Magma is molten rock beneath Earth's surface that rises toward the surface due to being less dense than surrounding rock. Magma that reaches the surface erupts through volcanoes. There are different types of volcanoes that can have eruptions ranging from gentle lava flows to catastrophic explosions. The composition of magmas varies but is dominated by silica and results in three main types: basaltic, andesitic, and rhyolitic. Basaltic magma is erupted by most volcanoes and forms lava flows, while more viscous andesitic and rhyolitic magmas can lead to explosive eruptions due to gas bubbles rising slowly in the thick lava.
The rock cycle document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and how they are related through geological processes. It focuses on igneous rocks, which form from cooling magma, and can cool underground to form intrusive rocks or above ground to form extrusive rocks like lava. The composition and cooling rate of magma determines the type of igneous rock formed. Magma is hot melted rock from deep in the Earth, and its viscosity is affected by temperature and silica content.
This document summarizes the key characteristics and types of magma. It defines magma as a mixture of molten or semi-molten rock found beneath the Earth's surface. Magma forms through mechanisms like decompression melting when hot mantle material rises and melts lower pressure rock, or flux melting when water or carbon dioxide lowers the melting temperature of mantle rock. Magma can be classified based on its chemical composition into basaltic, andesitic, or rhyolitic types depending on silicon and iron/magnesium content, and each type has distinct physical properties like temperature, viscosity, and gas content that determine explosiveness. Magma is also differentiated based on how it formed, such as primitive, primary, parental
Origin& evolution of magma ,magmatism related to plate tectonics.Devashish Sahu
This document summarizes a seminar on the origin and evolution of magma and its relationship to plate tectonics. It discusses how magma originates from partial melting of the solid earth due to increased temperature and pressure. Magma composition evolves through processes like fractional crystallization, assimilation, and magma mixing. Magmatism is related to plate tectonics through mechanisms like decompression melting at mid-ocean ridges and continental rifts, flux melting near subduction zones, and intraplate volcanism from mantle plumes not associated with plate boundaries. Examples discussed include the Deccan Traps basalts formed by a mantle plume in India.
- Magma forms by partial melting of the mantle or crust and consists of molten or semi-molten rock. It varies in temperature, pressure, density and composition depending on its origin and evolution.
- Magma evolves as it differentiates through fractional crystallization, assimilation, and mixing. Early crystallizing minerals remove elements from the magma, changing its composition over time according to Bowen's reaction series.
- Magma rises towards the Earth's surface where it cools and crystallizes to form either plutonic or volcanic rocks, depending on the cooling rate. Slow cooling results in large mineral crystals in plutonic rocks, while rapid cooling of lava forms volcanic rocks like obsidian with little
The document discusses the formation and characteristics of magma and igneous rocks. It explains that magma is formed through the partial melting of rocks in the mantle and crust due to heat from radioactive decay and changes in temperature and pressure. Magma can form different rock types as it evolves through processes like crystallization, assimilation, and magma mixing. Basalt forms from mantle melting, andesite from basalt interacting with crustal rocks, and granite from the crystallization of andesite magma.
Magma And classification Of Magma by junaidurrehmanJunaidurrehman26
Magma is formed from heating of the earth's interior. It exists in two main types - felsic and mafic. Heat sources that contribute to magma generation include the earth's core and radioactive elements. Magma composition depends on whether it forms from the mantle or crust. Igneous rocks form from the solidification of magma or lava. They are classified based on composition, texture and mode of formation. Bowen's reaction series describes the order in which minerals crystallize from cooling magma. Magma differentiation occurs through processes like crystal settling that separate minerals and change the magma's composition.
Mantle melting occurs when heat and pressure cause partial melting of the mantle, producing basaltic magma. Basalt is the most common volcanic rock on Earth and can be further differentiated to form other igneous rock types. Evidence for the composition and processes of the mantle comes from ophiolites, dredged samples from ocean floors, nodules contained in basalts, and xenoliths brought up from deep in the mantle via kimberlite eruptions. Together this evidence indicates that the upper mantle is composed predominantly of the minerals olivine, orthopyroxene, and clinopyroxene which make up the rocks dunite, harzburgite, and lherzol
The document discusses plate tectonics and magma genesis. It describes how the Earth's crust is divided into 12 major plates that move in various directions, causing them to collide, pull apart, or scrape against each other. It also explains that magma can only be created at plate boundaries where there are significant local changes in pressure and temperature. The three main types of plate boundaries are divergent boundaries, where plates separate and new crust is formed; convergent boundaries, where plates collide and one slides under the other; and transform boundaries, where plates slide past each other.
The rock cycle document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and how they are related through geological processes. It focuses on igneous rocks, which form from cooling magma, and can cool underground to form intrusive rocks or above ground to form extrusive rocks like lava. The composition and cooling rate of magma determines the type of igneous rock formed. Magma is hot melted rock from deep in the Earth, and its viscosity is affected by temperature and silica content.
This document summarizes the key characteristics and types of magma. It defines magma as a mixture of molten or semi-molten rock found beneath the Earth's surface. Magma forms through mechanisms like decompression melting when hot mantle material rises and melts lower pressure rock, or flux melting when water or carbon dioxide lowers the melting temperature of mantle rock. Magma can be classified based on its chemical composition into basaltic, andesitic, or rhyolitic types depending on silicon and iron/magnesium content, and each type has distinct physical properties like temperature, viscosity, and gas content that determine explosiveness. Magma is also differentiated based on how it formed, such as primitive, primary, parental
Origin& evolution of magma ,magmatism related to plate tectonics.Devashish Sahu
This document summarizes a seminar on the origin and evolution of magma and its relationship to plate tectonics. It discusses how magma originates from partial melting of the solid earth due to increased temperature and pressure. Magma composition evolves through processes like fractional crystallization, assimilation, and magma mixing. Magmatism is related to plate tectonics through mechanisms like decompression melting at mid-ocean ridges and continental rifts, flux melting near subduction zones, and intraplate volcanism from mantle plumes not associated with plate boundaries. Examples discussed include the Deccan Traps basalts formed by a mantle plume in India.
- Magma forms by partial melting of the mantle or crust and consists of molten or semi-molten rock. It varies in temperature, pressure, density and composition depending on its origin and evolution.
- Magma evolves as it differentiates through fractional crystallization, assimilation, and mixing. Early crystallizing minerals remove elements from the magma, changing its composition over time according to Bowen's reaction series.
- Magma rises towards the Earth's surface where it cools and crystallizes to form either plutonic or volcanic rocks, depending on the cooling rate. Slow cooling results in large mineral crystals in plutonic rocks, while rapid cooling of lava forms volcanic rocks like obsidian with little
The document discusses the formation and characteristics of magma and igneous rocks. It explains that magma is formed through the partial melting of rocks in the mantle and crust due to heat from radioactive decay and changes in temperature and pressure. Magma can form different rock types as it evolves through processes like crystallization, assimilation, and magma mixing. Basalt forms from mantle melting, andesite from basalt interacting with crustal rocks, and granite from the crystallization of andesite magma.
Magma And classification Of Magma by junaidurrehmanJunaidurrehman26
Magma is formed from heating of the earth's interior. It exists in two main types - felsic and mafic. Heat sources that contribute to magma generation include the earth's core and radioactive elements. Magma composition depends on whether it forms from the mantle or crust. Igneous rocks form from the solidification of magma or lava. They are classified based on composition, texture and mode of formation. Bowen's reaction series describes the order in which minerals crystallize from cooling magma. Magma differentiation occurs through processes like crystal settling that separate minerals and change the magma's composition.
Mantle melting occurs when heat and pressure cause partial melting of the mantle, producing basaltic magma. Basalt is the most common volcanic rock on Earth and can be further differentiated to form other igneous rock types. Evidence for the composition and processes of the mantle comes from ophiolites, dredged samples from ocean floors, nodules contained in basalts, and xenoliths brought up from deep in the mantle via kimberlite eruptions. Together this evidence indicates that the upper mantle is composed predominantly of the minerals olivine, orthopyroxene, and clinopyroxene which make up the rocks dunite, harzburgite, and lherzol
The document discusses plate tectonics and magma genesis. It describes how the Earth's crust is divided into 12 major plates that move in various directions, causing them to collide, pull apart, or scrape against each other. It also explains that magma can only be created at plate boundaries where there are significant local changes in pressure and temperature. The three main types of plate boundaries are divergent boundaries, where plates separate and new crust is formed; convergent boundaries, where plates collide and one slides under the other; and transform boundaries, where plates slide past each other.
The document discusses the Earth's internal structure and how it is studied using seismic waves. There are three main layers within Earth - the core, mantle, and crust. The core is the innermost layer and makes up about 1/3 of Earth's mass. The mantle is the middle layer and comprises about 2/3 of Earth's mass. The crust is the outermost layer and is a very small fraction of Earth's total mass. Seismic waves generated by earthquakes travel through Earth at different speeds depending on the material, allowing scientists to map its internal structure.
This document discusses factors that affect the viscosity of magma, including temperature, chemical composition/silica content, and amount of dissolved gases. It then provides examples of how viscosity is affected in different lava conditions. Specifically, lava with less silica content and more gases has lower viscosity and can flow farther, while lava with high silica content and fewer gases has higher viscosity and may dome or plug a vent without flowing far. Viscosity decreases with higher temperature and increases with higher silica content or lower gas content.
This document summarizes igneous petrology and the structure and composition of the Earth's interior. It discusses how the Earth is composed of layers including the crust, mantle, outer core, and inner core. The crust is divided into oceanic and continental crust. The mantle makes up most of the Earth's volume and is composed of ultramafic rock. Heat transfer mechanisms like conduction, convection, and advection are described. The geothermal gradient and how temperature increases with depth is also summarized. Plate tectonics and mantle convection are driving the dynamic cooling of the Earth.
The document discusses factors that influence the explosiveness of volcanic eruptions. Three main factors are the composition, temperature, and dissolved gas content of magma. These factors control magma viscosity, with more viscous magmas producing more explosive eruptions. The type of volcanic eruption depends on magma viscosity. Less viscous basaltic magmas produce effusive eruptions like lava fountains, while more viscous rhyolitic and andesitic magmas have more explosive eruptions ejecting pyroclastic material. Different volcanic features like shield volcanoes, cinder cones, and composite stratovolcanoes form based on the magma viscosity and volume erupted. Plate tectonics also
The document discusses factors that determine the explosiveness of volcanic eruptions and the different types of volcanic activity. The three main factors are the composition, temperature, and dissolved gases in magma. More viscous magmas with high silica and gas content produce more explosive eruptions, while fluid basaltic magmas erupt quietly. Volcanic eruptions can produce lava flows, pyroclastic materials like ash and tephra, and volcanic gases. Different volcanoes like shield volcanoes, cinder cones, and composite stratovolcanoes form based on the magma composition and tectonic environment. Stratovolcanoes near subduction zones are prone to violent, explosive eruptions producing
This document provides an overview of igneous rocks and magma. It defines igneous rocks as those formed from cooled magma. Magma forms from melting of rock in the crust or upper mantle, driven by mechanisms like pressure release, heat transfer, and addition of volatiles. Magma composition varies based on its source and processes during ascent, with the main types defined by their silica content. Composition controls eruption style, from explosive for silica-rich magmas to effusive for mafic ones. Igneous rocks form intrusively underground or extrusive at the surface, exhibiting different textures based on their cooling rate.
The document describes two types of endogenous (internally driven) landform-building processes: igneous and tectonic processes. Igneous processes create landforms such as volcanoes through volcanic eruptions and igneous intrusions. Tectonic processes like folding, faulting, and lateral faulting form landforms including mountains, rift valleys, escarpments, and are responsible for earthquakes through ongoing tectonic activity.
This document discusses mechanisms of magma diversification, including partial melting, crystal fractionation, thermogravitational diffusion, liquid immiscibility, vapor transport, magma mixing, and assimilation. Partial melting refers to processes where a magmatic melt is created from a portion of solid rock. Crystal fractionation involves the separation of crystals from melt through settling, filtering, or flow. Thermogravitational diffusion causes components to separate due to temperature and density gradients. Liquid immiscibility can cause magma to split into immiscible liquid fractions. Vapor transport involves volatile release upon pressure reduction. Magma mixing combines magmas of different compositions. Assimilation incorporates country rock into magma through reaction.
Assimilation is the process by which magma incorporates country rock. As magma passes through the crust, it can break off and melt pieces of the surrounding rock. There are three processes of assimilation: melting, diffusion and dissolution, and reaction. Assimilation requires large amounts of heat from the magma in order to melt the country rock. Evidence of assimilation can be seen in xenoliths and isotopic signatures within the igneous rock. Assimilation affects the composition and evolution of magmas.
Earth Materials and Processes : ENDOGENIC PROCESSSimple ABbieC
Earth Materials and Processes : ENDOGENIC PROCESS
Content Standard:
The learners demonstrate an understanding of:
geologic processes that occur within the Earth and
the folding and faulting of rocks
EARTH MATERIALS AND PROCESSES
Topic: Classification of Rocks / Types of Rocks
Senior High School | Earth and Life Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11/12ES-Ib-10)
Senior High School | Earth Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11ES-Ic-6)
Please LIKE / FOLLOW and SHARE my other social media accounts.
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The document describes three endogenous processes that occur within the Earth:
Magmatism, where rocks reach high temperatures and melt to form magma, which is then pushed through the mantle by convection currents. Volcanism occurs as magma escapes through openings, erupting at the surface with extreme heat and pressure. Metamorphism is the process by which the mineral components and textures of rocks change due to increases in heat, pressure, and fluids, occurring through contact or regional metamorphism on large scales.
The document discusses the rock cycle and the relationships between the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from magma, either slowly below ground as plutonic rocks or quickly at the surface as volcanic rocks. Sedimentary rocks form at the surface from eroded materials that are transported and deposited. Metamorphic rocks form from changes to existing rocks through pressure, temperature, and fluids deep underground. The rock cycle is powered by the Earth's interior heat and momentum, as well as energy from the sun, and involves surface and subsurface geological processes that connect the hydrologic and tectonic cycles.
The document provides information on igneous petrology including definitions of key terms like petrography, petrology, and petrogenesis. It describes techniques for classifying igneous rocks based on their texture, mineralogy, chemistry and other properties. Bowen's reaction series is explained as the process by which magma cools and crystallizes into rocks of different compositions. Diagrams like Harker variation diagrams and triangular variation diagrams are used to visualize chemical variations in rock compositions.
The document summarizes endogenous processes that generate heat within the Earth and how that heat is transferred. It discusses two main sources of internal heat: primordial heat generated during Earth's formation through accretion and radioactive decay of isotopes. Heat is transferred through convection in the mantle and conduction at boundaries. Magmas form through decompression melting at mid-ocean ridges and mantle plumes, or flux and heat transfer melting at subduction zones. Endogenous processes like magmatism, volcanism/plutonism, and metamorphism influence rock behavior and landform evolution.
A volcano is a vent in the Earth's crust that allows magma and erupted material to reach the surface. It includes the cone of erupted material surrounding the vent. The main parts of a volcano are the vent, crater, and volcanic cone. Volcanoes can have different shapes depending on the type of material they erupt, including shield, cinder cone, and composite cone volcanoes. Volcanic eruptions can be either explosive or effusive and pose hazards like pyroclastic flows, lava flows, ash falls, and noxious gases.
Volcanoes form at boundaries where tectonic plates meet or at hotspots within plates. There are three main types of volcanic eruptions based on the driving mechanism: magmatic eruptions driven by gas decompression, phreatomagmatic eruptions driven by gas compression, and phreatic eruptions driven by steam superheating. Lava is molten rock expelled during an eruption that can flow long distances before solidifying into igneous rock, while volcanic ash and fragments are produced during explosive eruptions.
The document discusses igneous rocks, which form from molten rock material known as magma or lava. Igneous rocks can form underground from cooling magma (intrusive rocks) or on the surface from cooling lava (extrusive rocks). The temperature of magma/lava influences igneous activity and rock properties, ranging from 1,170°C for basalt to 800-1,100°C for dacite. Intrusive rocks form large visible crystals as they cool slowly underground, while extrusive rocks cool too quickly to form crystals. Igneous rocks are an important economic resource, as precious metals and gems are often associated with them.
The document defines key terms related to the rock cycle, including the three main types of rock - igneous, sedimentary, and metamorphic. It explains that igneous rock forms from cooling magma, sedimentary rock forms through compaction and cementation of sediments, and metamorphic rock forms from changes to existing rock by heat and pressure. The rock cycle is also defined as the process where rocks slowly transform between these three types over time through weathering, erosion, deposition and metamorphism.
Mineral dapat dikelompokkan menjadi silikat dan non-silikat. Mineral silikat mengandung silika dan membentuk 90% batuan, sedangkan non-silikat terbentuk dari kombinasi logam dan non-logam seperti oksigen, sulfur, karbonat, hidroksida, dan halida.
The document discusses the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma, either underground (intrusive) or above ground (extrusive). Sedimentary rocks form through the compaction and cementation of sediments. Metamorphic rocks are formed from existing rocks undergoing heat and pressure without melting. The rock cycle diagram shows how rocks continuously change between these three types through various geologic processes.
Este documento describe los factores que influyen en la actividad volcánica, incluyendo la composición, temperatura y cantidad de gases del magma. Explica cómo estos factores afectan el flujo de lava y la formación de columnas eruptivas, rocas piroclásticas y depósitos como coladas y lahares. También cubre estructuras ígneas como plutones, sills y lacolitos.
The document discusses the Earth's internal structure and how it is studied using seismic waves. There are three main layers within Earth - the core, mantle, and crust. The core is the innermost layer and makes up about 1/3 of Earth's mass. The mantle is the middle layer and comprises about 2/3 of Earth's mass. The crust is the outermost layer and is a very small fraction of Earth's total mass. Seismic waves generated by earthquakes travel through Earth at different speeds depending on the material, allowing scientists to map its internal structure.
This document discusses factors that affect the viscosity of magma, including temperature, chemical composition/silica content, and amount of dissolved gases. It then provides examples of how viscosity is affected in different lava conditions. Specifically, lava with less silica content and more gases has lower viscosity and can flow farther, while lava with high silica content and fewer gases has higher viscosity and may dome or plug a vent without flowing far. Viscosity decreases with higher temperature and increases with higher silica content or lower gas content.
This document summarizes igneous petrology and the structure and composition of the Earth's interior. It discusses how the Earth is composed of layers including the crust, mantle, outer core, and inner core. The crust is divided into oceanic and continental crust. The mantle makes up most of the Earth's volume and is composed of ultramafic rock. Heat transfer mechanisms like conduction, convection, and advection are described. The geothermal gradient and how temperature increases with depth is also summarized. Plate tectonics and mantle convection are driving the dynamic cooling of the Earth.
The document discusses factors that influence the explosiveness of volcanic eruptions. Three main factors are the composition, temperature, and dissolved gas content of magma. These factors control magma viscosity, with more viscous magmas producing more explosive eruptions. The type of volcanic eruption depends on magma viscosity. Less viscous basaltic magmas produce effusive eruptions like lava fountains, while more viscous rhyolitic and andesitic magmas have more explosive eruptions ejecting pyroclastic material. Different volcanic features like shield volcanoes, cinder cones, and composite stratovolcanoes form based on the magma viscosity and volume erupted. Plate tectonics also
The document discusses factors that determine the explosiveness of volcanic eruptions and the different types of volcanic activity. The three main factors are the composition, temperature, and dissolved gases in magma. More viscous magmas with high silica and gas content produce more explosive eruptions, while fluid basaltic magmas erupt quietly. Volcanic eruptions can produce lava flows, pyroclastic materials like ash and tephra, and volcanic gases. Different volcanoes like shield volcanoes, cinder cones, and composite stratovolcanoes form based on the magma composition and tectonic environment. Stratovolcanoes near subduction zones are prone to violent, explosive eruptions producing
This document provides an overview of igneous rocks and magma. It defines igneous rocks as those formed from cooled magma. Magma forms from melting of rock in the crust or upper mantle, driven by mechanisms like pressure release, heat transfer, and addition of volatiles. Magma composition varies based on its source and processes during ascent, with the main types defined by their silica content. Composition controls eruption style, from explosive for silica-rich magmas to effusive for mafic ones. Igneous rocks form intrusively underground or extrusive at the surface, exhibiting different textures based on their cooling rate.
The document describes two types of endogenous (internally driven) landform-building processes: igneous and tectonic processes. Igneous processes create landforms such as volcanoes through volcanic eruptions and igneous intrusions. Tectonic processes like folding, faulting, and lateral faulting form landforms including mountains, rift valleys, escarpments, and are responsible for earthquakes through ongoing tectonic activity.
This document discusses mechanisms of magma diversification, including partial melting, crystal fractionation, thermogravitational diffusion, liquid immiscibility, vapor transport, magma mixing, and assimilation. Partial melting refers to processes where a magmatic melt is created from a portion of solid rock. Crystal fractionation involves the separation of crystals from melt through settling, filtering, or flow. Thermogravitational diffusion causes components to separate due to temperature and density gradients. Liquid immiscibility can cause magma to split into immiscible liquid fractions. Vapor transport involves volatile release upon pressure reduction. Magma mixing combines magmas of different compositions. Assimilation incorporates country rock into magma through reaction.
Assimilation is the process by which magma incorporates country rock. As magma passes through the crust, it can break off and melt pieces of the surrounding rock. There are three processes of assimilation: melting, diffusion and dissolution, and reaction. Assimilation requires large amounts of heat from the magma in order to melt the country rock. Evidence of assimilation can be seen in xenoliths and isotopic signatures within the igneous rock. Assimilation affects the composition and evolution of magmas.
Earth Materials and Processes : ENDOGENIC PROCESSSimple ABbieC
Earth Materials and Processes : ENDOGENIC PROCESS
Content Standard:
The learners demonstrate an understanding of:
geologic processes that occur within the Earth and
the folding and faulting of rocks
EARTH MATERIALS AND PROCESSES
Topic: Classification of Rocks / Types of Rocks
Senior High School | Earth and Life Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11/12ES-Ib-10)
Senior High School | Earth Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11ES-Ic-6)
Please LIKE / FOLLOW and SHARE my other social media accounts.
Facebook: https://www.facebook.com/Simple-ABbieC-131584525051378/
-----------------------------------------------------------------------
Youtube:
http://tiny.cc/SimpleABbieC
-----------------------------------------------------------------------
Slideshare:
https://www.slideshare.net/AbbieMahinay
-----------------------------------------------------------------------
Blogger:
https://simpleabbiec.blogspot.com/?m=1
The document describes three endogenous processes that occur within the Earth:
Magmatism, where rocks reach high temperatures and melt to form magma, which is then pushed through the mantle by convection currents. Volcanism occurs as magma escapes through openings, erupting at the surface with extreme heat and pressure. Metamorphism is the process by which the mineral components and textures of rocks change due to increases in heat, pressure, and fluids, occurring through contact or regional metamorphism on large scales.
The document discusses the rock cycle and the relationships between the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from magma, either slowly below ground as plutonic rocks or quickly at the surface as volcanic rocks. Sedimentary rocks form at the surface from eroded materials that are transported and deposited. Metamorphic rocks form from changes to existing rocks through pressure, temperature, and fluids deep underground. The rock cycle is powered by the Earth's interior heat and momentum, as well as energy from the sun, and involves surface and subsurface geological processes that connect the hydrologic and tectonic cycles.
The document provides information on igneous petrology including definitions of key terms like petrography, petrology, and petrogenesis. It describes techniques for classifying igneous rocks based on their texture, mineralogy, chemistry and other properties. Bowen's reaction series is explained as the process by which magma cools and crystallizes into rocks of different compositions. Diagrams like Harker variation diagrams and triangular variation diagrams are used to visualize chemical variations in rock compositions.
The document summarizes endogenous processes that generate heat within the Earth and how that heat is transferred. It discusses two main sources of internal heat: primordial heat generated during Earth's formation through accretion and radioactive decay of isotopes. Heat is transferred through convection in the mantle and conduction at boundaries. Magmas form through decompression melting at mid-ocean ridges and mantle plumes, or flux and heat transfer melting at subduction zones. Endogenous processes like magmatism, volcanism/plutonism, and metamorphism influence rock behavior and landform evolution.
A volcano is a vent in the Earth's crust that allows magma and erupted material to reach the surface. It includes the cone of erupted material surrounding the vent. The main parts of a volcano are the vent, crater, and volcanic cone. Volcanoes can have different shapes depending on the type of material they erupt, including shield, cinder cone, and composite cone volcanoes. Volcanic eruptions can be either explosive or effusive and pose hazards like pyroclastic flows, lava flows, ash falls, and noxious gases.
Volcanoes form at boundaries where tectonic plates meet or at hotspots within plates. There are three main types of volcanic eruptions based on the driving mechanism: magmatic eruptions driven by gas decompression, phreatomagmatic eruptions driven by gas compression, and phreatic eruptions driven by steam superheating. Lava is molten rock expelled during an eruption that can flow long distances before solidifying into igneous rock, while volcanic ash and fragments are produced during explosive eruptions.
The document discusses igneous rocks, which form from molten rock material known as magma or lava. Igneous rocks can form underground from cooling magma (intrusive rocks) or on the surface from cooling lava (extrusive rocks). The temperature of magma/lava influences igneous activity and rock properties, ranging from 1,170°C for basalt to 800-1,100°C for dacite. Intrusive rocks form large visible crystals as they cool slowly underground, while extrusive rocks cool too quickly to form crystals. Igneous rocks are an important economic resource, as precious metals and gems are often associated with them.
The document defines key terms related to the rock cycle, including the three main types of rock - igneous, sedimentary, and metamorphic. It explains that igneous rock forms from cooling magma, sedimentary rock forms through compaction and cementation of sediments, and metamorphic rock forms from changes to existing rock by heat and pressure. The rock cycle is also defined as the process where rocks slowly transform between these three types over time through weathering, erosion, deposition and metamorphism.
Mineral dapat dikelompokkan menjadi silikat dan non-silikat. Mineral silikat mengandung silika dan membentuk 90% batuan, sedangkan non-silikat terbentuk dari kombinasi logam dan non-logam seperti oksigen, sulfur, karbonat, hidroksida, dan halida.
The document discusses the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from cooling magma, either underground (intrusive) or above ground (extrusive). Sedimentary rocks form through the compaction and cementation of sediments. Metamorphic rocks are formed from existing rocks undergoing heat and pressure without melting. The rock cycle diagram shows how rocks continuously change between these three types through various geologic processes.
Este documento describe los factores que influyen en la actividad volcánica, incluyendo la composición, temperatura y cantidad de gases del magma. Explica cómo estos factores afectan el flujo de lava y la formación de columnas eruptivas, rocas piroclásticas y depósitos como coladas y lahares. También cubre estructuras ígneas como plutones, sills y lacolitos.
Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma builds up at the vent, it forms the volcano structure above ground. The main parts of a volcano include the vent, conduit that carries magma from the magma chamber below, and the cone or mountain shape built from erupted material. Volcanic eruptions can be explosive or quiet depending on the magma composition and amount of trapped gases.
The document describes four types of volcanoes and their locations: 1) submarine volcanoes form at mid-ocean ridges where tectonic plates are spreading apart, 2) composite cone volcanoes form in island arcs at convergent plate boundaries, 3) stratovolcanoes form where oceanic plates subduct under continental plates and erupt acidic lava, and 4) shield volcanoes form at hotspots and erupt basic lava non-violently. It also mentions calderas formed by collapse of magma chambers.
This document discusses hazard identification, risk assessment, and risk control. It defines key terms like hazard, danger, and risk. It outlines the risk management process of classifying activities, identifying hazards, assessing risks, implementing risk controls, and reviewing controls. Different types of risks are described like mechanical, electrical, chemical, and ergonomic risks. Methods of risk assessment include qualitative, semi-quantitative, and quantitative assessments using risk matrices to evaluate likelihood and severity of risks. Risk control actions are recommended to eliminate, substitute, isolate, use engineering or administrative controls, or personal protective equipment.
The document discusses volcanic eruptions, including the process by which they occur, different types of eruptions, reasons for eruptions, and effects. It provides details on the top 10 deadliest eruptions in history. Safety tips are also listed, such as staying away from active volcanoes, keeping emergency supplies, knowing evacuation routes, and closing windows if ash is present.
Minerals are naturally occurring solid substances with repeating crystalline patterns. They form deep within the Earth through heat and pressure or near the surface when elements like oxygen, calcium, and carbon combine. Minerals have properties like streak, luster, and hardness that can be tested. Many common items are made from minerals, such as quartz in glass, diamonds in jewelry, and hematite in art. Rocks are composed of two or more minerals and do not have a crystalline structure. There are three main types of rocks: igneous rocks form from cooled lava or magma, sedimentary rocks form from compressed layers of sediment, and metamorphic rocks form from the alteration of existing rocks under heat and pressure.
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.
A PowerPoint Presentation for Grade 9 teachers. This presentation is ONLY suggested guide for teachers to assist them on the discussion after the activities as suggested in the Learner's Module were performed. Please feel free to add comments and suggestions. Thanks!
Magma and Volcanoes
The document discusses magma, volcanoes, and volcanic eruptions. It defines magma as molten rock beneath Earth's surface that rises toward the surface through vents called volcanoes. There are different types of volcanoes that produce different styles of eruptions from gentle to explosive, depending on factors like magma composition and viscosity. The three main types of magma are basaltic, andesitic, and rhyolitic. Explosive eruptions can produce devastating pyroclastic flows and tephra falls while nonexplosive eruptions form lava flows.
This document provides an overview of magma, volcanoes, and volcanic eruptions. It discusses the following key points in 3 sentences:
Magma is molten rock beneath the Earth's surface that rises towards the surface through vents called volcanoes. There are different types of volcanoes that produce eruptions ranging from gentle flows to catastrophic explosions, depending on the viscosity and gas content of the magma. The composition and viscosity of magmas influence the type of eruption, whether nonexplosive eruptions producing lava flows or explosive eruptions ejecting tephra and forming eruption columns and pyroclastic flows.
This document provides an overview of magma, volcanoes, and volcanic eruptions. It discusses how magma forms below Earth's surface and rises toward the surface through volcanoes. There are different types of volcanoes that produce nonexplosive or explosive eruptions depending on factors like magma viscosity and gas content. Eruptions can produce hazards like pyroclastic flows, tephra falls, lahars, and poisonous gases. The majority of volcanic activity occurs under the oceans and goes unobserved.
The document provides an overview of igneous rocks, including their formation from magma and lava, classification based on texture and composition, and key characteristics. Igneous rocks can be extrusive or intrusive, and their texture depends on the cooling rate - rapidly cooled rocks are fine-grained while slowly cooled rocks are coarse-grained. Magma composition also influences rock type, ranging from ultramafic to felsic. Bowen's reaction series describes the order minerals crystallize from magma as it cools.
Volcanic eruptions occur when hot material from Earth's interior is ejected from a volcano. Eruptions can range from non-explosive lava outflows to violent explosions that eject rock and ash. Geologists classify eruptions as magmatic, phreatomagmatic, or phreatic based on their driving mechanisms. Magmatic eruptions involve magma and produce different styles like Hawaiian, Strombolian, and Vulcanian. Phreatomagmatic eruptions result from magma interacting with water, exemplified by Surtseyan eruptions. Phreatic eruptions are driven solely by steam from water heating rock. Many countries monitor volcanoes and use alert
This document discusses volcanoes, including how they form, the different types of volcanoes, and where they are located. It provides details on four main types of volcanoes: cinder cones, composite volcanoes, shield volcanoes, and lava domes. Cinder cones are simple structures built from ejected cinders. Composite volcanoes are large symmetrical cones made of layers of material. Shield volcanoes are broad structures composed of fluid lava flows. Lava domes are small, bulbous masses that pile over the vent. Volcanoes can be located both under water and on land.
Volcanoes form when magma reaches the surface of the Earth. They can be found along plate boundaries where magma is able to reach the surface. There are over 1300 potentially active volcanoes worldwide. Volcanoes have different features like craters, vents, and magma chambers. They also go through life cycle stages of being active, dormant, or extinct. Eruptions can produce different types of lava and ash deposits that build different types of volcanic cones over time. While volcanoes provide fertile soils and minerals, their eruptions can negatively impact the environment through poisonous gases, lava flows, ash falls, pyroclastic flows, and lahars that damage infrastructure and agriculture.
The document summarizes igneous structures and field relationships. It describes how the style of volcanic eruption depends on the viscosity and gas content of magma. Basaltic magma has lower viscosity than rhyolitic magma due to differences in polymerization. Viscosity and gas content determine eruption styles from violent to quiescent. Central volcanoes include shield volcanoes formed from fluid basalt and composite volcanoes with interlayered lava and ash. Other structures include cinder cones, domes, and calderas formed by chamber collapse.
This document discusses igneous rock classifications and Bowen's reaction series. It begins by classifying igneous rocks based on their silica content into felsic, intermediate, mafic and ultramafic compositions. It then explains Bowen's reaction series, which showed that minerals crystallize from magma at different temperatures in a predictable order. Certain minerals tend to form together based on their crystallization temperatures. The document also discusses how igneous intrusive bodies like sills, dikes, batholiths and stocks form underground from crystallizing magma.
This document summarizes key concepts about igneous rocks and magma from Chapter 4 of Essentials of Geology 3rd Edition. Magma forms from the partial melting of rocks in the crust and upper mantle due to processes like pressure release, volatile addition, and heat transfer. As magma cools, igneous rocks form with different textures and compositions depending on the cooling environment. Intrusive igneous rocks cool slowly underground, while extrusive rocks cool rapidly at the surface. Magma composition is influenced by the source rock and processes like fractional crystallization during cooling.
The types and abundances of igneous rocks found are closely related to their tectonic setting. Basalt and gabbro are most common at divergent plate boundaries like ocean ridges, while rhyolite and granite are found more within continental interiors. Convergent plate boundaries produce andesitic and rhyolitic volcanoes along with intrusions of diorite and granite. The compositions of magmas range from mafic to felsic depending on the tectonic setting, source rock composition, assimilation, differentiation over time, and other factors. Common volcanic features include shield volcanoes, cinder cones, composite volcanoes, and calderas.
Volcanoes form when tectonic plates collide and one plate slides under another in the process of subduction. Most volcanoes occur near plate boundaries, especially around the Pacific Ocean basin known as the Ring of Fire. The Ring of Fire contains over 75% of the world's active volcanoes, including 452 volcanoes dotted around the boundary. Volcanic hotspots also cause volcanism, where thermal plumes rise from the Earth's mantle and melt the overlying rock. Different types of volcanic eruptions occur depending on the viscosity of the magma and amount of dissolved gases. Explosive eruptions are violent while effusive eruptions steadily flow lava. Scientists monitor ground deformation, gas emissions, and
MODULE 2- VOLCANIC ERUPTIONS & ITS CHARACTERISTICS.pptxFrenzDelaCruz3
Volcanic eruptions occur when magma rises from below the Earth's crust and erupts through a vent. The document defines different types of volcanic eruptions based on their characteristics, such as phreatic eruptions which involve water or phreatomagmatic eruptions which involve violent interactions between water and magma. It also explains how properties of magma like temperature, viscosity, crystal content and volatile gases affect the type of eruption that occurs. During an eruption, gas bubbles form in magma through processes like decompression or crystallization. When magma reaches the surface, it can produce volcanic hazards like ash falls, lava flows, pyroclastic flows, and mudflows that endanger
The document discusses the processes involved in rock formation. It describes how igneous rocks form from the crystallization of magma, either below the Earth's surface (intrusive) or on the surface (extrusive). Sedimentary rocks form from the compaction and cementation of sediments, and metamorphic rocks form from changes to existing rocks via heat, pressure and fluid processes in the Earth. The rock cycle illustrates how different rock types are interrelated as they form and are transformed over time through geological processes associated with plate tectonics.
Volcanoes,Fault Zone And Earthquakes,,Seismograph,Body Waves,Features Of Volc...Dhrupal Patel
briefly introduction about Volcanoes,Fault Zone And Earthquakes,,Seismograph,Body Waves,Features Of Volcanism,Volcanic EruptionsVolcanic Products,Locating Earthquakes,Measuring The “Size” Of Earthquakes,World Earthquake Distribution,Effects Of Earthquakes
The Earth's crust is made up of large tectonic plates that are cracked and move, with magma from the mantle able to rise up through these cracks. When pressure builds from below, volcanoes erupt as the magma finds a way to escape either through faults between plates or by bursting through weak spots in the crust. Inside volcanoes is a magma chamber where magma collects until pressure is great enough for an eruption to occur, expelling lava, tephra, ash, and gases. The type of eruption depends on the viscosity of the magma and amount of dissolved gases, with more gas and thick magma causing explosive eruptions that blast material high into the air.
1) Volcanoes form primarily at plate boundaries but some occur within plates due to mantle plumes. Their behavior depends on magma composition - mafic magmas erupt gently while intermediate to felsic magmas erupt explosively due to high viscosity and volatiles.
2) The most common volcano types are shield volcanoes which erupt large volumes of basalt, stratovolcanoes which have layered deposits from eruptions, and cinder cones which form small, steep cones of pyroclastic material.
3) Large explosive eruptions can inject ash into the atmosphere and lower global temperatures for years, as with the 1815 eruption of Tambora which inspired Mary
This document discusses volcanic eruptions, describing the differences between nonexplosive and explosive eruptions. Nonexplosive eruptions produce slow lava flows while explosive eruptions blast debris into the air. The type of eruption depends on the composition of the magma, particularly its silica, water, and gas content. Magma erupts as either lava or pyroclastic material like volcanic ash, bombs, and blocks.
Volcanoes form at boundaries where tectonic plates meet. The Earth's surface is composed of tectonic plates that fit together like a jigsaw puzzle. Volcanic eruptions occur when magma from the Earth's interior reaches the surface through weaknesses along plate boundaries. There are different types of volcanoes that form depending on the viscosity of the lava, including shield, composite, cinder cone, and lava dome volcanoes. Major volcanic eruptions can cause dangerous natural disasters like tsunamis, floods, earthquakes, mudflows and rockfalls.
Metamorphism occurs when rocks undergo changes in temperature and pressure due to burial or intrusion. There are several types of metamorphism that produce different textures and minerals depending on factors like stress, fluids, time, and temperature/pressure conditions. Regional metamorphism results from tectonic forces building mountains and produces foliated rocks through recrystallization and deformation. Plate tectonics drives metamorphism through processes like subduction and burial that subject rocks to high pressures and temperatures.
Igneous rocks form from the cooling and solidification of magma or lava. They can be intrusive or extrusive, depending on where the magma cools. Intrusive igneous rocks cool slowly underground, resulting in large mineral grains, while extrusive rocks cool rapidly at the surface, resulting in small mineral grains or a glassy texture. The mineral assemblage and texture of an igneous rock provides clues about its composition and conditions of formation. Bowen's reaction series describes the order in which minerals crystallize as magma cools.
Weathering is the breaking down of rocks, soils and minerals through direct contact with the atmosphere. It occurs through both physical and chemical processes. Chemical weathering involves chemical reactions that transform rocks and minerals into new combinations, through processes like dissolution, hydrolysis, oxidation, and carbonation. The effectiveness of chemical weathering increases with greater surface area exposure and is influenced by factors like mineralogy, rock type, climate, and the presence of moisture and heat.
This chapter discusses sedimentary rocks and the processes involved in their formation. It describes how clastic and chemical sediments are formed from weathering and precipitation, respectively, and how they are transported, deposited, and lithified into sedimentary rocks. Clastic sediments like gravel, sand, silt and clay are sorted by size and shape during transport. Chemical sediments form through inorganic precipitation or biochemical processes. Sedimentary structures and fossils within the rocks provide clues about the depositional environment. Compaction and cementation convert sediments into solid sedimentary rocks such as sandstone, siltstone, mudstone, conglomerate and various chemical rocks.
This document discusses different types of sedimentary rocks including clastic sedimentary rocks like breccia, conglomerate, sandstone, siltstone and shale formed from weathered debris. It also discusses chemical sedimentary rocks like limestone, evaporites including rock salt and gypsum, chert and coal. Finally, it mentions several sedimentary structures including cross bedded sandstone, graded bedding, mud cracks, ripple marks and trace fossils.
The document discusses the rock cycle and how different types of rocks are formed. It defines rocks as aggregates of minerals and describes the three main types - igneous, sedimentary, and metamorphic - based on their mode of origin. The rock cycle describes how rocks can be transformed into different types through geological processes like crystallization, weathering and erosion, deposition, lithification, and metamorphism due to pressure and heat within the Earth. Plate tectonics also influence the rock cycle as rocks form at sites of volcanic activity, mountain building, and sediment deposition at plate boundaries.
Minerals are naturally occurring inorganic solids with a defined chemical composition and crystalline structure. Most minerals are made up of combinations of common elements like oxygen, silicon, aluminum, iron, calcium, and magnesium. Minerals form in different crystal structures and exhibit physical properties like cleavage, hardness, luster, and streak that can be used to identify them. There are several classes of minerals including silicates, carbonates, and sulfides, with silicate minerals making up over 90% of the Earth's crust. Important rock-forming minerals are quartz, feldspar, mica, amphibole, pyroxene and olivine in the silicate class and calcite in the carbonate class.
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How to Setup Warehouse & Location in Odoo 17 InventoryCeline George
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LAND USE LAND COVER AND NDVI OF MIRZAPUR DISTRICT, UPRAHUL
This Dissertation explores the particular circumstances of Mirzapur, a region located in the
core of India. Mirzapur, with its varied terrains and abundant biodiversity, offers an optimal
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advanced technologies such as GIS (Geographic Information Systems) and Remote sensing to
analyze the transformations that have taken place over the course of a decade.
The complex relationship between human activities and the environment has been the focus
of extensive research and worry. As the global community grapples with swift urbanization,
population expansion, and economic progress, the effects on natural ecosystems are becoming
more evident. A crucial element of this impact is the alteration of vegetation cover, which plays a
significant role in maintaining the ecological equilibrium of our planet.Land serves as the foundation for all human activities and provides the necessary materials for
these activities. As the most crucial natural resource, its utilization by humans results in different
'Land uses,' which are determined by both human activities and the physical characteristics of the
land.
The utilization of land is impacted by human needs and environmental factors. In countries
like India, rapid population growth and the emphasis on extensive resource exploitation can lead
to significant land degradation, adversely affecting the region's land cover.
Therefore, human intervention has significantly influenced land use patterns over many
centuries, evolving its structure over time and space. In the present era, these changes have
accelerated due to factors such as agriculture and urbanization. Information regarding land use and
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providing crucial environmental data for scientific, resource management, policy purposes, and
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Remote Sensing and Geographic Information Systems
9
Changes in vegetation cover refer to variations in the distribution, composition, and overall
structure of plant communities across different temporal and spatial scales. These changes can
occur natural.
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
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Chapter wise All Notes of First year Basic Civil Engineering.pptxDenish Jangid
Chapter wise All Notes of First year Basic Civil Engineering
Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
Text Books:
1. Palancharmy, Basic Civil Engineering, McGraw Hill publishers.
2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
Communicating effectively and consistently with students can help them feel at ease during their learning experience and provide the instructor with a communication trail to track the course's progress. This workshop will take you through constructing an engaging course container to facilitate effective communication.
2. Earth’s Internal Thermal EngineEarth’s Internal Thermal Engine
Magma is molten rock beneath Earth’sMagma is molten rock beneath Earth’s
surface.surface.
Because liquid magma is less dense thanBecause liquid magma is less dense than
surrounding solid rock, and obviously moresurrounding solid rock, and obviously more
mobile, magma, once formed, rises towardmobile, magma, once formed, rises toward
the surface.the surface.
Magma that reaches the surface does so byMagma that reaches the surface does so by
erupting through vents we call volcanoes.erupting through vents we call volcanoes.
3. VolcanoesVolcanoes
The termThe term volcanovolcano comes from the name ofcomes from the name of
the Roman god of fire, Vulcan.the Roman god of fire, Vulcan.
There are different types of volcanoes.There are different types of volcanoes.
– Eruption vary from gentle flows (Hawaii andEruption vary from gentle flows (Hawaii and
Iceland) to catastrophic explosions (Mount St.Iceland) to catastrophic explosions (Mount St.
Helens, Mt. Pinatubo, Soufriere Hills).Helens, Mt. Pinatubo, Soufriere Hills).
The majority of eruption never make theThe majority of eruption never make the
news because they occur beneath the ocean,news because they occur beneath the ocean,
unobservedunobserved..
4. MagmaMagma
Magma has a wide range of compositions,Magma has a wide range of compositions,
but silica (SiObut silica (SiO22) always dominates the mix.) always dominates the mix.
Magma has high temperatures.Magma has high temperatures.
Magma is fluid—it has the ability to flow.Magma is fluid—it has the ability to flow.
Most magma actually is a mixture of liquidMost magma actually is a mixture of liquid
(often referred to as melt) and solid mineral(often referred to as melt) and solid mineral
grains.grains.
5. Composition of Magmas and LavasComposition of Magmas and Lavas
The composition of magmas and lavas isThe composition of magmas and lavas is
controlled by the most abundant elements incontrolled by the most abundant elements in
the Earth—Si, Al, Fe, Ca, Mg, Na, K, H, and O.the Earth—Si, Al, Fe, Ca, Mg, Na, K, H, and O.
Three distinct types of magma are moreThree distinct types of magma are more
common than others:common than others:
– Basaltic (mafic), containing about 50 percent SiOBasaltic (mafic), containing about 50 percent SiO2.2.
– Andesitic (intermediate), about 60 percent SiOAndesitic (intermediate), about 60 percent SiO2.2.
– Rhyolitic (felsic), about 70 percent SiORhyolitic (felsic), about 70 percent SiO2.2.
7. Mafic or Basaltic MagmasMafic or Basaltic Magmas
Mafic or Basaltic magmas are erupted byMafic or Basaltic magmas are erupted by
approximately 80 percent of volcanoesapproximately 80 percent of volcanoes
worldwide (the seafloor worldwide is mostlyworldwide (the seafloor worldwide is mostly
basalt).basalt).
Magma from Hawaiian volcanoes such asMagma from Hawaiian volcanoes such as
Kilauea and Mauna Loa is basaltic.Kilauea and Mauna Loa is basaltic.
The entire island of Iceland is basaltic.The entire island of Iceland is basaltic.
8. Intermediate or Andesitic andIntermediate or Andesitic and
Felsic or Rhyolitic MagmasFelsic or Rhyolitic Magmas
Intermediate or Andesitic magmas are aboutIntermediate or Andesitic magmas are about
10 percent of the total magma.10 percent of the total magma.
– Magma from Mount St. Helens in WashingtonMagma from Mount St. Helens in Washington
State and Krakatau in Indonesia is usuallyState and Krakatau in Indonesia is usually
andesitic.andesitic.
Felsic or Rhyolitic magmas are about 10Felsic or Rhyolitic magmas are about 10
percent of the total magma.percent of the total magma.
– Magmas erupted from volcanoes that once wereMagmas erupted from volcanoes that once were
active at Yellowstone Park are mostly rhyolitic.active at Yellowstone Park are mostly rhyolitic.
11. Gases Dissolved in MagmaGases Dissolved in Magma
Small amounts of gas (0.2 to 3% by weight)Small amounts of gas (0.2 to 3% by weight)
are dissolved in all magma.are dissolved in all magma.
The principal gas inThe principal gas in water vapor,water vapor, which,which,
together with carbon dioxide, accounts fortogether with carbon dioxide, accounts for
more than 98 percent of all gases emittedmore than 98 percent of all gases emitted
from volcanoes.from volcanoes.
12. Temperature of Magmas and LavasTemperature of Magmas and Lavas
Magma temperatures range from 1000Magma temperatures range from 1000oo
toto
12001200oo
C (1832˚F – 2192˚F).C (1832˚F – 2192˚F).
Magma temperatures can reach 1400Magma temperatures can reach 1400oo
CC
(2552˚F) under some conditions.(2552˚F) under some conditions.
13. Viscosity of Magmas and LavasViscosity of Magmas and Lavas
The internal property of a substance thatThe internal property of a substance that
offers resistance to flow is calledoffers resistance to flow is called viscosity.viscosity.
The more viscous a magma, the less easily itThe more viscous a magma, the less easily it
flows.flows.
Viscosity of a magma depends onViscosity of a magma depends on
temperature and composition (especially thetemperature and composition (especially the
silica and dissolved-gas contents).silica and dissolved-gas contents).
14. Viscosity of Magmas and LavasViscosity of Magmas and Lavas
The higher the temperature, the lower theThe higher the temperature, the lower the
viscosity, and the more readily magma flows.viscosity, and the more readily magma flows.
The smooth, ropy-surfaced lava in Hawaii,The smooth, ropy-surfaced lava in Hawaii,
formed from a very hot, very fluid lava isformed from a very hot, very fluid lava is
calledcalled pahoehoe.pahoehoe.
The rough-looking lava formed from a coolerThe rough-looking lava formed from a cooler
lava having a high viscosity is calledlava having a high viscosity is called aaaa (ah(ah
ah).ah).
15. Viscosity of Magmas and LavasViscosity of Magmas and Lavas
Felsic or rhyolitic magma (70% silica) isFelsic or rhyolitic magma (70% silica) is
always more viscous than mafic (basaltic)always more viscous than mafic (basaltic)
magma (50% silica).magma (50% silica).
Intermediate or Andesitic magma has aIntermediate or Andesitic magma has a
viscosity that is intermediate between theviscosity that is intermediate between the
two (60% silica).two (60% silica).
16. How Buoyant Magma Erupts onHow Buoyant Magma Erupts on
the Surfacethe Surface
Magma is less dense than the solid rock fromMagma is less dense than the solid rock from
which it forms.which it forms.
The pressure is proportional to depthThe pressure is proportional to depth
(thickness of overlying rock).(thickness of overlying rock).
– Therefore, as magma rises upward, the pressureTherefore, as magma rises upward, the pressure
on it decreases.on it decreases.
17. How Buoyant Magma Erupts onHow Buoyant Magma Erupts on
the Surfacethe Surface
Pressure controls the amount of gas aPressure controls the amount of gas a
magma can dissolve—more at high pressure,magma can dissolve—more at high pressure,
less at low.less at low.
Gas dissolved in an upward-moving magmaGas dissolved in an upward-moving magma
comes out of solution and forms bubbles.comes out of solution and forms bubbles.
18. Eruption Style—Nonexplosive orEruption Style—Nonexplosive or
Explosive?Explosive?
The difference between nonexplosive andThe difference between nonexplosive and
explosive eruptions depends largely onexplosive eruptions depends largely on
magma viscosity and dissolved-gas content.magma viscosity and dissolved-gas content.
Low viscosity magmas and low dissolved gasLow viscosity magmas and low dissolved gas
contents produce nonexplosive eruptions.contents produce nonexplosive eruptions.
19. Eruption Style—Nonexplosive orEruption Style—Nonexplosive or
Explosive?Explosive?
Nonexplosive eruptions may appear violentNonexplosive eruptions may appear violent
during their initial stages.during their initial stages.
– The reason is that gas bubbles in a low-viscosityThe reason is that gas bubbles in a low-viscosity
basaltic magma will rise rapidly upward, like thebasaltic magma will rise rapidly upward, like the
gas bubbles in a glass of soda.gas bubbles in a glass of soda.
– If a basaltic magma rises rapidly, spectacular lavaIf a basaltic magma rises rapidly, spectacular lava
fountains will occurfountains will occur..
20. Eruption Style—Nonexplosive orEruption Style—Nonexplosive or
Explosive?Explosive?
Because heat is lost quickly at the surface ofBecause heat is lost quickly at the surface of
the flowing lava, the surface solidifies into athe flowing lava, the surface solidifies into a
crust, beneath which the liquid lavacrust, beneath which the liquid lava
continues to flow in well-defined channelscontinues to flow in well-defined channels
called lava tubes.called lava tubes.
The very fluid lava initially forms thinThe very fluid lava initially forms thin
pahoehoe flows.pahoehoe flows.
With increasing viscosity the rate ofWith increasing viscosity the rate of
movement slows and the stickier lava maymovement slows and the stickier lava may
be transformed into a rough surfaced aabe transformed into a rough surfaced aa
flow that moves very slowly.flow that moves very slowly.
22. Vesicles and AmygdulesVesicles and Amygdules
When lava finally solidified to rock, the last-When lava finally solidified to rock, the last-
formed bubbles become trapped; theseformed bubbles become trapped; these
bubble preserved in the rock are calledbubble preserved in the rock are called
vesicles.vesicles.
Vesicles filled by secondary minerals areVesicles filled by secondary minerals are
calledcalled amygdules.amygdules.
24. Explosive EruptionsExplosive Eruptions
In viscous andesitic or rhyolitic magmas, gasIn viscous andesitic or rhyolitic magmas, gas
bubbles can rise only very slowly.bubbles can rise only very slowly.
When confining pressure drops quickly, theWhen confining pressure drops quickly, the
gas in a magma expand into a froth ofgas in a magma expand into a froth of
innumerable glass-walled bubbles calledinnumerable glass-walled bubbles called
pumice.pumice.
25. Explosive EruptionsExplosive Eruptions
In many instances, instead of formingIn many instances, instead of forming
pumice, small bubbles expanding within apumice, small bubbles expanding within a
huge mass of sufficiently gas-rich, viscoushuge mass of sufficiently gas-rich, viscous
magma will shatter the magma into tinymagma will shatter the magma into tiny
fragments called volcanic ash.fragments called volcanic ash.
Volcanic ash is the most abundant product ofVolcanic ash is the most abundant product of
explosive eruptions.explosive eruptions.
26. Eruption Columns and Tephra FallsEruption Columns and Tephra Falls
The largest and the most violent eruptionsThe largest and the most violent eruptions
are associated with silica-rich magmas havingare associated with silica-rich magmas having
a high dissolved-gas content.a high dissolved-gas content.
This hot, turbulent mixture rises rapidly inThis hot, turbulent mixture rises rapidly in
the cooler air above the vent to form anthe cooler air above the vent to form an
eruption column that may tower as high aseruption column that may tower as high as
45 km in the atmosphere.45 km in the atmosphere.
27. Eruption Columns and Tephra FallsEruption Columns and Tephra Falls
A violent eruption of this kind is called aA violent eruption of this kind is called a
plinian eruption, named after the Romanplinian eruption, named after the Roman
author and statesman, Pliny, who lost his lifeauthor and statesman, Pliny, who lost his life
in the A.D. 79 eruption of Mt. Vesuvius.in the A.D. 79 eruption of Mt. Vesuvius.
The particles of debris rain down in a tephraThe particles of debris rain down in a tephra
fall and eventually accumulate on the groundfall and eventually accumulate on the ground
as tephra deposits.as tephra deposits.
28. Pyroclastic FlowsPyroclastic Flows
When the mixture of hot gases andWhen the mixture of hot gases and
pyroclasts is more dense than thepyroclasts is more dense than the
atmosphere, the turbulent mixture flowsatmosphere, the turbulent mixture flows
down the side of the volcano rather thandown the side of the volcano rather than
forming an eruption column.forming an eruption column.
A hot, highly mobile flow of tephra thatA hot, highly mobile flow of tephra that
rushes down the flank of a volcano during arushes down the flank of a volcano during a
major eruption is called a pyroclastic flowmajor eruption is called a pyroclastic flow
(the most devastating and lethal forms of(the most devastating and lethal forms of
volcanic eruption).volcanic eruption).
29. Pyroclastic FlowsPyroclastic Flows
Pyroclastic flows are also known asPyroclastic flows are also known as nunuééee
ardenteardente (glowing cloud).(glowing cloud).
Historic observations indicate thatHistoric observations indicate that
pyroclastic flows can reach velocities of morepyroclastic flows can reach velocities of more
than 700 km/h.than 700 km/h.
In 1902, a pyroclastic flow rushed down theIn 1902, a pyroclastic flow rushed down the
flanks of Mont Pelee Volcano at an estimatedflanks of Mont Pelee Volcano at an estimated
speed of 200 KM/h, instantly killing 29,000speed of 200 KM/h, instantly killing 29,000
peoplepeople..
30. Lateral Blast—Mount St. HelensLateral Blast—Mount St. Helens
In 1980, Mount St. Helens, a volcano inIn 1980, Mount St. Helens, a volcano in
Washington, erupted violently.Washington, erupted violently.
As magma rose under the volcano, theAs magma rose under the volcano, the
mountain’s north flank began to bulgemountain’s north flank began to bulge
upward and outward.upward and outward.
The initial blast was sideways rather thanThe initial blast was sideways rather than
upward.upward.
– 600 km600 km22
of trees in the once-dense forest wereof trees in the once-dense forest were
leveled.leveled.
32. VolcanoesVolcanoes
There are two broad families of volcanoes:There are two broad families of volcanoes:
– Those formed by eruptions from a central vent.Those formed by eruptions from a central vent.
– Those that erupt through a long fissure.Those that erupt through a long fissure.
Central-vent eruptions build mounds of theCentral-vent eruptions build mounds of the
kind most people associate with volcanoes.kind most people associate with volcanoes.
Fissure eruptions build plateaus.Fissure eruptions build plateaus.
33. Central-vent VolcanoesCentral-vent Volcanoes
Based on their size and shape, there areBased on their size and shape, there are
three broad classes of central-ventthree broad classes of central-vent
volcanoes:volcanoes:
– Shield volcanoes.Shield volcanoes.
– Tephra cones.Tephra cones.
– Stratovolcanoes.Stratovolcanoes.
34. Shield Volcanoes (1)Shield Volcanoes (1)
A shield volcano produces a broad, dome-A shield volcano produces a broad, dome-
shaped mountain with an average surfaceshaped mountain with an average surface
slope of only a few degrees.slope of only a few degrees.
Low-viscosity basaltic lavas can flow forLow-viscosity basaltic lavas can flow for
kilometers down gentle slopes.kilometers down gentle slopes.
The accumulated lava from repeatedThe accumulated lava from repeated
eruptions of low-viscosity lava build a shielderuptions of low-viscosity lava build a shield
volcano.volcano.
35. Shield Volcanoes (2)Shield Volcanoes (2)
The farther lava flows down the flank, theThe farther lava flows down the flank, the
cooler and more viscous it becomes, so thecooler and more viscous it becomes, so the
steeper the slope must be for it to flow.steeper the slope must be for it to flow.
Large shield volcanoes rise as islands in theLarge shield volcanoes rise as islands in the
ocean (Hawaiian Islands, Tahiti, Samoa, theocean (Hawaiian Islands, Tahiti, Samoa, the
Galapagos, and many others).Galapagos, and many others).
38. Shield Volcanoes (3)Shield Volcanoes (3)
Mauna Loa volcano, for example, rises to aMauna Loa volcano, for example, rises to a
height of 4169 m above sea level, but ifheight of 4169 m above sea level, but if
measured from the seafloor the height ismeasured from the seafloor the height is
10,000 m, making Mauna Loa the tallest10,000 m, making Mauna Loa the tallest
mountain on Earth.mountain on Earth.
39. Tephra ConesTephra Cones
Tephra cone is built by shower of pyroclasticTephra cone is built by shower of pyroclastic
debris around a volcanic vent.debris around a volcanic vent.
The slopes of tephra cones are steep,The slopes of tephra cones are steep,
typically about 30typically about 30oo
..
40. Statovolcanoes (1)Statovolcanoes (1)
Some volcanoes (andesitic composition)Some volcanoes (andesitic composition)
emit both viscous lava flows and tephra.emit both viscous lava flows and tephra.
The emissions tend to alternate, formingThe emissions tend to alternate, forming
alternating strata of lava and tephra,alternating strata of lava and tephra,
building a stratovolcano.building a stratovolcano.
Stratovolcanoes are:Stratovolcanoes are:
– Large.Large.
– Conical.Conical.
– Steep-sided.Steep-sided.
41. Statovolcanoes (2)Statovolcanoes (2)
Near the summit, a stratovolcano’s slopeNear the summit, a stratovolcano’s slope
may reach 40may reach 40oo
..
Toward the base, the slope flattens to aboutToward the base, the slope flattens to about
66oo
toto1010oo
..
As a stratovolcano develops, lava flows act asAs a stratovolcano develops, lava flows act as
a cap to slow erosion of the loose tephra.a cap to slow erosion of the loose tephra.
42. Statovolcanoes (3)Statovolcanoes (3)
The volcano becomes much larger andThe volcano becomes much larger and
steeper than a typical tephra cone.steeper than a typical tephra cone.
Mount Fuji (Japan), Mount Rainier, MountMount Fuji (Japan), Mount Rainier, Mount
Baker in Washington State, Mount Hood inBaker in Washington State, Mount Hood in
Oregon, Mt Mayon in the Philippines areOregon, Mt Mayon in the Philippines are
stratovolcanoes.stratovolcanoes.
43. Other Features of CentralOther Features of Central
Eruptions (1)Eruptions (1)
Craters:Craters:
– Funnel-shaped depressions with steep-sidedFunnel-shaped depressions with steep-sided
walls that open upward.walls that open upward.
– Craters form in two ways:Craters form in two ways:
By the collapse of the steep sides of the vent.By the collapse of the steep sides of the vent.
By an explosive eruption.By an explosive eruption.
– In subsequent eruptions, pressure blasts openIn subsequent eruptions, pressure blasts open
the vent, removing both the solidified magmathe vent, removing both the solidified magma
from the previous eruption and part of thefrom the previous eruption and part of the
crater wall.crater wall.
– A crater can grow slowly larger, eruption byA crater can grow slowly larger, eruption by
44. Other Features of CentralOther Features of Central
Eruptions (2)Eruptions (2)
Lava domes:Lava domes:
– If the magma is very viscous (as in a rhyolitic orIf the magma is very viscous (as in a rhyolitic or
andesitic magma), it squeezes out to form a lavaandesitic magma), it squeezes out to form a lava
dome.dome.
46. Other Features of CentralOther Features of Central
Eruptions (3)Eruptions (3)
Calderas:Calderas:
– CalderaCaldera is from the Spanish word for cauldron.is from the Spanish word for cauldron.
– A roughly circular, steep-walled basin about aA roughly circular, steep-walled basin about a
kilometer in diameter or larger.kilometer in diameter or larger.
– Calderas are created by collapse of the surfaceCalderas are created by collapse of the surface
rock following an eruption and partial emptyingrock following an eruption and partial emptying
of the underlying magma chamber.of the underlying magma chamber.
– Crater lake in Oregon occupies a circularCrater lake in Oregon occupies a circular
caldera 8 km in diameter.caldera 8 km in diameter.
48. Other Features of CentralOther Features of Central
Eruptions (4)Eruptions (4)
Resurgent domes:Resurgent domes:
– Often, more magma enters the chamber and liftsOften, more magma enters the chamber and lifts
the collapsed caldera floor to form a resurgentthe collapsed caldera floor to form a resurgent
dome.dome.
Diatremes:Diatremes:
– Volcanic pipes filled with a rubbles of brokenVolcanic pipes filled with a rubbles of broken
rock.rock.
– The walls are vertical, or very nearly so.The walls are vertical, or very nearly so.
– A famous diatreme is the diamond mine inA famous diatreme is the diamond mine in
Kimberly, South Africa.Kimberly, South Africa.
49. Fissure Eruptions (1)Fissure Eruptions (1)
Fissure eruptions extrude lava along anFissure eruptions extrude lava along an
elongate fracture in the crust.elongate fracture in the crust.
– When fissure eruptions occur on land, the low-When fissure eruptions occur on land, the low-
viscosity basaltic lava tends to spread widely andviscosity basaltic lava tends to spread widely and
to create flat lava plains.to create flat lava plains.
Such lavas are calledSuch lavas are called plateau basalts.plateau basalts.
51. Fissure Eruptions (2)Fissure Eruptions (2)
The Laki eruption, in Iceland in1783, occurredThe Laki eruption, in Iceland in1783, occurred
along a 32 km long fracture. Lava from italong a 32 km long fracture. Lava from it
flowed 64 km from one side of the fractureflowed 64 km from one side of the fracture
and nearly 48 km from the other, coveringand nearly 48 km from the other, covering
588 km588 km22
..
– The Laki eruption is the largest lava flow of anyThe Laki eruption is the largest lava flow of any
kind in historic times.kind in historic times.
– Famine followed and more than 9000 died (20Famine followed and more than 9000 died (20
percent of the Icelandic population).percent of the Icelandic population).
52. Fissure Eruptions (3)Fissure Eruptions (3)
Pillow basalts:Pillow basalts:
– When the basaltic magma erupts under theWhen the basaltic magma erupts under the
ocean, seawater cools it so rapidly that pillow-ocean, seawater cools it so rapidly that pillow-
shaped masses of basalt, ranging from a fewshaped masses of basalt, ranging from a few
centimeters to a meter or more in greatestcentimeters to a meter or more in greatest
dimension form.dimension form.
Fissure eruptions of andesitic or rhyoliticFissure eruptions of andesitic or rhyolitic
magma are much less common than fissuremagma are much less common than fissure
eruptions of basaltic lava.eruptions of basaltic lava.
55. Fissure Eruptions (4)Fissure Eruptions (4)
Sometimes the pyroclasts in the tephra areSometimes the pyroclasts in the tephra are
so hot that the fragments form welded tuff.so hot that the fragments form welded tuff.
Some 40 to 50 million years ago, huge ash-Some 40 to 50 million years ago, huge ash-
flow eruptions happened in Nevada.flow eruptions happened in Nevada.
– The erupted product covered an area in excess ofThe erupted product covered an area in excess of
200,000 km200,000 km22
..
56. Posteruption effectsPosteruption effects
When active volcanism finally ceases, rockWhen active volcanism finally ceases, rock
in and near an old magma chamber mayin and near an old magma chamber may
remain hot for hundreds of thousands ofremain hot for hundreds of thousands of
years.years.
Thermal spring at many volcanic sites (Italy,Thermal spring at many volcanic sites (Italy,
Japan, and New Zealand) have becomeJapan, and New Zealand) have become
famous health spas and sources of energy.famous health spas and sources of energy.
– A thermal spring that intermittently eruptsA thermal spring that intermittently erupts
water and steam is awater and steam is a geyser.geyser.
Most of the world’s geysers outside Iceland are inMost of the world’s geysers outside Iceland are in
New Zealand and in Yellowstone National Park.New Zealand and in Yellowstone National Park.
59. Volcanic Hazards (1)Volcanic Hazards (1)
Volcanic eruptions are not rare on land, andVolcanic eruptions are not rare on land, and
are essentially continuous on the seafloor.are essentially continuous on the seafloor.
Every year about 50 volcanoes erupt on theEvery year about 50 volcanoes erupt on the
Earth’s continents.Earth’s continents.
Most eruptions are basaltic.Most eruptions are basaltic.
Tephra eruptions from andesitic or rhyoliticTephra eruptions from andesitic or rhyolitic
stratovolcanoes like Mount St. Helens andstratovolcanoes like Mount St. Helens and
Krakatau can be disastrous.Krakatau can be disastrous.
60. Volcanic Hazards (2)Volcanic Hazards (2)
Eruptions present five kinds of hazards:Eruptions present five kinds of hazards:
– Hot, rapidly moving pyroclastic flows andHot, rapidly moving pyroclastic flows and
laterally directed blasts can overwhelm peoplelaterally directed blasts can overwhelm people
before they can evacuate.before they can evacuate.
Mont Pelee in 1902 and Mount St. Helens in 1980.Mont Pelee in 1902 and Mount St. Helens in 1980.
– Tephra and hot poisonous gases can bury orTephra and hot poisonous gases can bury or
suffocate people.suffocate people.
79 Mount Vesuvius in A.D. 79.79 Mount Vesuvius in A.D. 79.
61. Volcanic Hazards (3)Volcanic Hazards (3)
– Mudflows, calledMudflows, called lahars,lahars, can be devastating.can be devastating.
In 1985, the Colombian volcano Nevado del RuizIn 1985, the Colombian volcano Nevado del Ruiz
experienced a small, nonthreatening eruption. But,experienced a small, nonthreatening eruption. But,
when glaciers at the summit melted, massivewhen glaciers at the summit melted, massive
mudflows of volcanic debris moved swiftly down themudflows of volcanic debris moved swiftly down the
mountain , killing 20,000.mountain , killing 20,000.
– Violent undersea eruptions can cause powerfulViolent undersea eruptions can cause powerful
sea waves calledsea waves called tsunamis.tsunamis.
Krakatau, in 1883, killed more than 36,000 on JavaKrakatau, in 1883, killed more than 36,000 on Java
and nearby Indonesia islands.and nearby Indonesia islands.
– A tephra eruption can disrupt agriculture,A tephra eruption can disrupt agriculture,
creating a famine.creating a famine.