GEOGRAPHY IGCSE: PLATE TECTONICS. Earth's layers. Inner core, outer core, mantle, crust, the structure of Earth, plate boundaries and interactions, magma and igneous rocks, forming a volcano, compressional boundaries, folding.
GEOGRAPHY IGCSE: EARTHQUAKES. It contains: earthquakes, energy and epicentre, measuring the power, effects of an earthquake, factors affecting the impact, earthquakes and volcanoes in LEDC and MEDC. Kobe 1995, Kashmir 2005.
AS Level Physical Geography - Rocks and WeatheringArm Punyathorn
The earth's surface is an ever-changing entity. With the forces of weather and climate and tectonic variability, the rocks and minerals that make up the earth are always changing in size, shape and forms - a fascinating, ancient, never-ending process.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS. It contains: difference between weather and climate, measuring the weather, what do we measure, temperature, precipitation, wind direction, Beaufort scale, cloud cover, air pressure, glossary.
GEOGRAPHY IGCSE: EARTHQUAKES. It contains: earthquakes, energy and epicentre, measuring the power, effects of an earthquake, factors affecting the impact, earthquakes and volcanoes in LEDC and MEDC. Kobe 1995, Kashmir 2005.
AS Level Physical Geography - Rocks and WeatheringArm Punyathorn
The earth's surface is an ever-changing entity. With the forces of weather and climate and tectonic variability, the rocks and minerals that make up the earth are always changing in size, shape and forms - a fascinating, ancient, never-ending process.
GEOGRAPHY IGCSE: WEATHER MEASUREMENTS. It contains: difference between weather and climate, measuring the weather, what do we measure, temperature, precipitation, wind direction, Beaufort scale, cloud cover, air pressure, glossary.
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZONGeorge Dumitrache
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON. It contains: tropical rainforests, average rainfall in Brazil, rainforest ecosystems, disadvantages of human intervention, rainforest water cycle, rainforest nutrient cycle, rainforest soils, vegetation layers, fan palms, buttress roots, lianas, strangler figs, case study, humans and the Amazon.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDOUS ENVIRONMENTS RESULTING FROM MASS MOVEMENTS. It contain case studies: Italian Mudslides 1998, New Zealand Landslip 1979, European Avalanches 1999.
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by Maria Jesús Campos, Social Studies, Geography and History teacher in a bilingual section in Madrid (Spain)
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...George Dumitrache
A presentation of the first subchapter (Drainage Basin Systems) from the first chapter (Hydrology and Fluvial Geomorphology) of Revision for Geography AS Cambridge exam.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...George Dumitrache
A comprehensive presentation of subchapter 2.3 Weather Processes and Phenomena, from the second chapter of Physical Geography, AS Cambridge, Atmosphere and Weather.
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRICULTURAL SYSTEMS AND FOOD PRODUCTION. It contains: ley terms and definitions, topic summary, additional work and suggested websites.
GEOGRAPHY IGCSE: TOURISM - TRENDS. It contains: trends in tourism, the growth of tourism, trends, infrastructure, reasons behind the trends in tourism.
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZONGeorge Dumitrache
GEOGRAPHY IGCSE: TROPICAL RAINFORESTS. DEFORESTATION ON THE AMAZON. It contains: tropical rainforests, average rainfall in Brazil, rainforest ecosystems, disadvantages of human intervention, rainforest water cycle, rainforest nutrient cycle, rainforest soils, vegetation layers, fan palms, buttress roots, lianas, strangler figs, case study, humans and the Amazon.
A2 CAMBRIDGE GEOGRAPHY: HAZARDOUS ENVIRONMENTS - HAZARDOUS ENVIRONMENTS RESULTING FROM MASS MOVEMENTS. It contain case studies: Italian Mudslides 1998, New Zealand Landslip 1979, European Avalanches 1999.
learningfromgeography.wikispaces.com
learningfromhistory.wikispaces.com
Developed by Maria Jesús Campos, Social Studies, Geography and History teacher in a bilingual section in Madrid (Spain)
CAMBRIDGE AS GEOGRAPHY REVISION: HYDROLOGY AND FLUVIAL GEOMORPHOLOGY - 1.1 DR...George Dumitrache
A presentation of the first subchapter (Drainage Basin Systems) from the first chapter (Hydrology and Fluvial Geomorphology) of Revision for Geography AS Cambridge exam.
CAMBRIDGE AS GEOGRAPHY REVISION: ATMOSPHERE AND WEATHER - 2.3 WEATHER PROCESS...George Dumitrache
A comprehensive presentation of subchapter 2.3 Weather Processes and Phenomena, from the second chapter of Physical Geography, AS Cambridge, Atmosphere and Weather.
CAMBRIDGE GEOGRAPHY A2 REVISION - PRODUCTION, LOCATION AND CHANGE: 11.1 AGRICULTURAL SYSTEMS AND FOOD PRODUCTION. It contains: ley terms and definitions, topic summary, additional work and suggested websites.
GEOGRAPHY IGCSE: TOURISM - TRENDS. It contains: trends in tourism, the growth of tourism, trends, infrastructure, reasons behind the trends in tourism.
Google is a powerhouse of information and it continues to add millions of bytes of data on every conceivable topic you can imagine. That said, it’s imperative to not get lost in pages after pages of irrelevant search results. Most people just key-in their search query, expecting Google to do the rest. However, there are a number of search operatives that can yield refined results. Whether you want to search for an exact phrase or omit certain types of results for your search query, you can get it all using these pro-tips.
This infographic at WhoIsHostingThis? illustrates the lesser known tips to using Google to get the most accurate results and shortest possible time.
GEOGRAPHY YEAR 10: RIVERS AND FLOODING. Contains: river floods, factors to increase flooding, human factors, storm hydrographs, Boscastle 2004, Bangladesh 2007, the red mud in Hungary 2010.
GEOGRAPHY YEAR 10: RIVER LANDFORMS. Contains: river landforms, across the rivers, v-shapped valleys, waterfalls, formation of the waterfalls, meanders and ox-bow lakes, braiding and deltas, the formation of a delta.
Each month, join us as we highlight and discuss hot topics ranging from the future of higher education to wearable technology, best productivity hacks and secrets to hiring top talent. Upload your SlideShares, and share your expertise with the world!
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CSEC Geography- Internal Forces - Plate Tectonics and EarthquakesOral Johnson
This document looks at the Earth's internal forces. The main layers of the earth are described. The history surrounding plate tectonics is discussed. The different types of plate boundaries is also explained.
GEOPHYSICS
Introduction
Geophysics is the branch of science that is concerned with the physical, chemical, geological, astronomical -and other characteristic properties of the earth.
It deals with geological phenomena such as the temperature distribution of the earth's interior, the source, configuration and the geomagnetic field.
Interior structure of the earth
The structure of the earth is composed of three major zones arranged in a concentric manner. These are crust, mantle and core;
Chemical and Physical Properties of Earth's Layers and the Tectonic Plates (G...Raboon Redar
To determine the chemical composition inside the Earth indirect measurements are used. One way to determine composition is to measure how the density of rock changes with depth below the Earth’s surface. We can do this by measuring the speeds, because they move more quickly through dense rocks than through less dense rocks. From such measurements we know that density increases with depth, but not evenly. Knowing these different densities, we can estimate what the composition of the different layers must be. The layers of different chemical composition outward from the centre of the Earth are as follows: core, mantle, and crust.
This is the entire CSEC geography syllabus (some things might be missing). The information was collected from various websites and textbooks. The topics are:
- Internal forces
-External forces
-Rivers
-Limestone
-Coasts
-Coral reefs and Mangroves
-Weather and Climate
- Ecosystems (vegetation and soils)
-Natural hazards
- Urbanization
-Economic activity
-Environmental degradation
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE SOURCESGeorge Dumitrache
07. DEPTH STUDY GERMANY: NAZI REGIME - REICHSTAG FIRE
On February 27, 1933, the German parliament (Reichstag) building burned down. The Nazi leadership and its coalition partners used the fire to claim that Communists were planning a violent uprising. They claimed that emergency legislation was needed to prevent this. The resulting act, commonly known as the Reichstag Fire Decree, abolished a number of constitutional protections and paved the way for Nazi dictatorship.
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTXGeorge Dumitrache
05. DEPTH STUDY GERMANY: NAZI REGIME - HITLER CONSOLIDATING POWER 1933-34.PPTX
Following Hitler’s appointment as chancellor the Nazis were finally in a position of power.
However, this power was limited, as the Nazis were just one party in a three party coalition government, under President Hindenburg.
This topic will explore how the Nazis managed to eliminate their opposition and consolidate ultimate power over Germany, whilst maintaining an illusion of democracy.
It will first explore this topic in chronological order, from the Reichstag Fire through to the death of President Hindenburg, and then explore it thematically in the last section. On the 31 January 1933, Hitler, conscious of his lack of a majority in the Reichstag, immediately called for new elections to try and strengthen his position. The Nazis aimed to increase their share of the vote so that they would have a majority in the Reichstag. This would allow them to rule unopposed and unhindered by coalition governments.
Over the next two months, they launched themselves into an intense election campaign.
On 27 February 1933, as the campaign moved into its final, frantic days, the Reichstag, the German Parliament building, was set on fire and burnt down. An atmosphere of panic and terror followed the event.
This continued when a young Dutch communist, Van der Lubbe was arrested for the crime.
The Nazi Party used the atmosphere of panic to their advantage, encouraging anti-communism. Göring declared that the communists had planned a national uprising to overthrow the Weimar Republic. This hysteria helped to turn the public against the communists, one of the Nazis main opponents, and 4000 people were imprisoned.
The day after the fire, Hindenburg signed the Emergency Decree for the Protection of the German People. On the 28 February 1933, President Hindenburg signed the Emergency Decree for the Protection of the German People. This decree suspended the democratic aspects of the Weimar Republic and declared a state of emergency.
This decree gave the Nazis a legal basis for the persecution and oppression of any opponents, who were be framed as traitors to the republic. People could be imprisoned for any or no reason.
The decree also removed basic personal freedoms, such as the freedom of speech, the right to own property, and the right to trial before imprisonment.
Through these aspects the Nazis suppressed any opposition to their power, and were able to start the road from democracy to a dictatorship. The atmosphere of uncertainty following the Reichstag Fire secured many voters for the Nazi party.
The SA also ran a violent campaign of terror against any and all opponents of the Nazi regime. Many were terrified of voting of at all, and many turned to voting for the Nazi Party out of fear for their own safety. The elections were neither free or fair.
On the 5 March 1933, the elections took place, with an extremely high turnout of 89%.
The Nazis secured 43.9% of the vote.
DEPTH STUDY GERMANY: NAZI REGIME - 04. HITLER BECOMING CHANCELLOR 1933George Dumitrache
Hitler was not immediately appointed chancellor after the success of the July 1932 elections, despite being leader of the largest party in the Reichstag. It took the economic and political instability (with two more chancellors failing to stabilise the situation) to worsen, and the support of the conservative elite, to convince Hindenburg to appoint Hitler.
Hitler was sworn in as the chancellor of Germany on the 30 January 1933. The Nazis were now in power.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 08. NAZIS IN THE WILDERNESSGeorge Dumitrache
The “Lean Years” (also called the "wilderness" years) of Hitler and the Nazi Party in Germany refer to the period between 1924 and 1928 when the Nazi party did not have high levels of support and still suffered from humiliation over the Munich Putsch. Why where these years “lean”?
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 07. STRESEMMAN ERA 1924-1929George Dumitrache
The period 1924-1929 was a time when the Weimar economy recovered and cultural life in Germany flourished. This dramatic turnabout happened in large part because of the role played by Gustav Stresemann who became Chancellor in August 1923 during the hyperinflation crisis.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 06. THE BEER HALL PUTSCH 1923George Dumitrache
The Beer Hall Putsch, also known as the Munich Putsch, was a failed coup d'état by Nazi Party (Nationalsozialistische Deutsche Arbeiterpartei or NSDAP) leader Adolf Hitler, Generalquartiermeister Erich Ludendorff and other Kampfbund leaders in Munich, Bavaria, on 8–9 November 1923, during the Weimar Republic. Approximately two thousand Nazis marched on the Feldherrnhalle, in the city centre, but were confronted by a police cordon, which resulted in the deaths of 16 Nazi Party members and four police officers. Hitler escaped immediate arrest and was spirited off to safety in the countryside. After two days, he was arrested and charged with treason. The putsch brought Hitler to the attention of the German nation for the first time and generated front-page headlines in newspapers around the world. His arrest was followed by a 24-day trial, which was widely publicised and gave him a platform to express his nationalist sentiments to the nation. Hitler was found guilty of treason and sentenced to five years in Landsberg Prison, where he dictated Mein Kampf to fellow prisoners Emil Maurice and Rudolf Hess. On 20 December 1924, having served only nine months, Hitler was released. Once released, Hitler redirected his focus towards obtaining power through legal means rather than by revolution or force, and accordingly changed his tactics, further developing Nazi propaganda.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 05. HYPERINFLATIONGeorge Dumitrache
Hyperinflation affected the German Papiermark, the currency of the Weimar Republic, between 1921 and 1923, primarily in 1923. It caused considerable internal political instability in the country, the occupation of the Ruhr by France and Belgium, and misery for the general populace.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 03. THE TREATY OF VERSAILLES IMPACT ON...George Dumitrache
Thanks to the Treaty of Versailles, Germany's ability to produce revenue-generating coal and iron ore decreased. As war debts and reparations drained its coffers, the German government was unable to pay its debts. Some of the former World War I Allies didn't buy Germany's claim that it couldn't afford to pay.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 02. THE NOVEMBER REVOLUTION 1918George Dumitrache
The German Revolution or November Revolution was a civil conflict in the German Empire at the end of the First World War that resulted in the replacement of the German federal constitutional monarchy with a democratic parliamentary republic that later became known as the Weimar Republic. The revolutionary period lasted from November 1918 until the adoption of the Weimar Constitution in August 1919. Among the factors leading to the revolution were the extreme burdens suffered by the German population during the four years of war, the economic and psychological impacts of the German Empire's defeat by the Allies, and growing social tensions between the general population and the aristocratic and bourgeois elite.
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANYGeorge Dumitrache
DEPTH STUDY GERMANY: WEIMAR REPUBLIC - 01. THE EFFECT OF WW1 ON GERMANY. This presentation covers the social, economic and political impact of war along with a brief analysis of the physical cost of war.
QUESTIONS AND ANSWERS - LEAGUE OF NATIONS. The League of Nations was an international organization, headquartered in Geneva, Switzerland, created after the First World War to provide a forum for resolving international disputes.
ABYSSINIAN CRISIS. The Abyssinian Crisis was over in 1936. Italy and Mussolini continually ignored the League of Nations and fully annexed Abyssinia on May 9th 1936. The League of Nations was shown to be ineffective. The League had not stood up against one of the strongest members and fulfilled the promise of collective security.
Manchurian Crisis. On September 18, 1931, an explosion destroyed a section of railway track near the city of Mukden. The Japanese, who owned the railway, blamed Chinese nationalists for the incident and used the opportunity to retaliate and invade Manchuria.
05. LEAGUE OF NATIONS - Great Depression and LON.pptxGeorge Dumitrache
GREAT DEPRESSION AND THE LEAGUE OF NATIONS. The Great Depression of 1930-33 meant people turned to extremist dictators such as Hitler and Mussolini, who were keen to invade other countries. This made it hard for the League to maintain peace. The League had some very ambitious plans and ideals – to stop war and make the world a better place.
The Roman Empire A Historical Colossus.pdfkaushalkr1407
The Roman Empire, a vast and enduring power, stands as one of history's most remarkable civilizations, leaving an indelible imprint on the world. It emerged from the Roman Republic, transitioning into an imperial powerhouse under the leadership of Augustus Caesar in 27 BCE. This transformation marked the beginning of an era defined by unprecedented territorial expansion, architectural marvels, and profound cultural influence.
The empire's roots lie in the city of Rome, founded, according to legend, by Romulus in 753 BCE. Over centuries, Rome evolved from a small settlement to a formidable republic, characterized by a complex political system with elected officials and checks on power. However, internal strife, class conflicts, and military ambitions paved the way for the end of the Republic. Julius Caesar’s dictatorship and subsequent assassination in 44 BCE created a power vacuum, leading to a civil war. Octavian, later Augustus, emerged victorious, heralding the Roman Empire’s birth.
Under Augustus, the empire experienced the Pax Romana, a 200-year period of relative peace and stability. Augustus reformed the military, established efficient administrative systems, and initiated grand construction projects. The empire's borders expanded, encompassing territories from Britain to Egypt and from Spain to the Euphrates. Roman legions, renowned for their discipline and engineering prowess, secured and maintained these vast territories, building roads, fortifications, and cities that facilitated control and integration.
The Roman Empire’s society was hierarchical, with a rigid class system. At the top were the patricians, wealthy elites who held significant political power. Below them were the plebeians, free citizens with limited political influence, and the vast numbers of slaves who formed the backbone of the economy. The family unit was central, governed by the paterfamilias, the male head who held absolute authority.
Culturally, the Romans were eclectic, absorbing and adapting elements from the civilizations they encountered, particularly the Greeks. Roman art, literature, and philosophy reflected this synthesis, creating a rich cultural tapestry. Latin, the Roman language, became the lingua franca of the Western world, influencing numerous modern languages.
Roman architecture and engineering achievements were monumental. They perfected the arch, vault, and dome, constructing enduring structures like the Colosseum, Pantheon, and aqueducts. These engineering marvels not only showcased Roman ingenuity but also served practical purposes, from public entertainment to water supply.
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.
A Strategic Approach: GenAI in EducationPeter 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.
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
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!
Instructions for Submissions thorugh G- Classroom.pptxJheel Barad
This presentation provides a briefing on how to upload submissions and documents in Google Classroom. It was prepared as part of an orientation for new Sainik School in-service teacher trainees. As a training officer, my goal is to ensure that you are comfortable and proficient with this essential tool for managing assignments and fostering student engagement.
Unit 8 - Information and Communication Technology (Paper I).pdfThiyagu K
This slides describes the basic concepts of ICT, basics of Email, Emerging Technology and Digital Initiatives in Education. This presentations aligns with the UGC Paper I syllabus.
Welcome to TechSoup New Member Orientation and Q&A (May 2024).pdfTechSoup
In this webinar you will learn how your organization can access TechSoup's wide variety of product discount and donation programs. From hardware to software, we'll give you a tour of the tools available to help your nonprofit with productivity, collaboration, financial management, donor tracking, security, and more.
Introduction to AI for Nonprofits with Tapp NetworkTechSoup
Dive into the world of AI! Experts Jon Hill and Tareq Monaur will guide you through AI's role in enhancing nonprofit websites and basic marketing strategies, making it easy to understand and apply.
2. The Earth is made up of four distinct layers:
The inner core is in the centre and is the hottest part of the
Earth. It is solid and made up of iron and nickel with
temperatures of up to 5,500°C.
With its immense heat energy, the inner core is like the
engine room of the Earth.
3. The outer core is the layer surrounding the inner core.
It is a liquid layer, also made up of iron and nickel.
It is still extremely hot, with temperatures similar to the
inner core.
4. The mantle is the widest section of the Earth.
It has a diameter of approximately 2,900 km.
The mantle is made up of semi-molten rock called magma.
In the upper parts of the mantle the rock is hard, but lower
down the rock is soft and beginning to melt.
5. The crust is the outer layer of the earth.
It is a thin layer between 0-60 km thick.
The crust is the solid rock layer upon which we live.
6. There are two different types of crust: continental crust, which
carries land, and oceanic crust, which carries water.
The diagram below shows the structure of the earth.
In geography, taking a slice through a structure to see inside is
called a cross section.
7.
8. The Earth's crust is broken up into pieces called plates.
Heat rising and falling inside the mantle creates convection
currents generated by radioactive decay in the core. The
convection currents move the plates.
Where convection currents diverge near the Earth's crust,
plates move apart. Where convection currents converge, plates
move towards each other. The movement of the plates, and the
activity inside the Earth, is called plate tectonics.
Plate tectonics cause earthquakes and volcanoes.
The point where two plates meet is called a plate boundary.
Earthquakes and volcanoes are most likely to occur either on or
near plate boundaries.
9.
10. At a tensional, constructive or divergent boundary the plates
move apart.
At a compressional, destructive or convergent boundary the
plates move towards each other.
At a conservative or transform boundary the plates slide past
each other.
11. At a tensional or constructive boundary the plates are moving
apart.
The plates move apart due to convection currents inside the
Earth.
12.
13. As the plates move apart (very slowly), magma rises from the
mantle. The magma erupts to the surface of the Earth. This is
also accompanied by earthquakes.
When the magma reaches the surface, it cools and solidifies to
form a new crust of igneous rock. This process is repeated
many times, over a long period of time.
14. Eventually the new rock builds up to form a volcano.
Constructive boundaries tend to be found under the sea, eg the
Mid Atlantic Ridge. Here, chains of underwater volcanoes have
formed along the plate boundary.
One of these volcanoes may become so large that it erupts out
of the sea to form a volcanic island, eg Surtsey and the
Westman Islands near Iceland.
The diagram below shows how magma pushes up between the
two plates, causing a chain of volcanoes along the constructive
plate boundary.
15.
16. At a compressional or destructive boundary the plates are
moving towards each other. This usually involves a continental
plate and an oceanic plate.
The oceanic plate is denser than the continental plate so, as
they move together, the oceanic plate is forced underneath the
continental plate. The point at which this happens is called the
subduction zone.
As the oceanic plate is forced below the continental plate it
melts to form magma and earthquakes are triggered. The
magma collects to form a magma chamber. This magma then
rises up through cracks in the continental crust. As pressure
builds up, a volcanic eruption may occur.
17.
18. As the plates push together, the continental crust is squashed
together and forced upwards. This is called folding.
The process of folding creates fold mountains. Fold mountains
can also be formed where two continental plates push towards
each other.
This is how mountain ranges such as the Himalayas and the
Alps were formed.