This document summarizes different types of volcanoes based on their activity, location, structure, and explosiveness. Volcanoes are classified as active, dormant, or extinct based on their recent eruptive history. Additional classifications include the volcano's shape as a shield cone, cinder cone, or composite/stratovolcano. Stratovocanoes are tall and cone-shaped volcanoes formed from layers of erupted materials. The document also provides examples of notable volcanoes that fit different classifications.
Volcanoes are openings in the earth's crust that allow magma, hot lava, volcanic ash, and gases to escape from below the surface. The earth's crust is broken into tectonic plates that move and occasionally cause pressure to build under the surface, resulting in volcanic eruptions when the pressure is released. There are three main types of volcanoes: composite volcanoes, shield volcanoes, and dome volcanoes, which erupt in different ways depending on the viscosity of the lava. Several active volcanoes in the Philippines are discussed, including Mayon Volcano, Taal Volcano, and Kanlaon Volcano. Volcanic eruptions can have both positive and negative environmental impacts
Volcanoes form when magma rises from below the Earth's crust and erupts onto the surface. There are three main types of volcanoes: shield volcanoes which have gentle slopes and non-explosive eruptions, composite volcanoes which have steep slopes and more explosive eruptions, and super volcanoes which have massive eruptions over 1,000 cubic km. Volcanic eruptions can have both positive impacts such as fertilizing soils and negative impacts like killing people and damaging property. Scientists monitor volcanoes using techniques like seismometers and tilt meters to predict eruptions.
Volcanoes form at locations where magma reaches the Earth's surface. There are three main types of volcanoes classified based on their composition and eruption style. Composite volcanoes like Mayon Volcano are tall and steep due to explosive eruptions of thick, andesitic magma. Shield volcanoes like those in Hawaii erupt basalt quietly as low-viscosity lava flows great distances. Cinder cones are small and formed from accumulated ejecta from Strombolian eruptions. A volcano's anatomy includes features like the vent, lava domes, and pyroclastic flows that can have hazardous impacts.
Volcanoes are formed when magma from the Earth's upper mantle works its way to the surface and erupts. They can erupt explosively, ejecting ash and rock fragments into the air, or effusively, oozing lava onto the surface. The largest active volcano is Mauna Loa in Hawaii. Major volcanic eruptions, like Krakatoa in 1883 and Mount Pelee in 1902, can have devastating impacts and cause loss of life. Plate tectonics and the movement of tectonic plates under the Earth's surface is a major factor in where volcanoes are located.
Volcanoes-Explosive-Wonders-of-the-Earth.pptxPRAMODA G
油
Volcanoes are among the most awe-inspiring and powerful natural phenomena on our planet. These geological marvels have shaped the Earth's surface for billions of years, creating breathtaking landscapes and influencing the course of human history. This presentation will delve into the fascinating world of volcanoes, exploring their formation, structure, and impact on both the environment and human civilization.
From the fiery depths of the Earth to the majestic peaks that pierce the sky, volcanoes represent a dynamic interplay between the planet's internal forces and its surface. As we embark on this journey through volcanic science, we will uncover the mysteries behind these explosive wonders and gain a deeper appreciation for their role in shaping our world.
Volcanoes are classified by their shape and size, which are determined by factors like the material ejected and type of eruptions. The main types are shield volcanoes, composite cones, and cinder cones. Shield volcanoes have broad, low profiles created by fluid basalt flows, while composite cones have alternating layers of lava and ash from explosive eruptions. Cinder cones are small and steep with loose cinder fragments. The document provides examples like Hawaii's shield volcanoes, Colombia's Nevado del Ruiz composite cone, and Mexico's Par鱈cutin cinder cone to illustrate each type.
1) Volcanoes form at boundaries where tectonic plates meet, such as where plates are subducting or spreading apart.
2) There are two main types of volcanoes - cone-shaped volcanoes which form from thick, slow-moving lava and shield volcanoes which have flatter slopes due to more fluid lava.
3) Examples of highly active volcanic regions include the Pacific Ring of Fire and areas around Alaska, Hawaii, and the Cascade Range in the western United 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.
There are three main types of volcanoes:
1) Cinder cones erupt small pieces of scoria and pyroclastics that build up around the vent to form cone-shaped hills. Examples include Par鱈cutin in Mexico and Sunset Crater in Arizona.
2) Stratovolcanoes are tall conical mountains composed of layered lava flows and ejecta. Examples include Mt. Fuji in Japan and Mount Vesuvius in Italy. Their explosive eruptions have posed great hazards.
3) Subglacial volcanoes form underneath ice sheets, leaving flat-topped mountains when the ice melts. Good examples are found in Iceland and British Columbia.
Earth Science 6.2 : Effects of Volcanic EruptionsChris Foltz
油
Volcanic eruptions can profoundly impact climate and the Earth's surface. Large eruptions eject ash and gases into the atmosphere, which can block sunlight and cause global temperatures to drop. There are three main types of volcanoes: shield volcanoes formed from nonexplosive eruptions creating gentle slopes; cinder cone volcanoes from moderately explosive eruptions forming steep slopes; and composite volcanoes from alternating explosive and lava flows creating broad bases that steepen toward their summits. In addition to volcanoes, other volcanic landforms include craters at volcano tops, calderas which are large depressions formed when the magma chamber empties, and lava plateaus resulting from nonexplosive eruptions
This document provides an overview of volcanoes and volcanic eruptions. It defines different types of volcanoes according to their shape, including stratovolcanoes, shield volcanoes, and cinder cone volcanoes. Examples of each type from the Philippines and around the world are given. The document also discusses types of volcanic eruptions from less to more violent, including Hawaiian, Strombolian, Vulcanian, Plinian, phreatic, and phreatomagmatic eruptions. Active volcanoes in the Philippines are listed.
Volcanoes form as magma rises from below the Earth's surface due to movement of tectonic plates. There are three main types of volcanoes - shield volcanoes which erupt fluid lava to form broad, low cones; cinder cone volcanoes which form steep slopes of pyroclastic fragments; and composite or stratovolcanoes which are tall cones built up of hardened lava and ash. Examples include Hawaii's shield volcanoes Kilauea and Mauna Loa, Mexico's Paricutin cinder cone volcano, and the Philippines' composite Mayon volcano. Volcanic eruptions can negatively impact human health through ash, gases and dust inhalation leading to respiratory and other illnesses.
A volcano is a mountain formed by erupted lava and ash from vents in the Earth's crust. It consists of a magma chamber, conduit, and vent. Volcanoes can have different features like rugged peaks or summit craters depending on how lava is emitted. Magma rises from underground chambers and erupts due to pressure or plate collisions. When magma reaches the surface it is called lava. Volcanoes are classified as active, dormant, or extinct based on recent eruption activity. Eruptions can endanger nearby populations through poisonous gases and have caused over 200,000 deaths in the last 500 years.
Volcanoes (GENEVEVE MAGPATOC & JORDAN ABRAHAM)magene
油
Volcanoes form at three main types of plate boundaries: divergent boundaries where plates split apart, convergent boundaries where one plate subducts beneath another, and at hotspots within plates. The type of boundary controls the composition of magma erupted - divergent boundaries produce basalt, convergent produce andesite, and hotspots can produce either depending on the plate composition. Major hazards from volcanoes include lava flows, explosive eruptions of ash and pyroclastic flows, lahars, and gas emissions. Large eruptions can impact global climate through atmospheric dust veiling sunlight. Volcanoes are monitored to determine activity levels and eruptions can be predicted based on increased seismicity, gas emissions,
Volcanoes
Volcanoes are geological formations that occur when magma, molten rock from beneath the Earth's crust, escapes to the surface. This can happen through cracks or vents in the Earth's crust. When magma reaches the surface, it is called lava. Volcanoes can be found both on land and beneath the ocean. There are several types of volcanoes, including shield volcanoes, stratovolcanoes, and cinder cone volcanoes, each characterized by their shape and eruption style. Volcanic eruptions can be explosive or effusive, producing various volcanic materials such as ash, pumice, and volcanic gases. The formation and activity of volcanoes are primarily driven by tectonic plate movements and the presence of hotspots.
Volcanoes form when magma rises up from below the Earth's surface and erupts through openings called vents. There are several types of volcanoes defined by their shape and eruption characteristics. Shield volcanoes have gentle slopes and erupt runny basalt lava, while composite volcanoes are steep-sided and erupt thicker, stickier magma in more explosive eruptions. Cinder cones erupt small fragments and form small, cone-shaped volcanoes. Lava domes form when thick lava piles up in mounds. Volcanoes are caused by the movement of tectonic plates, which can allow magma to rise up in between the plates. Geysers, which are hot springs
The document discusses different types of volcanoes and how they can change Earth's surface quickly. It describes cinder cone, shield cone, and composite cone volcanoes. Cinder cones are small and circular, forming from ejected cinders. Shield cones are large and shield-shaped, building up from lava flows. Composite cones like Mount St. Helens are steep-sided and cone-shaped, often erupting explosively due to trapped viscous magma. Volcanoes can quickly change Earth's surface through lava flows and explosive eruptions that spread rock and ash over wide areas.
The document discusses volcanoes and how they form. It explains that volcanoes form at subduction zones, where tectonic plates collide and one plate slides under another. This causes friction and melting within the Earth, and magma rises up through the crust. When it reaches the surface, it erupts as lava from a vent to form a volcano. Many volcanoes are located on the Pacific Ring of Fire, which is a horseshoe-shaped area in the Pacific Ocean known for seismic activity and volcanoes. Within this area are several subduction zones, including those responsible for the over 20 active volcanoes located in the Philippines.
1. Volcanoes are natural openings in the Earth's crust where molten rock and gases erupt.
2. The Philippines has many active volcanoes due to its location along the Pacific Ring of Fire. Some of the most notable active volcanoes include Taal Volcano, Mount Mayon, and Bulusan.
3. Volcanoes are classified based on their eruption history as either active or inactive, and by their shape as shield, cinder cone, or composite volcanoes.
Presentation of Group 2 - Topic Volcanoeshendrix18
油
A volcano is a rupture in a planet's crust that allows magma, ash, and gases to escape from underground. They form at tectonic plate boundaries and underwater, with about 1,500 potentially active worldwide. Volcanoes are classified as active, dormant, or extinct based on recent eruptions. The three main types are cinder cones made of pyroclastic debris, shield volcanoes built from fluid lava, and composite or stratovolcanoes with steep sides formed from viscous lava. The 1815 eruption of Mount Tambora in Indonesia was the largest in recorded history, killing over 10,000 and contributing to global climate changes and crop failures for years after.
Characteristics of different volcanoes and their typesManojSaini01
油
Volcanoes can be classified in several ways:
1) By frequency of eruption - active, dormant, or extinct
2) By shape and mode of eruption - shield, composite, caldera, cinder cone, lava domes
3) By lava composition - those with basic or acidic lava
Other types include supervolcanoes, flood basalt provinces, and submarine volcanoes. Volcanoes form due to pressure from magma escaping through cracks in the earth's crust.
This document discusses key aspects of volcanism including:
- Volcanoes form due to movement of tectonic plates and magma rising from below Earth's surface.
- Most volcanoes occur at plate boundaries like divergent and convergent margins.
- The degree of violence in a volcanic eruption depends on factors like the gas content and viscosity of the magma as well as the silica content which determines eruption style.
- There are several types of volcanoes that differ in size and eruption type including composite, cinder cone, and shield volcanoes.
1) Volcanoes form at boundaries where tectonic plates meet, such as where plates are subducting or spreading apart.
2) There are two main types of volcanoes - cone-shaped volcanoes which form from thick, slow-moving lava and shield volcanoes which have flatter slopes due to more fluid lava.
3) Examples of highly active volcanic regions include the Pacific Ring of Fire and areas around Alaska, Hawaii, and the Cascade Range in the western United 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.
There are three main types of volcanoes:
1) Cinder cones erupt small pieces of scoria and pyroclastics that build up around the vent to form cone-shaped hills. Examples include Par鱈cutin in Mexico and Sunset Crater in Arizona.
2) Stratovolcanoes are tall conical mountains composed of layered lava flows and ejecta. Examples include Mt. Fuji in Japan and Mount Vesuvius in Italy. Their explosive eruptions have posed great hazards.
3) Subglacial volcanoes form underneath ice sheets, leaving flat-topped mountains when the ice melts. Good examples are found in Iceland and British Columbia.
Earth Science 6.2 : Effects of Volcanic EruptionsChris Foltz
油
Volcanic eruptions can profoundly impact climate and the Earth's surface. Large eruptions eject ash and gases into the atmosphere, which can block sunlight and cause global temperatures to drop. There are three main types of volcanoes: shield volcanoes formed from nonexplosive eruptions creating gentle slopes; cinder cone volcanoes from moderately explosive eruptions forming steep slopes; and composite volcanoes from alternating explosive and lava flows creating broad bases that steepen toward their summits. In addition to volcanoes, other volcanic landforms include craters at volcano tops, calderas which are large depressions formed when the magma chamber empties, and lava plateaus resulting from nonexplosive eruptions
This document provides an overview of volcanoes and volcanic eruptions. It defines different types of volcanoes according to their shape, including stratovolcanoes, shield volcanoes, and cinder cone volcanoes. Examples of each type from the Philippines and around the world are given. The document also discusses types of volcanic eruptions from less to more violent, including Hawaiian, Strombolian, Vulcanian, Plinian, phreatic, and phreatomagmatic eruptions. Active volcanoes in the Philippines are listed.
Volcanoes form as magma rises from below the Earth's surface due to movement of tectonic plates. There are three main types of volcanoes - shield volcanoes which erupt fluid lava to form broad, low cones; cinder cone volcanoes which form steep slopes of pyroclastic fragments; and composite or stratovolcanoes which are tall cones built up of hardened lava and ash. Examples include Hawaii's shield volcanoes Kilauea and Mauna Loa, Mexico's Paricutin cinder cone volcano, and the Philippines' composite Mayon volcano. Volcanic eruptions can negatively impact human health through ash, gases and dust inhalation leading to respiratory and other illnesses.
A volcano is a mountain formed by erupted lava and ash from vents in the Earth's crust. It consists of a magma chamber, conduit, and vent. Volcanoes can have different features like rugged peaks or summit craters depending on how lava is emitted. Magma rises from underground chambers and erupts due to pressure or plate collisions. When magma reaches the surface it is called lava. Volcanoes are classified as active, dormant, or extinct based on recent eruption activity. Eruptions can endanger nearby populations through poisonous gases and have caused over 200,000 deaths in the last 500 years.
Volcanoes (GENEVEVE MAGPATOC & JORDAN ABRAHAM)magene
油
Volcanoes form at three main types of plate boundaries: divergent boundaries where plates split apart, convergent boundaries where one plate subducts beneath another, and at hotspots within plates. The type of boundary controls the composition of magma erupted - divergent boundaries produce basalt, convergent produce andesite, and hotspots can produce either depending on the plate composition. Major hazards from volcanoes include lava flows, explosive eruptions of ash and pyroclastic flows, lahars, and gas emissions. Large eruptions can impact global climate through atmospheric dust veiling sunlight. Volcanoes are monitored to determine activity levels and eruptions can be predicted based on increased seismicity, gas emissions,
Volcanoes
Volcanoes are geological formations that occur when magma, molten rock from beneath the Earth's crust, escapes to the surface. This can happen through cracks or vents in the Earth's crust. When magma reaches the surface, it is called lava. Volcanoes can be found both on land and beneath the ocean. There are several types of volcanoes, including shield volcanoes, stratovolcanoes, and cinder cone volcanoes, each characterized by their shape and eruption style. Volcanic eruptions can be explosive or effusive, producing various volcanic materials such as ash, pumice, and volcanic gases. The formation and activity of volcanoes are primarily driven by tectonic plate movements and the presence of hotspots.
Volcanoes form when magma rises up from below the Earth's surface and erupts through openings called vents. There are several types of volcanoes defined by their shape and eruption characteristics. Shield volcanoes have gentle slopes and erupt runny basalt lava, while composite volcanoes are steep-sided and erupt thicker, stickier magma in more explosive eruptions. Cinder cones erupt small fragments and form small, cone-shaped volcanoes. Lava domes form when thick lava piles up in mounds. Volcanoes are caused by the movement of tectonic plates, which can allow magma to rise up in between the plates. Geysers, which are hot springs
The document discusses different types of volcanoes and how they can change Earth's surface quickly. It describes cinder cone, shield cone, and composite cone volcanoes. Cinder cones are small and circular, forming from ejected cinders. Shield cones are large and shield-shaped, building up from lava flows. Composite cones like Mount St. Helens are steep-sided and cone-shaped, often erupting explosively due to trapped viscous magma. Volcanoes can quickly change Earth's surface through lava flows and explosive eruptions that spread rock and ash over wide areas.
The document discusses volcanoes and how they form. It explains that volcanoes form at subduction zones, where tectonic plates collide and one plate slides under another. This causes friction and melting within the Earth, and magma rises up through the crust. When it reaches the surface, it erupts as lava from a vent to form a volcano. Many volcanoes are located on the Pacific Ring of Fire, which is a horseshoe-shaped area in the Pacific Ocean known for seismic activity and volcanoes. Within this area are several subduction zones, including those responsible for the over 20 active volcanoes located in the Philippines.
1. Volcanoes are natural openings in the Earth's crust where molten rock and gases erupt.
2. The Philippines has many active volcanoes due to its location along the Pacific Ring of Fire. Some of the most notable active volcanoes include Taal Volcano, Mount Mayon, and Bulusan.
3. Volcanoes are classified based on their eruption history as either active or inactive, and by their shape as shield, cinder cone, or composite volcanoes.
Presentation of Group 2 - Topic Volcanoeshendrix18
油
A volcano is a rupture in a planet's crust that allows magma, ash, and gases to escape from underground. They form at tectonic plate boundaries and underwater, with about 1,500 potentially active worldwide. Volcanoes are classified as active, dormant, or extinct based on recent eruptions. The three main types are cinder cones made of pyroclastic debris, shield volcanoes built from fluid lava, and composite or stratovolcanoes with steep sides formed from viscous lava. The 1815 eruption of Mount Tambora in Indonesia was the largest in recorded history, killing over 10,000 and contributing to global climate changes and crop failures for years after.
Characteristics of different volcanoes and their typesManojSaini01
油
Volcanoes can be classified in several ways:
1) By frequency of eruption - active, dormant, or extinct
2) By shape and mode of eruption - shield, composite, caldera, cinder cone, lava domes
3) By lava composition - those with basic or acidic lava
Other types include supervolcanoes, flood basalt provinces, and submarine volcanoes. Volcanoes form due to pressure from magma escaping through cracks in the earth's crust.
This document discusses key aspects of volcanism including:
- Volcanoes form due to movement of tectonic plates and magma rising from below Earth's surface.
- Most volcanoes occur at plate boundaries like divergent and convergent margins.
- The degree of violence in a volcanic eruption depends on factors like the gas content and viscosity of the magma as well as the silica content which determines eruption style.
- There are several types of volcanoes that differ in size and eruption type including composite, cinder cone, and shield volcanoes.
QuickBooks Desktop to QuickBooks Online How to Make the MoveTechSoup
油
If you use QuickBooks Desktop and are stressing about moving to QuickBooks Online, in this webinar, get your questions answered and learn tips and tricks to make the process easier for you.
Key Questions:
* When is the best time to make the shift to QuickBooks Online?
* Will my current version of QuickBooks Desktop stop working?
* I have a really old version of QuickBooks. What should I do?
* I run my payroll in QuickBooks Desktop now. How is that affected?
*Does it bring over all my historical data? Are there things that don't come over?
* What are the main differences between QuickBooks Desktop and QuickBooks Online?
* And more
How to Setup WhatsApp in Odoo 17 - Odoo 際際滷sCeline George
油
Integrate WhatsApp into Odoo using the WhatsApp Business API or third-party modules to enhance communication. This integration enables automated messaging and customer interaction management within Odoo 17.
APM People Interest Network Conference 2025
-Autonomy, Teams and Tension: Projects under stress
-Tim Lyons
-The neurological levels of
team-working: Harmony and tensions
With a background in projects spanning more than 40 years, Tim Lyons specialised in the delivery of large, complex, multi-disciplinary programmes for clients including Crossrail, Network Rail, ExxonMobil, Siemens and in patent development. His first career was in broadcasting, where he designed and built commercial radio station studios in Manchester, Cardiff and Bristol, also working as a presenter and programme producer. Tim now writes and presents extensively on matters relating to the human and neurological aspects of projects, including communication, ethics and coaching. He holds a Masters degree in NLP, is an NLP Master Practitioner and International Coach. He is the Deputy Lead for APMs People Interest Network.
Session | The Neurological Levels of Team-working: Harmony and Tensions
Understanding how teams really work at conscious and unconscious levels is critical to a harmonious workplace. This session uncovers what those levels are, how to use them to detect and avoid tensions and how to smooth the management of change by checking you have considered all of them.
Prelims of Kaun TALHA : a Travel, Architecture, Lifestyle, Heritage and Activism quiz, organized by Conquiztadors, the Quiz society of Sri Venkateswara College under their annual quizzing fest El Dorado 2025.
Computer Network Unit IV - Lecture Notes - Network LayerMurugan146644
油
Title:
Lecture Notes - Unit IV - The Network Layer
Description:
Welcome to the comprehensive guide on Computer Network concepts, tailored for final year B.Sc. Computer Science students affiliated with Alagappa University. This document covers fundamental principles and advanced topics in Computer Network. PDF content is prepared from the text book Computer Network by Andrew S. Tenanbaum
Key Topics Covered:
Main Topic : The Network Layer
Sub-Topic : Network Layer Design Issues (Store and forward packet switching , service provided to the transport layer, implementation of connection less service, implementation of connection oriented service, Comparision of virtual circuit and datagram subnet), Routing algorithms (Shortest path routing, Flooding , Distance Vector routing algorithm, Link state routing algorithm , hierarchical routing algorithm, broadcast routing, multicast routing algorithm)
Other Link :
1.Introduction to computer network - /slideshow/lecture-notes-introduction-to-computer-network/274183454
2. Physical Layer - /slideshow/lecture-notes-unit-ii-the-physical-layer/274747125
3. Data Link Layer Part 1 : /slideshow/lecture-notes-unit-iii-the-datalink-layer/275288798
Target Audience:
Final year B.Sc. Computer Science students at Alagappa University seeking a solid foundation in Computer Network principles for academic.
About the Author:
Dr. S. Murugan is Associate Professor at Alagappa Government Arts College, Karaikudi. With 23 years of teaching experience in the field of Computer Science, Dr. S. Murugan has a passion for simplifying complex concepts in Computer Network
Disclaimer:
This document is intended for educational purposes only. The content presented here reflects the authors understanding in the field of Computer Network
APM People Interest Network Conference 2025
- Autonomy, Teams and Tension
- Oliver Randall & David Bovis
- Own Your Autonomy
Oliver Randall
Consultant, Tribe365
Oliver is a career project professional since 2011 and started volunteering with APM in 2016 and has since chaired the People Interest Network and the North East Regional Network. Oliver has been consulting in culture, leadership and behaviours since 2019 and co-developed HPTM速an off the shelf high performance framework for teams and organisations and is currently working with SAS (Stellenbosch Academy for Sport) developing the culture, leadership and behaviours framework for future elite sportspeople whilst also holding down work as a project manager in the NHS at North Tees and Hartlepool Foundation Trust.
David Bovis
Consultant, Duxinaroe
A Leadership and Culture Change expert, David is the originator of BTFA and The Dux Model.
With a Masters in Applied Neuroscience from the Institute of Organisational Neuroscience, he is widely regarded as the Go-To expert in the field, recognised as an inspiring keynote speaker and change strategist.
He has an industrial engineering background, majoring in TPS / Lean. David worked his way up from his apprenticeship to earn his seat at the C-suite table. His career spans several industries, including Automotive, Aerospace, Defence, Space, Heavy Industries and Elec-Mech / polymer contract manufacture.
Published in Londons Evening Standard quarterly business supplement, James Caans Your business Magazine, Quality World, the Lean Management Journal and Cambridge Universities PMA, he works as comfortably with leaders from FTSE and Fortune 100 companies as he does owner-managers in SMEs. He is passionate about helping leaders understand the neurological root cause of a high-performance culture and sustainable change, in business.
Session | Own Your Autonomy The Importance of Autonomy in Project Management
#OwnYourAutonomy is aiming to be a global APM initiative to position everyone to take a more conscious role in their decision making process leading to increased outcomes for everyone and contribute to a world in which all projects succeed.
We want everyone to join the journey.
#OwnYourAutonomy is the culmination of 3 years of collaborative exploration within the Leadership Focus Group which is part of the APM People Interest Network. The work has been pulled together using the 5 HPTM速 Systems and the BTFA neuroscience leadership programme.
https://www.linkedin.com/showcase/apm-people-network/about/
How to Manage Putaway Rule in Odoo 17 InventoryCeline George
油
Inventory management is a critical aspect of any business involved in manufacturing or selling products.
Odoo 17 offers a robust inventory management system that can handle complex operations and optimize warehouse efficiency.
How to Configure Restaurants in Odoo 17 Point of SaleCeline George
油
Odoo, a versatile and integrated business management software, excels with its robust Point of Sale (POS) module. This guide delves into the intricacies of configuring restaurants in Odoo 17 POS, unlocking numerous possibilities for streamlined operations and enhanced customer experiences.
Prelims of Rass MELAI : a Music, Entertainment, Literature, Arts and Internet Culture Quiz organized by Conquiztadors, the Quiz society of Sri Venkateswara College under their annual quizzing fest El Dorado 2025.
How to Modify Existing Web Pages in Odoo 18Celine George
油
In this slide, well discuss on how to modify existing web pages in Odoo 18. Web pages in Odoo 18 can also gather user data through user-friendly forms, encourage interaction through engaging features.
Finals of Kaun TALHA : a Travel, Architecture, Lifestyle, Heritage and Activism quiz, organized by Conquiztadors, the Quiz society of Sri Venkateswara College under their annual quizzing fest El Dorado 2025.
How to use Init Hooks in Odoo 18 - Odoo 際際滷sCeline George
油
In this slide, well discuss on how to use Init Hooks in Odoo 18. In Odoo, Init Hooks are essential functions specified as strings in the __init__ file of a module.
Eng7-Q4-Lesson 1 Part 1 Understanding Discipline-Specific Words, Voice, and T...sandynavergas1
油
types of volcano.pptx
1. Types of Volcanoes
As you may have noticed, not all volcanoes are created the
same. Some are found on land, while others are found
underneath the ocean. Location is just one way of
categorizing them, but volcanoes are also differentiated
and classified based on their volcanic activity, structure,
and explosiveness.
2. Types of Volcanoes according to
Activity
1. Active volcano
2. Dormant volcano
3. Extinct volcano
3. 1. An ACTIVE VOLCANO is one that has erupted at least once since the last Ice Age,
or in the last 10 000 years, and is expected to erupt again in the future.
Active volcanoes are often regarded as the most dangerous type.
Based on the most recent findings of the United States Geological Survey, there
are about 1 500 active volcanoes in the world today.
In the Philippines, around 23 volcanoes are considered active; one of them is
Mayon Volcano. Mayon is the most active volcano in the country. It is found in
Albay, Bicol.
Its most recent volcanic activity was recorded last January 22, 2018, when it
started to spew lava and ash after several months of silence.
One of its deadliest eruptions occurred on February 1, 1814, when about 1 200
people from the nearby town of Cagsawa lost their lives.
4. 1. An ACTIVE VOLCANO is one that has erupted at least once since the last
Ice Age, or in the last 10 000 years, and is expected to erupt again in the
future.
According to former Philippine Institute of Volcanology and Seismology
(PHIVOLCS) director Renato Solidum, the 1814 eruption is the most
destructive in terms of the number of casualties and the distance reached
by the volcanic hazards.
Lava stream and ash fall caused by the eruption had extended over to the
Cagsawa church which stood at a ten-kilometer distance away from the
volcano.
5. 1. An ACTIVE VOLCANO is one that has erupted at least once since the last Ice Age,
or in the last 10 000 years, and is expected to erupt again in the future.
Another hot spot for active volcanoes is Hawaii in the U.S.A.
A hot spot is an area in Earths mantle where magma is generated and causes
volcanic activity.
Volcanic activity in Hawaii has, in act, helped shape its islands.
The Big Island of Hawaii contains five active volcanoes: Mauna Kea, Hualalai,
Mauna Loa, Loihi, and Kilauea.
Mount Kilauea is one of the most active among the five volcanoes in the
Hawaiian islands.
The name Kilauea literally means spewing in Hawaiian language, referring to
the frequent outpouring of lava.
6. 2. A dormant volcano is a volcano that has the capacity to erupt but
has not erupted in the last 10 000 years.
Mount Pinatubo, prior to its cataclysmic VEI 5 eruption in 1991,
had no historical record of eruption.
Its unforeseen explosion caused the destruction of thousands of
homes and the demise of about 800 casualties.
7. 3. An EXTINCT VOLCANO is an inactive volcano that has not erupted over the last
10,000 years and is not expected to erupt in the future.
Mount Malinao and Mount Masaraga, both located in Albay, are two extinct
stratovolcanoes that have no recorded historical eruptions in the last 10 000 years.
With Mt. Mayon, these volcanic mountains make up the Magayan Trio.
A volcano becomes extinct when it is disconnected from its supply of magma.
The tectonic plates underneath the volcanic region continue to move, separating the
magma chamber and the vent from the hotspot in Earths mantle. As a result, the chamber
dries up and remains empty. After a long time of inactivity, the volcano goes extinct.
Although, extinct volcanoes are not expected to erupt again, geographic and seismic
records show that this is not always true.
For example, Mount Vesuvius in Italy erupted suddenly in 79 A.D. destroying the
towns of Herculaneum and Pompeii. On the other hand, the Soufri竪re Hills volcano on the
island of Montserrat in the Caribbean resumed activity only in 1995.
8. Types of Volcanoes according to Shape and
Explosiveness
The plate tectonics theory suggests that the surface of the planet is not one big
piece of land. According to World Atlas, the planets surface is broken into micro
minor and major tectonic plates which move in relation to one another. The
plates float on the layer in Earths mantle called the asthenosphere. When
that hot and viscous layer melts because of tectonic activity, it produces magma.
As mentioned earlier, the Pacific Ring of Fire is the most seismically active region
on the planet. About 90% of earthquakes occur in the Pacific Ring of Fire.
According to the United States Geological Survey (USGS), an average of 12 000
earthquakes has happened annually in this region over the past ten years. It has
more exploding volcanoes than any other region on Earth.
9. Types of Volcanoes according to Shape
and Explosiveness
Aside from their activity, volcanoes are also
classified, based on their shape and the
explosiveness of their eruption.
1. Shield Cone Volcanoes
2. Cinder Cone Volcano
3. Composite Volcano/Stratovolcano
10. 1. Shield Cone Volcanoes are low mountains with broad sloping sides, formed by flowing
lava.
The lava flows in all directions from the central vent, creating a seemingly flattered
cone with a domical summit similar to that of a hill.
Magma escapes either from the central vent or from the fractures on the flanks of the cone. The
accumulation of erupted lava spread across great distances, forming a thin, dipping sheet on the
surface.
Shield cone volcanoes are some of the largest volcanoes in the world.
They have a diameter that occupies hundreds of kilometers and a height that reaches up to
10,000 feet or about 3 000 meters.
The largest shield cone volcano in the world is Mauna Lao in Hawaii, standing 13 677 feet or
about 4 168 meters above sea level.
Most shield cone volcanoes, as well as stratovolcanoes, have summit calderas.
Summit calderas are volcanic craters that are formed by an explosive eruption or a collapsed
peak surface because of an empty magma chamber.
Shield cone volcano calderas result from periodic eruptions that create rock terraces at the crater
rather than a big bowl-shaped depression.
11. 2. Cinder Cone Volcano. The simplest type of volcanoes are the
cinder cone volcanoes.
These are steep conical hills of volcanic debris formed by
particles and blobs of erupted lava.
When a cinder cone volcano explodes, a gas-filled lava blows up
into the air and breaks into small fragments that gather at the vent,
forming a circular oval cone.
A cinder cone stands at about 1 200 feet or 366 meters above its
surroundings.
It usually has a low-impact eruption.
Many cinder cones are found in North America.
In the Philippines, there is the Smith Volcano on the western part
of the Babuyan Island.
12. 3. Composite Volcano/Stratovolcano. Composite volcanoes, also called
stratovolcanoes, are made of alternating layers of volcanic debris, lava flows,
and cinders that run down steep, symmetrical flanks.
A stratovolcano rises up to 8 000 feet or 2 438 meters above the
surroundings.
It is usually formed by the accumulation of erupted volcanic materials in
its slope.
The crater of a composite volcano is connected to a central vent filled with
magma.
The magma flows through the crater wall or in the fissures on the flanks of
its cone, and the solidified lava forms dikes which are like ribs that
strengthen the cones frame.
13. 3. Composite Volcano/Stratovolcano. Composite volcanoes, also called
stratovolcanoes, are made of alternating layers of volcanic debris, lava flows, and
cinders that run down steep, symmetrical flanks.
The dormancy of composite volcanoes is the beginning of its destruction. When
magma hardens, it plugs the conduit system and strips away the fissures on the flanks,
making it prone to erosion.
An example of a dormant composite volcano is Mt. Mazama in Oregon,
United States. Because of tremendous explosions thousands of years ago, Mt.
Mazama lost its top section. Large amounts of volcanic ash and dust rolled down the
slopes, draining the lava beneath and weakening the upper part. The peak collapsed
and formed a large depression that eventually filled with water and became a
beautiful crater lake.
A few examples of the worlds most beautiful composite volcanoes are Mt. Fuji in
Japan, Mt. Cotopaxi in Ecuador, Mt. St. Helens in the U.S.A. and Mt. Mayon in the
Philippines.
24. CATACLYSMIC - an event that causes a lot of
destruction, or a sudden, violent change.
The Volcanic Explosivity Index ( VEI) is a relative
measure of the explosiveness of volcanic eruptions.
It was devised by Chris Newhall of the United States
Geological Survey and Stephen Self at the University
of Hawaii in 1982.
27. A stratovolcano is a tall volcano shaped like a cone, formed by
various layers of materials such as volcanic ash, hardened lava,
pumice, and tephra.
28. Tectonic plates are pieces of Earth's crust and uppermost mantle,
together referred to as the lithosphere.
- the Earth's lithosphere to comprise a number of large tectonic
plates which have been slowly moving since about 3.4 billion years
ago.