The document discusses different types of volcanoes and volcanic eruptions. It describes composite volcanoes which erupt violently due to sticky magma. Shield volcanoes form gentle slopes from runny lava. Cinder cones are small and formed from ejected fragments. Icelandic eruptions come from long fissures building lava plateaus. Hawaiian eruptions also come from fissures, forming shield volcanoes from fluid lava. Strombolian eruptions involve moderate bursts ejecting lava clots.
Story mode about volcanic eruption preparedness, Philippine setting
credits to Internet and book sources for information and data
Links are broken
(created for a group/school presentation)
Energy from Volcanoes ppt. is the next topic/ lesson from grade 9 LM Module 1 Quarter 3. The presentation is a discussion guide for teachers about geothermal energy and gives video suggestions in order for the students to understand the lesson well especially in showing how geothermal energy is harnessed. Feedbacks, reactions and suggestions are very much welcomed. Thanks!
All about Volcanoes (presented by Angel) .pptxSheluMayConde
All About Volcanoes
Volcanoes are remarkable geological structures formed by the eruption of molten rock, ash, and gases from the Earth's mantle. These natural phenomena can shape landscapes, create new landforms, and significantly impact both the environment and human societies. Understanding volcanoes involves exploring their types, formation processes, eruption mechanisms, and effects.
What is a Volcano?
A volcano is an opening in the Earth's crust through which magma, gases, and ash are expelled. When magma reaches the surface, it is called lava. Over time, repeated eruptions can build up a mountain or other landform around the volcanic vent.
Types of Volcanoes:
Shield Volcanoes:
Characteristics: Broad, gently sloping sides formed by the flow of low-viscosity basaltic lava that can travel long distances.
Examples: Mauna Loa and Kilauea in Hawaii.
Composite Volcanoes (Stratovolcanoes):
Characteristics: Steep, conical volcanoes made up of alternating layers of lava, ash, and volcanic debris. They are known for their explosive eruptions.
Examples: Mount Fuji in Japan, Mount St. Helens in the USA, and Mount Vesuvius in Italy.
Cinder Cone Volcanoes:
Characteristics: Small, steep-sided cones built from volcanic fragments such as ash, tephra, and volcanic rocks ejected during eruptions.
Examples: Parícutin in Mexico and Sunset Crater in the USA.
Lava Domes:
Characteristics: Rounded, steep-sided mounds formed by the slow extrusion of viscous lava.
Examples: Mount St. Helens’ Lava Dome in the USA.
Volcanic Features:
Crater:
Description: A bowl-shaped depression at the summit of a volcano, typically formed by explosive eruptions.
Caldera:
Description: A large depression formed when a volcano's summit collapses or is blown away during a massive eruption.
Examples: Yellowstone Caldera in the USA.
Lava Flows:
Description: Streams of molten rock that pour from a volcanic vent and solidify as they cool.
Pyroclastic Flows:
Description: Fast-moving currents of hot gas and volcanic material that can travel down the sides of a volcano during explosive eruptions.
Volcanic Ash:
Description: Fine particles of pulverized rock and glass created during volcanic eruptions that can travel long distances.
Formation of Volcanoes:
Subduction Zones:
Description: Volcanoes often form at convergent plate boundaries where an oceanic plate subducts beneath a continental plate, leading to magma formation.
Examples: The Ring of Fire around the Pacific Ocean.
Rift Zones:
Description: Volcanoes can also form at divergent plate boundaries where tectonic plates are pulling apart, allowing magma to rise.
Examples: Mid-Atlantic Ridge and East African Rift.
Hotspots:
Description: Volcanic activity that occurs away from plate boundaries, caused by plumes of hot material rising from deep within the mantle.
Examples: Hawaiian Islands and Yellowstone.
Story mode about volcanic eruption preparedness, Philippine setting
credits to Internet and book sources for information and data
Links are broken
(created for a group/school presentation)
Energy from Volcanoes ppt. is the next topic/ lesson from grade 9 LM Module 1 Quarter 3. The presentation is a discussion guide for teachers about geothermal energy and gives video suggestions in order for the students to understand the lesson well especially in showing how geothermal energy is harnessed. Feedbacks, reactions and suggestions are very much welcomed. Thanks!
All about Volcanoes (presented by Angel) .pptxSheluMayConde
All About Volcanoes
Volcanoes are remarkable geological structures formed by the eruption of molten rock, ash, and gases from the Earth's mantle. These natural phenomena can shape landscapes, create new landforms, and significantly impact both the environment and human societies. Understanding volcanoes involves exploring their types, formation processes, eruption mechanisms, and effects.
What is a Volcano?
A volcano is an opening in the Earth's crust through which magma, gases, and ash are expelled. When magma reaches the surface, it is called lava. Over time, repeated eruptions can build up a mountain or other landform around the volcanic vent.
Types of Volcanoes:
Shield Volcanoes:
Characteristics: Broad, gently sloping sides formed by the flow of low-viscosity basaltic lava that can travel long distances.
Examples: Mauna Loa and Kilauea in Hawaii.
Composite Volcanoes (Stratovolcanoes):
Characteristics: Steep, conical volcanoes made up of alternating layers of lava, ash, and volcanic debris. They are known for their explosive eruptions.
Examples: Mount Fuji in Japan, Mount St. Helens in the USA, and Mount Vesuvius in Italy.
Cinder Cone Volcanoes:
Characteristics: Small, steep-sided cones built from volcanic fragments such as ash, tephra, and volcanic rocks ejected during eruptions.
Examples: Parícutin in Mexico and Sunset Crater in the USA.
Lava Domes:
Characteristics: Rounded, steep-sided mounds formed by the slow extrusion of viscous lava.
Examples: Mount St. Helens’ Lava Dome in the USA.
Volcanic Features:
Crater:
Description: A bowl-shaped depression at the summit of a volcano, typically formed by explosive eruptions.
Caldera:
Description: A large depression formed when a volcano's summit collapses or is blown away during a massive eruption.
Examples: Yellowstone Caldera in the USA.
Lava Flows:
Description: Streams of molten rock that pour from a volcanic vent and solidify as they cool.
Pyroclastic Flows:
Description: Fast-moving currents of hot gas and volcanic material that can travel down the sides of a volcano during explosive eruptions.
Volcanic Ash:
Description: Fine particles of pulverized rock and glass created during volcanic eruptions that can travel long distances.
Formation of Volcanoes:
Subduction Zones:
Description: Volcanoes often form at convergent plate boundaries where an oceanic plate subducts beneath a continental plate, leading to magma formation.
Examples: The Ring of Fire around the Pacific Ocean.
Rift Zones:
Description: Volcanoes can also form at divergent plate boundaries where tectonic plates are pulling apart, allowing magma to rise.
Examples: Mid-Atlantic Ridge and East African Rift.
Hotspots:
Description: Volcanic activity that occurs away from plate boundaries, caused by plumes of hot material rising from deep within the mantle.
Examples: Hawaiian Islands and Yellowstone.
GEOGRAPHY YEAR 10: VOLCANIC ACTIVITY. What is a volcano? Where volcanoes take place? Where do they form? Creating a new volcano. Types of volcanoes. Cone-shape volcanoes. Shield volcanoes.
Earth is the third planet from the Sun and the only object in the Universe known to harbor life. According to radiometric dating and other sources of evidence, Earth formed over 4 billion years ago.[24][25][26] Earth's gravity interacts with other objects in space, especially the Sun and the Moon, Earth's only natural satellite. Earth revolves around the Sun in 365.26 days, a period known as an Earth year. During this time, Earth rotates about its axis about 366.26 times.[n 5]
Earth's axis of rotation is tilted, producing seasonal variations on the planet's surface.[27] The gravitational interaction between the Earth and Moon causes ocean tides, stabilizes the Earth's orientation on its axis, and gradually slows its rotation.[28] Earth is the densest planet in the Solar System and the largest of the four terrestrial planets.
Earth's lithosphere is divided into several rigid tectonic plates that migrate across the surface over periods of many millions of years. About 71% of Earth's surface is covered with water, mostly by oceans.[29] The remaining 29% is land consisting of continents and islands that together have many lakes, rivers and other sources of water that contribute to the hydrosphere. The majority of Earth's polar regions are covered in ice, including the Antarctic ice sheet and the sea ice of the Arctic ice pack. Earth's interior remains active with a solid iron inner core, a liquid outer core that generates the Earth's magnetic field, and a convecting mantle that drives plate tectonics.
Within the first billion years of Earth's history, life appeared in the oceans and began to affect the Earth's atmosphere and surface, leading to the proliferation of aerobic and anaerobic organisms. Some geological evidence indicates that life may have arisen as much as 4.1 billion years ago. Since then, the combination of Earth's distance from the Sun, physical properties, and geological history have allowed life to evolve and thrive.[30][31] In the history of the Earth, biodiversity has gone through long periods of expansion, occasionally punctuated by mass extinction events. Over 99% of all species[32] that ever lived on Earth are extinct.[33][34] Estimates of the number of species on Earth today vary widely;[35][36][37] most species have not been described.[38] Over 7.4 billion humans live on Earth and depend on its biosphere and natural resources for their survival. Humans have developed diverse societies and cultures; politically, the world has about 200 sovereign states.
what are Volcanism and volcano,
Distribution of Volcanoes
Kinds of Volcanoes
Types of Volcanic Hazards
Preparing for Volcanic Emergencies
A volcano is generally a conical shaped hill or mountain built by accumulations of lava flows, tephra, and volcanic ash. About 95% of active volcanoes occur at the plate subduction zones and at the mid-oceanic ridges. The other 5% occur in areas associated with lithospheric hot spots. These hot spots have no direct relationships with areas of crustal creation or subduction zones. It is believed that hot spots are caused by plumes of rising magma that have their origin within the asthenosphere.
Over the last 2 million years, volcanoes have been depositing lava, tephra, and ash in particular areas of the globe. These areas occur at hot spots, rift zones, and along plate boundaries where tectonic subduction is taking place within the asthenosphere.
The most prevalent kinds of volcanoes on the Earth's surface are the kind which form the "Pacific Rim of Fire". Those are volcanoes which form as a result of subduction of the nearby lithosphere.
Slide 1: Title Slide
Extrachromosomal Inheritance
Slide 2: Introduction to Extrachromosomal Inheritance
Definition: Extrachromosomal inheritance refers to the transmission of genetic material that is not found within the nucleus.
Key Components: Involves genes located in mitochondria, chloroplasts, and plasmids.
Slide 3: Mitochondrial Inheritance
Mitochondria: Organelles responsible for energy production.
Mitochondrial DNA (mtDNA): Circular DNA molecule found in mitochondria.
Inheritance Pattern: Maternally inherited, meaning it is passed from mothers to all their offspring.
Diseases: Examples include Leber’s hereditary optic neuropathy (LHON) and mitochondrial myopathy.
Slide 4: Chloroplast Inheritance
Chloroplasts: Organelles responsible for photosynthesis in plants.
Chloroplast DNA (cpDNA): Circular DNA molecule found in chloroplasts.
Inheritance Pattern: Often maternally inherited in most plants, but can vary in some species.
Examples: Variegation in plants, where leaf color patterns are determined by chloroplast DNA.
Slide 5: Plasmid Inheritance
Plasmids: Small, circular DNA molecules found in bacteria and some eukaryotes.
Features: Can carry antibiotic resistance genes and can be transferred between cells through processes like conjugation.
Significance: Important in biotechnology for gene cloning and genetic engineering.
Slide 6: Mechanisms of Extrachromosomal Inheritance
Non-Mendelian Patterns: Do not follow Mendel’s laws of inheritance.
Cytoplasmic Segregation: During cell division, organelles like mitochondria and chloroplasts are randomly distributed to daughter cells.
Heteroplasmy: Presence of more than one type of organellar genome within a cell, leading to variation in expression.
Slide 7: Examples of Extrachromosomal Inheritance
Four O’clock Plant (Mirabilis jalapa): Shows variegated leaves due to different cpDNA in leaf cells.
Petite Mutants in Yeast: Result from mutations in mitochondrial DNA affecting respiration.
Slide 8: Importance of Extrachromosomal Inheritance
Evolution: Provides insight into the evolution of eukaryotic cells.
Medicine: Understanding mitochondrial inheritance helps in diagnosing and treating mitochondrial diseases.
Agriculture: Chloroplast inheritance can be used in plant breeding and genetic modification.
Slide 9: Recent Research and Advances
Gene Editing: Techniques like CRISPR-Cas9 are being used to edit mitochondrial and chloroplast DNA.
Therapies: Development of mitochondrial replacement therapy (MRT) for preventing mitochondrial diseases.
Slide 10: Conclusion
Summary: Extrachromosomal inheritance involves the transmission of genetic material outside the nucleus and plays a crucial role in genetics, medicine, and biotechnology.
Future Directions: Continued research and technological advancements hold promise for new treatments and applications.
Slide 11: Questions and Discussion
Invite Audience: Open the floor for any questions or further discussion on the topic.
Richard's aventures in two entangled wonderlandsRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Seminar of U.V. Spectroscopy by SAMIR PANDASAMIR PANDA
Spectroscopy is a branch of science dealing the study of interaction of electromagnetic radiation with matter.
Ultraviolet-visible spectroscopy refers to absorption spectroscopy or reflect spectroscopy in the UV-VIS spectral region.
Ultraviolet-visible spectroscopy is an analytical method that can measure the amount of light received by the analyte.
Richard's entangled aventures in wonderlandRichard Gill
Since the loophole-free Bell experiments of 2020 and the Nobel prizes in physics of 2022, critics of Bell's work have retreated to the fortress of super-determinism. Now, super-determinism is a derogatory word - it just means "determinism". Palmer, Hance and Hossenfelder argue that quantum mechanics and determinism are not incompatible, using a sophisticated mathematical construction based on a subtle thinning of allowed states and measurements in quantum mechanics, such that what is left appears to make Bell's argument fail, without altering the empirical predictions of quantum mechanics. I think however that it is a smoke screen, and the slogan "lost in math" comes to my mind. I will discuss some other recent disproofs of Bell's theorem using the language of causality based on causal graphs. Causal thinking is also central to law and justice. I will mention surprising connections to my work on serial killer nurse cases, in particular the Dutch case of Lucia de Berk and the current UK case of Lucy Letby.
Nutraceutical market, scope and growth: Herbal drug technologyLokesh Patil
As consumer awareness of health and wellness rises, the nutraceutical market—which includes goods like functional meals, drinks, and dietary supplements that provide health advantages beyond basic nutrition—is growing significantly. As healthcare expenses rise, the population ages, and people want natural and preventative health solutions more and more, this industry is increasing quickly. Further driving market expansion are product formulation innovations and the use of cutting-edge technology for customized nutrition. With its worldwide reach, the nutraceutical industry is expected to keep growing and provide significant chances for research and investment in a number of categories, including vitamins, minerals, probiotics, and herbal supplements.
Introduction:
RNA interference (RNAi) or Post-Transcriptional Gene Silencing (PTGS) is an important biological process for modulating eukaryotic gene expression.
It is highly conserved process of posttranscriptional gene silencing by which double stranded RNA (dsRNA) causes sequence-specific degradation of mRNA sequences.
dsRNA-induced gene silencing (RNAi) is reported in a wide range of eukaryotes ranging from worms, insects, mammals and plants.
This process mediates resistance to both endogenous parasitic and exogenous pathogenic nucleic acids, and regulates the expression of protein-coding genes.
What are small ncRNAs?
micro RNA (miRNA)
short interfering RNA (siRNA)
Properties of small non-coding RNA:
Involved in silencing mRNA transcripts.
Called “small” because they are usually only about 21-24 nucleotides long.
Synthesized by first cutting up longer precursor sequences (like the 61nt one that Lee discovered).
Silence an mRNA by base pairing with some sequence on the mRNA.
Discovery of siRNA?
The first small RNA:
In 1993 Rosalind Lee (Victor Ambros lab) was studying a non- coding gene in C. elegans, lin-4, that was involved in silencing of another gene, lin-14, at the appropriate time in the
development of the worm C. elegans.
Two small transcripts of lin-4 (22nt and 61nt) were found to be complementary to a sequence in the 3' UTR of lin-14.
Because lin-4 encoded no protein, she deduced that it must be these transcripts that are causing the silencing by RNA-RNA interactions.
Types of RNAi ( non coding RNA)
MiRNA
Length (23-25 nt)
Trans acting
Binds with target MRNA in mismatch
Translation inhibition
Si RNA
Length 21 nt.
Cis acting
Bind with target Mrna in perfect complementary sequence
Piwi-RNA
Length ; 25 to 36 nt.
Expressed in Germ Cells
Regulates trnasposomes activity
MECHANISM OF RNAI:
First the double-stranded RNA teams up with a protein complex named Dicer, which cuts the long RNA into short pieces.
Then another protein complex called RISC (RNA-induced silencing complex) discards one of the two RNA strands.
The RISC-docked, single-stranded RNA then pairs with the homologous mRNA and destroys it.
THE RISC COMPLEX:
RISC is large(>500kD) RNA multi- protein Binding complex which triggers MRNA degradation in response to MRNA
Unwinding of double stranded Si RNA by ATP independent Helicase
Active component of RISC is Ago proteins( ENDONUCLEASE) which cleave target MRNA.
DICER: endonuclease (RNase Family III)
Argonaute: Central Component of the RNA-Induced Silencing Complex (RISC)
One strand of the dsRNA produced by Dicer is retained in the RISC complex in association with Argonaute
ARGONAUTE PROTEIN :
1.PAZ(PIWI/Argonaute/ Zwille)- Recognition of target MRNA
2.PIWI (p-element induced wimpy Testis)- breaks Phosphodiester bond of mRNA.)RNAse H activity.
MiRNA:
The Double-stranded RNAs are naturally produced in eukaryotic cells during development, and they have a key role in regulating gene expression .
The increased availability of biomedical data, particularly in the public domain, offers the opportunity to better understand human health and to develop effective therapeutics for a wide range of unmet medical needs. However, data scientists remain stymied by the fact that data remain hard to find and to productively reuse because data and their metadata i) are wholly inaccessible, ii) are in non-standard or incompatible representations, iii) do not conform to community standards, and iv) have unclear or highly restricted terms and conditions that preclude legitimate reuse. These limitations require a rethink on data can be made machine and AI-ready - the key motivation behind the FAIR Guiding Principles. Concurrently, while recent efforts have explored the use of deep learning to fuse disparate data into predictive models for a wide range of biomedical applications, these models often fail even when the correct answer is already known, and fail to explain individual predictions in terms that data scientists can appreciate. These limitations suggest that new methods to produce practical artificial intelligence are still needed.
In this talk, I will discuss our work in (1) building an integrative knowledge infrastructure to prepare FAIR and "AI-ready" data and services along with (2) neurosymbolic AI methods to improve the quality of predictions and to generate plausible explanations. Attention is given to standards, platforms, and methods to wrangle knowledge into simple, but effective semantic and latent representations, and to make these available into standards-compliant and discoverable interfaces that can be used in model building, validation, and explanation. Our work, and those of others in the field, creates a baseline for building trustworthy and easy to deploy AI models in biomedicine.
Bio
Dr. Michel Dumontier is the Distinguished Professor of Data Science at Maastricht University, founder and executive director of the Institute of Data Science, and co-founder of the FAIR (Findable, Accessible, Interoperable and Reusable) data principles. His research explores socio-technological approaches for responsible discovery science, which includes collaborative multi-modal knowledge graphs, privacy-preserving distributed data mining, and AI methods for drug discovery and personalized medicine. His work is supported through the Dutch National Research Agenda, the Netherlands Organisation for Scientific Research, Horizon Europe, the European Open Science Cloud, the US National Institutes of Health, and a Marie-Curie Innovative Training Network. He is the editor-in-chief for the journal Data Science and is internationally recognized for his contributions in bioinformatics, biomedical informatics, and semantic technologies including ontologies and linked data.
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- Geothermal Energy
- What is Geothermal
Energy?
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Steps to followed to generate electricity in a
geothermal power plant:
1. Wells are drilled deep into the earth to pump steam
or hot water to the surface.
2. When water reaches the surface, the drop in
pressure causes the water to turn into steam.
3. The steam spins a turbine, which is connected to a
generator that produces electricity.
4. Cooling tower cools the steam which it condenses
back to water.
5. The cooled water is pumped back into the earth to
begin the process again.
4. Have you ever thought about why volcanoes are actually called
'volcanoes'? Can you think of a reason why?
How do volcanic eruptions affect society?
5. What to Do Before, During, and After a
Volcanic Eruption?
6. Roman mythology says that Vulcan lived in a volcano. As well as being
the god of fire, he made many weapons and forged them using metal
and fire. He was a very skilled blacksmith.
The Roman God of Fire
Romans believed that if
Vulcan was made angry, the
volcano would erupt. So they
tried their best to please him
and not anger him.
Click on the word in bold to
find out what it means!
Forged: to have made or
shaped a metal object using
a fire or furnace.
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- According to Norse mythology, Loki, is the epitome
of both aspects of fire: the merry but potentially
dangerous hearth fire and the destructive fire of
forest and volcano. Because of his lies and
deceitful acts, he was punished by the gods and
goddesses by putting him into a dark cave.
- In Iceland, it was believed that the earthquakes
happens when Loki writhed with pain and terror
causing the earth to quake and tremble.
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- Pacific Northwest Indians regarded Mount Hood
and Mount Adams as warrior gods fighting over
Mount St. Helens, the prettiest ang youngest
volcano goddess.
- In Hawaii, eruptions are under the control of
Madame Pele. According to the legend, Pele and
her sister created the Hawaiian island chain by
tearing up the ocean floor. Native believe that Pele
dictates when and where eruption will happen.
When Kilauea began its eruption in the 1970s,
villagers hired an airplane and dropped flowers and
a bottle og gin into the lava vent to please Pele.
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- Christians explained volcanoes as
manipulations of Satan or manifestation of
the wrath of God. They believed that
miracles must take place; thus, parades of
several relics such as that of St. Agatha’s
along Mt. Catania and St. Januarius in Mt.
Vesuvius in Naples, Italy were initiated.
10. What Is Our Earth Made Of?
Click on the circles to reveal the information.
+
The Crust
This is the outer layer of the
earth. It varies in thickness
from 0 – 60km thick. It is
not even and is made up of
pieces which overlap to
cover the entire planet.
These pieces are called
‘tectonic plates’.
×
+
+
+
×
The Inner Core
This is a solid layer and is made of
iron and nickel. It is the hottest
part of the earth and can reach
temperatures of up to 5500ºC!
The Outer Core
The outer core is a liquid layer
made out of molten iron and
nickel. This liquid metal creates the
earth's magnetic field.
×
The Mantle
The mantle is approximately
2897km thick and is made of a
solid, rocky substance called
molten rock or magma. This is
what escapes when a volcano
erupts.
×
11. Where Are Most Volcanoes Located?
The ‘Ring of Fire’
is an area of the
Pacific Ocean that
is shaped like a
horseshoe. It is
home to 90% of
the world's
earthquakes and
75% of the
world's volcanoes.
It contains a string
of 452 volcanoes,
which stretches
from the southern
tip of South
America, up along
the coast of North
America, down
through Japan, and
into New Zealand.
12. How Are Volcanoes Formed?
Deep in the earth, it is extremely hot. It is so hot, in fact, that rocks
actually melt and form magma, which makes up the mantle of the earth.
The upper mantle mixes and moves,
which creates pressure underneath
the crust. This pressure can
sometimes cause the mantle
to leak out onto the
surface of the earth
– this is a
volcano!
Over time, as this magma leaks out,
the volcano will get bigger
and bigger.
13. The Three Stages of Volcanoes
Scientists have placed volcanoes in to three different categories.
What do you think each one is?
Active
Dormant
Extinct
An active volcano is one that has erupted recently, and there is the
possibility that it may erupt again.
A dormant volcano is one that has not erupted for a long time, however,
it may still erupt in the future.
An extinct volcano is one which has erupted
thousands of years ago, but it will
probably never erupt again.
14. Why Do Volcanoes Erupt?
We know that the earth's crust is made up of huge slabs called tectonic
plates. These fit together like a jigsaw puzzle and they sometimes move.
The movement causes friction
which causes earthquakes and
volcanic eruptions near the
edges of the plates. The theory
that explains this process is
called ‘plate tectonics’ – this
means the plates are moving in
different directions and at
different speeds. Sometimes
they collide or brush past each
other and cause these
earthquakes and volcanic
eruptions.
Click on the word in bold to
find out what it means!
Friction: the resistance created
when one surface rubs
against another.
15. What Are the Different Parts of a Volcano?
Click on each label to find out more. Click again to remove.
An opening in the
surface of the Earth
through which volcanic
materials, such as
magma, can escape.
A cloud of ash. It is
formed by volcanic
explosions
vent ash cloud
The mouth of a volcano.
It surrounds the vent.
crater
throat
The entrance of a
volcano. It ejects lava
and volcanic ash.
conduit
An underground
passage which magma
travels through.
A large underground
pool of liquid rock found
beneath the surface of
the Earth.
magma reservoir
16. How Many Volcanoes Are There?
There are more than 1500 active volcanoes on Earth. There are also
more than 80 volcanoes under the ocean, although these are just the
ones that have been discovered.
17. What Types of Volcano Are There?
Composite Volcanoes
These volcanoes are steep-sided volcanoes and are made up of lots of
layers of volcanic rocks. They usually erupt in an explosive way because
the magma in these volcanoes is quite sticky. It clogs up the passage
that it has to pass through. Pressure is built inside the volcanic chamber
and this results in the volcano erupting violently.
Mount St. Helens in Washington, USA is a composite volcano.
18. What Types of Volcano Are There?
Cinder Cones
Cinder cones are circular or oval cones. They are made up of small
fragments of lava, which are blown into the air through a single vent.
When they cool down, they form rock around the vent. They grow
quickly, but are not usually very big. They are not usually
dangerous either.
Sunset Crater in Arizona, USA is a cinder cone.
19. What Types of Volcano Are There?
Shield Volcanoes
Shield volcanoes are bowl or shield-shaped in the middle. When they
erupt, the lava is quite runny and it travels long distances down the side
of the volcano before it cools down. This lava forms long, gentle slopes
that look like a warrior's shield, which is how they got their name.
These volcanoes do not often explode.
Shield Volcanoes like this one in Hawaii are common in this part of the world.
20. OTHER ASSOCIATED VOLCANO LANDFORMS
A volcanic dome, also called lava dome, is a rounded, steep-sided
mound that is formed by small, bulging masses of lava primarily
composed of either dacite or rhyolite. Lava coming from a dome is too
viscous to flow from the vent, hence, lava piles over and around the vent
until it cools down and solidifies. A dome grows mainly by expansion
from within. It usually occurs within the craters or on the flanks of
large composite volcanoes.
21. As termed, super volcanoes are described to produce the largest eruptions
on Earth. The term super volcano implies a volcanic center that has
recorded an eruption with a magnitude of 8 on the Volcano Explosivity
Index (EVI), meaning a single volcano of this type can eject magma and
other materials up to a volume greater than 1,000 𝑘𝑚3 (240 𝑚𝑖3). The VEI
scale was created by Christopher G. Newhall of the United States
Geological Survey and Stephen Self at the University of Hawaii in 1982 to
provide general measurements of explosiveness of volcanic eruptions.
22. Submarine Volcano
This type of volcano is created when magma erupts in the underwater
fissures of the earth. Majority of these volcanoes are found near ocean
ridges while some can exist in shallow water. Submarine volcanoes in
shallow water can eject basaltic magma and the lava formed is known as
“pillow lava”.
23. Subglacial volcano, also called glaciovolcano, is created by eruptions
beneath the surface of a glacier or sheets which is then melted into a lake
by the rising lava that resembles to the pillow lava formed by submarine
volcanoes. As the pillow lava is ejected upward, it melts the overlying ice
while the water cools the lava flows down.
24. Volcanic Eruption
•ICELANDIC TYPE is characterized by effusions of molten basaltic lava
that flows from long parallel fissures, and the outpourings often build
lava plateaus.
25. Volcanic Eruption
•HAWAIIAN TYPE is similar to the Icelandic variety but in this case,
fluid lava flows from summit and radial fissures to form shield
volcanoes.
26. Volcanic Eruption
•STROMBOLIAN TYPE shows moderate bursts of expanding gases that
eject clots of incandescent lava in cyclical or nearly continuous small
eruptions. Because of such small intermittent outbursts, Stromboli
Volcano (off the west coast of Italy) has been called the “lighthouse of
the Mediterranean”.
27. Volcanic Eruption
•VULCANIAN TYPE named for the island of Volcano near Stromboli,
generally exhibits moderate explosions of gas laden with volcanic ash.
This mixture forms dark, turbulent eruption clouds that rapidly ascend
and expands in convoluted shapes.
28. Volcanic Eruption
•VESUVIAN TYPE is associated with explosive outbursts that generate
dense mixtures of hot volcanic fragments and gas. It is so named for the
destructive eruption of Mount Pele in Martinique in 1902.
29. Volcanic Eruption
•PLINIAN TYPE is an intensely violent kind of volcanic eruption
exemplified by the outburst of Mount Vesuvius in AD 79 that killed the
famous Roman scholar Pliny the elder, from whom the name is taken.
30. More Volcano Facts
What is the difference between
magma and lava?
Magma is liquid rock inside a
volcano. Lava is the name for
liquid rock that has flowed out of
a volcano. Lava takes a long time
to cool down as it is not a good
heat conductor. As a lava flow
cools down, it gets slower and
thicker.
What is a ‘pyroclastic flow’?
This is the most deadly of all
volcano activities.
It is a liquidised mixture of solid
and part-solid fragments and hot,
expanding gases.
They look like a snow avalanche
but are extremely hot and
contain poisonous gases. They
move at the speed of a hurricane.
Click on the word
in bold to find
out more!
Heat Conductor:
something which can
transfer heat from one
object to another.
31. What Is the Largest Active Volcano?
The largest, active volcano in the world is Mauna Loa in Hawaii. It is
13,677 feet above sea level. From its base below sea level to its summit,
Mauna Loa is taller than Mount Everest.
Mauna Loa
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Volcanoes of the World
Mount St Helens
Mount St Helens is an active
volcano located in
Washington, USA in the
Cascade Mountain Range.
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Click on the numbers to reveal the facts.
On 18th
May 1980, it erupted and
killed 57 people and destroyed
lots of roads and homes.
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5
3
This was the first time
pyroclastic flows (the clouds
of hot gas, ash and rock) were
studied using new scientific
techniques.
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4
Mount St Helens is still
active, and is monitored
closely by geologists to
predict if it will erupt again.
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An earthquake triggered a
landslide, which caused a
sideways blast, sending
clouds of ash, gas and rock
speeding away from the
volcano.
×
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1
Mount Vesuvius, Naples, Italy
Mount Vesuvius has a very
famous history. Its base is 30
miles wide and it is estimated
to be around 17,000 years old.
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Click on the numbers to reveal the facts.
In 79AD, Vesuvius erupted for a
whole day. Thousands of people
were killed, and the city of
Pompeii was buried.
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5
3
In 1995, Vesuvius was made a
National Park. Visitors can
climb the mountain.
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Vesuvius has erupted over 50
times in the last 200 years. The
last time was in 1944 during
the Second World War.
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Volcanoes of the World
Over the years, archaeologists
have found bodies preserved
by the ash from the volcano
along with other items, such
as heating stoves and cooking
utensils.
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34. 2
1
Mount Fuji, Japan
Mount Fuji is the highest
mountain in Japan. It is 3776m
high. It is on the island of Honshu,
about 100km from Tokyo.
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Click on the numbers to reveal the facts.
Over 100,000 people climb Mount
Fuji every year. It is the most
climbed mountain in the world.
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5
3
A forest named
Aokigahara lies at the
foot of the mountain and
is said to be haunted by
ghosts and goblins.
× 4
The volcano is actually
three separate volcanoes
piled one on top of the
other with Fuji at the top.
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Volcanoes of the World
Mount Fuji last erupted in
1708. It has become a symbol
of the country and is featured
in lots of paintings.
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1
Popocatépetl, Mexico
Until it erupted in 1994,
Popocatépetl was
dormant for 50 years.
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Click on the numbers to reveal the facts.
It is nicknamed 'El Popo'. It has
erupted several times since 1994.
×
4
It is considered one of the
world’s most dangerous
volcanoes. It last erupted in
January 2020.
×
3
Flights over Mexico have
been cancelled several times
due to ash and steam being
produced by the volcano.
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Volcanoes of the World
36. Are There Volcanoes on Other Planets?
Earth is not the only planet to have volcanoes, although most of the
volcanoes on other planets are now extinct.
Mercury used to
have volcanoes
but when the
planet's interior
cooled down,
the volcanoes
died.
Mars has the
largest known
volcano called
Olympus Mons.
It is no longer
active and will
probably never
erupt again.
Io is one of
Jupiter's moons
and has
several active
volcanoes.
Triton is
Neptune's
largest moon.
Instead of lava,
the volcanoes on
Triton actually
release ice.
37. Glossary
Forged: to have made or shaped a metal object using a fire or furnace.
Molten: something made in to a liquid by heat.
Magma: hot fluid or semi-fluid below the earth's crust.
Friction: the resistance created when one surface rubs against another.
Heat conductor: something which can transfer heat from one object to
another.
Archaeologist: someone who studies history using evidence from fossils
and artefacts.