danger of it causing any damage or injuries this far offshore. It was felt in the Clevelys area.

The approximate location of the 31 August 2013 Irish Sea Earthquake. Google Maps.

Earthquakes become more common as you travel north and west in Great Britain, with the west coast of Scotland being the most quake-prone part of the island and the northwest of Wales being more prone  to quakes than the rest of Wales or most of England.

The precise cause of Earthquakes in the UK can be hard to determine; the country is not close to any obvious single cause of such activity such as a plate margin, but is subject to tectonic pressures from several different sources, with most quakes probably being the result of the interplay between these forces.

Britain is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the south. It is also affected by lesser areas of tectonic spreading beneath the North Sea, Rhine Valley and Bay of Biscay. Finally the country is subject to glacial rebound; until about 10 000 years ago much of the north of the country was covered by a thick layer of glacial ice (this is believed to have been thickest on the west coast of Scotland), pushing the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks are springing (slowly) back into their original position, causing the occasional Earthquake in the process. 

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. If you felt this quake, or were in the area but did not (which is also useful information) then you can report it to the British Geological Survey here.


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Tuesday, 27 August 2013

Earthquakes off the Lancashire coast.

Slightly before 6.40 am British Summertime (slightly before 5.40 am GMT) on Sunday 25 August 2013, a Magnitude 2.4 Earthquake at a depth of 5 km occurred beneath the Irish Sea, roughly 25 km off the Lancashire Coast, according to the British Geological Survey. This was followed by a second quake slightly before 11.00 am British Summertime (slightly before 10.00 am GMT), this time with a Magnitude of 3.2 at a depth of 8 km, and roughly 1 km to the southwest of the original tremor. These are quite large events for the UK, although unlikely to cause any problems this far offshore. Both quakes were felt in the Fleetwood and Barrow-in-Furness areas.


The approximate locations of the 25 August 2013 Irish Sea Earthquakes. Google Maps.


Earthquakes become more common as you travel north and west in Great Britain, with the west coast of Scotland being the most quake-prone part of the island and the northwest of Wales and England being more prone  to quakes than the rest of the countries.

The precise cause of Earthquakes in the UK can be hard to determine; the country is not close to any obvious single cause of such activity such as a plate margin, but is subject to tectonic pressures from several different sources, with most quakes probably being the result of the interplay between these forces.

Britain is being pushed to the east by the expansion of the Atlantic Ocean and to the north by the impact of Africa into Europe from the south. It is also affected by lesser areas of tectonic spreading beneath the North Sea, Rhine Valley and Bay of Biscay. Finally the country is subject to glacial rebound; until about 10 000 years ago much of the north of the country was covered by a thick layer of glacial ice (this is believed to have been thickest on the west coast of Scotland), pushing the rocks of the British lithosphere down into the underlying mantle. This ice is now gone, and the rocks are springing (slowly) back into their original position, causing the occasional Earthquake in the process.

Witness accounts of Earthquakes can help geologists to understand these events, and the structures that cause them. If you felt either of these quakes, or were in the area but did not (which is also useful information) then you can report it to the British Geological Survey here (first quake) or here (second quake).

See also Magnitude 1.3 Earthquake of the Isle of the Isle of ArranMagnitude 2.1 Earthquake in Cheshire, EnglandMagnitude 1.2 Earthquake in the Peak District, DerbyshireMagnitude 3.8 Earthquake off the Lleyn Peninsula, North Wales and Earthquake in Shropshire.

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Friday, 25 May 2012

Earthquake near Rochdale, Lancashire.

On Friday 25 May 2012, slightly before 4.25 British Summertime (slightly before 3.25 GMT) the British Geological Survey recorded an Earthquake roughly 1 km south of the Lancashire village of Bacup, or 10 km north of Rochdale, at a depth of 7 km, measuring 1.2 on the Richter Scale. An Earthquake this deep and this small is highly unlikely to have caused any damage or injuries, and may not have been felt by anyone.

Map showing the approximate location of the quake. BGS.

As a rough rule of thumb, the further north and west you go in Great Britain the more Earthquakes there are; thus Lancashire is one of the most quake-prone counties in England.

The causes of Earthquakes in the UK are complex, as the country is not near any active tectonic margins. Europe is being pushed to the East buy the expansion of the Atlantic Ocean and the North by the impact of Africa from the south. There are also lesser expansion centers beneath the North Sea, the Bay of Biscay and the Rhine Valley, which all excerpt stresses on UK rocks. Finally there is glacial rebound; the northernmost parts of Britain were covered by hundreds of meters of ice until about 10 000 years ago. This pushed the rocks of the crust down into the underlying mantle, and now that the ice is gone these rocks are slowly rebounding.

If you did feel the quake, or were in the area at the time but did not feel it, then you can inform the British Geological Survey here. Statements from people who have felt shaking help geologists to build up a better understanding of the movement of the rocks under the UK.

See also Earthquake in Burnley, LancashireEarthquake in CumbriaEarthquake in Yorkshire and Earthquakes on Sciency Thoughts YouTube.

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Tuesday, 8 May 2012

Earthquake in Burnley, Lancashire.

On Monday 7 May 2012, at 8.20 pm GMT (9.20 pm British Summertime), the British Geological Survey recorded an Earthquake slightly to the northeast of Burnley in Lancashire, measuring 1.6 on the Richter Scale, at a depth of 17 km. Such a small quake at this depth is highly unlikely to have been felt, much less to have caused any damage or injuries at the surface.

The location of the 7 May quake. BGS.

The UK is not considered a particularly quake-prone country as it is not close to any tectonic margins and seldom suffers large quakes, but small quakes like this are not uncommon, and as a rule-of-thumb are more common the further north and west you go in the country. A number of sources of tectonic stress contribute to this. Firstly the Atlantic is spreading along its central ridge, pushing Eurasia eastwards (and North America to the west). Then Africa is pushing into Europe from the south, which causes uplift in the Alps and tectonic stress across Europe; this causes more tremors in the east Mediterranean region, but the rest of the continent is not immune. Then there are smaller spreading centers beneath the North Sea, Bay of Biscay and Rhine Valley, all of which excerpt some pressure on the UK. Finally there is glacial rebound; the north of Britain was covered by ice several hundred meters thick till about 10 000 years ago, which pushed the rocks of the lithosphere down into the underlying mantle slightly. Now this ice has gone the rocks are rebounding, at geological speeds, a process that will probably continue for thousands of years yet to come.


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Tuesday, 17 April 2012

Report recommends Fracking should be allowed to continue in the UK.

Fracking, or Hydraulic Fracturing, is a process by which water, sand and chemicals are forced into buried sediments in order to shock them into releasing trapped hydrocarbons, which can then be extracted for commercial use. This has proved highly controversial with environmentalists, who accuse the process of causing Earthquakes, polluting groundwater, and using large amounts of fresh water.

To date the UK has been host to only a single, experimental, fracking project, at Preese Hall near Blackpool in Lancashire. Operations were stopped at Preese Hall in 2011, after two small Earthquakes in April and May were connected to activities there.

The Preese Hall well site in Lancashire. The Australian.

This week a report commissioned by the Department of Energy and Climate Change was published, entitled 'Preese Hall Shale Gas Fracturing: Review and Recommendations for Induced Seismic Mitigation'. This was written by Peter Styles of the Department of Geography, Geology and the Environment at Keele University, Brian Baptie of the British Geological Survey and Christopher Green, director of GFrac Technologies, and concludes that fracking should be allowed to continue in the UK, as long as certain conditions are met.

The team recognize that the Preese Hall operations were the most likely cause of the Lancashire Earthquakes, and that there was a high likelyhood of continued operations in the same area causing further quakes. In addition the report found that the quakes caused deformation in the structure of the well - deformation that could lead to chemicals used in the process leaking into other strata than the ones intended.

An earlier report in the US found that chemicals from a fracking operation there had entered aquifers, but was unable to say whether this was due to the process itself, or due to spillages at ground level. This was widely cited as vindication of the process, which is odd since clearing the fracking element of the operation could only be achieved by claiming blundering incompetence in another part of the process, but spin often seems to overtake logic in debates over fracking (and the energy industry in general).

Fracking undoubtably does cause Earthquakes. An Earthquake is shaking in the ground, a large truck driving past your house doesn't just feel like an Earthquake, it is an Earthquake. Blasting pressurized water and sand into buried rocks in the hope of causing them to fracture will definitely cause Earthquakes (if it didn't there wouldn't be any fracturing, and the process would not work). Unfortunately extraction companies involved in hydraulic fracturing employ lobbyists and press spokesmen who do not always appreciate this, and who may not be concerned too much if the truth gets slightly obscured in getting their side of the story across, leading to some confusion on this point.

What should be being discussed is the scale of Earthquakes that can be caused by fracking. Engineers in the industry have repeatedly estimated that the process should not be causing quakes greater than magmitude 1.0 on the Richter Scale, but several areas in the US where fracking operations are underway have suffered increases in seismic activity with quakes in excess of 3.0 being reported. The Richter Scale is logarithmic, so a magnitude 3.0 quake is 100 times as powerful as a 1.0 quake. Nobody has been able to explain how fracking could be causing quakes this much larger than predicted, leading the industry to claim that the increases are co-incidental, and that without a proposed mechanism they cannot be held responsible. In this light the UK report, which directly links fracking to two Earthquakes measuring 1.5 and 2.3 on the Richter Scale is a blow to the industry.

The report recommends that all hyrdraulic fractioning operations in the UK should be carefully monitored for seismic activity, at the operators expense, and any operation shown to have caused a quake in excess of 0.5 on the Richter Scale should be halted immediately. They furthermore note that it is highly unlikely that a fracking operation in the UK could ever cause a quake in excess of 3.0 on the Richter Scale, and that a quake on that scale could not cause any serious damage.

While this has widely been reported as a green-light for the fracking industry in the UK, it potentially places a considerable additional burden upon them, since the expense of installing seismic monitors would add significantly to the cost of the operation, and the possibility of being forced to close down at any point would make investing in any such operation highly risky (an industry that cannot explain how it causes larger quakes would probably be unable to prevent or predict this).

Environmental groups in the UK have expressed a great deal of concern at the report, even though it recommends tight regulation of the industry. This is not surprising, as the current UK government has a track record of friendliness towards the hydrocarbons industry (Business Secretary Vince Cable is a former oil-man), and of opposing environmental regulation of any sort. In addition Chancellor of the Exchequer George Osborne recently announced plans to encourage the building of gas-fired power stations in the UK, which suggests that fracking operations targeting natural gas are likely to be welcomed. In the light of this there is clearly a concern that the report could be used to justify resumption and expansion of fracking operations in the UK, without putting into place the recommended regulatory measures.

The operators of the Preese Hall site, Cuadrilla Resources, are certainly keen to resume operations. They estimate that the Lancashire field contains about 11.3 trillion m³ of natural gas; enough to power the UK for over 50 years. However the British Geological Survey estimate the field contains much less gas, 0.13 trillion m³, and that only 5-10% of this will be recoverable - enough to power the UK for 21 days. This big a disparity in estimates shows a surprising degree of optimism on the part of Cuadrilla Resourses, which if extended to other areas of the business would in themselves raise concerns about the companies safety and environmental policies.

In addition to the Lancashire field the company has obtained licenses for sites in Sussex, Kent and Surrey. There are thought to be reserves of shale gas suitable for extracting by fracking in Wales, Northern Ireland and Scotland as well as in England.


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