The Hell of High Water: Tsunami and the Cornish Coast.
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Invited lecture by Professor Simon Haslett at University College, Falmouth on Tuesday 28th September 2010. Simon Haslett is Professor of Physical Geography.
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The Hell of High Water: Tsunami and the Cornish Coast
The 2011 Annual Kelliwic Lecture presented by Professor Simon Haslett at Callington Town Hall, Cornwall, on Sunday 29th May 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
The British Tsunami: the 1607 flood.
1. Professor Simon Haslett and Dr. Ted Bryant presented evidence that a tsunami, rather than a storm, caused widespread flooding along the coasts of Wales and Somerset in 1607 that resulted in over 2000 deaths.
2. They conducted fieldwork along the coast to examine landscapes and sediment layers for signs of a tsunami, and sampled and analyzed sediments from locations mentioned in historic accounts of the 1607 flooding.
3. Their research and a BBC documentary about the 1607 tsunami received significant interest, with viewers providing new information and locations for further study, and inspiring other researchers to study tsunami history.
The 1607 Flood: a tsunami in the Bristol Channel?
Presentation by Professor Simon Haslett to the Geographical Association at King's College, Taunton, on Tuesday 15th November 2012.
A presentation based on research featured in 'Killer Wave of 1607' as broadcast by BBC2 Timewatch. The flood of that year in the Bristol Channel and Severn Estuary was the worst ever recorded in the British Isles. The area affected stretched from North Devon, through Somerset and Gloucestershire, and along the South Wales coast from Monmouthshire to Carmarthenshire, some 570 km of coast! The coastal population was devastated with at least 2000 fatalities according to one of the contemporary sources. In some parts of the coast the population never recovered from the social and economic disaster. Simon and his co-worker have used documentary and fieldwork evidence to propose a new interpretation of its cause as a tsunami. The BBC produced a follow-up Timewatch programme entitled 'Britain’s Forgotten Floods' that followed Simon around the British coastline examining further evidence for tsunami impact.
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Mount Vesuvius is a volcano located near Naples, Italy that has erupted eight times in the last 17,000 years. On August 24, 79 AD, a major eruption buried the cities of Pompeii and Herculaneum under ash, killing over 16,000 people. The eruption preserved the cities and their victims, leaving casts of their bodies. Since then, Vesuvius has had several more eruptions, the most recent in 1944, which caused damage during World War II. Today, nearly 3 million people live in the area and would be at risk from a future eruption.
Cumbria Flooding
Heavy rainfall caused widespread flooding across Cumbria in northern England in 2009, with a conveyor of warm, moist air from the Azores bringing 34 hours of steady rain to the region. The floods were especially severe where rivers converged in towns like Cockermouth, due to the heavy rain overwhelming drainage systems. Thousands of homes and businesses were damaged by the flooding, costing over £3 billion to repair the infrastructure and helping to make 2009 the wettest year on record for the UK.
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The 2009 flood in the River Derwent, Cumbria was caused by both physical and human factors. Physically, warm moist air dropped over 400mm of rain in 24 hours, breaking the UK record, which was too much for the ground to absorb. This caused overflow that rapidly filled streams and rivers like the Derwent and Cocker. At their confluence, high discharges combined to cause flooding in Workington. Human factors were urbanization increasing impermeable surfaces and faster water flow into rivers, and blocked or inadequate sewers in towns like Cockermouth and Keswick that caused flooding.
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Carlisle, located on the flood plain of the River Eden where three rivers meet, has a long history of flooding. The January 2005 floods were caused by exceptionally heavy rainfall that saturated the ground and led to rapid rising of river levels. Over 2,700 homes were affected, three people died, and costs were estimated at over £400 million. Impacts included homes flooded to the second floor, emergency services stations flooded, and difficulties with evacuation efforts. Responses involved immediate evacuation of people and relief centers, as well as long-term plans for flood management schemes and engineering solutions.
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Mount Vesuvius is a volcano located near Naples, Italy that erupted catastrophically in 79 AD. The eruption buried the towns of Pompeii and Herculaneum under ash and rock, killing approximately 16,000 people. Vesuvius had shown signs of activity in previous decades, including a large earthquake in 63 AD. When it erupted in 79 AD, it expelled molten rock and ash at a high rate, quickly covering the towns. The region was not rebuilt after the disaster due to the extensive damage, though it has since become an important archaeological site and tourist attraction. Vesuvius remains an active volcano today.
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The Hell of High Water: Tsunami and the Cornish Coast
The 2011 Annual Kelliwic Lecture presented by Professor Simon Haslett at Callington Town Hall, Cornwall, on Sunday 29th May 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
The British Tsunami: the 1607 flood.
1. Professor Simon Haslett and Dr. Ted Bryant presented evidence that a tsunami, rather than a storm, caused widespread flooding along the coasts of Wales and Somerset in 1607 that resulted in over 2000 deaths.
2. They conducted fieldwork along the coast to examine landscapes and sediment layers for signs of a tsunami, and sampled and analyzed sediments from locations mentioned in historic accounts of the 1607 flooding.
3. Their research and a BBC documentary about the 1607 tsunami received significant interest, with viewers providing new information and locations for further study, and inspiring other researchers to study tsunami history.
The 1607 Flood: a tsunami in the Bristol Channel?
Presentation by Professor Simon Haslett to the Geographical Association at King's College, Taunton, on Tuesday 15th November 2012.
A presentation based on research featured in 'Killer Wave of 1607' as broadcast by BBC2 Timewatch. The flood of that year in the Bristol Channel and Severn Estuary was the worst ever recorded in the British Isles. The area affected stretched from North Devon, through Somerset and Gloucestershire, and along the South Wales coast from Monmouthshire to Carmarthenshire, some 570 km of coast! The coastal population was devastated with at least 2000 fatalities according to one of the contemporary sources. In some parts of the coast the population never recovered from the social and economic disaster. Simon and his co-worker have used documentary and fieldwork evidence to propose a new interpretation of its cause as a tsunami. The BBC produced a follow-up Timewatch programme entitled 'Britain’s Forgotten Floods' that followed Simon around the British coastline examining further evidence for tsunami impact.
Mt. vesuvius eruption
Mount Vesuvius is a volcano located near Naples, Italy that has erupted eight times in the last 17,000 years. On August 24, 79 AD, a major eruption buried the cities of Pompeii and Herculaneum under ash, killing over 16,000 people. The eruption preserved the cities and their victims, leaving casts of their bodies. Since then, Vesuvius has had several more eruptions, the most recent in 1944, which caused damage during World War II. Today, nearly 3 million people live in the area and would be at risk from a future eruption.
Cumbria Flooding
Heavy rainfall caused widespread flooding across Cumbria in northern England in 2009, with a conveyor of warm, moist air from the Azores bringing 34 hours of steady rain to the region. The floods were especially severe where rivers converged in towns like Cockermouth, due to the heavy rain overwhelming drainage systems. Thousands of homes and businesses were damaged by the flooding, costing over £3 billion to repair the infrastructure and helping to make 2009 the wettest year on record for the UK.
Causes of the River Derwent Flood, 2009
The 2009 flood in the River Derwent, Cumbria was caused by both physical and human factors. Physically, warm moist air dropped over 400mm of rain in 24 hours, breaking the UK record, which was too much for the ground to absorb. This caused overflow that rapidly filled streams and rivers like the Derwent and Cocker. At their confluence, high discharges combined to cause flooding in Workington. Human factors were urbanization increasing impermeable surfaces and faster water flow into rivers, and blocked or inadequate sewers in towns like Cockermouth and Keswick that caused flooding.
Carlisle floods jan 2005
Carlisle, located on the flood plain of the River Eden where three rivers meet, has a long history of flooding. The January 2005 floods were caused by exceptionally heavy rainfall that saturated the ground and led to rapid rising of river levels. Over 2,700 homes were affected, three people died, and costs were estimated at over £400 million. Impacts included homes flooded to the second floor, emergency services stations flooded, and difficulties with evacuation efforts. Responses involved immediate evacuation of people and relief centers, as well as long-term plans for flood management schemes and engineering solutions.
Mount Vesuvius
Mount Vesuvius is a volcano located near Naples, Italy that erupted catastrophically in 79 AD. The eruption buried the towns of Pompeii and Herculaneum under ash and rock, killing approximately 16,000 people. Vesuvius had shown signs of activity in previous decades, including a large earthquake in 63 AD. When it erupted in 79 AD, it expelled molten rock and ash at a high rate, quickly covering the towns. The region was not rebuilt after the disaster due to the extensive damage, though it has since become an important archaeological site and tourist attraction. Vesuvius remains an active volcano today.
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La pandemia de COVID-19 ha tenido un impacto significativo en la economía mundial y las vidas de las personas. Muchos países han impuesto medidas de confinamiento que han cerrado negocios y escuelas. Aunque estas medidas han ayudado a reducir la propagación del virus, también han causado un aumento en el desempleo y problemas económicos. Se espera que la recuperación económica lleve tiempo a medida que los países reabran gradualmente y las personas se sientan seguras para volver a trabajar y gastar.
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This is a call. The best Geography presentation that you are going to see.It contains all you want to need about a flash flood .Enjoy!
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평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『LG777』.『XYZ』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션//BU797。СΟΜ//여권비자//평창허브나라펜션『BU797』.『COM』여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션＼【 FUN88。CO。ＫＲ】＼여권비자//평창허브나라펜션//LG77。XYZ//여권비자//평창허브나라펜션//LG77。XYZ//여권비자
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La pandemia de COVID-19 ha tenido un impacto significativo en la economía mundial y las vidas de las personas. Muchos países han impuesto medidas de confinamiento que han cerrado negocios y escuelas. Aunque estas medidas han ayudado a reducir la propagación del virus, también han causado un aumento en el desempleo y problemas económicos. Se espera que la recuperación económica lleve tiempo a medida que los países reabran gradualmente y las personas se sientan seguras para volver a trabajar y gastar.
코롱호텔//BU797。СΟΜ//독일호텔
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제주도버스여행 미국비자서류
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2007 07 Working Together for Coastal Planning - Tim Stojanovic, EU Corepoint ...
This document discusses strategic coastal planning and policy integration around the Severn Estuary. It outlines the purpose of strategic environmental assessments (SEA) in evaluating the environmental impacts of development plans near coastal areas. The SEA process assesses plans and policies to ensure sustainable development and improved environmental outcomes through identifying issues, consulting stakeholders, evaluating alternatives and monitoring impacts.
Dope quiz
1) The Doors of Perception was originally a phrase from a William Blake poem that was later used as the title of a book by Aldous Huxley about his experiences on psychedelic drugs. Jim Morrison named his band The Doors after Huxley's book.
2) The next person on an exclusive list of members of the "27 Club" who died at age 27 is Amy Winehouse.
3) Pablo Escobar was the head of the Medellin drug cartel and one of the most powerful drug lords, making money from cocaine smuggling with help from George Jung. The last image depicts Escobar being shot by Colombian authorities.
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2007 07 Working Together for Coastal Planning - Tim Stojanovic, EU Corepoint ...
2007 07 Working Together for Coastal Planning - Tim Stojanovic, EU Corepoint ...
Similar to The Hell of High Water: Tsunami and the Cornish Coast.
The 1607 Flood: A Tsunami in the Bristol Channel?
The document summarizes research into the possible causes of the 1607 flood in the Bristol Channel area of the UK. It describes evidence from historical documents of a catastrophic flooding event. The researchers investigated the theory that it was caused by a tsunami rather than a storm surge, through field work examining coastal landscapes and sediment layers for tsunami signatures. While the data collected added to the debate, the researchers were unable to conclusively determine whether a storm surge or tsunami caused the 1607 flood.
A tsunami in South Wales? The 1607 flood in the Bristol Channel and Severn Es...
The flood of 1607 was the worst natural disaster ever recorded in the British Isles. The flood affected most of the South Wales coast from Carmarthenshire in the west to Monmouthshire in the east. On the other side of the Bristol Channel and Severn Estuary, parts of Southwest England were also severely affected stretching from North Devon, through to Somerset and Gloucestershire, which together with South Wales amounts to 570 km of coastline. The coastal population was devastated with at least 2000 fatalities according to one of the contemporary sources. In some parts of the coast the population never recovered from the social and economic disaster. But what caused the flood? This seminar looks at historical documentary and geographical fieldwork evidence collected by Professor Simon Haslett and co-workers in proposing that the 1607 flood may have been due to a tsunami.
Plate Tectonics, Earthquake & Volcano
This document discusses plate tectonics and related landforms, earthquakes, and volcanoes. It begins by describing the four main types of plate boundaries and associated landforms such as mid-oceanic ridges, trenches, and island arcs. It then covers causes of earthquakes including sudden stress release along faults, and factors that influence earthquake damage such as magnitude, building design, and population density. Prediction methods like elastic rebound theory and seismic gaps are also mentioned. Finally, it discusses volcanoes, noting where they form at plate boundaries and hotspots, how scientists monitor and predict eruptions, associated hazards from lava to tsunamis, and ways to reduce risks like controlling lava flows and using hazard maps.
Tsunami
This document provides information about tsunamis through several examples of destructive tsunamis throughout history. It discusses what causes tsunamis, how they propagate and grow in shallow water, and their devastating effects on coastlines. Specific tsunamis summarized include the 1929 Grand Banks tsunami that killed 29 in Newfoundland, the 1946 Aleutian tsunami that caused over $165 million in damage and deaths in Hawaii, and the 1996 Peru tsunami that struck cities along 590 km of coastline.
Boscastle flood North Cornwall Council
This document summarizes a history of flash flooding events in Boscastle, Cornwall and surrounding areas in the UK dating back to the 18th century. It notes several major flooding events that caused significant damage, including in 1827, 1847, 1952 and most recently in 2004 when over 1,000 residents and visitors were affected in Boscastle. The 2004 flooding was described as the largest peacetime rescue in British history, with 58 properties flooded and thousands of pounds needed for infrastructure repairs. While views on climate change conflict, the document acknowledges climate is changing and instances of severe storms and floods are expected to increase.
2011 04 Coastal Flooding, 1607 Floods, recent Storm Surges and Weather Events...
Coastal Flooding, 1607 Floods, recent Storm Surges and Weather Events in the Severn Estuary – Kevin Horsburgh
tsunami[1].ppt
The document provides information about tsunamis, including what causes them, how they behave in deep ocean versus shallow coastal waters, examples of destructive past tsunamis, and tips for preparing for tsunamis. It discusses how tsunamis are formed by earthquakes, landslides, volcanic eruptions and other events. It also explains that while tsunamis have long wavelengths and travel fast in deep ocean, they slow down and grow taller as they reach shallow coastal waters, potentially reaching over 100 feet high. Examples of destructive tsunamis discussed include those in Hawaii in 1975 and 1960, Alaska in 1964, Chile in 1960, and Peru in 1996.
TSUNAMI
The document discusses various types of tsunamis including those caused by landslides, meteorological conditions, and human activities. It provides examples of destructive meteotsunamis and discusses attempts to artificially trigger tsunamis through explosions. The characteristics of tsunamis are explained, noting that while waves have short wavelengths in deep ocean, they have much longer wavelengths and travel very quickly. The document also discusses drawback effects, forecasting tsunami probability, anatomy of tsunamis, facts about tsunamis, and preparation and safety during and after tsunamis.
Plate Geology
The canyon provides a green oasis closer than one may think. Hiking its trails can be treacherous but rewarding. The author describes their experience hiking difficult trails in Spearfish Canyon. They had to climb steep hills with loose rocks and heave over fallen trees and boulders, tiring themselves as the trails got steeper. Their ankles relied on sturdy boots as they hiked hundreds of feet up the mountain.
Glacial Outburst Flooding
1) Glacial Lake Missoula formed during the last ice age when an ice dam blocked the Clark Fork River, causing a huge lake to form. The lake drained catastrophically when the ice dam failed, carving out features like ripple marks and waterfalls.
2) These floods discharged at rates over 600 times the modern Amazon River and formed huge ripple marks up to 30 meters tall. Analysis of sediment layers indicates periods of both low and high energy deposition from the filling and draining of the lakes.
3) Flood waters from Lake Missoula entered a second ice-dammed lake, Glacial Lake Columbia, and found outlets through channels now known as the Channeled Sc
Tsunami
This document is a PowerPoint presentation on tsunamis submitted by Jisha Antony for their social science class. It introduces tsunamis, explaining that they are a series of waves caused by displacement of water, generally in oceans or large lakes, due to earthquakes, volcanic eruptions, landslides or other disturbances above or below water. It then covers the etymology, history, effects and warnings of tsunamis, noting Japan's long history with tsunamis and the devastating 2004 Indian Ocean tsunami. The presentation discusses drawbacks like deceptive troughs and receding waters, and concludes that while tsunami prediction has improved, much remains unknown about what triggers them.
VolcanoesII.ppt
This document discusses the prediction and impacts of volcanic eruptions. It describes methods for long-term and short-term prediction of eruptions based on monitoring factors like gas emissions, surface tilting, and earthquake activity. The impacts discussed include hazards from lava flows, ash falls, pyroclastic flows, lahars, nuée ardentes, landslides, volcanic gases, tsunamis, and potential effects on global climate. Examples of historically deadly eruptions like Mount Pelée and Krakatoa are provided. The document also introduces the concept of supervolcanic eruptions ejecting over 1,000 cubic km of material.
Assessing Tsunami Hazard for Hong Kong: INQUA 2007
Presentation given during the 2007 INQUA Congress in Cairns, Abstract published under Quaternary International Vol 167-168, Supplement 1, Pp. 69
Earthquakes
1) The document discusses earthquakes, including what causes them, where they are located, and their effects. Most earthquakes occur at plate boundaries where tectonic plates meet.
2) Specific examples of earthquake events are described, such as the 1906 San Francisco earthquake which was caused by movement on the San Andreas Fault.
3) Consequences of earthquakes like building damage, fires, landslides and tsunamis are explained. Mitigation strategies to reduce earthquake risks are also outlined.
Tsunami Hazards in Cascadia
Speaker: Timothy Walsh, Washington Department of Natural Resources Division of Geology and Earth Resources.
TSUNAMI NATURES FURY
Tsunami is a Japanese word meaning harbor wave. Tsunamis are series of large waves generated by earthquakes, landslides, volcanic eruptions, or other disturbances that displace large volumes of water. The first recorded tsunami was in 1480 BC in the Mediterranean. Tsunamis cause devastating damage when they reach coastal areas due to their ability to flood large areas inland with fast-moving water. Proper warning systems and evacuation of coastal areas can help reduce loss of life from tsunamis.
Tsunami a natural disaster
A tsunami is a series of enormous ocean waves generated by earthquakes, landslides, volcanic eruptions, or meteor impacts that displace large volumes of water and cause catastrophic damage when they reach land. Tsunamis are very difficult to detect when they approach coastal areas out in the open ocean, and can travel at over 500 mph. Areas near fault lines in the Pacific Ocean called "seismic zones" are particularly at high risk of experiencing tsunamis. On December 26, 2004, a 9.3 magnitude earthquake in the Indian Ocean triggered a devastating tsunami that killed over 230,000 people across 14 countries, with deaths reported as far away as Africa.
Earthquakes
Earthquakes occur along plate boundaries due to the buildup and sudden release of energy from shifting tectonic plates. When plates lock, potential energy builds until released as seismic waves that propagate outward from the earthquake focus. Most earthquakes occur along oceanic and continental plate edges or along faults like normal, reverse, and transform boundaries. P and S waves are the primary seismic waves, with P waves traveling faster and S waves causing the shaking felt during quakes. Earthquake magnitude measures the energy released using the Richter scale, while intensity qualitatively describes the shaking effects on a place using the Mercalli scale.
NATURAL AND MAN MADE DISASTERS
This document lists and provides details about various natural and man-made disasters. It discusses the top 10 natural disasters including earthquakes, tornados, volcanic eruptions, tsunamis, floods, wildfires, droughts, avalanches, and landslides. For each type of disaster, it gives examples of significant events and impacts, such as the 1960 Chile earthquake being the largest ever recorded or the 2004 Indian Ocean tsunami killing over 230,000 people. Man-made disasters discussed include the 1945 atomic bombings of Hiroshima and Nagasaki, the 9/11 terrorist attacks, and the 2010 Deepwater Horizon oil spill.
Transform boundary
A transform boundary is a plate boundary where plates move horizontally past each other in opposite directions. Convection currents in the mantle cause plate movement. Transform boundaries collect energy from plate movement that is eventually released through earthquakes and tsunamis, as seen at the San Andreas Fault and from a Pacific Ocean earthquake that caused a major tsunami. While they do not form volcanoes or mountains, transform boundaries can create dangerous earthquakes and tsunamis.
Similar to The Hell of High Water: Tsunami and the Cornish Coast. (20)
A tsunami in South Wales? The 1607 flood in the Bristol Channel and Severn Es...
A tsunami in South Wales? The 1607 flood in the Bristol Channel and Severn Es...
2011 04 Coastal Flooding, 1607 Floods, recent Storm Surges and Weather Events...
2011 04 Coastal Flooding, 1607 Floods, recent Storm Surges and Weather Events...
Assessing Tsunami Hazard for Hong Kong: INQUA 2007
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More from Prof Simon Haslett
Getting Published! Exploring strategies, myths and barriers of academic publi...
Publications are an important aspect of the work of an academic; remaining the principal vehicle through which research is reported, opinions aired, reviews undertaken, and knowledge transferred, and writing is also a useful learning exercise. For many, it also underpins teaching and curricula, means greater success in research grant applications, and a good publication track record is still seen by many institutions as a key recruitment and promotion criteria. Yet traditionally how to get your work published has not been taught, but learnt through trial and error, mainly from rejection by journal editors. This seminar is aimed at inexperienced academic authors and explores and discusses the issues surrounding the strategy and publication of academic work, and addresses some of the myths and barriers that might discourage would-be authors after the research and writing process is complete.
A geological journey along the south Ceredigion coast.
This document provides a summary of the geology along the southern coast of Ceredigion, Wales. It describes the different geological time periods represented in the local rock formations, from the Quaternary period to the Ordovician period from over 400 million years ago. It focuses on the Yr Allt Formation from the Ashgill series of the Silurian period, which dates to the Hirnantian global ice age around 445 million years ago. Features of this formation like slumping, ripples marks, and dewatering structures provide evidence of rapid deposition in shallow seas during a period of falling sea levels.
The Geology of the south Cardigan Bay coast.
Presented to the Yangzte University Geology Group at the University of Wales Trinity Saint David, Carmarthen campus, on 11th March 2020.
Projection of Wales as an internationally engaged/forward-looking nation.
Presented at the 'Universities as Global Communities' event at Bangor University on Thursday 13th February 2020. The event was jointly organised by the Learned Society of Wales and Universities Wales, and is part of the 'Wales and the World' series.
Academic Publication
This seminar presentation aimed to help academics overcome barriers to publishing their research. It explored motivations for publishing, approaches to writing for publication, and submitting work to publishers. The presenter, who has extensive publishing experience, provided tips on choosing the right journal, preparing manuscripts, common reasons for rejection, and responding to editor and reviewer feedback. The presentation encouraged participants to develop plans and timelines for their own publishing goals.
Flexible Provision: Rising to Challenges in Learning and Teaching - An Inst...
Presentation by Professor Simon Haslett at the Annual Learning and Teaching Conference 2015 at the University of Wales Trinity Saint David, Carmarthen Campus.
Sustaining research-informed teaching: institutional and individual approaches.
Collective Address presented by Professor Simon Haslett on 4th April 2014 at the Higher Education Academy Awards Day at the Open University, Cardiff.
Academic Publication Workshop
A presentation by Professor Simon Haslett (University of Wales) at the International University of Malaya-Wales (IUMW) on Wednesday 19th February 2014.
Getting Published Workshop
This workshop aimed to help participants overcome barriers to publishing their research. It covered motivations for publishing, choosing appropriate journals, writing manuscripts, submitting papers, and responding to reviewer feedback. The facilitator had extensive publishing experience and shared tips on getting started, choosing journals, writing strategies, common reasons for rejection, and responding to editorial decisions. Participants were encouraged to develop plans and timelines for their own publishing goals.
Getting Published: The Wales Context
Keynote presentation by Professor Simon Haslett at the University of Wales: Trinity Saint David Research, Innovation, Enterprise & Commercialisation Staff Development Day at the Townhill Campus, Swansea, on Monday 16th December 2013.
Exploring Links between Research and Teaching in Higher Education
A presentation by Professor Simon Haslett, Associate Pro Vice-Chancellor of the University of Wales. The presentation is part of the HEA Research Seminar/Webinar Series, 11th June 2013, at The Higher Education Academy, York. This seminar examines the ways in which research and teaching may be linked in academic practice in Higher Education. It seeks to unravel the various linkages through scholarship, research (both subject-based and pedagogic) and curriculum. The presentation draws upon the presenters’ recent experience as a leader in learning and teaching in Wales, including the activity and contribution of the Research-Teaching Nexus Action Set, and the current challenges to forging and maintaining research-teaching links in Higher Education. He also provides examples of research-teaching links from his own professional practice.
Publishing in Academic Journals
The document provides an overview of publishing in academic journals presented by Professor Simon Haslett. It discusses the academic writing process, making your name known, choosing the right journal, preparing manuscripts, dealing with rejection, and responding to reviewer comments. The goal is to guide researchers through getting published, including tips on collaboration, networking, choosing suitable journals, writing for specific publications, and overcoming rejection.
Mendip Hills: Geology and Landforms.
Presentation by Professor Simon Haslett at the University of the Third Age Mendip Hills Study Day at Draycott, Somerset, on 1st March 2012.
Simon Haslett is Professor of Physical Geography and Associate Pro Vice-Chancellor at the University of Wales.
The talk is based on extracts from S. K. Haslett (2010) Somerset Landscapes: Geology and Landforms. Blackbarn Books. Available from:
https://sites.google.com/site/blackbarnbooks/publications/somerset-landscapes-geology-and-landforms
Literature review and the PhD
Presentation by Professor Simon Haslett at the Institute of Life Science, Swansea University, Monday 4th July 2011.
Promoting Professional Standards in Higher Education
Presentation by Professor Simon Haslett at the Aegean Omiros College, Athens, Greece, on Thursday 19th May 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
Publishing in Academic Journals
Lecture by Professor Simon Haslett at the University of Wales Student Research Conference, Cardiff, on Friday 13th May 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
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Presentation by Professor Simon Haslett at the University of Wales, Newport, Centre for Excellence in Learning and Teaching (CELT) Writing Retreat Workshop at Gregynog Hall, Wales, on Wedmesday 11th May 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales. He is also Visiting Professor of Pedagogic Research at the University of Wales, Newport.
Using social media/online platforms in learning and teaching.
Presentation by Professor Simon Haslett at the University of Wales Annual Moderators Conference at City Hall, Cardiff (Wales, UK), on Friday 15th April 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
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Presentation by Professor Simon Haslett at the University of Wales Annual Moderators Conference at City Hall, Cardiff (Wales, UK), on Friday 15th April 2011. Simon Haslett is Professor of Physical Geography and Dean of the School of STEM at the University of Wales.
Getting Published Workshop
This document summarizes a workshop on getting published. The workshop aims to explore motivations for publishing, overcome barriers to writing and submission, and discuss approaches to writing for publication and responding to editor/reviewer comments. Attendees will discuss their motivations, writing experiences, and barriers in small groups and develop personal action plans for next steps in publishing their work. The facilitator has extensive publishing experience and resources on academic publishing will be provided.
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The Hell of High Water: Tsunami and the Cornish Coast.
- 1. The Hell of High Water:Tsunami and the Cornish Coast. Professor Simon K. Haslett University of Wales, Newport Presentation on 28th September 2010 at University College Falmouth
- 2. From McGuire (2005, New Scientist)
- 3. From Allen & Haslett (2002)
- 4. Somerset Levels from Brean Down.
- 5. Evidence of the 1607 flood 1 Contemporary historic pamphlets giving the: date (20th Jan 1606 = 30th Jan 1607) timing (“about nine in the morning” in Somerset) details of damage (2000 deaths and great economic loss).
- 6. Burnham 1607 tides (HW at 8.28am)
- 8. Evidence of the 1607 flood 2 Commemorative plaques and inscriptions in/on churches in South Wales and Somerset.
- 9. Tsunami theory for the 1607 flood Some contradictory meteorological reports e.g. “a violent sea wind” (Camden, 1607) vs. “the morning … so fayrely and brightly spred” (Harleian Miscellany, 1607). Descriptions of a “wave” reminiscent of a tsunami rather than a storm e.g. “wave’s furie”. Extract from God’s warning to his people of England
- 10. Extracts from Lamentable Newes out of Monmouthshire Wave velocity Inland Penetration There is an extract from St. Uny’s Church that “a great influx of sand might have happened at Hayle” during the 1607 event.
- 20. 1607 Earthquake hypothesis Prof Michael Disney (Cardiff University) published in The Times(5th Jan 2005): “The sky was blue, the tide was high, there is a second-hand report of an earth tremor felt earlier that morning”. Local seismic activity (earthquakes) in Feb and May 1607.
- 21. GEBCO Bathymetry
- 22. Other British tsunami? 33 other possible UK tsunami-like events 12 recorded in Cornwall!
- 23. 28th September 1014 Accounts suggest that a flood affected Kent, Sussex, Hampshire, Cumbria, and Mount’s Bay in Cornwall, where the Bay was “inundated by a ‘mickleseaflood’ when many towns and people were drowned”. Marazion Marsh
- 24. 28th September 1014 William of Malmesbury in The History of the English Kings (vol. 1) states that “a tidal wave ….. grew to an astonishing size such as the memory of man cannot parallel, so as to submerge villages many miles inland and overwhelm and drown their inhabitants”. the Anglo-Saxon Chronicle states that “on the eve of St. Michael’s Day [28th September], came the great sea-flood, which spread wide over this land, and ran so far up as it never did before, overwhelming many towns, and an innumerable multitude of people”
- 25. 28th September 1014 Baillie (2007) considers this flood to have been a tsunami caused by a comet impact. Ice core data indicates that the highest ammonium spike within the historic period occurs in 1014.
- 26. 28th September 1014 Baillie (2007) cites Chinese astronomy in support of comet (debris?) impact. In Nova Scotia, Micmac legends include reference to possible comet impacts.
- 27. 28th September 1014 Tsunami models show it is possible that a large tsunami would be able to wrap around the British Isles, affecting Cumbria, Cornwall and English Channel. Dr Steven Ward (UCSC) has produced animated impact tsunami models of the Atlantic and around the British Isles. http://www.youtube.com/watch?v=4hQqp2JxBM8
- 29. Documented sites in Southwest Mount’s Bay – arrival of 4 tsunami over 2 hours (<3m high). Stonehouse Creek (Plymouth) – sand sheets deposited. Lamorna Cove – boulders tossed around like pebbles. Big Pool, St. Agnes – sand sheet deposited.
- 31. Lamorna Cove
- 32. Big Pool, St. Agnes
- 33. 19th Century Tsunami 23 May 1842 – after an earthquake felt in the Scillies , several waves <2m high came ashore in Mount’s Bay creating “a very extraordinary commotion of the sea”. 18 August 1892 – after an earthquake felt from South Wales to the Scillies, “there was a rapid rise in the River Fowey as a great tidal wave”.