Volcanoes form through two main processes: the convergence of tectonic plates and hot spots in the mantle. When plates converge, one plate subducts and melts, forming magma that rises to the surface and erupts, eventually building a volcano. Hot spots are areas of high heat in the mantle that melt rock below, causing volcanoes to form over hot spots as plates move. The viscosity of magma depends on its temperature and silica content, determining the type of volcano and eruption: more viscous magma with low heat and high silica becomes stuck and erupts explosively, while less viscous magma flows easily in gentle eruptions.
A brief explanation of what a volcano is, its parts, and how it erupts.
Link to Powerpoint presentation with animations:
https://1drv.ms/p/s!AqlgXtwNT9zAgihsvLpaBRIUmINw?e=ThXPlx
A brief explanation of what a volcano is, its parts, and how it erupts.
Link to Powerpoint presentation with animations:
https://1drv.ms/p/s!AqlgXtwNT9zAgihsvLpaBRIUmINw?e=ThXPlx
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.
1.new terms
2.What is a volcano?
3.How and why do volcanoes erupt?
4.Explosive Eruptions
5.Parts of Volcanoes
6. subduction
7.how are they formed
8.volcanic activity levels
9. types of volcanos
10.SHIELD VOLCANO
11. Mt. Kilauea
12.CINDER CONE VOLCANO
13.COMPOSITE VOLCANO
14.Volcanoes around the world
15.Multiple Eruption volcanoes
made by :RATIKA,Delhi,India
This is a PowerPoint Presentation about Magmatism, a lesson in Earth and Life Science, First quarter for Grade 11/12 Students. This will help them understand the lesson and make them familiar with the topic.
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.
1.new terms
2.What is a volcano?
3.How and why do volcanoes erupt?
4.Explosive Eruptions
5.Parts of Volcanoes
6. subduction
7.how are they formed
8.volcanic activity levels
9. types of volcanos
10.SHIELD VOLCANO
11. Mt. Kilauea
12.CINDER CONE VOLCANO
13.COMPOSITE VOLCANO
14.Volcanoes around the world
15.Multiple Eruption volcanoes
made by :RATIKA,Delhi,India
This is a PowerPoint Presentation about Magmatism, a lesson in Earth and Life Science, First quarter for Grade 11/12 Students. This will help them understand the lesson and make them familiar with the topic.
Grade 8 Integrated Science Chapter 15 Lesson 2 on volcanoes. This lesson goes into detail about volcanoes, plate boundaries, lava chemistry, eruption types, and volcano types. The purpose of this lesson is for students to understand where and why volcanoes form and what factors cause differing volcanic features.
The French Revolution, which began in 1789, was a period of radical social and political upheaval in France. It marked the decline of absolute monarchies, the rise of secular and democratic republics, and the eventual rise of Napoleon Bonaparte. This revolutionary period is crucial in understanding the transition from feudalism to modernity in Europe.
For more information, visit-www.vavaclasses.com
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
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Model Attribute Check Company Auto PropertyCeline George
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Embracing GenAI - A Strategic ImperativePeter Windle
Artificial Intelligence (AI) technologies such as Generative AI, Image Generators and Large Language Models have had a dramatic impact on teaching, learning and assessment over the past 18 months. The most immediate threat AI posed was to Academic Integrity with Higher Education Institutes (HEIs) focusing their efforts on combating the use of GenAI in assessment. Guidelines were developed for staff and students, policies put in place too. Innovative educators have forged paths in the use of Generative AI for teaching, learning and assessments leading to pockets of transformation springing up across HEIs, often with little or no top-down guidance, support or direction.
This Gasta posits a strategic approach to integrating AI into HEIs to prepare staff, students and the curriculum for an evolving world and workplace. We will highlight the advantages of working with these technologies beyond the realm of teaching, learning and assessment by considering prompt engineering skills, industry impact, curriculum changes, and the need for staff upskilling. In contrast, not engaging strategically with Generative AI poses risks, including falling behind peers, missed opportunities and failing to ensure our graduates remain employable. The rapid evolution of AI technologies necessitates a proactive and strategic approach if we are to remain relevant.
Read| The latest issue of The Challenger is here! We are thrilled to announce that our school paper has qualified for the NATIONAL SCHOOLS PRESS CONFERENCE (NSPC) 2024. Thank you for your unwavering support and trust. Dive into the stories that made us stand out!
Biological screening of herbal drugs: Introduction and Need for
Phyto-Pharmacological Screening, New Strategies for evaluating
Natural Products, In vitro evaluation techniques for Antioxidants, Antimicrobial and Anticancer drugs. In vivo evaluation techniques
for Anti-inflammatory, Antiulcer, Anticancer, Wound healing, Antidiabetic, Hepatoprotective, Cardio protective, Diuretics and
Antifertility, Toxicity studies as per OECD guidelines
2. Volcano History
The word volcano comes from
Vulcan, the Roman god of fire and
metalworking who “lived” under Mt.
Etna.
The Study of Volcanoes is
referred to as volcanology.
Volcano: A landform that
develops where lava, ash, and
gas erupt.
3. How do volcanoes Form?
There are two major ways volcanoes
form:
Convergence of Tectonic Plates
Hot Spots
4.
5. Convergence
When two tectonic plates collide:
1. There is subduction of a plate into the
asthenosphere.
2. The plate begins to melt rock, forming magma.
3. The hot, low density magma rises toward Earth’s
surface.
6. Convergence
When two tectonic plates collide:
4. Pressure pushing up on Earth’s crust
gets higher and higher.
5. Eventually, magma pushing up forms a
crack called a fissure.
6. Magma erupts through the fissure and
onto Earth’s surface.
7. Magma that is above Earth’s surface is
called lava.
After several eruptions, lava builds up and a
rocky hill, a volcano is formed.
7.
8.
9. Hot Spot
A hot spot can also form a volcano:
1. A hot spot is an area in the lower mantle that is really hot.
2. Since it is so hot, parts of the mantle melt and form magma.
3. Hot magma rises because it is less dense.
4. Pressure is put onto the surface of the Earth, forming a fissure.
5. A volcano is formed over many eruptions.
Examples: Hawaii, Yellowstone
Hot spots are normally found inside of plates, not at boundaries.
10. Hot Spot Example: Hawaii
1. Hawaii sits on the Pacific Plate, which is moving Northwest.
2. There is a hot spot under Hawaii causing magma to rise.
3. The hot spot is located in the mantle, and is not moving.
4. The plate moves over the hot spot, forming a line of volcanoes.
Which islands are the oldest, the northern or the southern islands?
11.
12. The type of volcano and how it erupts
depends on magma’s viscosity:
Thick / Viscous Magma
Honey or Molasses
Does not flow very easily.
Why is Magma Viscous?
Low temperatures
High Silica content
• Thin/ Non-Viscous
Magma
– Water
– Flows very easily.
• Why is Magma Non-
Viscous?
– High temperatures
– Low Silica content
VISCOSITY: How easily a liquid will flow
13. Why Silica?
The more Silica in magma, the thicker and more
viscous it is.
Silica tetrahedrons link together in long chains that
stop magma from flowing easily.
16. What about the Magma?
Magma with Silica content that is…
HIGH
Granitic Magma
Medium
Andesitic Magma
Low
Basaltic Magma
VISCOUS MAGMA
• Low Temperature
• High Silica
• Called Granitic Magma
Medium Viscous Magma
• Medium Temperature
• Medium Silica
• Called Andesitic Magma
Non-Viscous Magma
• High Temperature
• Low Silica
• Called Basaltic Magma
17. Why is Viscosity so important
anyway?
Thick and Viscous Magma
1. There are gasses in magma, such as Water Vapor and
CO2.
2. Gasses rise up toward Earth’s surface with the magma.
3. If the magma is thick, it does not flow up easily and
GETS STUCK!
4. Rising gasses also get stuck and can not escape.
5. The gasses build up pressure until they explosively erupt.
18.
19. Why is Viscosity so important
anyway?
Thin and Non-Viscous Magma
1. If the magma is thin, it flows up easily and
DOES NOT GET STUCK.
2. Rising gasses also flow up and can easily
escape.
3. Pressure does not build up and magma
gently erupts.
20. GENTLE
ERUPTION
MODERATELY
EXPLOSIVE ERUPTION
EXPLOSIVE
ERUPTION
Volcanoes
The type of volcano and how it erupts depends on…MAGMA’s
VISCOSITY.
VISCOUS MAGMA
• Low Temperature
• High Silica
• Called Granitic Magma
Medium Viscous Magma
• Medium Temperature
• Medium Silica
• Called Andesitic Magma
Non-Viscous Magma
• High Temperature
• Low Silica
• Called Basaltic Magma
21.
22. Volcanoes
You must know the following:
Type of Volcano
Temperature
Silica Content
Eruption Style