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November 3, 2013 Volcano Sinabung on north Sumatra, Indonesia erupts 
November 3, 2013 Volcano Sinabung on north Sumatra, Indonesia erupts Professor Eric K. Noji, M.D., MPH, DTMH(Lon), FRCP(UK)hon
Mount Sinabung, an inactive volcano located in North Sumatra, Indonesia, erupted multiple times in late 2013, prompting evacuations of nearby villages. After being dormant for 400 years, Sinabung erupted in August 2010 and has had increasing activity since, including eruptions in September and October 2013 that forced the evacuation of over 3,500 villagers within 3 km of the volcano each time. The largest eruption was on November 3, 2013, when the volcano sent an ash plume 7,000 feet into the air, prompting another 1,500 people to evacuate within 3 km of the volcano. Indonesian authorities subsequently increased the alert level for Sinabung.Tectonics or magma intrusion? New results from multi-parameter study at Gede ...
This study uses multi-parameter data to analyze activity at Gede Volcano in West Java, Indonesia. Seismic and deformation monitoring detected swarms of small earthquakes in early 2012 beneath Gede that may have been caused by magma intrusion, though no eruption occurred. Tiltmeter data showed a change in deformation pattern in late 2011 from tectonic to inflation, coinciding with the earthquake swarms in early 2012. Gas measurements found elevated CO2 flux around the northeast flank of Gede. The volcanoes require continued monitoring as any increases in seismicity, deformation or gas could signal future eruptive activity posing a threat to nearby communities.
Role of local wisdom in rapidity of rehabilitation and reconstruction post ea...
Role of local wisdom in rapidity of rehabilitation and reconstruction post ea...Global Risk Forum GRFDavos
1. The document discusses a case study comparing the rapidity of rehabilitation and reconstruction efforts in mono-religious and multi-religious villages in Bantul, Indonesia following an earthquake disaster.
2. Key differences in local wisdom between the villages included differences in local leadership and institutions, availability of local resources, and reliance on external funding for reconstruction in the multi-religious village.
3. The study found that rehabilitation and house reconstruction was faster in the mono-religious village, with 80% of housing units rebuilt within a year, compared to the multi-religious village which relied more on external financial aid and resources.Experience Gedepahala Corridor Programme
The Gedepahala Corridor Program is a 5-year forest landscape restoration project aimed at protecting the last mountain rainforests in Java, Indonesia. The program covers 135,332 hectares across Gunung Gede Pangrango National Park and Gunung Halimun Salak National Park, which are home to many threatened species. The goals are to ensure the continuity of the national parks as natural resources, rehabilitate degraded lands, involve communities and the private sector, and increase environmental awareness. Key activities include creating "green walls" of vegetation along borders, tree planting, species conservation programs, livelihood projects, and environmental education.
Followup Japan Volcano Eruption Part II
Dormant for over 30 years, Mt Ontake is a popular climbing destination, and at least 250 people were initially trapped on the slopes. At least 30 were killed; most made their way down by Saturday night, but the injured, unable to descend the 10,062-foot mountain on their own, stayed in mountain lodges. Rescue workers had to suspend operations on sunday due to nauxious gases and volcano-induced seismic activity. The keys to resilience: 1) know the eruptive history of your region’s volcanoes,2) be prepared 3) have a warning system 4) evacuate 5) learn from the experience and start over. Technologies for monitoring, forecasting, and warning are vital for survival.
Purbinwanata wirakusumah 16_10
The document discusses the crisis preparedness of the people of Tarogong-Garut, a small town located 5km from the active Guntur volcano in West Java, Indonesia. It notes that while Guntur volcano has been dormant since 1847, an eruption could threaten the town. The people of Tarogong lack eruption experience over the past 150+ years. The Directorate of Volcanology has established monitoring networks around Guntur volcano and shares information with local governments and communities to improve crisis preparedness through evacuation planning and education. Continued efforts are needed to ensure the people of Tarogong are ready if Guntur volcano becomes active again.
Disaster mitigation
Computer-mediated communication is being used in all phases of disaster management including preparation, response, recovery, and mitigation. However, the internet has only been used to a limited extent for disaster management and prevention. Geospatial techniques like remote sensing, GIS, and geophysics can help minimize destruction from natural disasters. These techniques have short term and long term response, recovery, and rehabilitation components. Engineers play important roles in disaster management through designing earthquake resistant structures, seismic evaluation of buildings, classifying damaged structures, and proposing repair methods.
Tectonics: Volcanic hazards
A description of the main types of hazards produced by volcanoes, and some notes on case studies and management.
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November 3, 2013 Volcano Sinabung on north Sumatra, Indonesia erupts
November 3, 2013 Volcano Sinabung on north Sumatra, Indonesia erupts Professor Eric K. Noji, M.D., MPH, DTMH(Lon), FRCP(UK)hon
Mount Sinabung, an inactive volcano located in North Sumatra, Indonesia, erupted multiple times in late 2013, prompting evacuations of nearby villages. After being dormant for 400 years, Sinabung erupted in August 2010 and has had increasing activity since, including eruptions in September and October 2013 that forced the evacuation of over 3,500 villagers within 3 km of the volcano each time. The largest eruption was on November 3, 2013, when the volcano sent an ash plume 7,000 feet into the air, prompting another 1,500 people to evacuate within 3 km of the volcano. Indonesian authorities subsequently increased the alert level for Sinabung.Tectonics or magma intrusion? New results from multi-parameter study at Gede ...
This study uses multi-parameter data to analyze activity at Gede Volcano in West Java, Indonesia. Seismic and deformation monitoring detected swarms of small earthquakes in early 2012 beneath Gede that may have been caused by magma intrusion, though no eruption occurred. Tiltmeter data showed a change in deformation pattern in late 2011 from tectonic to inflation, coinciding with the earthquake swarms in early 2012. Gas measurements found elevated CO2 flux around the northeast flank of Gede. The volcanoes require continued monitoring as any increases in seismicity, deformation or gas could signal future eruptive activity posing a threat to nearby communities.
Role of local wisdom in rapidity of rehabilitation and reconstruction post ea...
Role of local wisdom in rapidity of rehabilitation and reconstruction post ea...Global Risk Forum GRFDavos
1. The document discusses a case study comparing the rapidity of rehabilitation and reconstruction efforts in mono-religious and multi-religious villages in Bantul, Indonesia following an earthquake disaster.
2. Key differences in local wisdom between the villages included differences in local leadership and institutions, availability of local resources, and reliance on external funding for reconstruction in the multi-religious village.
3. The study found that rehabilitation and house reconstruction was faster in the mono-religious village, with 80% of housing units rebuilt within a year, compared to the multi-religious village which relied more on external financial aid and resources.Experience Gedepahala Corridor Programme
The Gedepahala Corridor Program is a 5-year forest landscape restoration project aimed at protecting the last mountain rainforests in Java, Indonesia. The program covers 135,332 hectares across Gunung Gede Pangrango National Park and Gunung Halimun Salak National Park, which are home to many threatened species. The goals are to ensure the continuity of the national parks as natural resources, rehabilitate degraded lands, involve communities and the private sector, and increase environmental awareness. Key activities include creating "green walls" of vegetation along borders, tree planting, species conservation programs, livelihood projects, and environmental education.
Followup Japan Volcano Eruption Part II
Dormant for over 30 years, Mt Ontake is a popular climbing destination, and at least 250 people were initially trapped on the slopes. At least 30 were killed; most made their way down by Saturday night, but the injured, unable to descend the 10,062-foot mountain on their own, stayed in mountain lodges. Rescue workers had to suspend operations on sunday due to nauxious gases and volcano-induced seismic activity. The keys to resilience: 1) know the eruptive history of your region’s volcanoes,2) be prepared 3) have a warning system 4) evacuate 5) learn from the experience and start over. Technologies for monitoring, forecasting, and warning are vital for survival.
Purbinwanata wirakusumah 16_10
The document discusses the crisis preparedness of the people of Tarogong-Garut, a small town located 5km from the active Guntur volcano in West Java, Indonesia. It notes that while Guntur volcano has been dormant since 1847, an eruption could threaten the town. The people of Tarogong lack eruption experience over the past 150+ years. The Directorate of Volcanology has established monitoring networks around Guntur volcano and shares information with local governments and communities to improve crisis preparedness through evacuation planning and education. Continued efforts are needed to ensure the people of Tarogong are ready if Guntur volcano becomes active again.
Disaster mitigation
Computer-mediated communication is being used in all phases of disaster management including preparation, response, recovery, and mitigation. However, the internet has only been used to a limited extent for disaster management and prevention. Geospatial techniques like remote sensing, GIS, and geophysics can help minimize destruction from natural disasters. These techniques have short term and long term response, recovery, and rehabilitation components. Engineers play important roles in disaster management through designing earthquake resistant structures, seismic evaluation of buildings, classifying damaged structures, and proposing repair methods.
Tectonics: Volcanic hazards
A description of the main types of hazards produced by volcanoes, and some notes on case studies and management.
Concept of disaster risk management
This document discusses the concept of disaster risk management. It begins by showing pictures of recent disasters in India to illustrate the risks faced. It then defines key terms like hazard, vulnerability, capacity and disaster risk. Disaster risk is explained as being a function of hazard x vulnerability - capacity. Recent examples of disasters across India from 2011-2012 are provided, including earthquakes, floods, cyclones and landslides. The document emphasizes that communities must be aware and prepared in order to minimize losses from disasters. It outlines the disaster management cycle and different approaches like emergency management and disaster risk management.
Volcanoes and volcanic erruptions
The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
Mt St Helens case study
Mt. St. Helens is a volcano located in Washington State that last erupted in 1980. [1] The eruption killed 57 people and caused widespread damage and environmental impacts. [2] It produced a landslide and later pyroclastic flows that destroyed forests, homes and infrastructure. [3] The eruption had significant economic and social costs for the region.
Volcano science 6
Volcanoes are openings in the earth's crust that eject lava, pyroclasts, and gases during eruptions. There are three main types of volcanoes: shield volcanoes, cinder cone volcanoes, and composite or stratovolcanoes. Cinder cone volcanoes are small, steep-sided hills made of loose cinders ejected during eruptions. Volcanic eruptions can be either explosive or violent, ejecting pyroclasts and ash, or quiet and non-explosive, with gentle lava flows.
13398107 volcanoes-a-presentation
Volcanoes form when magma rises up from the Earth's mantle and crust and erupts. There are three main types of volcanoes defined by their activity level - active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted in a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions expel gases, ash, lava, and other materials from the vent of the volcano. The movement of tectonic plates is responsible for volcanism in many parts of the world.
The Phenomenology of Lamban Tuha: The Local Wisdom of South Sumatra Tradition...
The document summarizes a study on Lamban Tuha, a type of traditional house in South Sumatra, Indonesia. It discusses the following key points:
1. Lamban Tuha has demonstrated local wisdom in its construction techniques, which provide flexibility and help the structures withstand earthquakes. Notable elements include the use of nail-less timber joinery and a separation of the house into lower, middle, and upper parts.
2. A phenomenological study examined the physical characteristics and construction of two surviving Lamban Tuha houses. These houses date back over 100 years and were the only structures left standing after a devastating 1933 earthquake.
3. The simple and symmetrical design of Lamban Tuha, use
Volcanic Hazards Slides
The document discusses various volcanic hazards including primary hazards of ash fall and lava flow. It also discusses pyroclastic flows which can travel at 200 km/hr, volcanic gases such as CO2, H2O and SO2, secondary hazards of lahars from eruptions such as Nevado del Ruiz in 1985, and tertiary hazards of global climate change from large eruptions like Mt. Tambora in 1815 and Mt. Pinatubo in 1991.
Volcanoes
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates at the vent it builds up a mountain-like structure called a volcano. There are three main types of volcanoes defined by their shape and eruption characteristics: shield volcanoes which have broad bases and gentle slopes formed by fluid basaltic lava flows; cinder cone volcanoes which are steep-sided with a small base formed from explosive eruptions of thick sticky lava; and composite or stratovolcanoes which are large mountains formed by alternating explosive and effusive eruptions that build tall layers of ash and lava.
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
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Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
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Training: ISO/IEC 27001 Information Security Management System - EN | PECB
ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
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Webinars: https://pecb.com/webinars
Article: https://pecb.com/article
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Concept of disaster risk management
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Volcanoes and volcanic erruptions
The document provides information about different types of volcanoes and volcanic features including:
- Shield volcanoes which are built by basalt lava flows and have gentle slopes.
- Lava domes which are built by thick, viscous lava that cools too quickly to flow very far from the eruption.
- Cinder cones which are steep sided hills made of volcanic fragments blown from eruptions of stratovolcanoes.
- Stratovolcanoes which have steep sides and are formed by violent eruptions of lava flows, tephra, and pyroclastic flows from multiple vents.
- Mud volcanoes which form from eruptions of wet
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Mt. St. Helens is a volcano located in Washington State that last erupted in 1980. [1] The eruption killed 57 people and caused widespread damage and environmental impacts. [2] It produced a landslide and later pyroclastic flows that destroyed forests, homes and infrastructure. [3] The eruption had significant economic and social costs for the region.
Volcano science 6
Volcanoes are openings in the earth's crust that eject lava, pyroclasts, and gases during eruptions. There are three main types of volcanoes: shield volcanoes, cinder cone volcanoes, and composite or stratovolcanoes. Cinder cone volcanoes are small, steep-sided hills made of loose cinders ejected during eruptions. Volcanic eruptions can be either explosive or violent, ejecting pyroclasts and ash, or quiet and non-explosive, with gentle lava flows.
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Volcanoes form when magma rises up from the Earth's mantle and crust and erupts. There are three main types of volcanoes defined by their activity level - active volcanoes that are currently erupting or may erupt soon, dormant volcanoes that have not erupted in a long time, and extinct volcanoes that have not erupted for over 10,000 years. Volcanic eruptions expel gases, ash, lava, and other materials from the vent of the volcano. The movement of tectonic plates is responsible for volcanism in many parts of the world.
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The document summarizes a study on Lamban Tuha, a type of traditional house in South Sumatra, Indonesia. It discusses the following key points:
1. Lamban Tuha has demonstrated local wisdom in its construction techniques, which provide flexibility and help the structures withstand earthquakes. Notable elements include the use of nail-less timber joinery and a separation of the house into lower, middle, and upper parts.
2. A phenomenological study examined the physical characteristics and construction of two surviving Lamban Tuha houses. These houses date back over 100 years and were the only structures left standing after a devastating 1933 earthquake.
3. The simple and symmetrical design of Lamban Tuha, use
Volcanic Hazards Slides
The document discusses various volcanic hazards including primary hazards of ash fall and lava flow. It also discusses pyroclastic flows which can travel at 200 km/hr, volcanic gases such as CO2, H2O and SO2, secondary hazards of lahars from eruptions such as Nevado del Ruiz in 1985, and tertiary hazards of global climate change from large eruptions like Mt. Tambora in 1815 and Mt. Pinatubo in 1991.
Volcanoes
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates at the vent it builds up a mountain-like structure called a volcano. There are three main types of volcanoes defined by their shape and eruption characteristics: shield volcanoes which have broad bases and gentle slopes formed by fluid basaltic lava flows; cinder cone volcanoes which are steep-sided with a small base formed from explosive eruptions of thick sticky lava; and composite or stratovolcanoes which are large mountains formed by alternating explosive and effusive eruptions that build tall layers of ash and lava.
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Webinars: https://pecb.com/webinars
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LinkedIn: https://www.linkedin.com/company/pecb/
Facebook: https://www.facebook.com/PECBInternational/
Slideshare: http://www.slideshare.net/PECBCERTIFICATION
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