This presentation was offered by Carlos Jose Ramirez on behalf of Holbrook Travel's NSTA expedition to Costa Rica for educators July 2010. The presentation echoed a hands-on visit to seismology monitoring devices on Arenal Volcano.
The document provides information about volcanic eruptions, including:
1. It describes the different types of volcanic eruptions such as magmatic, phreatomagmatic, and phreatic eruptions. Specific subtypes of eruptions like Hawaiian, Strombolian, Vulcanian, and Plinian eruptions are also discussed.
2. The causes and mechanisms of different types of eruptions are explained. Magmatic eruptions are caused by gas release during decompression, while phreatomagmatic eruptions result from thermal contraction when magma interacts with water.
3. Details are given about what causes volcanoes, with an overview of the structure of
This document summarizes a study that used interferometric synthetic aperture radar (InSAR) observations to analyze ground deformation from the 1995 eruption of Fogo volcano in Cape Verde. The key findings were:
1. InSAR data showed ground deformation due to intrusion of a two-segment feeder dike for the eruption, but no evidence of deformation from changes in a shallow magma reservoir.
2. Modeling suggests the dike intruded at a depth of around 2 km.
3. The lack of shallow reservoir involvement and modeling of eruption volumes indicates the magma source was deep, at least 16.5 km below the surface.
4. This supports the
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, nu辿e ardentes, landslides, volcanic gases, tsunamis, and potential effects on global climate. Examples of historically deadly eruptions like Mount Pel辿e and Krakatoa are provided. The document also introduces the concept of supervolcanic eruptions ejecting over 1,000 cubic km of material.
The document summarizes information about earthquakes and volcanoes. It discusses what causes earthquakes, provides examples of major earthquakes including photos, and describes effects like ground shaking, surface faulting, liquefaction, landslides, fires, and tsunamis. It also defines what a volcano is, describes the different parts of a volcano, classifies the main types of volcanoes, and explains volcanic eruptions and their products. Safety tips are also mentioned. Maps of fault zones in the Philippines are presented.
A presentation on Volcanoes, Plate Tectonics and Igneous Rocks for high school use.
Compiled by James Campbell with resources from the Geological Society of the UK which has wealth of useful material.
This document provides information about volcanoes and igneous activity. It discusses the factors that influence volcanic eruptions such as the composition, temperature and gases in magma as well as viscosity. It describes the different types of materials associated with eruptions like lava flows, gases and pyroclastic materials. The document also outlines the general features of volcanoes and identifies three main types: shield volcanoes, cinder cones and composite cones. It explains other volcanic landforms and intrusive igneous features. In concluding, it discusses the origin of magma and the factors involved in melting solid rock located in the crust and upper mantle.
This document provides an overview of volcanoes and geysers, including:
1) It defines volcanoes and describes different types of volcanoes based on their shape, composition, and eruption patterns.
2) It explains the composition of lava and different types of lava flows.
3) It classifies common eruption types based on the magma composition and describes characteristics of each type.
4) It defines geysers and conditions required for their formation.
5) It discusses volcanic activity in Spain, including past eruptions in the Canary Islands and speculation about future eruptions.
2019-10-07 Small-scale deformation of active volcanoes measured by Synthetic ...Yosuke Aoki
油
The document summarizes research on measuring small-scale deformation at active volcanoes using synthetic aperture radar (SAR). It discusses studies of deformation at Usu Volcano and Mt. Asama in Japan. For Usu Volcano, InSAR data show subsidence concentrated around previous eruption vents that is explained by thermal contraction of intruded lava domes. At Mt. Asama, InSAR reveals flank instability dominated by subsidence and eastward motion in an area corresponding to a historical lava flow, possibly indicating flank instability rather than thermoelastic deformation.
Volcanoes are openings in the Earth's crust that allow lava, ash, and gases to escape from underground. There are several types of volcanoes defined by their activity level. An active volcano has erupted within the last 10,000 years, while a dormant volcano is considered active but is not currently erupting. An extinct volcano has not erupted for over 10,000 years. The 1815 eruption of Mount Tambora in Indonesia was one of the most devastating eruptions in history. It exploded with huge ash plumes and pyroclastic flows that destroyed surrounding villages and darkened skies for over 1,000 miles. Mount Tambora had been dormant for centuries before its massive eruption, which was the largest known
Volcanoes Presentation with material chiefly drawn from the Geological Society of the UK.
Presented to Reddam House Waterfall learners on 14 March 2022
Volcanism describes the constructive geological process where molten rock erupts from within the earth's crust. There are currently around 550 volcanoes that are considered active. Different types of volcanoes include shield volcanoes like Mauna Loa which erupt fluid basalt lava, cinder cones which form small bowls from ash eruptions, and composite or stratovolcanoes like Mount Rainier that have steep slopes and erupt andesite lava. Monitoring of volcanoes uses techniques like measuring volcanic gas emissions, ground deformation, and remote sensing to detect changes that may forecast eruptions.
"Hazard Mitigation: Volc叩n Bar炭, Panama"
By Julie A. Herrick
A review of mitigation efforts at the potentially active volcano, Volc叩n Bar炭. Historical seismicity, geologic mapping, lahar flow modeling, recent studies, and international efforts have developed hazard preparedness within the Chiriqui Province of western Panama."
Volcanoes form at plate boundaries where magma rises to the surface. There are two main types - acid/explosive volcanoes found at subduction zones and basaltic/shield volcanoes at hotspots. Mount Vesuvius near Naples, Italy is a composite acid volcano that has erupted frequently throughout history, most notably destroying Pompeii in 79AD. With over 3 million people now living nearby, Vesuvius presents a significant risk and authorities monitor it closely and have evacuation plans in place in case of a future eruption.
Volcanoes can be summarized as follows:
1. Volcanoes are openings in the earth's crust through which heated materials from the interior are ejected.
2. The materials ejected include gases, water, lava, and rock fragments. Gases make up 60-90% of total volcanic discharge and include water vapor, carbon dioxide, sulfur and chlorine compounds.
3. There are two main types of volcanoes - central/explosive volcanoes which eject pyroclastic materials and fissure/quiet volcanoes which erupt slowly along fractures.
Volcanoes occur primarily at plate boundaries and above hot spots in the mantle. There are currently around 1,500 active volcanoes worldwide. Volcanoes can be classified based on their structure and eruption type as shield volcanoes, cinder cone volcanoes, or composite volcanoes. The style of a volcanic eruption depends on factors like the amount of water vapor, trapped gases, and magma composition.
This document discusses both intrusive and extrusive volcanic features. Intrusive features include dykes, sills, laccoliths, batholiths, and plugs, which form when magma penetrates underground. Extrusive features result from magma emerging at the surface and include different types of lava (acid vs basic), dome volcanoes, ash/cinder cones, composite/shield volcanoes, calderas, and basalt plateaus. The document provides details on the formation and characteristics of these various volcanic landforms.
This document discusses both intrusive and extrusive volcanic features. Intrusive features include dykes, sills, laccoliths, batholiths, and plugs, which form when magma solidifies below the surface. Extrusive features include different types of volcanoes like dome, cinder cone, composite, and shield volcanoes that form when magma reaches the surface and solidifies as lava. The document also discusses volcanic eruptions and their associated hazards like lava flows, tephra, pyroclastic flows, gases, lahars, and tsunamis.
The document discusses plate tectonics and associated hazards. It describes the structure of the Earth's interior with an inner core, outer core, mantle and crust. The crust is divided into plates that move via convection currents in the asthenosphere. Plates interact at boundaries that are either constructive, destructive, or conservative. Destructive boundaries result in volcanoes, earthquakes and fold mountains through processes like subduction. Plate movement is evidenced by magnetic striping in ocean crust. Hazards vary depending on the type of boundary and are managed differently in LEDCs and MEDCs.
Volcanoes are openings in the Earth's crust where magma and gases escape. They are found at boundaries where tectonic plates are diverging or converging. When magma reaches the surface it is called lava, and eruptions produce lava, rock fragments, ashes, dust, and gases. There are over 550 active volcanoes distributed around plate boundaries on land and undersea. The type of eruption depends on factors like the crust's strength, pressure, and magma composition. Volcanoes are classified based on their shape, eruptive behavior, and deposits. Major hazards include lava flows, eruption columns, pyroclastic flows, and volcanic mudflows.
Volcanoes form at plate boundaries where tectonic plates are diverging or converging. There are three main types of volcanoes based on location: shield volcanoes at divergent boundaries, stratovolcanoes at subduction zones, and hotspots formed by mantle plumes. Volcanoes pose hazards from lava flows, explosions, and ashfall. Classification systems describe volcanoes based on activity levels from dormant to active. Monitoring systems use alert levels and colors to communicate volcanic unrest and eruptions.
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates in underground chambers, it can build up conical mountains at the vents. There are three main types of volcanoes defined by their shape and eruptive behavior: cinder cones are small and steep; shield volcanoes are broad with gentle slopes; and composite volcanoes are tall with alternating layers of ash and lava. Volcanoes can be active, dormant, or extinct depending on their history of recent eruptions.
Volcanic eruptions occur when magma reaches the Earth's surface through cracks in the crust. They can be devastating in the short term but also beneficial in the long run by enriching soils. Two main types are shield volcanoes, which erupt gently and form low slopes, and composite volcanoes with alternating lava and ash layers that can produce deadly pyroclastic flows. The eruption of Yellowstone supervolcano thousands of years ago was catastrophic globally. Montserrat was devastated in the 1990s when the Soufriere Hills volcano erupted, destroying the capital and forcing mass evacuations, though it has since calmed and rebuilding is underway.
The document discusses volcanoes, including:
- Volcanoes form when magma is forced from below the Earth's surface. There are currently around 50-60 volcanic eruptions per year.
- The main types of erupted material are lava and ash. The three main types of volcanoes are cinder cones, shield volcanoes, and composite volcanoes.
- Composite volcanoes are the most explosive and dangerous type, examples being Mount St. Helens and Mount Fuji. Large eruptions can have devastating effects like pyroclastic flows and ash falls.
Volcanoes are formed when magma from the Earth's upper mantle works its way to the surface and erupts. They can erupt explosively, ejecting ash and rock fragments into the air, or effusively, oozing lava onto the surface. The largest active volcano is Mauna Loa in Hawaii. Major volcanic eruptions, like Krakatoa in 1883 and Mount Pelee in 1902, can have devastating impacts and cause loss of life. Plate tectonics and the movement of tectonic plates under the Earth's surface is a major factor in where volcanoes are located.
Mount Etna located on the east coast of Sicily is classified as a stratovolcano and is the tallest active volcano in Europe at 3,329 m (10,922 ft). It remains one of the most active and dangerous volcanoes in the world. A major eruption of Etna and other volcanoes close to large cities such as Messina and Catania would be devastating to people, property, infrastructure, the environment, and the global economy.
The document summarizes a 5-day tour of botanical gardens and natural areas in South Florida led by Mary Pat Matheson and Ron Determann. The tour includes visits to Kampong Gardens, Montgomery Botanical Center, Fairchild Tropical Botanic Garden, Fruit & Spice Park, R.F. Orchids, Everglades National Park, Vizcaya Museum & Gardens, Fakahatchee Strand Preserve State Park, and Naples Botanical Garden. The document provides details about each location, including descriptions, directors, and planned activities.
Pasco and Holbrook Travel are eager to share in the resource support for enhanced inquiry-based learning within International Studies. This presentations showcases some key elements of this partnership
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2019-10-07 Small-scale deformation of active volcanoes measured by Synthetic ...Yosuke Aoki
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The document summarizes research on measuring small-scale deformation at active volcanoes using synthetic aperture radar (SAR). It discusses studies of deformation at Usu Volcano and Mt. Asama in Japan. For Usu Volcano, InSAR data show subsidence concentrated around previous eruption vents that is explained by thermal contraction of intruded lava domes. At Mt. Asama, InSAR reveals flank instability dominated by subsidence and eastward motion in an area corresponding to a historical lava flow, possibly indicating flank instability rather than thermoelastic deformation.
Volcanoes are openings in the Earth's crust that allow lava, ash, and gases to escape from underground. There are several types of volcanoes defined by their activity level. An active volcano has erupted within the last 10,000 years, while a dormant volcano is considered active but is not currently erupting. An extinct volcano has not erupted for over 10,000 years. The 1815 eruption of Mount Tambora in Indonesia was one of the most devastating eruptions in history. It exploded with huge ash plumes and pyroclastic flows that destroyed surrounding villages and darkened skies for over 1,000 miles. Mount Tambora had been dormant for centuries before its massive eruption, which was the largest known
Volcanoes Presentation with material chiefly drawn from the Geological Society of the UK.
Presented to Reddam House Waterfall learners on 14 March 2022
Volcanism describes the constructive geological process where molten rock erupts from within the earth's crust. There are currently around 550 volcanoes that are considered active. Different types of volcanoes include shield volcanoes like Mauna Loa which erupt fluid basalt lava, cinder cones which form small bowls from ash eruptions, and composite or stratovolcanoes like Mount Rainier that have steep slopes and erupt andesite lava. Monitoring of volcanoes uses techniques like measuring volcanic gas emissions, ground deformation, and remote sensing to detect changes that may forecast eruptions.
"Hazard Mitigation: Volc叩n Bar炭, Panama"
By Julie A. Herrick
A review of mitigation efforts at the potentially active volcano, Volc叩n Bar炭. Historical seismicity, geologic mapping, lahar flow modeling, recent studies, and international efforts have developed hazard preparedness within the Chiriqui Province of western Panama."
Volcanoes form at plate boundaries where magma rises to the surface. There are two main types - acid/explosive volcanoes found at subduction zones and basaltic/shield volcanoes at hotspots. Mount Vesuvius near Naples, Italy is a composite acid volcano that has erupted frequently throughout history, most notably destroying Pompeii in 79AD. With over 3 million people now living nearby, Vesuvius presents a significant risk and authorities monitor it closely and have evacuation plans in place in case of a future eruption.
Volcanoes can be summarized as follows:
1. Volcanoes are openings in the earth's crust through which heated materials from the interior are ejected.
2. The materials ejected include gases, water, lava, and rock fragments. Gases make up 60-90% of total volcanic discharge and include water vapor, carbon dioxide, sulfur and chlorine compounds.
3. There are two main types of volcanoes - central/explosive volcanoes which eject pyroclastic materials and fissure/quiet volcanoes which erupt slowly along fractures.
Volcanoes occur primarily at plate boundaries and above hot spots in the mantle. There are currently around 1,500 active volcanoes worldwide. Volcanoes can be classified based on their structure and eruption type as shield volcanoes, cinder cone volcanoes, or composite volcanoes. The style of a volcanic eruption depends on factors like the amount of water vapor, trapped gases, and magma composition.
This document discusses both intrusive and extrusive volcanic features. Intrusive features include dykes, sills, laccoliths, batholiths, and plugs, which form when magma penetrates underground. Extrusive features result from magma emerging at the surface and include different types of lava (acid vs basic), dome volcanoes, ash/cinder cones, composite/shield volcanoes, calderas, and basalt plateaus. The document provides details on the formation and characteristics of these various volcanic landforms.
This document discusses both intrusive and extrusive volcanic features. Intrusive features include dykes, sills, laccoliths, batholiths, and plugs, which form when magma solidifies below the surface. Extrusive features include different types of volcanoes like dome, cinder cone, composite, and shield volcanoes that form when magma reaches the surface and solidifies as lava. The document also discusses volcanic eruptions and their associated hazards like lava flows, tephra, pyroclastic flows, gases, lahars, and tsunamis.
The document discusses plate tectonics and associated hazards. It describes the structure of the Earth's interior with an inner core, outer core, mantle and crust. The crust is divided into plates that move via convection currents in the asthenosphere. Plates interact at boundaries that are either constructive, destructive, or conservative. Destructive boundaries result in volcanoes, earthquakes and fold mountains through processes like subduction. Plate movement is evidenced by magnetic striping in ocean crust. Hazards vary depending on the type of boundary and are managed differently in LEDCs and MEDCs.
Volcanoes are openings in the Earth's crust where magma and gases escape. They are found at boundaries where tectonic plates are diverging or converging. When magma reaches the surface it is called lava, and eruptions produce lava, rock fragments, ashes, dust, and gases. There are over 550 active volcanoes distributed around plate boundaries on land and undersea. The type of eruption depends on factors like the crust's strength, pressure, and magma composition. Volcanoes are classified based on their shape, eruptive behavior, and deposits. Major hazards include lava flows, eruption columns, pyroclastic flows, and volcanic mudflows.
Volcanoes form at plate boundaries where tectonic plates are diverging or converging. There are three main types of volcanoes based on location: shield volcanoes at divergent boundaries, stratovolcanoes at subduction zones, and hotspots formed by mantle plumes. Volcanoes pose hazards from lava flows, explosions, and ashfall. Classification systems describe volcanoes based on activity levels from dormant to active. Monitoring systems use alert levels and colors to communicate volcanic unrest and eruptions.
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates in underground chambers, it can build up conical mountains at the vents. There are three main types of volcanoes defined by their shape and eruptive behavior: cinder cones are small and steep; shield volcanoes are broad with gentle slopes; and composite volcanoes are tall with alternating layers of ash and lava. Volcanoes can be active, dormant, or extinct depending on their history of recent eruptions.
Volcanic eruptions occur when magma reaches the Earth's surface through cracks in the crust. They can be devastating in the short term but also beneficial in the long run by enriching soils. Two main types are shield volcanoes, which erupt gently and form low slopes, and composite volcanoes with alternating lava and ash layers that can produce deadly pyroclastic flows. The eruption of Yellowstone supervolcano thousands of years ago was catastrophic globally. Montserrat was devastated in the 1990s when the Soufriere Hills volcano erupted, destroying the capital and forcing mass evacuations, though it has since calmed and rebuilding is underway.
The document discusses volcanoes, including:
- Volcanoes form when magma is forced from below the Earth's surface. There are currently around 50-60 volcanic eruptions per year.
- The main types of erupted material are lava and ash. The three main types of volcanoes are cinder cones, shield volcanoes, and composite volcanoes.
- Composite volcanoes are the most explosive and dangerous type, examples being Mount St. Helens and Mount Fuji. Large eruptions can have devastating effects like pyroclastic flows and ash falls.
Volcanoes are formed when magma from the Earth's upper mantle works its way to the surface and erupts. They can erupt explosively, ejecting ash and rock fragments into the air, or effusively, oozing lava onto the surface. The largest active volcano is Mauna Loa in Hawaii. Major volcanic eruptions, like Krakatoa in 1883 and Mount Pelee in 1902, can have devastating impacts and cause loss of life. Plate tectonics and the movement of tectonic plates under the Earth's surface is a major factor in where volcanoes are located.
Mount Etna located on the east coast of Sicily is classified as a stratovolcano and is the tallest active volcano in Europe at 3,329 m (10,922 ft). It remains one of the most active and dangerous volcanoes in the world. A major eruption of Etna and other volcanoes close to large cities such as Messina and Catania would be devastating to people, property, infrastructure, the environment, and the global economy.
The document summarizes a 5-day tour of botanical gardens and natural areas in South Florida led by Mary Pat Matheson and Ron Determann. The tour includes visits to Kampong Gardens, Montgomery Botanical Center, Fairchild Tropical Botanic Garden, Fruit & Spice Park, R.F. Orchids, Everglades National Park, Vizcaya Museum & Gardens, Fakahatchee Strand Preserve State Park, and Naples Botanical Garden. The document provides details about each location, including descriptions, directors, and planned activities.
Pasco and Holbrook Travel are eager to share in the resource support for enhanced inquiry-based learning within International Studies. This presentations showcases some key elements of this partnership
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This presentation was provided to NSTA 2010 Delegates traveling to Costa Rica with Holbrook Travel and PASCO Scientific utilizing the Spark Mobile Learning Labs and sensors for inquiry based learning
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Holbrook Travel was founded on the mission of connecting travelers to nature and people in destinations through culturally immersive experiences facilitated by their deep local knowledge and reliable support services. For 35 years, Holbrook has specialized in natural history expeditions, sustainability, expertise, reliability, personalized service, global accessibility, and handcrafted itineraries to promote travel as a means of understanding diversity through research, adventure, discovery, education, understanding, perspective, friendship, community, and opportunity.
For more information about my speaking and training work, visit: https://www.pookyknightsmith.com/speaking/
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Maslows Toolbox: Creating Classrooms Where Every Child Thrives
Using Maslows Hierarchy of Needs as a practical lens, this session explores how meeting childrens basic physical, emotional, and psychological needs can transform behaviour, engagement, and learning. With a strong focus on inclusion, well look at how small, manageable changes can create classrooms where all childrenincluding autistic pupils, ADHD learners, and those with experiences of traumafeel safe, valued, and ready to thrive. Youll leave with simple, low-cost strategies that are easy to implement and benefit every student, without singling anyone out.
By the end of this session, participants will be able to:
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Apply practical tools the very next dayno extra budget required
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Visit:- https://onlinecollegehomeworkhelp.com/aerospace-engineering-assignment-help
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1. GEOLOGA, VOLCANOLOGA Y SISMOLOGA Red Sismol坦gica National (UCR-ICE) Universidad de Costa Rica (UCR) Instituto Costarricense de Electricidad (ICE) Volcan坦logos Carlos Jos辿 Ramirez
25. First Volcanological Observatory on Central America (1964) Central America School of Geology, UCR (1970) Center for Geophysics Reseach, CIGEFI (1979) National Seismological Network (ICE-UCR, 1974)
36. FUMAROLES 90 属遺 Iraz 炭 Crater Diego de la Haya Crater Main Crater Diameter 賊 1000 m Deep 賊 250 m Lagoon Diameter 賊 150 m Lagoon 14 to 20 m depth pH 3.5 to 4.5, 18 to 25 属遺
105. Volatiles and Fluids in Subduction Zones : Climate feedback and trigger mechanisms for natural disasters An overview. 3 Themes, each with 4 Subprojects A Input, subduction processes and structure B Volatiles and fluids in the forearc (continental slope) C Volatile transfer through the volcanic arc into the atmosphere
106. 9属30 9属20 9属10 9属00 8属50 8属40 -2000 0 85属90 85属80 85属70 85属60 85属50 85属00 84属90 84属80 Nicoya Slump Tectonic oversteepening at erosive convergent margins: example: Costa Rica SFB 574, Collaborative Research Centre Volatiles and Fluids in Subduction Zones
107. Nicoya Slump slope failure caused by ridge and seamount subduction likely a single, catastrophic (tsunamigenic) event SFB 574, Collaborative Research Centre Volatiles and Fluids in Subduction Zones -2000 0 9属30 9属20 9属10 9属00 85属90 85属80 85属70 85属60 85属50 84属00
108. 9属30 9属20 9属10 9属00 8属50 8属40 -2000 0 85属90 85属80 85属70 85属60 85属50 85属00 84属90 84属80 Nicoya Slump Jaco Scarp Tectonic oversteepening at erosive convergent margins: example: Costa Rica SFB 574, Collaborative Research Centre Volatiles and Fluids in Subduction Zones
109. Jaco Scarp continous slope indentation and failure caused by seamount subduction in a series of small scale slide events SFB 574, Collaborative Research Centre Volatiles and Fluids in Subduction Zones
110. 9属30 9属20 9属10 9属00 8属50 8属40 -2000 0 85属90 85属80 85属70 85属60 85属50 85属00 84属90 84属80 Nicoya Slump Jaco Scarp small scale slumping Tectonic oversteepening at erosive convergent margins: example: Costa Rica SFB 574, Collaborative Research Centre Volatiles and Fluids in Subduction Zones