Introduction to europe's history extension
•Download as PPTX, PDF•
1 like•615 views
The document provides instructions for creating a timeline of important events in European history before exploration. It instructs students to fold paper into a timeline, mark and illustrate several key events, and color the illustrations. It then lists 10 major events in European history to include on the timeline, ranging from the first Greek Olympic Games in 776 BC to Christopher Columbus setting sail in 1492 AD.
Report
Share
Report
Share
Recommended
Dark Ages Geography
This document provides information about the Dark Ages in Europe and the influence of geography on medieval society. It begins with questions for students to answer about the Dark Ages and European geography. It then defines the Dark Ages as the period from 476-1000 CE after the fall of Rome when Europe lacked leadership. Historians call it "Dark" due to lack of information and little cultural advancement. The document describes the different climates and crops of Northern and Southern Europe and how abundant resources like forests and farmland allowed small self-sufficient kingdoms to form. Geography shaped medieval society by providing good conditions for farming and production across Europe.
A Timeline Of Europe
This document provides a timeline of major events in European history from 400 BC to 2007 AD. It outlines the rise and fall of civilizations like Greece, Rome, and the Byzantine Empire. It then discusses the Middle Ages and events like the Crusades, Renaissance, Reformation, and Industrial Revolution. Major power shifts are noted, such as the rise of Prussia/Germany and decline of empires like the Ottoman Empire. Both World Wars and the Cold War period profoundly impacted Europe and led to increased nationalism and the development of the European Union.
European middle ages upload
The document discusses several factors that contributed to the decline and revival of European cities during the Middle Ages. Factors that led to urban decline included Viking invasions, the Black Death plague, a decline in agricultural production due to warfare and early feudalism, and the Little Ice Age. Factors that contributed to urban revival included the end of invasions, safer transportation enabling trade and commerce, warmer temperatures between 800-1300 CE which increased agricultural production and population, and a larger available labor force. The document prompts the reader to analyze and evaluate which factors were most significant in causing urban decline and revival.
A history of photography
The document provides a history of photography from its origins to its widespread adoption in the late 1800s. It describes how the camera obscura was used by early artists before the invention of photography. Joseph Nicephore Niepce created the first permanent photograph in 1826 and Louis Daguerre later invented the daguerreotype process in 1839, which became very popular for portraits. William Henry Fox Talbot also developed the calotype process using negatives. The American Civil War was a turning point where photography was used extensively to document battles and soldiers.
Historical and cultural context prsentation [autosaved]
This chapter discusses eight major milestones in the development of human communication: language, writing, printing, the telegraph, telephone, photography, motion pictures, radio, television, and digital/mobile media. Each new technology increased society's ability to convey and store information, with impacts such as the growth of knowledge and scholarship as well as changes in politics, commerce, and culture.
Cruising the World (colonization)
The document discusses how exploration during the Age of Exploration was motivated by similar human emotions and ambitions as people today. It notes that while explorers of the past dressed differently and used different technology, their dreams and desires to explore were the same. The document encourages students to think about what motivations they might share with historical explorers as they learn about the Age of Exploration.
Seventh grade unit 2b - olmec grasp time capsule directions
This document provides instructions for an activity to help students understand the Olmec civilization through creating a shoebox time capsule. Students will draw and caption images representing the Olmec's geography, cities, agriculture, art, religion, and intellectual legacy. They will then write a conclusion explaining why the Olmec civilization is considered Mesoamerica's "mother culture".
Inventorssunu1
The document outlines many important inventions and discoveries throughout human history from early toolmaking by Homo erectus to more modern developments like the internet and cloning of Dolly the sheep. It traces technological advances in fields such as transportation, communication, construction, materials, energy, and space exploration that have occurred over millennia and accelerated greatly in recent centuries. Many pivotal inventions like the wheel, printing press, railroad, light bulb, airplane, and computer transformed civilization and human capabilities.
Recommended
Dark Ages Geography
This document provides information about the Dark Ages in Europe and the influence of geography on medieval society. It begins with questions for students to answer about the Dark Ages and European geography. It then defines the Dark Ages as the period from 476-1000 CE after the fall of Rome when Europe lacked leadership. Historians call it "Dark" due to lack of information and little cultural advancement. The document describes the different climates and crops of Northern and Southern Europe and how abundant resources like forests and farmland allowed small self-sufficient kingdoms to form. Geography shaped medieval society by providing good conditions for farming and production across Europe.
A Timeline Of Europe
This document provides a timeline of major events in European history from 400 BC to 2007 AD. It outlines the rise and fall of civilizations like Greece, Rome, and the Byzantine Empire. It then discusses the Middle Ages and events like the Crusades, Renaissance, Reformation, and Industrial Revolution. Major power shifts are noted, such as the rise of Prussia/Germany and decline of empires like the Ottoman Empire. Both World Wars and the Cold War period profoundly impacted Europe and led to increased nationalism and the development of the European Union.
European middle ages upload
The document discusses several factors that contributed to the decline and revival of European cities during the Middle Ages. Factors that led to urban decline included Viking invasions, the Black Death plague, a decline in agricultural production due to warfare and early feudalism, and the Little Ice Age. Factors that contributed to urban revival included the end of invasions, safer transportation enabling trade and commerce, warmer temperatures between 800-1300 CE which increased agricultural production and population, and a larger available labor force. The document prompts the reader to analyze and evaluate which factors were most significant in causing urban decline and revival.
A history of photography
The document provides a history of photography from its origins to its widespread adoption in the late 1800s. It describes how the camera obscura was used by early artists before the invention of photography. Joseph Nicephore Niepce created the first permanent photograph in 1826 and Louis Daguerre later invented the daguerreotype process in 1839, which became very popular for portraits. William Henry Fox Talbot also developed the calotype process using negatives. The American Civil War was a turning point where photography was used extensively to document battles and soldiers.
Historical and cultural context prsentation [autosaved]
This chapter discusses eight major milestones in the development of human communication: language, writing, printing, the telegraph, telephone, photography, motion pictures, radio, television, and digital/mobile media. Each new technology increased society's ability to convey and store information, with impacts such as the growth of knowledge and scholarship as well as changes in politics, commerce, and culture.
Cruising the World (colonization)
The document discusses how exploration during the Age of Exploration was motivated by similar human emotions and ambitions as people today. It notes that while explorers of the past dressed differently and used different technology, their dreams and desires to explore were the same. The document encourages students to think about what motivations they might share with historical explorers as they learn about the Age of Exploration.
Seventh grade unit 2b - olmec grasp time capsule directions
This document provides instructions for an activity to help students understand the Olmec civilization through creating a shoebox time capsule. Students will draw and caption images representing the Olmec's geography, cities, agriculture, art, religion, and intellectual legacy. They will then write a conclusion explaining why the Olmec civilization is considered Mesoamerica's "mother culture".
Inventorssunu1
The document outlines many important inventions and discoveries throughout human history from early toolmaking by Homo erectus to more modern developments like the internet and cloning of Dolly the sheep. It traces technological advances in fields such as transportation, communication, construction, materials, energy, and space exploration that have occurred over millennia and accelerated greatly in recent centuries. Many pivotal inventions like the wheel, printing press, railroad, light bulb, airplane, and computer transformed civilization and human capabilities.
European economies
The document compares the economies of the United Kingdom, Germany, and Russia. The UK has a mixed market economy and is one of the world's leading industrial powers, with major industries including machinery, vehicles, chemicals, and food processing. Germany has the largest economy in Europe and is third largest in the world, with industries like iron, steel, chemicals, vehicles, and machinery. Russia has a mixed economy moving from communist command to market principles; it has a large natural resource base but exploitation is challenging due to climate and infrastructure.
Deformation
The video discusses the different types of forces that can act on and deform the Earth's crust, including compression, tension, and shearing. Compression causes squeezing and folding of rocks to form structures like anticlines and synclines. Tension causes pulling apart and thinning of the crust to form rift valleys. Shearing causes twisting and tearing of rocks. Different rock types and environmental conditions influence whether the crust folds or faults under geological forces.
Volcanoes
Volcanoes form where magma reaches the Earth's surface through openings called vents. There are several types of volcanoes defined by their eruptive activity and structure. Cinder cones have short eruptions that build steep slopes from ejected cinders. Shield volcanoes have long-lasting eruptions that spread lava over large areas to form broad dome shapes like Hawaii's Mauna Loa. Composite volcanoes like Italy's Mount Etna are made of layers from violent and quiet eruptions. Volcanoes can be classified as active if currently erupting, dormant if not currently erupting but historically active, or extinct if no known eruptions in history. Most volcanism occurs along zones of
Seismic waves
Deep underground, rocks are under constant pressure until the strain becomes too great and the rocks suddenly break, releasing seismic waves. These waves travel outward from the hypocenter in three types - P waves which push and pull, S waves which move sides to side, and L waves which cause surfaces to bob up and down. When recorded by a seismograph, the first indication of an earthquake is typically the P waves, followed by larger S waves, with surface L waves arriving last.
Earthquakes
An earthquake is caused by the sudden movement of parts of the Earth's crust and results in shaking and trembling of the ground. There are over one million earthquakes each year, with around twenty having the potential to cause severe damage. Earthquakes are caused by faults in the Earth's crust, such as the San Andreas Fault in California where the land west of the fault moves north and the land east moves south. Underwater earthquakes can generate destructive tsunamis. The focus is the depth below the surface where the earthquake occurs, and the epicenter is directly above on the surface. Seismographs detect seismic waves that travel out from the epicenter, including fast P waves and slower S waves.
Deformation
The video discusses the different forces that act on the earth's crust and how they cause deformation through various mechanisms. Compression causes squeezing and increases density, tension causes pulling and decreases density, and shearing causes twisting. These forces result in fracturing, faulting, and folding of rocks in the crust. Fractures are cracks, faults are cracks with lateral movement, and folds are bends in rock layers. Anticlines are upward folds and synclines are downward folds. Various factors like temperature, pressure, rock type, and rate of force application determine whether rocks fault or fold when subjected to deformation.
European governments
The document summarizes the government and political systems of the United Kingdom, Germany, and Russia. It describes that the UK has a Parliament with two houses, the House of Commons and House of Lords, and citizens elect members of Commons while Lords are inherited titles. Germany is a federal republic with a Chancellor as head of government and largely ceremonial President. Russia transitioned to a federal republic after the Soviet fall, with a dominant presidential system and a two-chamber Parliament.
Plate tectonics review #2
The document discusses different types of plate boundaries, including divergent boundaries where plates move apart, such as at mid-ocean ridges which form undersea mountain ranges as oceanic crust spreads away from the ridge. It also describes transform boundaries where plates slide past each other in opposite directions, such as at the San Andreas Fault in California.
Plate tectonics review
The plates are moving at a very slow rate of between one to ten centimeters per year. In some areas plates are moving together through a process called convergence, while in other areas they are moving apart. There are three main types of convergent boundaries: continental-continental, continental-oceanic, and oceanic-oceanic. At convergent boundaries, one plate dives beneath the other through subduction, which can cause volcanic activity at the surface.
Plate tectonics
The document discusses the theory of plate tectonics. It explains that the Earth's lithosphere is broken into plates that move slowly over time due to convection currents in the mantle. There are three types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where plates slip past each other.
Systems of government powerpoint (unitary, confederation, federal)updated 2010
Systems of government powerpoint (unitary, confederation, federal)updated 2010North Gwinnett Middle School
This document discusses different systems of government and how power is distributed in each. It begins by asking the reader to identify the different levels of government where they live. It then explains that governments are organized to protect citizens and manage conflict. There are different types of governments like democracies, republics, and monarchies. Geographers study the types of governments and how power is distributed through systems. The main systems are unitary, confederation, and federal. Unitary governments have one central power. Confederation governments give some power to members. Federal governments share power between a central and state/provincial governments. Diagrams and country examples are provided to illustrate each system.Continental drift
Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together in a super continent called Pangaea before drifting apart to their current locations. Wegener's theory was initially rejected because he could not explain the driving force behind continental movement. Evidence that later emerged in support of continental drift includes: matching fossil and rock formations between continents, matching climate zones in pole and equatorial regions, and magnetic pole reversal patterns in ocean floor sediments. This evidence helped prove that continents have shifted positions over time.
Sea floor spreading
1) The Mid-Ocean Ridge system circles the Earth along the ocean floor and is over 56,000 km long. It forms at divergent plate boundaries where new oceanic crust is continually being formed.
2) Scientists use sonar to map the ocean floor and study its features like the Mid-Ocean Ridge. Sonar bounces sound waves off underwater objects to image the seafloor.
3) Evidence like magnetic stripes in ocean crust and samples dug from the seafloor support the theory of sea floor spreading, where new crust forms at ridges and spreads out over time.
Earths structure
The document discusses the four main layers of the Earth - the crust, mantle, outer core, and inner core. It explains that the crust is the outermost layer and includes both continental and oceanic crust, with oceanic crust being denser. The mantle is below the crust and contains hot, dense rock. The outer core is a liquid layer surrounding the solid inner core, where extreme pressure causes iron and nickel atoms to remain solid.
Geologic time magazine
This document outlines the requirements for a group project where students work with a partner to create a magazine. Each person must complete two 20 point activities and one 10 point activity by certain checkpoint dates. They must also turn in their completed magazine by October 15th, which can include different formats like articles, interviews, or political cartoons, but each format can only be used once and one activity must use a longer writing format.
Geological time scale
The document summarizes the geologic time scale, which is divided into eras, periods, and epochs based on fossil evidence showing changes in Earth's organisms over its 4.56 billion year history. The largest divisions are eras, including Precambrian, Paleozoic, Mesozoic, and current Cenozoic. Each era is characterized by the dominant lifeforms and events of that time period. The geologic time scale helps break up Earth's history into more manageable chunks for study.
Fossils
Fossils are the remains or traces of prehistoric life found in sedimentary rocks. The type of fossil formed depends on how and where the organism died and was buried. Fossils can be unaltered remains like teeth and shells, or altered remains that have changed over time through processes like petrification or carbonization. Trace fossils provide indirect evidence of prehistoric life through things like tracks, burrows, and coprolites. Fossils are important for interpreting ancient environments and changes over time.
Relative and absolute dating
The document discusses methods for dating geological materials and events. Relative dating methods, like the law of superposition and index fossils, are used to determine the sequence of events but not calculate specific ages. Absolute dating methods, such as radiocarbon dating, are used to determine specific numerical ages by measuring radioactive decay. Radiocarbon dating works by comparing the ratio of carbon-14 to carbon-12 in once-living materials, as carbon-14 decays at a known rate. Together, relative and absolute dating methods provide information about the timing of geological events and processes.
Paleontology and uniformitariansm
Paleontology is the study of past life through the examination of plant and animal fossils. Paleontologists study fossils and the environments they formed in to piece together details about past ecosystems. The principle of uniformitarianism, first developed by James Hutton in 1788, holds that the same geological processes shaping Earth today have operated throughout its history. This theory helped establish that Earth is much older than previously believed. Relative dating methods like the law of superposition and use of index fossils allow paleontologists to determine the sequential order of geological events and changing life forms without knowing exact time periods.
BIOLOGY NATIONAL EXAMINATION COUNCIL (NECO) 2024 PRACTICAL MANUAL.pptx
Practical manual for National Examination Council, Nigeria.
Contains guides on answering questions on the specimens provided
Andreas Schleicher presents PISA 2022 Volume III - Creative Thinking - 18 Jun...
Andreas Schleicher, Director of Education and Skills at the OECD presents at the launch of PISA 2022 Volume III - Creative Minds, Creative Schools on 18 June 2024.
More Related Content
More from North Gwinnett Middle School
European economies
The document compares the economies of the United Kingdom, Germany, and Russia. The UK has a mixed market economy and is one of the world's leading industrial powers, with major industries including machinery, vehicles, chemicals, and food processing. Germany has the largest economy in Europe and is third largest in the world, with industries like iron, steel, chemicals, vehicles, and machinery. Russia has a mixed economy moving from communist command to market principles; it has a large natural resource base but exploitation is challenging due to climate and infrastructure.
Deformation
The video discusses the different types of forces that can act on and deform the Earth's crust, including compression, tension, and shearing. Compression causes squeezing and folding of rocks to form structures like anticlines and synclines. Tension causes pulling apart and thinning of the crust to form rift valleys. Shearing causes twisting and tearing of rocks. Different rock types and environmental conditions influence whether the crust folds or faults under geological forces.
Volcanoes
Volcanoes form where magma reaches the Earth's surface through openings called vents. There are several types of volcanoes defined by their eruptive activity and structure. Cinder cones have short eruptions that build steep slopes from ejected cinders. Shield volcanoes have long-lasting eruptions that spread lava over large areas to form broad dome shapes like Hawaii's Mauna Loa. Composite volcanoes like Italy's Mount Etna are made of layers from violent and quiet eruptions. Volcanoes can be classified as active if currently erupting, dormant if not currently erupting but historically active, or extinct if no known eruptions in history. Most volcanism occurs along zones of
Seismic waves
Deep underground, rocks are under constant pressure until the strain becomes too great and the rocks suddenly break, releasing seismic waves. These waves travel outward from the hypocenter in three types - P waves which push and pull, S waves which move sides to side, and L waves which cause surfaces to bob up and down. When recorded by a seismograph, the first indication of an earthquake is typically the P waves, followed by larger S waves, with surface L waves arriving last.
Earthquakes
An earthquake is caused by the sudden movement of parts of the Earth's crust and results in shaking and trembling of the ground. There are over one million earthquakes each year, with around twenty having the potential to cause severe damage. Earthquakes are caused by faults in the Earth's crust, such as the San Andreas Fault in California where the land west of the fault moves north and the land east moves south. Underwater earthquakes can generate destructive tsunamis. The focus is the depth below the surface where the earthquake occurs, and the epicenter is directly above on the surface. Seismographs detect seismic waves that travel out from the epicenter, including fast P waves and slower S waves.
Deformation
The video discusses the different forces that act on the earth's crust and how they cause deformation through various mechanisms. Compression causes squeezing and increases density, tension causes pulling and decreases density, and shearing causes twisting. These forces result in fracturing, faulting, and folding of rocks in the crust. Fractures are cracks, faults are cracks with lateral movement, and folds are bends in rock layers. Anticlines are upward folds and synclines are downward folds. Various factors like temperature, pressure, rock type, and rate of force application determine whether rocks fault or fold when subjected to deformation.
European governments
The document summarizes the government and political systems of the United Kingdom, Germany, and Russia. It describes that the UK has a Parliament with two houses, the House of Commons and House of Lords, and citizens elect members of Commons while Lords are inherited titles. Germany is a federal republic with a Chancellor as head of government and largely ceremonial President. Russia transitioned to a federal republic after the Soviet fall, with a dominant presidential system and a two-chamber Parliament.
Plate tectonics review #2
The document discusses different types of plate boundaries, including divergent boundaries where plates move apart, such as at mid-ocean ridges which form undersea mountain ranges as oceanic crust spreads away from the ridge. It also describes transform boundaries where plates slide past each other in opposite directions, such as at the San Andreas Fault in California.
Plate tectonics review
The plates are moving at a very slow rate of between one to ten centimeters per year. In some areas plates are moving together through a process called convergence, while in other areas they are moving apart. There are three main types of convergent boundaries: continental-continental, continental-oceanic, and oceanic-oceanic. At convergent boundaries, one plate dives beneath the other through subduction, which can cause volcanic activity at the surface.
Plate tectonics
The document discusses the theory of plate tectonics. It explains that the Earth's lithosphere is broken into plates that move slowly over time due to convection currents in the mantle. There are three types of plate boundaries: divergent boundaries where plates move apart, convergent boundaries where they move together, and transform boundaries where plates slip past each other.
Systems of government powerpoint (unitary, confederation, federal)updated 2010
Systems of government powerpoint (unitary, confederation, federal)updated 2010North Gwinnett Middle School
This document discusses different systems of government and how power is distributed in each. It begins by asking the reader to identify the different levels of government where they live. It then explains that governments are organized to protect citizens and manage conflict. There are different types of governments like democracies, republics, and monarchies. Geographers study the types of governments and how power is distributed through systems. The main systems are unitary, confederation, and federal. Unitary governments have one central power. Confederation governments give some power to members. Federal governments share power between a central and state/provincial governments. Diagrams and country examples are provided to illustrate each system.Continental drift
Alfred Wegener first proposed the theory of continental drift, which suggested that the continents were once joined together in a super continent called Pangaea before drifting apart to their current locations. Wegener's theory was initially rejected because he could not explain the driving force behind continental movement. Evidence that later emerged in support of continental drift includes: matching fossil and rock formations between continents, matching climate zones in pole and equatorial regions, and magnetic pole reversal patterns in ocean floor sediments. This evidence helped prove that continents have shifted positions over time.
Sea floor spreading
1) The Mid-Ocean Ridge system circles the Earth along the ocean floor and is over 56,000 km long. It forms at divergent plate boundaries where new oceanic crust is continually being formed.
2) Scientists use sonar to map the ocean floor and study its features like the Mid-Ocean Ridge. Sonar bounces sound waves off underwater objects to image the seafloor.
3) Evidence like magnetic stripes in ocean crust and samples dug from the seafloor support the theory of sea floor spreading, where new crust forms at ridges and spreads out over time.
Earths structure
The document discusses the four main layers of the Earth - the crust, mantle, outer core, and inner core. It explains that the crust is the outermost layer and includes both continental and oceanic crust, with oceanic crust being denser. The mantle is below the crust and contains hot, dense rock. The outer core is a liquid layer surrounding the solid inner core, where extreme pressure causes iron and nickel atoms to remain solid.
Geologic time magazine
This document outlines the requirements for a group project where students work with a partner to create a magazine. Each person must complete two 20 point activities and one 10 point activity by certain checkpoint dates. They must also turn in their completed magazine by October 15th, which can include different formats like articles, interviews, or political cartoons, but each format can only be used once and one activity must use a longer writing format.
Geological time scale
The document summarizes the geologic time scale, which is divided into eras, periods, and epochs based on fossil evidence showing changes in Earth's organisms over its 4.56 billion year history. The largest divisions are eras, including Precambrian, Paleozoic, Mesozoic, and current Cenozoic. Each era is characterized by the dominant lifeforms and events of that time period. The geologic time scale helps break up Earth's history into more manageable chunks for study.
Fossils
Fossils are the remains or traces of prehistoric life found in sedimentary rocks. The type of fossil formed depends on how and where the organism died and was buried. Fossils can be unaltered remains like teeth and shells, or altered remains that have changed over time through processes like petrification or carbonization. Trace fossils provide indirect evidence of prehistoric life through things like tracks, burrows, and coprolites. Fossils are important for interpreting ancient environments and changes over time.
Relative and absolute dating
The document discusses methods for dating geological materials and events. Relative dating methods, like the law of superposition and index fossils, are used to determine the sequence of events but not calculate specific ages. Absolute dating methods, such as radiocarbon dating, are used to determine specific numerical ages by measuring radioactive decay. Radiocarbon dating works by comparing the ratio of carbon-14 to carbon-12 in once-living materials, as carbon-14 decays at a known rate. Together, relative and absolute dating methods provide information about the timing of geological events and processes.
Paleontology and uniformitariansm
Paleontology is the study of past life through the examination of plant and animal fossils. Paleontologists study fossils and the environments they formed in to piece together details about past ecosystems. The principle of uniformitarianism, first developed by James Hutton in 1788, holds that the same geological processes shaping Earth today have operated throughout its history. This theory helped establish that Earth is much older than previously believed. Relative dating methods like the law of superposition and use of index fossils allow paleontologists to determine the sequential order of geological events and changing life forms without knowing exact time periods.
More from North Gwinnett Middle School (20)
Systems of government powerpoint (unitary, confederation, federal)updated 2010
Systems of government powerpoint (unitary, confederation, federal)updated 2010
Recently uploaded
BIOLOGY NATIONAL EXAMINATION COUNCIL (NECO) 2024 PRACTICAL MANUAL.pptx
Practical manual for National Examination Council, Nigeria.
Contains guides on answering questions on the specimens provided
Andreas Schleicher presents PISA 2022 Volume III - Creative Thinking - 18 Jun...
Andreas Schleicher, Director of Education and Skills at the OECD presents at the launch of PISA 2022 Volume III - Creative Minds, Creative Schools on 18 June 2024.
How Barcodes Can Be Leveraged Within Odoo 17
In this presentation, we will explore how barcodes can be leveraged within Odoo 17 to streamline our manufacturing processes. We will cover the configuration steps, how to utilize barcodes in different manufacturing scenarios, and the overall benefits of implementing this technology.
HYPERTENSION - SLIDE SHARE PRESENTATION.
IT WILL BE HELPFULL FOR THE NUSING STUDENTS
IT FOCUSED ON MEDICAL MANAGEMENT AND NURSING MANAGEMENT.
HIGHLIGHTS ON HEALTH EDUCATION.
CHUYÊN ĐỀ ÔN TẬP VÀ PHÁT TRIỂN CÂU HỎI TRONG ĐỀ MINH HỌA THI TỐT NGHIỆP THPT ...
CHUYÊN ĐỀ ÔN TẬP VÀ PHÁT TRIỂN CÂU HỎI TRONG ĐỀ MINH HỌA THI TỐT NGHIỆP THPT ...Nguyen Thanh Tu Collection
https://app.box.com/s/qspvswamcohjtbvbbhjad04lg65waylfElevate Your Nonprofit's Online Presence_ A Guide to Effective SEO Strategies...
Whether you're new to SEO or looking to refine your existing strategies, this webinar will provide you with actionable insights and practical tips to elevate your nonprofit's online presence.
Jemison, MacLaughlin, and Majumder "Broadening Pathways for Editors and Authors"
Jemison, MacLaughlin, and Majumder "Broadening Pathways for Editors and Authors"National Information Standards Organization (NISO)
This presentation was provided by Racquel Jemison, Ph.D., Christina MacLaughlin, Ph.D., and Paulomi Majumder. Ph.D., all of the American Chemical Society, for the second session of NISO's 2024 Training Series "DEIA in the Scholarly Landscape." Session Two: 'Expanding Pathways to Publishing Careers,' was held June 13, 2024.RHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
Physical pharmaceutics notes for B.pharm students
Wound healing PPT
This document provides an overview of wound healing, its functions, stages, mechanisms, factors affecting it, and complications.
A wound is a break in the integrity of the skin or tissues, which may be associated with disruption of the structure and function.
Healing is the body’s response to injury in an attempt to restore normal structure and functions.
Healing can occur in two ways: Regeneration and Repair
There are 4 phases of wound healing: hemostasis, inflammation, proliferation, and remodeling. This document also describes the mechanism of wound healing. Factors that affect healing include infection, uncontrolled diabetes, poor nutrition, age, anemia, the presence of foreign bodies, etc.
Complications of wound healing like infection, hyperpigmentation of scar, contractures, and keloid formation.
Temple of Asclepius in Thrace. Excavation results
The temple and the sanctuary around were dedicated to Asklepios Zmidrenus. This name has been known since 1875 when an inscription dedicated to him was discovered in Rome. The inscription is dated in 227 AD and was left by soldiers originating from the city of Philippopolis (modern Plovdiv).
How to Predict Vendor Bill Product in Odoo 17
This slide will guide us through the process of predicting vendor bill products based on previous purchases from the vendor in Odoo 17.
Recently uploaded (20)
BIOLOGY NATIONAL EXAMINATION COUNCIL (NECO) 2024 PRACTICAL MANUAL.pptx
BIOLOGY NATIONAL EXAMINATION COUNCIL (NECO) 2024 PRACTICAL MANUAL.pptx
Andreas Schleicher presents PISA 2022 Volume III - Creative Thinking - 18 Jun...
Andreas Schleicher presents PISA 2022 Volume III - Creative Thinking - 18 Jun...
REASIGNACION 2024 UGEL CHUPACA 2024 UGEL CHUPACA.pdf
REASIGNACION 2024 UGEL CHUPACA 2024 UGEL CHUPACA.pdf
CHUYÊN ĐỀ ÔN TẬP VÀ PHÁT TRIỂN CÂU HỎI TRONG ĐỀ MINH HỌA THI TỐT NGHIỆP THPT ...
CHUYÊN ĐỀ ÔN TẬP VÀ PHÁT TRIỂN CÂU HỎI TRONG ĐỀ MINH HỌA THI TỐT NGHIỆP THPT ...
Elevate Your Nonprofit's Online Presence_ A Guide to Effective SEO Strategies...
Elevate Your Nonprofit's Online Presence_ A Guide to Effective SEO Strategies...
Jemison, MacLaughlin, and Majumder "Broadening Pathways for Editors and Authors"
Jemison, MacLaughlin, and Majumder "Broadening Pathways for Editors and Authors"
NEWSPAPERS - QUESTION 1 - REVISION POWERPOINT.pptx
NEWSPAPERS - QUESTION 1 - REVISION POWERPOINT.pptx
RHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
RHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
Introduction to europe's history extension
- 1. European History Picture Timeline Extension Directions
- 2. Step 1: Create a timeline. • Fold computer paper “hotdog” style. • Draw a line down the center of your paper. • Write your name on the back of your paper. • Title your paper Events in TITLE European History Before Exploration.
- 3. Step 2: Mark events on timeline. Event #1 Event #3 Event #2
- 4. Step 3: Draw an illustration representing each event. I LOVE being Greek! Event #1 Event #3 Event #2
- 5. Step 4: Color your illustrations. I LOVE being Greek! Event #1 Event #3 Event #2
- 6. Timeline Events 1. 776 B.C. the First Greek Olympic Games 2. 356 B.C. Alexander the Great is born 3. 44 B.C. Julius Caesar is assassinated 4. 476 A.D. Roman Empire falls 5. 1096 A.D. First Crusade begins 6. 1348 A.D. Black Plague hits Europe 7. 1350(ish) A.D. Renaissance begins in Italy 8. 1517 A.D. Protestant Reformation begins 9. 1450 A.D. Prince Henry funds navigation improvements 10. 1492 A.D. Christopher Columbus sets sail