1. The document discusses a field seismology course covering topics such as faults, discontinuities, voids, aquifers, and how seismic velocity varies in rocks and is measured.
2. It includes lists of students and their exam scores, as well as expected major earthquake areas and references to external resources on field seismology and geophysics.
3. The instructor is Professor Ali Osman Öncel of Istanbul University's Engineering Faculty Department of Geophysical Engineering.
Three strong earthquakes struck Japan in April 2016, including a magnitude 7.0 quake near Kumamoto on April 15. The quake caused extensive damage from shaking and landslides, destroying buildings and homes. Over 92,000 people were evacuated from the area. The quake was caused by movement on a shallow crustal fault, and was preceded by foreshocks on April 14, including a magnitude 6.2 quake that killed 9 people. Aftershocks continued following the main quake.
Anlässlich der kommenden Bundespräsidentenwahl wurden in den ersten beiden April-Wochen 600 Österreicherinnen und Österreicher befragt. Hauptziel der Studie war es herauszufinden, welche Emotionen die 6 Kandidatinnen und Kandidaten bei den Wählerinnen und Wählern hervorrufen.
En el pasado Azure Bootcamp 2015 pudimos ver cómo conocer técnicas avanzadas de debugging en Azure viendo cómo detectar problemas tanto en desarrollo como en producción. En esta sesión veremos cómo han avanzado estas técnicas con nuevas herramientas que han ido apareciendo y/o evolucionando a lo largo del último año. No apto para todos los públicos.
This document discusses conservation agriculture experiences in North Africa. It describes how no-till systems were introduced in Morocco, Tunisia, and Algeria starting in the 1980s and mid-1990s. No-till has proven an alternative for sustainable agriculture by improving water use efficiency and wheat yields while reducing impacts of variable rainfall. However, challenges remain around residue management, developing affordable no-till equipment, and optimizing crop rotations and management practices under the integrated crop-livestock systems common in North Africa. Overcoming constraints like knowledge-sharing and equipment access will be important for further adoption of conservation agriculture.
This document discusses conservation agriculture practices in Zambia and Malawi based on research from Noragric. It finds that adoption of conservation agriculture has been partial, around 26-30% on average, due to various constraints including risks, labor requirements, and capital costs. Conservation agriculture techniques like planting basins increased yields over traditional tillage but required high labor. Ripping had lower labor needs than basins or plowing. The document emphasizes that ecological benefits of conservation agriculture, like increased organic matter and water infiltration, depend on recycling plant residues as mulch. It concludes full benefits require integrating fertilizers, trees, livestock, and improved grazing management with conservation agriculture systems.
Three strong earthquakes struck Japan in April 2016, including a magnitude 7.0 quake near Kumamoto on April 15. The quake caused extensive damage from shaking and landslides, destroying buildings and homes. Over 92,000 people were evacuated from the area. The quake was caused by movement on a shallow crustal fault, and was preceded by foreshocks on April 14, including a magnitude 6.2 quake that killed 9 people. Aftershocks continued following the main quake.
Anlässlich der kommenden Bundespräsidentenwahl wurden in den ersten beiden April-Wochen 600 Österreicherinnen und Österreicher befragt. Hauptziel der Studie war es herauszufinden, welche Emotionen die 6 Kandidatinnen und Kandidaten bei den Wählerinnen und Wählern hervorrufen.
En el pasado Azure Bootcamp 2015 pudimos ver cómo conocer técnicas avanzadas de debugging en Azure viendo cómo detectar problemas tanto en desarrollo como en producción. En esta sesión veremos cómo han avanzado estas técnicas con nuevas herramientas que han ido apareciendo y/o evolucionando a lo largo del último año. No apto para todos los públicos.
This document discusses conservation agriculture experiences in North Africa. It describes how no-till systems were introduced in Morocco, Tunisia, and Algeria starting in the 1980s and mid-1990s. No-till has proven an alternative for sustainable agriculture by improving water use efficiency and wheat yields while reducing impacts of variable rainfall. However, challenges remain around residue management, developing affordable no-till equipment, and optimizing crop rotations and management practices under the integrated crop-livestock systems common in North Africa. Overcoming constraints like knowledge-sharing and equipment access will be important for further adoption of conservation agriculture.
This document discusses conservation agriculture practices in Zambia and Malawi based on research from Noragric. It finds that adoption of conservation agriculture has been partial, around 26-30% on average, due to various constraints including risks, labor requirements, and capital costs. Conservation agriculture techniques like planting basins increased yields over traditional tillage but required high labor. Ripping had lower labor needs than basins or plowing. The document emphasizes that ecological benefits of conservation agriculture, like increased organic matter and water infiltration, depend on recycling plant residues as mulch. It concludes full benefits require integrating fertilizers, trees, livestock, and improved grazing management with conservation agriculture systems.
This document provides evaluation questions and instructions for Kate Horn's A2 coursework on creating a media product. It includes four evaluation questions to answer, using a combination of formats like PowerPoints, press articles, word documents, and video. For the first question, Kate is asked to take nine frames from her video and explain how they fit the brief in 2-3 sentences each. She is also asked to take screen grabs from other music videos and provide a similar analysis of how those nine frames meet the brief. The brief focuses on shots that link to lyrics/music, represent the artist, illustrate genre, include intertextual references, demonstrate camera/lighting/mise-en-scene use, and show influences from other music
El documento presenta una introducción al libro El Quijote de Miguel de Cervantes. Explica que aunque es considerada la obra más importante de España, no siempre ha sido bien recibida. También destaca que fue pionera en el desarrollo de la novela moderna y ha influido enormemente en el arte y la cultura española. Finalmente, resume la vida de Cervantes, que incluyó varios periodos en prisión y cinco años como cautivo en Argelia.
Opening Educational Practices in Scotland - OER16OEPScotland
The Opening Educational Practices in Scotland project is a three-year initiative led by the Open University in Scotland to promote open educational practices. It includes analyzing current practices, hosting events, developing an online hub for sharing resources and best practices, creating open educational resources, and researching barriers and economic models related to open education. The project aims to extend thinking about open practices to include learning design, co-creation, social and peer-supported learning, and networks.
Muhammad Yasir Satti has over 4 years of experience as a Contact Center Supervisor at wi-tribe Pakistan. He has held positions including Inbound Floor Supervisor, Backend Support Floor Supervisor, and roles in Retention & Outsourcing and Quality Assurance. Yasir has an MBA from Bahria University and seeks an exciting new position to continue his career progression focused on customer-centric operations. He has strong communication, planning, and people motivation skills.
This curriculum vitae is for a fast food manager and senior operations manager with over 16 years of experience in the food service industry. Currently working as a fast food manager for Kudu Corporation in Saudi Arabia, managing 285 fast food outlets across multiple countries. Previous experience includes working as a sales manager for a garments company from 1993-1999. Education includes a BBA in Food & Beverage Management and higher secondary education. Strengths include management skills, problem solving, communication, and understanding food and labor cost controls. Industry references are available upon request.
This document provides the strategy for developing the safety case for the Kraken oil field development project located in the UK North Sea. It outlines the regulatory requirements and framework for safety cases in the UK as well as the objectives, scope and structure of the Kraken safety case. The strategy describes the formal safety assessment process that will be used to identify hazards and assess risks to demonstrate risks are tolerable and ALARP. It also addresses safety case establishment, maintenance and the roles and responsibilities for developing and approving the safety case.
The document discusses the basic structures and functions of cells and tissues in the human body. It defines the processes of diffusion and osmosis that allow for the movement of molecules across cell membranes. It also describes the five stages of cell division: interphase, prophase, metaphase, anaphase, and telophase. Furthermore, it lists and describes the main types of epithelial tissue, connective tissue, cartilage, and membranes that make up the human body.
Maker Faire Vienna 2016 Vortrag: http://makerfairevienna.com/vortrag
Make it happen Kompass (Kombination von Zukunftsforschung- Techniken und Mental Training)
5 Schritte, 2 Fragen und mehrere Wege, die dich motivieren, inspirieren und vor allem Startklar machen wird!
A magnitude 7.8 earthquake struck near Kathmandu, Nepal, killing over 2,300 people and injuring more than 5,000. The earthquake destroyed homes and buildings in Kathmandu and nearby areas. It also triggered avalanches on Mount Everest that killed at least 17 climbers. The earthquake was caused by the ongoing collision between the Indian and Eurasian tectonic plates, which is responsible for the uplift of the Himalayas.
A magnitude 7.8 earthquake struck near Kathmandu, Nepal, killing over 2,300 people and injuring more than 5,000. The earthquake destroyed homes and buildings in Kathmandu and nearby areas. It also triggered avalanches on Mount Everest that killed at least 17 climbers. The earthquake was caused by the ongoing collision between the Indian and Eurasian tectonic plates, which is what generates earthquakes in this region of the Himalayas.
Incorporated Research Institue for Seismology does an amazing job at providing detailed information shortly after large earthquakes. Learn more at: http://www.iris.edu/hq/retm
Earthquakes are caused by the abrupt rupture and rebound of rocks in the earth's crust where elastic strain has accumulated slowly over time. They are measured using devices that detect seismic waves, and their magnitude refers to their size or intensity. Major earthquakes can cause damage through tsunamis and aftershocks, resulting in death and destruction of infrastructure and the environment. There are two main types of seismic waves - P waves and S waves - with P waves traveling faster through solids and liquids. The 2011 Tohoku earthquake in Japan registered a magnitude 9.0 and had devastating effects, including tsunamis, destroyed cities, loss of life, and damage to Japan's economy and global supply chains.
A magnitude 8.8 earthquake struck off the coast of Chile, 200 miles from Santiago. It caused major damage in Concepcion, Chile's second largest city near the epicenter. Over 100 deaths were reported so far and the numbers were expected to rise due to damage to infrastructure and remote locations still unreachable. A tsunami was generated which caused damage along the Chilean coast and warnings were issued for other Pacific areas.
A magnitude 8.8 earthquake struck off the coast of Chile, 200 miles from Santiago. It caused major damage in Concepcion, Chile's second largest city near the epicenter. Over 100 deaths were reported so far and the numbers were expected to rise due to damage to infrastructure and remote locations still unreachable. A tsunami was generated which caused damage along the Chilean coast and warnings were issued for other Pacific areas.
Earthquakes are caused by the sudden release of built-up stress along geological faults. The document summarizes information about earthquakes in Pakistan including historical quakes, measuring magnitudes, locating epicenters, and classifying earthquake types and effects. It describes the elastic rebound theory of earthquakes, seismic wave propagation, uses of seismographs to measure quakes, and scales for quantifying magnitudes and intensities.
A magnitude 6.5 earthquake struck offshore of Northern California, centered 22 miles west of Ferndale. The quake caused power outages and damage to buildings in communities up to 300 miles away. Aftershocks continued for several hours but there were no serious injuries reported. While tsunami risks exist for the region, no destructive Pacific-wide tsunami was expected from this particular quake due to its nature as a strike-slip earthquake.
Giant Earthquake in Japan (Mw=9.0), March 11, 2011Ali Osman Öncel
A magnitude 8.9 earthquake struck off the coast of Japan on March 11, 2011, generating a powerful tsunami. The earthquake was one of the largest ever recorded in Japan and caused widespread damage, including fires and flooding in Tokyo from the tsunami. The tsunami waves traveled far inland, sweeping away buildings and vehicles and claiming many lives. A tsunami warning was issued for the Pacific basin due to the potential for destructive waves over a wide area.
The document provides information about earthquakes including what they are, how they are measured on the Richter scale, the types of damage they can cause such as cracks, damage to buildings and infrastructure, and tsunamis. It also discusses the different types of seismic waves called P and S waves that travel through both solids and liquids. The document then focuses on the 2011 Tohoku earthquake in Japan, noting its magnitude of 9.0, the effects like homes destroyed and lives lost, and impacts to the economy and environment from issues like radiation from the Fukushima Daiichi nuclear disaster.
This document provides information about earthquakes. It defines an earthquake as a series of vibrations in the earth's crust. Earthquakes are measured by their magnitude on the Richter scale, which indicates their strength. Major earthquakes can cause damage like cracks in the crust, broken pipelines, and damaged housing and buildings, as well as tsunamis and landslides. The document discusses seismic waves, including primary and secondary waves, and how primary waves travel faster and arrive at the surface first. It provides details about a specific large 2011 earthquake in Japan and its effects, including homes destroyed, deaths, and economic impacts.
This document provides evaluation questions and instructions for Kate Horn's A2 coursework on creating a media product. It includes four evaluation questions to answer, using a combination of formats like PowerPoints, press articles, word documents, and video. For the first question, Kate is asked to take nine frames from her video and explain how they fit the brief in 2-3 sentences each. She is also asked to take screen grabs from other music videos and provide a similar analysis of how those nine frames meet the brief. The brief focuses on shots that link to lyrics/music, represent the artist, illustrate genre, include intertextual references, demonstrate camera/lighting/mise-en-scene use, and show influences from other music
El documento presenta una introducción al libro El Quijote de Miguel de Cervantes. Explica que aunque es considerada la obra más importante de España, no siempre ha sido bien recibida. También destaca que fue pionera en el desarrollo de la novela moderna y ha influido enormemente en el arte y la cultura española. Finalmente, resume la vida de Cervantes, que incluyó varios periodos en prisión y cinco años como cautivo en Argelia.
Opening Educational Practices in Scotland - OER16OEPScotland
The Opening Educational Practices in Scotland project is a three-year initiative led by the Open University in Scotland to promote open educational practices. It includes analyzing current practices, hosting events, developing an online hub for sharing resources and best practices, creating open educational resources, and researching barriers and economic models related to open education. The project aims to extend thinking about open practices to include learning design, co-creation, social and peer-supported learning, and networks.
Muhammad Yasir Satti has over 4 years of experience as a Contact Center Supervisor at wi-tribe Pakistan. He has held positions including Inbound Floor Supervisor, Backend Support Floor Supervisor, and roles in Retention & Outsourcing and Quality Assurance. Yasir has an MBA from Bahria University and seeks an exciting new position to continue his career progression focused on customer-centric operations. He has strong communication, planning, and people motivation skills.
This curriculum vitae is for a fast food manager and senior operations manager with over 16 years of experience in the food service industry. Currently working as a fast food manager for Kudu Corporation in Saudi Arabia, managing 285 fast food outlets across multiple countries. Previous experience includes working as a sales manager for a garments company from 1993-1999. Education includes a BBA in Food & Beverage Management and higher secondary education. Strengths include management skills, problem solving, communication, and understanding food and labor cost controls. Industry references are available upon request.
This document provides the strategy for developing the safety case for the Kraken oil field development project located in the UK North Sea. It outlines the regulatory requirements and framework for safety cases in the UK as well as the objectives, scope and structure of the Kraken safety case. The strategy describes the formal safety assessment process that will be used to identify hazards and assess risks to demonstrate risks are tolerable and ALARP. It also addresses safety case establishment, maintenance and the roles and responsibilities for developing and approving the safety case.
The document discusses the basic structures and functions of cells and tissues in the human body. It defines the processes of diffusion and osmosis that allow for the movement of molecules across cell membranes. It also describes the five stages of cell division: interphase, prophase, metaphase, anaphase, and telophase. Furthermore, it lists and describes the main types of epithelial tissue, connective tissue, cartilage, and membranes that make up the human body.
Maker Faire Vienna 2016 Vortrag: http://makerfairevienna.com/vortrag
Make it happen Kompass (Kombination von Zukunftsforschung- Techniken und Mental Training)
5 Schritte, 2 Fragen und mehrere Wege, die dich motivieren, inspirieren und vor allem Startklar machen wird!
A magnitude 7.8 earthquake struck near Kathmandu, Nepal, killing over 2,300 people and injuring more than 5,000. The earthquake destroyed homes and buildings in Kathmandu and nearby areas. It also triggered avalanches on Mount Everest that killed at least 17 climbers. The earthquake was caused by the ongoing collision between the Indian and Eurasian tectonic plates, which is responsible for the uplift of the Himalayas.
A magnitude 7.8 earthquake struck near Kathmandu, Nepal, killing over 2,300 people and injuring more than 5,000. The earthquake destroyed homes and buildings in Kathmandu and nearby areas. It also triggered avalanches on Mount Everest that killed at least 17 climbers. The earthquake was caused by the ongoing collision between the Indian and Eurasian tectonic plates, which is what generates earthquakes in this region of the Himalayas.
Incorporated Research Institue for Seismology does an amazing job at providing detailed information shortly after large earthquakes. Learn more at: http://www.iris.edu/hq/retm
Earthquakes are caused by the abrupt rupture and rebound of rocks in the earth's crust where elastic strain has accumulated slowly over time. They are measured using devices that detect seismic waves, and their magnitude refers to their size or intensity. Major earthquakes can cause damage through tsunamis and aftershocks, resulting in death and destruction of infrastructure and the environment. There are two main types of seismic waves - P waves and S waves - with P waves traveling faster through solids and liquids. The 2011 Tohoku earthquake in Japan registered a magnitude 9.0 and had devastating effects, including tsunamis, destroyed cities, loss of life, and damage to Japan's economy and global supply chains.
A magnitude 8.8 earthquake struck off the coast of Chile, 200 miles from Santiago. It caused major damage in Concepcion, Chile's second largest city near the epicenter. Over 100 deaths were reported so far and the numbers were expected to rise due to damage to infrastructure and remote locations still unreachable. A tsunami was generated which caused damage along the Chilean coast and warnings were issued for other Pacific areas.
A magnitude 8.8 earthquake struck off the coast of Chile, 200 miles from Santiago. It caused major damage in Concepcion, Chile's second largest city near the epicenter. Over 100 deaths were reported so far and the numbers were expected to rise due to damage to infrastructure and remote locations still unreachable. A tsunami was generated which caused damage along the Chilean coast and warnings were issued for other Pacific areas.
Earthquakes are caused by the sudden release of built-up stress along geological faults. The document summarizes information about earthquakes in Pakistan including historical quakes, measuring magnitudes, locating epicenters, and classifying earthquake types and effects. It describes the elastic rebound theory of earthquakes, seismic wave propagation, uses of seismographs to measure quakes, and scales for quantifying magnitudes and intensities.
A magnitude 6.5 earthquake struck offshore of Northern California, centered 22 miles west of Ferndale. The quake caused power outages and damage to buildings in communities up to 300 miles away. Aftershocks continued for several hours but there were no serious injuries reported. While tsunami risks exist for the region, no destructive Pacific-wide tsunami was expected from this particular quake due to its nature as a strike-slip earthquake.
Giant Earthquake in Japan (Mw=9.0), March 11, 2011Ali Osman Öncel
A magnitude 8.9 earthquake struck off the coast of Japan on March 11, 2011, generating a powerful tsunami. The earthquake was one of the largest ever recorded in Japan and caused widespread damage, including fires and flooding in Tokyo from the tsunami. The tsunami waves traveled far inland, sweeping away buildings and vehicles and claiming many lives. A tsunami warning was issued for the Pacific basin due to the potential for destructive waves over a wide area.
The document provides information about earthquakes including what they are, how they are measured on the Richter scale, the types of damage they can cause such as cracks, damage to buildings and infrastructure, and tsunamis. It also discusses the different types of seismic waves called P and S waves that travel through both solids and liquids. The document then focuses on the 2011 Tohoku earthquake in Japan, noting its magnitude of 9.0, the effects like homes destroyed and lives lost, and impacts to the economy and environment from issues like radiation from the Fukushima Daiichi nuclear disaster.
This document provides information about earthquakes. It defines an earthquake as a series of vibrations in the earth's crust. Earthquakes are measured by their magnitude on the Richter scale, which indicates their strength. Major earthquakes can cause damage like cracks in the crust, broken pipelines, and damaged housing and buildings, as well as tsunamis and landslides. The document discusses seismic waves, including primary and secondary waves, and how primary waves travel faster and arrive at the surface first. It provides details about a specific large 2011 earthquake in Japan and its effects, including homes destroyed, deaths, and economic impacts.
This document appears to be a student project report on the study of earthquakes. It includes sections on the history of earthquake research, what causes earthquakes, how their locations and magnitudes are measured, the different types of seismic waves, the impacts of earthquakes, and approaches to predicting and controlling them. The project received certification from the University of Mumbai professors after satisfactory completion by the six listed students.
This document discusses earthquakes and landslides. It begins by explaining what causes earthquakes, how they are measured, and how scientists locate their epicenters. Large earthquakes can trigger landslides and rock avalanches. The document then examines case studies of the consequences of the 2015 Nepal earthquake, including damage to buildings, loss of life, and landslides that blocked roads and swept away villages. It describes the effects in India as well, with dozens of deaths. The second case study focuses on landslides in Gangtok, India triggered by heavy rainfall in 1997 that killed over 50 people and displaced thousands. Geological and rainfall data are presented relating to landslide risks in the area.
This document provides an overview of earthquakes including what they are, how they are measured, the damage and effects they can cause, the different types of seismic waves, and details about the 2011 Tohoku earthquake in Japan. Some key points covered include that earthquakes are caused by the abrupt movement of rocks along faults, they are measured by the Richter scale and Mercalli scale, can destroy infrastructure and harm populations, and the Tohoku quake was a 9.0 magnitude event that shifted Japan's coastline and caused a devastating tsunami.
This document provides an overview of earthquakes including how they are measured, the types of damage they can cause, the different types of seismic waves, and details about the 2011 Tohoku earthquake in Japan. It discusses how the Richter scale and Mercalli scale are used to measure the magnitude of earthquakes. It also explains elastic rebound theory and defines tsunamis, noting that the Tohoku earthquake generated massive tsunami waves and shifted the Earth's axis.
The document summarizes information about earthquakes and seismic waves. It describes how earthquakes are measured on the Richter scale and quantified by magnitude. It outlines the two main types of seismic waves - body waves and surface waves - and the types of damage caused by earthquakes, such as landslides, collapsed buildings, and tsunamis. It provides details about a specific earthquake that occurred in Japan in 2011, measuring 9.0 in magnitude, and its effects on the local environment, infrastructure, economy, and loss of life.
This document summarizes information about seismic waves and the 2011 Tohoku earthquake in Japan. It defines an earthquake as occurring when two blocks of earth slip past each other, and explains that they are measured by seismic waves on seismographs. It then discusses the damage caused by earthquakes through collapsing buildings and tsunamis. The document outlines the two types of seismic waves and how P and S waves travel. It also summarizes details about the 2011 Tohoku earthquake such as its magnitude of 9.0 and effects like damage to cities and the environment in Japan.
This document summarizes information about seismic waves and the 2011 Tohoku earthquake in Japan. It defines an earthquake as occurring when two blocks of earth slip past each other, and explains that they are measured by seismic waves on seismographs. It describes the damage caused by earthquakes, such as collapsed buildings and tsunamis. It also details the effects of the Tohoku earthquake on Japan's environment, people, and economy, such as damaged nuclear power plants, destroyed buildings, and lost jobs.
This document summarizes information about seismic waves and the 2011 Tohoku earthquake in Japan. It defines an earthquake as occurring when two blocks of earth slip past each other, and explains that they are measured by seismic waves on seismographs. It describes the damage caused by earthquakes, such as collapsed buildings and tsunamis. It also discusses the effects of the Tohoku earthquake on Japan's environment, people, and economy, including damaged nuclear power plants, destroyed buildings, and economic disruption.
This document summarizes information about seismic waves and the 2011 Tohoku earthquake in Japan. It defines an earthquake as occurring when two blocks of earth slip past each other, and explains that they are measured by seismic waves on seismographs. It then discusses the damage caused by earthquakes through collapsing buildings and tsunamis. The document outlines the two types of seismic waves and how P and S waves travel. It also summarizes details about the 2011 Tohoku earthquake such as its magnitude of 9.0 and effects like damage to cities and the environment in Japan.
Gravimetri Dersi için aşağıda ki videoları izleyebilirsiniz.
Link 01: https://www.youtube.com/watch?v=HTyjVaVGx0k
Link 02: https://www.youtube.com/watch?v=fUkfgI8XaOE
The document discusses gravity anomalies and density variations in different regions based on gravity data. It shows how gravity maps reveal details about crustal thickness, tectonic features like faults and volcanic zones, and plate boundaries. Specific examples discussed include the Tibetan Plateau, Central America subduction zone, an area in Chugoku, Japan, and the state of Florida in the US. Regional gravity data can be used to model density changes associated with plate tectonics, crustal evolution, and volcanic and tectonic activity.
The USF team reviewed a geophysical investigation of the Kar Kar region conducted by WesternGeco in 2011. They found that WesternGeco's magnetotelluric (MT) data and models were of high quality. Both the WesternGeco and USF MT models identified a low resistivity zone at 300m depth that correlates with a water-bearing zone found in Borehole 4. USF performed gravity modeling which identified a north-south trending basin reaching 1500m depth, consistent with mapped faults. A preliminary hydrothermal model suggested observed temperatures could result from deep circulation of meteoric waters in the basin without needing a localized heat source. Additional geophysical data is recommended around the Jermaghbyur hot springs to
This document summarizes a study that used gravity data to delineate underground structure in the Beppu geothermal field in Japan. Analysis of Bouguer anomaly maps revealed high anomalies in the southern and northern parts of the study area that correspond to known geological formations. Edge detection filtering of the gravity data helped identify subsurface faults, including the northern edge of the high southern anomaly corresponding to the Asamigawa Fault. Depth modeling of the gravity basement showed differences between the southern and northern hot spring areas, with steep basement slopes along faults in the south and uplifted basement in the north.
This document summarizes the development of a new ultra-high resolution model of Earth's gravity field called GGMplus. Key points:
- GGMplus combines satellite gravity data from GOCE and GRACE with terrestrial gravity data and topography to achieve unprecedented 200m spatial resolution globally.
- It provides gridded estimates of gravity, horizontal and radial field components, and quasi-geoid heights at over 3 billion points covering 80% of the Earth's land.
- GGMplus reveals new details of small-scale gravity variations and identifies locations of minimum and maximum gravity, suggesting peak-to-peak variations are 40% larger than previous estimates. The model will benefit scientific and engineering applications.
Gravity measurements were taken in a region of China covering the south-north earthquake belt in 1998, 2000, 2002, and 2005. Researchers noticed significant gravity changes in the region surrounding Wenchuan and suggested in 2006 that a major earthquake could occur there in 2007 or 2008. While gravity changes were significant at some locations, more research is needed to determine if they could be considered a precursor. Uncertainties exist from measurement errors, hydrologic effects, and crustal movements. Improved data collection and analysis could enhance using gravity monitoring for earthquake research.
The document provides guidelines for implementing the H/V spectral ratio technique using ambient vibration measurements to evaluate site effects. It recommends procedures for experimental design, data processing, and interpretation. The key recommendations include measuring for sufficient duration depending on expected frequency, using multiple measurement points, avoiding disturbances, and interpreting H/V peaks in context with geological and geophysical data. Reliable H/V peaks are defined as having a clear maximum within expected frequency ranges and uncertainties. The guidelines aim to help apply the technique while accounting for its limitations.
Geopsy yaygın olarak kullanılan profesyonel bir program. Özellikle, profesyonel program deneyimi yeni mezunlarda çok aranan bir özellik. Bir öğrencim çalışmasında kullanmayı planlıyor.
Physiology and chemistry of skin and pigmentation, hairs, scalp, lips and nail, Cleansing cream, Lotions, Face powders, Face packs, Lipsticks, Bath products, soaps and baby product,
Preparation and standardization of the following : Tonic, Bleaches, Dentifrices and Mouth washes & Tooth Pastes, Cosmetics for Nails.
हिंदी वर्णमाला पीपीटी, hindi alphabet PPT presentation, hindi varnamala PPT, Hindi Varnamala pdf, हिंदी स्वर, हिंदी व्यंजन, sikhiye hindi varnmala, dr. mulla adam ali, hindi language and literature, hindi alphabet with drawing, hindi alphabet pdf, hindi varnamala for childrens, hindi language, hindi varnamala practice for kids, https://www.drmullaadamali.com
This presentation includes basic of PCOS their pathology and treatment and also Ayurveda correlation of PCOS and Ayurvedic line of treatment mentioned in classics.
A Strategic Approach: GenAI in EducationPeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
This presentation was provided by Steph Pollock of The American Psychological Association’s Journals Program, and Damita Snow, of The American Society of Civil Engineers (ASCE), for the initial session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session One: 'Setting Expectations: a DEIA Primer,' was held June 6, 2024.
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.
18. Three strong to major earthquakes have occurred in Japan, including two
foreshocks of M 6.2 and M 6.0 on April 14th
and a M 7.0 early Saturday morning
local time. The foreshocks caused severe shaking in the region and resulted in
9 reported fatalities and more than 1000 injuries. Early reports indicate that 32
people have died in the M 7.0 earthquake.
Resident houses are seen
destroyed after an
earthquake in Mashiki,
Kumamoto prefecture,
southern Japan, Saturday,
April 16, 2016. Powerful
earthquakes a day apart
shook southern Japan,
trapping many beneath
flattened homes and sending
thousands to seek shelter in
gymnasiums and hotel
lobbies.
(Yusuke Ogata/Kyodo News
via AP)
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
19. The earthquakes have caused extensive damage, overturning cars, splitting
roads and triggering a landslide. These earthquakes were shallow (~10 km)
underneath the city of Kumamoto (~ population 700,000). Shallower
earthquakes result in more motion at the surface than do deeper earthquakes.
Early estimates report that over 92,000 people have been evacuated.
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
Buildings are collapsed
by a landslide caused by
an earthquake in
Minamiaso village,
Kumamoto prefecture,
Japan, Saturday, April
16, 2016 (local time).
The powerful
earthquake struck
southwestern Japan
early Saturday, barely 24
hours after a smaller
quake hit the same
region.
(Kyodo News via AP)
20. Heavy rains were expected through
Sunday adding to the complexity of
recovery efforts. The weather, together
with the aftershocks, contribute to the
threat of additional landslides.
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
This animation shows satellite imagery
from the Himawari series of
geostationary meteorological satellites
looped from shortly after the earthquake
for the following 24 hours.
Animation courtesy of the Japan
Meteorological Agency
21. Modified Mercalli Intensity
Perceived
Shaking
Extreme
Violent
Severe
Very Strong
Strong
Moderate
Light
Weak
Not Felt
USGS Estimated Shaking Intensity
The Modified-Mercalli
Intensity scale is a twelve-
stage scale, from I to XII,
that indicates the severity of
ground shaking.
This region has experienced
severe to violent shaking
from three earthquakes in
two days.
Image courtesy of the US Geological Survey
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
22. USGS PAGER
Population Exposed to Earthquake Shaking
Image courtesy of the US Geological Survey
The USGS PAGER map shows the population
exposed to different Modified Mercalli
Intensity (MMI) levels.
The USGS estimates that 716,000 people
experienced violent shaking from this
earthquake.
The color coded contour lines outline regions of
MMI intensity. The total population exposure to a
given MMI value is obtained by summing the
population between the contour lines. The
estimated population exposure to each MMI
Intensity is shown in the table below.
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
23. Image courtesy of the US Geological Survey
The plate tectonic map below shows rates of motion between the Pacific, Philippine, and
Eurasian plates. In the region of Kyushu Island, the Philippine Plate subducts beneath
the Eurasian Plate at a rate of about 5 cm/yr.
April 15
M7.0
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
24. On April 14, eighteen earthquakes occurred near Kumamoto, including a magnitude 6.2
event that killed 9 people. In retrospect, the April 14 events are recognized as foreshocks
to the April 15 magnitude 7.0 earthquake (main shock). In the 25 hours following the M7.0
earthquake, 25 aftershocks occurred with magnitudes up to 5.7.
April 14 Foreshocks
Maps generated using IRIS Interactive Earthquake
Browser
April 15
M7.0
April 15 M7.0
Eurasian Plate Philippine Plate
M 7.0 & April 15 – 16 Aftershocks
M7.0
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
25. Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
26. Image and text courtesy of the US Geological
Survey
In a sequence of earthquakes, the earthquake with the largest magnitude is
called the main shock; anything before it is a foreshock and anything after it
is an aftershock. There is no way to know before a main shock occurs that
the previous earthquakes have been foreshocks.
Aftershock
sequences follow
predictable patterns
as a group,
although the
individual
earthquakes are
themselves not
predictable.
The graph shows
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
27. The epicenter of the April 15 M 7.0
earthquake is shown on the
regional seismicity map at right.
The cross section below, shows
the Philippine Plate subducting
below the Eurasian Plate. The
April 15 earthquake occurred on a
crustal fault within the Eurasian
Plate.
Earthquake and Historic Seismicity
Area of Cross
Section
Map generated using IRIS Interactive Earthquake
Browser
April 15
M7.0
ilippinePlate
April 15 M7.0
Eurasian Plate
Eurasian Plate
Philippine Plate
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
28. The focal mechanism for the earthquake indicates this was a strike-slip fault. Slip
occurred on either a left -lateral fault striking to the northwest, or on a right -lateral fault
striking northeast. The northeast-southwest orientation of the aftershock distribution
speaks strongly that the fault plane is oriented in that direction and the earthquake was
caused by right-lateral strike-slip motion on a NE-SW oriented fault plane.
According to the USGS, while the earthquake occurred several hundred kilometers
northwest of the Ryukyu Trench where the Philippine Sea Plate begins its
northwestward subduction beneath Japan and the Eurasian Plate, the shallow depth
and faulting mechanism of this earthquake indicate it occurred on a crustal fault within
the overriding Eurasian Plate.
USGS Centroid Moment Tensor Solution
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
29. Following the earthquake, it took 11 minutes and 56 seconds for the
compressional
P waves to travel a curved path through the mantle to Portland, Oregon.PP waves are compressional waves that bounce off the Earth’s surface halfway
between the earthquake and the station and take 14 minutes 50 seconds to
arrive.
The record of the earthquake on the University of Portland seismometer (UPOR) is illustrated
below. Portland is 8587 km (5336 miles, 77.36°) from the location of this earthquake.
Surface waves traveled the 8587 km (5336 miles)
along the perimeter of the Earth from the earthquake
to the recording station.
P
PP
S
S waves are shear waves that follow the same path through
the mantle as P waves. S waves took 21 minutes and 48
seconds to travel from the earthquake to Portland.
Surface
waves
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
30. Teachable Moments are a service of
The Incorporated Research Institutions for Seismology
Education & Public Outreach
and
The University of Portland
Please send feedback to tkb@iris.edu
Magnitude 7.0 KYUSHU, JAPANMagnitude 7.0 KYUSHU, JAPAN
Friday, April 15, 2016 at 16:25:06 UTCFriday, April 15, 2016 at 16:25:06 UTC
42. The basic principle of
WARRP is utilizing the
amplitude burst when
P-wave energy is
totally reflected beyond
the critical angle of
incidence. To record at
wide angles large
offsets are required,
much larger than
conventional seismic
arrays can provide.
43. Fig. 1. (a) Tectonic context and general kinematics in the Eastern Mediterranean (from McClusky et al., 2000; Chaumillon et al.,
1996; Le Pichon et al., 1995). Main microplate boundaries are shown, as well as the Hellenic trough system and the Mediterranean
Ridge outer and inner fronts of deformation. Arrows with numeric values indicate regional motions. (b) Bathymetry map of the
Eastern Mediterranean Ridge where the 3-D gravity modelling (rectangle in (a)) was undertaken. Lines show the position of seismic
cross-sections in the Crete area (red lines, Bohnhoff et al., 2001) and in the Libyan Sea crossing the Mediterranean Ridge (yellow
dashed lines, Makris and Broenner, 2001; Broenner, 2003).
47. 1. Saha Çalışması Hangi Problemlere Çözüm Getirmek İçin Kullanılır?
2. Fay ve süreksizlik nedir? Nasıl araştırılır?
3. Boşluk nedir, ve nerelerde görülür? Nasıl araştırılır?
4. Kaç türlü su kaynakları vardır? Nasıl araştırılır?
5. Yer incelemesinde aranan parametreler Yer Bilimi Mühendisliklerine göre nasıl
değişir?
6. Kayalarda ki Sismik Hızın Neden Değiştiğini örnek vererek açıklayabilir misiniz?
7. Kayaların Sismik Hızlarının Ölçümünde Kullanılan Deney Düzeneği Nasıldır?
8. Basıncın büyümesiyle sismik hız nasıl değişir?
9. Farklı sıcaklıklarda, basıncın büyümesine bağlı olarak sismik hız nasıl değişir?
10. Farklı basınçlar altında, sıcaklığın değişimine bağlı olarak hız nasıl değişir?
11. Sismik Hız ve Yoğunluk birbirleriyle nasıl ilişkilidir?
12. Hız ve Yoğunluk Arasında Matematiksel Olarak Bir İlişki Belirlenmiş midir?
13. Porozite nedir, ve Sismik Hız değişimini Nasıl Etkiler?
Editor's Notes
Kentsel Risk Yönetimi Eğitiminin amacı ülkemizde yerleşim ve yapılaşma sürecinde uygulanması gerekli esasları, özellikle Riskli Yer ve Yapıların belirlenmesinde takip edilmesi gerekli çağdaş jeofizik yöntemler hakkında yöneticilerin, mühendislerin, vatandaşların bilgilendirilmesini sağlayacak eğitim paketidir.
Jeofizik Mühendisliği açısından Kentsel Riskin Tanımı ve Kentsel Yenilenmede Uygulanması gerekli Jeofizik Mühendisliği uygulamalarının tanıtılmasını amaçlamaktadır. Ülkemizde Kentsel Dönüşümün en temel nedeni -deprem odaklı riskin azaltılmasıdır. Çünkü ülkemizin ve özellikle İstanbul’un beklenen büyük deprem riski altında olmasına bağlı olarak yapılan deprem senaryolarında ortaya çıkacak afetin faturasını ülkemizin kaldıramayacağı gerçeğinin anlaşılmış olmasından kaynaklı olarak Kentsel Yenilenme kararı yasalaşmıştır.
Ülkemizde deprem sonrası müdahale çalışmaları kapsamında AFET eğitimi verilmektedir, ve ülkemiz AFETE müdahale konusunda marka olma yolunda çok önemli adımlar atmıştır. Özellikle Van depremi sonrasında yapılan müdahale ve deprem sonrası yapılaşmada ortaya konan performansa bağlı olarak yapılan değerlendirmelerin genel olarak olumlu olması afet mühendisliği konusunda önemli mesafe alındığını göstermektedir. Fakat insanların afete maruz bırakılmaması, evsiz kalanların, insanların ölmemesi ve sakat kalmaması için RİSK Mühendisliği çalışmalarının yapılması çok daha önemlidir. Kentsel Dönüşüm Yasası Risk Mühendisliği çalışmalarını önceleyen devrim niteliğinde atılmış önemli bir adımdır.
Kentsel Risk Yönetimi eğitimi beş aşamadan oluşmaktadır. Kısaca bunlara değinmek gerekirse aşağıda açıklamaları özet olarak verilecektir.
Bilinç: Risk ile ilgili olarak bilgilendirme ve daha büyük kayıpları önlemek için yapılacak küçük adımların ve katkıların yararlı olacağı hususunda bilgi verilmesi çalışmasıdır.
Değişim: Riskin değişimine etki eden faktörlerin anlatılması ve toplam riskin oluşmasında farklı faktörlerin nasıl etki ettiği hususunda bilgi verilmesini amaçlamaktadır.
İnsan: İnsanlarda bir talep oluşturulması ve riskin azaltılması hususunda katkı vermeye istekli olacak düzeye çıkarılması durumunda çok az maliyetle büyük kayıpların önlenmesine altlık oluşturulacak taban veri bankasının oluşturulmasıyla alakalı bir çalışmayı kapsar.
Yapı: Riskli Yapıların Belirlenmesi Kentsel Dönüşüm Yasalarında yapılması gerekli çalışmadır. Yapıların incelenmesinde öncelikli hedef yapılara zarar vermeyecek ve mevcut durumunu inceleme sürecinde olumsuz etkilemeyecek tekniklerin kullanılması gerekir. Yapıların risk amaçlı incelenmesinde Yapı Dostu Mühendislik çalışmalarının yapılmasıyla alakalı bilgilendirmeyi amaçlamaktadır.
Yapılaşma: Yapılaşmaya uygun alanların seçilmesi çalışmalarının yapılmasında Yer Dostu Mühendislik uygulamalarının yapılması hususunda bilgi verilmesi hedeflenmektedir. Meydana gelen risklerin veya afetin sebebi yapılaşmaya uygun olmayan yerlerin imara açılması olduğu bilinen bir gerçektir. Heyelan sahalarının, deprem üretecek aktif kırıklara çok yakın alanların, depremde açığa çıkan deprem dalgalarını büyütecek pasif kırıklar üzerinde yapılaşmanın olması ülkemizde bir deprem sonrasında kayıpların büyüten en önemli faktördür.
Shaking intensity scales were developed to standardize the measurements and ease comparison of different earthquakes. The Modified-Mercalli Intensity scale is a twelve-stage scale, from I to XII. Lower numbers represent imperceptible shaking while XII represents total destruction.
The USGS PAGER map shows the population exposed to different Modified Mercalli Intensity (MMI) levels. MMI describes the severity of an earthquake in terms of its effect on humans and structures and is a rough measure of the amount of shaking at a given location.
Shaded areas show quadrants of the focal sphere in which the P-wave first-motions are away from the source, and unshaded areas show quadrants in which the P-wave first-motions are toward the source. The dots represent the axis of maximum compressional strain (the "P-axis") and the axis of maximum extensional strain (the "T-axis") resulting from the earthquake.
Kentsel Risk Yönetimi eğitimi beş aşamadan oluşmaktadır. Kısaca bunlara değinmek gerekirse aşağıda açıklamaları özet olarak verilecektir.
Bilinç: Risk ile ilgili olarak bilgilendirme ve daha büyük kayıpları önlemek için yapılacak küçük adımların ve katkıların yararlı olacağı hususunda bilgi verilmesi çalışmasıdır.
Değişim: Riskin değişimine etki eden faktörlerin anlatılması ve toplam riskin oluşmasında farklı faktörlerin nasıl etki ettiği hususunda bilgi verilmesini amaçlamaktadır.
İnsan: İnsanlarda bir talep oluşturulması ve riskin azaltılması hususunda katkı vermeye istekli olacak düzeye çıkarılması durumunda çok az maliyetle büyük kayıpların önlenmesine altlık oluşturulacak taban veri bankasının oluşturulmasıyla alakalı bir çalışmayı kapsar.
Yapı: Riskli Yapıların Belirlenmesi Kentsel Dönüşüm Yasalarında yapılması gerekli çalışmadır. Yapıların incelenmesinde öncelikli hedef yapılara zarar vermeyecek ve mevcut durumunu inceleme sürecinde olumsuz etkilemeyecek tekniklerin kullanılması gerekir. Yapıların risk amaçlı incelenmesinde Yapı Dostu Mühendislik çalışmalarının yapılmasıyla alakalı bilgilendirmeyi amaçlamaktadır.
Yapılaşma: Yapılaşmaya uygun alanların seçilmesi çalışmalarının yapılmasında Yer Dostu Mühendislik uygulamalarının yapılması hususunda bilgi verilmesi hedeflenmektedir. Meydana gelen risklerin veya afetin sebebi yapılaşmaya uygun olmayan yerlerin imara açılması olduğu bilinen bir gerçektir. Heyelan sahalarının, deprem üretecek aktif kırıklara çok yakın alanların, depremde açığa çıkan deprem dalgalarını büyütecek pasif kırıklar üzerinde yapılaşmanın olması ülkemizde bir deprem sonrasında kayıpların büyüten en önemli faktördür.
Fault & Discontinuity
Map faults and lateral velocity variations in area characterized by basalts and low velocity sediments
Void Detection
Find buried utility tunnel and concrete pipe lining using S-wave 1st arrivals
Bay Geophyical of Traverse City, Michigan, used @2D to find voids and merging utilities along a buried concrete pipeline. The only data input used to produce the velocity model was the first arrival shear wave travel-time data, and array geometry. No other a priori data were used. This is a velocity model from one of the lines. Notice the detail at which near-surface velocities were modeled. In fact, the petroleum industry uses our software for near-surface velocity static corrections because of the detail in which near-surface velocities are revealed. The pipeline runs parallel to the seismic array. The poured concrete pipeline bed is shown correctly at about 15 feet depth (elevation of 11 feet). The soil above the pipeline shows a gradient as a result of burial pressure. A utility tunnel intersecting the pipeline was imaged at about offset 290 feet, centered at about 10 feet depth (elevation of about 16 feet). The velocity model also picked up some subtle lateral velocity features in the soil associated with the construction and burial of the tunnel. There is also a localized slight velocity reversal, indicating a void, at about offset 370 feet, elevation about 6 feet.
Water Reservoir Citing
Map velocities in area to build water reservoir
Profiles Pr 1, Pr 2 and the northern part of Pr 4 cross the area of Crete (Bohnhoff et al., 2001), profiles Pr 3, southern part of Pr 4
and Pr 5 (Makris and Broenner, 2001; Broenner, 2003) cross the Mediterranean Ridge. Numerical values indicate the Vp velocities in kilometers per
second.