This document discusses plate tectonics and the movement of tectonic plates. It provides evidence that supports plate tectonics including: the fit of continental landmasses, matching rock and fossil distributions, and magnetic reversals recorded in ocean crust. It describes the three main plate boundaries and associated landforms: divergent boundaries form mid-ocean ridges and rift valleys, convergent boundaries result in subduction zones and volcanic mountain ranges, and transform boundaries create strike-slip faults. Earthquakes and tsunamis are hazardous events caused by the movement and interactions of tectonic plates. Volcanoes form at plate boundaries and hotspots as magma rises up due to pressure in the crust and mantle.
This document discusses plate tectonics and the structure of the Earth. It describes the four main layers of the Earth - crust, mantle, outer core, and inner core. It explains Alfred Wegener's theory of Pangaea and continental drift. It provides evidence that supports plate tectonics including matching continents, matching rock types and fossils, and seismic activity. It describes the three main types of plate boundaries and the associated geological features - divergent, convergent, and transform. It discusses what causes plates to move via convection currents in the mantle.
This document summarizes information from a textbook about earth science topics including the structure of the earth, plate tectonics, rocks, weathering and erosion, glaciation, climate and weather. It contains questions and answers on these topics. Key points include:
- The three layers of the earth are the crust, mantle and core. Plates move around on the mantle and collide or separate.
- Weathering breaks rocks down through mechanical and chemical processes. Erosion then transports the weathered material.
- Glaciers shape the landscape through erosion and deposition, forming features like cirques, moraines and drumlins.
- Climate is influenced by factors like latitude, prevailing winds, altitude and proximity
EARTH MATERIALS AND PROCESSES
Topic: Classification of Rocks / Types of Rocks
Senior High School | Earth and Life Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11/12ES-Ib-10)
Senior High School | Earth Science
Learning Competency: Classify rocks into igneous, sedimentary, and metamorphic. (S11ES-Ic-6)
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The document discusses the three main types of rocks - igneous, sedimentary, and metamorphic. It describes the rock cycle by which rocks are formed from magma and transformed through weathering, sedimentation, and metamorphism. Key examples of rock types are discussed such as granite, limestone, chalk, slate, and marble.
The document summarizes key aspects of Earth science:
1) The Earth system consists of four main components - hydrosphere, atmosphere, biosphere, and geosphere.
2) The Earth has layers including the crust, mantle, and core. Rocks form through igneous, sedimentary, and metamorphic processes.
3) Endogenic and exogenic processes shape the Earth, including plate tectonics, volcanism, earthquakes, and weathering.
4) Geohazards result from these processes and include volcanoes, earthquakes, tsunamis, and landslides. Technology helps monitor and warn of geohazards.
The three main types, or classes, of rock are sedimentary, metamorphic, and igneous and the differences among them have to do with how they are formed. Sedimentary rocks are formed from particles of sand, shells, pebbles, and other fragments of material. Together, all these particles are called sediment.
The document discusses plate tectonics and how it has shaped the Earth's surface over geologic time. It describes how the Earth's crust is made up of large plates that move over convection currents in the mantle. When plates diverge new crust forms as magma rises, and when they converge mountains can form through collision or subduction zones can create volcanoes. It then outlines the four eras of geologic time - Precambrian, Paleozoic, Mesozoic, and Cenozoic - and some of the key events and lifeforms that emerged during each era, which ultimately gave the Earth its current shape and features through mountain building and erosion.
The rock cycle describes how rocks are formed from magma or other existing rocks and changed over time through geological processes. Igneous rocks form from cooling magma, metamorphic rocks form under heat and pressure, and sedimentary rocks form through the weathering of other rocks and deposition of sediments. Rocks are constantly changing between these three types as they move through the rock cycle.
The document discusses the rock cycle and the relationships between the three main rock groups: igneous, sedimentary, and metamorphic. Igneous rocks form from magma, either slowly below ground as plutonic rocks or quickly at the surface as volcanic rocks. Sedimentary rocks form at the surface from eroded materials that are transported and deposited. Metamorphic rocks form from changes to existing rocks through pressure, temperature, and fluids deep underground. The rock cycle is powered by the Earth's interior heat and momentum, as well as energy from the sun, and involves surface and subsurface geological processes that connect the hydrologic and tectonic cycles.
This document discusses the structural study of plutons and plugs. It defines plutons as large igneous rock bodies that formed below the Earth's surface as magma slowly cooled. Plutons can be of various sizes and shapes. The structural study of plutons involves examining their internal structure, shape and size, and structural relationship to surrounding rocks. Specific types of plutons discussed include batholiths, laccoliths, lopoliths, sills, dikes, and ring dikes. Plugs are described as volcanic necks eroded away at the root of volcanoes.
This document provides an overview of earth materials, geologic time, movements of the continents, tectonic forces, and gradational and erosional processes that shape landforms and landform regions. It describes the three main types of rocks - igneous, sedimentary, and metamorphic - and how they are formed. It also explains plate tectonics theory and how the movement of tectonic plates results in diverse landforms and geological phenomena like earthquakes and volcanoes globally.
Earth Materials and Processes : ENDOGENIC PROCESSSimple ABbieC
Earth Materials and Processes : ENDOGENIC PROCESS
Content Standard:
The learners demonstrate an understanding of:
geologic processes that occur within the Earth and
the folding and faulting of rocks
Here are the answers to the questions from the passages:
P226 –
1. Igneous, sedimentary, metamorphic
2. Sedimentary rocks form from sediments
3. Sedimentary rocks can tell us about the environment they were deposited in, such as depth of water or presence of fossils
5. Metamorphic rocks form when existing rocks are subjected to heat and pressure
8. During metamorphism, the mineral grains in sedimentary and igneous rocks recrystallize and change shape
P232 –
1. Intrusive igneous rocks form when magma cools and solidifies within the earth's crust
2. Extrusive igne
Prentice Hall Earth Science ch05 Weathering & ErosionTim Corner
This document discusses weathering and erosion. It defines weathering as the breaking down of rocks into smaller pieces through mechanical or chemical processes. Mechanical weathering occurs via physical forces like frost wedging and does not alter the rock's composition. Chemical weathering alters the rock through chemical reactions with water, oxygen, carbon dioxide, living organisms, and acid rain. Erosion is the movement and transport of weathered rock by forces like wind, water and gravity. The Grand Canyon formed through erosion by the Colorado River over millions of years.
This document describes rocks and the rock cycle. It defines rocks as mixtures of minerals or organic matter. The rock cycle describes how rocks constantly form from old rock material and change from one type to another through geological processes like weathering, erosion, deposition, heat, and pressure. These processes shape Earth's features and influence the types of rocks found in different areas. Rocks are classified into three main types - igneous, sedimentary, and metamorphic - based on their composition and texture.
Minerals are naturally occurring inorganic substances that make up rocks. They form through three main processes: magmatic, sedimentary, and metamorphic. Rocks are composed of minerals or organic materials and also form through igneous, sedimentary, and metamorphic processes. The Earth's interior is composed of layers including the crust, mantle, outer core, and inner core. Earthquakes occur along faults in the Earth's crust as the blocks of rock on either side move and release energy.
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
Design Steps for Earthquake Resistant StructuresIshan Garg
This document provides information about earthquakes and their causes. It discusses what earthquakes are, how they are caused by the movement of tectonic plates along faults, and defines key terms like epicenter. It describes the interior structure of the Earth and plate tectonics. Safety procedures during earthquakes are outlined. The types of earthquake waves and how they are measured on seismographs is explained. Finally, it discusses earthquake magnitude scales and seismic zoning in India.
Convection currents in the Earth's mantle and the movement of tectonic plates apply stress to the crust, causing it to break along faults or fold. This movement is responsible for earthquakes and volcanic activity, often occurring at plate boundaries. When stress exceeds rock strength, it releases suddenly in earthquakes. Seismic waves from quakes travel through the Earth and can be recorded on seismographs. Magma rises from hot spots in the mantle and at plate boundaries, fueling volcanic eruptions at the surface that pose hazards through lava flows, ash falls, and pyroclastic flows.
This document provides information about plate tectonics and the dynamics of the Earth. It discusses key topics such as continental drift, Earth's layered structure, types of plate boundaries including convergent, divergent and transform boundaries, seafloor spreading, plate motions, and forces driving plate tectonics. The objectives are to understand concepts like continental drift, Earth's structure, plate margins, seafloor spreading, how plates move on the surface of the sphere, and driving forces. Diagrams and figures are included to illustrate these topics.
This document provides information about plate tectonics and earthquakes. It defines key terms related to plate tectonics like continental drift, plates, mantle convection, and plate boundaries. It describes the three main types of plate boundaries: convergent where plates push together, divergent where they pull apart, and transform where they slide past each other. Evidence for plate tectonics includes matching continents, matching fossils, magnetic reversals in ocean floors, and crustal deformations. The document also defines earthquake terms and describes how seismic waves are used to determine the location and size of quakes.
According to the theory of plate tectonics:
- The Earth's crust is broken into plates that slowly move over time;
- Plates interact at boundaries where they can collide, pull apart, or slide past one another;
- These interactions are responsible for geologic events like earthquakes, volcanoes, and mountain building.
This document discusses elements of seismology and earthquake engineering. It covers topics such as causes of earthquakes including plate tectonic theory, elastic rebound theory, types of seismic waves, measurement of earthquakes through seismographs, magnitude and intensity scales, and characteristics of strong ground motion. Key concepts are the different types of plate boundaries that can cause earthquakes, as well as the different types of seismic waves like P, S, love, and rayleigh waves that radiate from earthquake sources.
Earth's dynamics, from Continental Drift to Global Tectonics.doctormaranon
The document summarizes the theory of plate tectonics. It describes early evidence from continental drift and how modern evidence established the theory during the 20th century. This includes seismometer networks, mapping ocean floors, dating oceanic rocks, and paleomagnetism studies. The theory proposes that lithospheric plates are dynamic, with new plates generated at mid-ocean ridges and old plates subducting at trenches. There are three types of plate boundaries: divergent where plates spread apart, convergent where they collide, and transform where they slide past each other. This cyclical process can be modeled by the Wilson cycle of supercontinent breakup and reunification over geological time.
Earth's dynamics. Plate Tectonics for secondary education.doctormaranon
The document summarizes the theory of plate tectonics. It describes early evidence from continental drift and how modern evidence established the theory during the 20th century. This includes seismometer networks, mapping ocean floors, dating oceanic rocks, and paleomagnetism studies. The theory proposes that lithospheric plates are dynamic, with new plates generated at divergent boundaries and old plates destroyed at convergent boundaries. Main plate boundaries are divergent, convergent, and transform. Convergent boundaries result in subduction and mountain building. Plates have moved in cycles of supercontinent assembly and breakup over geologic time.
The document summarizes key concepts in plate tectonics including:
1) The Earth's interior is divided into layers based on composition and physical state, including the crust, mantle, and core.
2) Seismic waves provide evidence of discontinuities between layers like the Mohorovicic discontinuity between the crust and mantle.
3) Early theories proposed continental drift but plate tectonics explains the movement of lithospheric plates at boundaries like divergent boundaries that create ocean floor.
The document discusses plate tectonics and the structure of the Earth. It describes how seismic waves can reveal layers inside the Earth like the crust, mantle, and core. It explains continental drift and how the theory of plate tectonics developed. Plates move at boundaries where they can spread apart, collide, or slide past each other, causing earthquakes and building landforms.
The document summarizes the theory of plate tectonics. It explains that the Earth's crust is broken into plates that are constantly moving due to convection currents in the mantle. There are three main types of plate boundaries: divergent where plates pull apart and new crust is formed; convergent where plates crash together and can cause volcanic activity and mountain building; and transform where plates slide past each other and can cause earthquakes. The theory integrated the earlier concepts of continental drift, which proposed the slow drifting of continents, and seafloor spreading, which showed new crust was forming under the oceans. Together, these theories explained how plate tectonics shapes the Earth's surface over millions of years through volcanic and seismic activity
The document summarizes the theory of plate tectonics. It explains that the Earth's crust is broken into plates that are constantly moving due to convection currents in the mantle. There are three main types of plate boundaries: divergent where plates pull apart and new crust is formed, convergent where plates crash together forming mountains or one plate slides under the other, and transform where plates slide past each other causing earthquakes. The theory developed from the theories of continental drift proposing the splitting of Pangaea and seafloor spreading explaining the patterns of aging rocks in the oceans. Together these theories explained how plate motions and interactions at their boundaries shape the Earth's surface over millions of years.
The document summarizes the composition and layers of Earth's geosphere. It describes the geosphere as consisting of the crust, mantle, and core. The crust and upper mantle make up the lithosphere, which is divided into tectonic plates. Plate tectonics, earthquakes, volcanoes, and erosion are geologic processes that shape the Earth's surface.
Earthquake Engineering Earthquake and Ground Motionodysonsantos3
The document discusses the interior structure of the Earth and causes of earthquakes. It describes the Earth's core, mantle, crust, and Moho discontinuity. The elastic rebound theory and plate tectonic theory are explained as the two main causes of earthquakes. Elastic rebound theory states that earthquakes occur due to a sudden release of built-up strain along faults, while plate tectonic theory attributes quakes to the movement and interactions of tectonic plates. Three types of plate boundaries are also summarized: divergent, convergent, and transform.
Plate tectonics involves the slow movement of tectonic plates across the Earth's surface, driven by convection currents in the mantle. Alfred Wegener first proposed continental drift in 1915, but it was not until the 1960s that seafloor spreading provided evidence that plates move independently. There are 7 major and many minor tectonic plates that either move apart at mid-ocean ridges or come together, causing earthquakes and volcanic activity at plate boundaries. Hazards are greatest where plates meet and include earthquakes, tsunamis, and eruptions that depend on the plate boundary setting and composition of the colliding plates.
Here are three questions from the section with the answers:
1. What causes convection currents in the mantle?
- Convection currents in the Earth are caused by the Earth's hot inner core heating the magma within the mantle.
2. What is a fault?
- A fault is a fracture, or break, in Earth's lithosphere. Rocks on either side can slide slowly along the fault or stick together, building stress until releasing in an earthquake.
3. Where do most earthquakes occur?
- About 80% of all earthquakes occur in a belt around the edges of the Pacific Ocean, near plate boundaries like the San Andreas Fault where the North American and Pacific plates meet.
This document discusses natural hazards caused by tectonic and climate-related events. It provides details on the internal structure of the Earth, including the crust and mantle. It then focuses on plate tectonics, explaining the three main types of plate boundaries and associated landforms. Specific examples are given for each plate boundary type. The document also addresses causes of earthquakes and their impacts, as well as types and characteristics of volcanoes.
1. The document discusses causes and predictions of earthquakes, summarizing their occurrence throughout history and defining key terms like focus, epicenter, magnitude, and intensity.
2. Major factors that cause earthquakes are the movement of tectonic plates and release of energy from within the Earth. Earthquakes typically occur along plate boundaries and faults in the lithosphere.
3. While long term earthquake predictions are possible based on historical patterns of activity, short term reliable prediction remains elusive given the unpredictability of the natural world. Preparedness through building codes, emergency planning, and public education can help mitigate damage from earthquakes.
1) The document discusses various weather phenomena including air pressure systems, wind, storms, and hurricanes. It describes how weather is measured and influenced by factors like pressure gradients, temperature differences, and the Coriolis effect.
2) Key terms are defined for various weather systems like high and low pressure areas, warm and cold fronts, and how they influence weather patterns. Different air mass types are also introduced.
3) Hazards from severe weather events like thunderstorms, tornadoes, and hurricanes are covered along with safety measures during such events. Historic storms like Katrina are summarized.
1. The document discusses various weather phenomena including air pressure, wind, air masses, fronts, and storms. It provides definitions and explanations of these concepts.
2. Key terms that are defined include high and low pressure systems, isobars, warm and cold fronts, thunderstorms, tornadoes, and hurricanes. Measurement tools like barometers and anemometers are also explained.
3. Visuals like diagrams and videos are referenced throughout to enhance understanding of complex weather patterns and interactions between different elements.
This document provides an overview of water quality and water systems. It discusses surface water features like rivers, watersheds, and groundwater. It explains the water cycle and how humans have altered it. Water quality is impacted by pollution, which can be from point sources like factories or non-point sources like urban runoff. Water is monitored through physical, chemical, and biological indicators. The document also summarizes specific issues with the Yadkin River watershed, including pollution from coal ash dumps, fracking, and GenX chemical contamination.
Water and Soil: Hydrosphere 2 Energy in WaterRobin Seamon
1) The document discusses the distribution and chemistry of Earth's oceans. 70% of Earth's surface is covered by oceans, which originally formed as one ocean but are now divided into five major basins.
2) It also describes ocean temperatures, currents, and how thermal and saline gradients drive global ocean circulation. Surface currents are wind-driven while deep currents are driven by water density from temperature and salt content.
3) The water and carbon cycles are interconnected as oceans absorb carbon dioxide from the atmosphere, regulating Earth's climate over long timescales. Chemical and physical weathering processes interact with oceans to shape the lithosphere.
The document provides an overview of key concepts related to biosphere and ecosystems. It discusses how the biosphere consists of biotic and abiotic factors that interact within different levels of organization from species to ecosystems. Energy and matter cycle through the biosphere, with the sun being the main source of energy that enters through photosynthesis and is transferred through food webs. Human activities can impact biodiversity by threatening keystone species and introducing invasive species. Maintaining biodiversity is important for healthy functioning of ecosystems.
1. The document provides definitions and questions about various topics in astronomy and earth science. It defines nuclear fusion and fission, and asks about the sun's phase and forms of energy transfer.
2. Questions are also asked about the Milankovich cycles, specifically eccentricity, axial tilt variations, and orbital variations that impact climate over long timescales.
3. Additional questions cover the shape of the Earth, and which materials (ocean, air, land) heat up faster.
This document contains two unit check questions about various scientific concepts:
1. The first section asks the student to identify concepts like nuclear fusion, nebula, electromagnetic radiation, and which phase the sun is currently in (main sequence).
2. The second section asks the student to identify the Milankovich cycle of eccentricity and the shape of the Earth as an oblate spheroid. It also asks which materials (ocean, air, land) heat faster.
3. The third section asks the student to label the interaction between solar wind and Earth's magnetic field that creates the aurora.
1. Copernicus proposed that the Sun, not Earth, was the center of the universe.
2. Galileo made important astronomical observations of the moon, planets, and stars using a telescope.
3. Ptolemy previously believed that everything revolved around the Earth.
1. The document discusses various hydrological concepts including erosion, sediment deposition, watersheds, discharge, load, gradient, porosity, permeability, turbidity, temperature, dissolved oxygen, pH, and nutrient pollution.
2. Key terms defined include discharge, load, gradient, porosity, permeability, and turbidity.
3. The effects of changes in discharge, load, and gradient on erosive energy are explored.
The document discusses the global water cycle and how it influences Earth's lithosphere. It describes various weathering processes like mechanical, chemical, and mass movement that break down rocks over time. Mechanical weathering is caused by ice, water, plants and animals while chemical weathering involves acidification and oxidation of minerals. Weathering rates depend on factors like climate, hardness of rock material, and surface area exposure. Erosion then transports weathered materials and deposits them elsewhere as sediments, shaping landscapes and forming geographic features over millions of years. Examples highlighted include the Grand Canyon, Death Valley, Great Sand Dunes, Arches, Antelope Canyon, Bryce Canyon, Zion Canyon, Carlsbad Caverns, Bad
This document provides information about water quality and issues affecting the Yadkin River watershed. It discusses how human activities like urbanization, agriculture, and industry introduce pollution into surface and groundwater sources. Specific issues impacting the Yadkin River watershed include high levels of nutrients and turbidity, toxic levels of mercury in fish, and coal ash spills from Duke Energy power plants contaminating the river. Maintaining water quality requires addressing both point source pollution from facilities and non-point source pollution from activities like construction and failing septic systems.
The document outlines the daily class schedule and various alternate schedules for Davie High School for the 2017-2018 school year. It includes the times for each class period under regular daily schedule with smart lunch, early release schedule, pep rally schedule, 2-hour delay schedule, 3-hour delay schedule. The regular daily schedule has 4 class periods from 8:15 AM to 3:25 PM with three lunch periods, while alternate schedules adjust class times and add or remove periods to accommodate things like pep rallies or delays.
This document provides an overview of different types of energy resources including fossil fuels, nuclear energy, and renewable resources. It discusses the science behind various energy production methods and summarizes pros and cons of each resource. Key points covered include how fossil fuels like coal, oil, and natural gas are non-renewable but currently provide most global energy, as well as safety and environmental issues associated with nuclear power and renewable alternatives like solar, wind, hydroelectric, geothermal and biomass energy. The document emphasizes the importance of sustainability and moving toward renewable resources.
This document discusses climate classification systems and the factors that cause climate change. It begins with an overview of weather versus climate and the Koppen climate classification system. The major climate types are then described in detail, including tropical, dry, mild, continental, and polar climates. Various natural and human factors that can disrupt climate patterns are outlined, such as solar activity, volcanic eruptions, greenhouse gases, and deforestation. Evidence of past climate changes is examined through paleoclimate research techniques. Feedback mechanisms are described that can amplify the impacts of initial changes.
This document provides an overview of water quality and sources. It discusses the water cycle, surface water features like rivers and watersheds, and groundwater systems like aquifers. It then covers topics like water monitoring, pollution sources, and current issues affecting the Yadkin River watershed like urbanization, coal ash spills, and emerging contaminants like GenX. Videos and links are provided for additional information.
This Biology EOC study guide covers several topics:
1) Cell organelles such as the nucleus, plasma membrane, mitochondria, chloroplasts, and their functions. It also discusses prokaryotic and eukaryotic cells.
2) Homeostasis and transport processes in cells, including diffusion, osmosis, and active transport. The cell cycle and mitosis are also described.
3) Ecology topics like the carbon and nitrogen cycles, energy flow through ecosystems in the form of energy pyramids, and life functions of plants and animals like transport and gas exchange.
The document summarizes the geology of North Carolina through time. It describes how North Carolina began with the ancient Appalachian mountains forming 480 million years ago during the collision of tectonic plates that built the supercontinent Pangea. Erosion of these mountains contributed sediment that was deposited in inland seas, forming the Coastal Plain regions. Changing sea levels over millions of years shaped the coastline, including the barrier islands along the Outer Banks. The geology of North Carolina was ultimately determined by plate tectonics and weathering processes acting over hundreds of millions of years.
Cellular respiration uses glucose and oxygen to produce ATP, the "energy currency" of cells. It occurs in three main stages: glycolysis, the Krebs cycle, and the electron transport chain. Glycolysis occurs in the cytoplasm and produces a small amount of ATP. The Krebs cycle and electron transport chain take place in the mitochondria and generate most of the cell's ATP through aerobic respiration. When oxygen is limited, fermentation pathways produce a small amount of ATP without using oxygen.
1. The document discusses how energy from the sun is transferred through ecosystems via various processes like photosynthesis, chemosynthesis, and cellular respiration. It moves from autotrophs to heterotrophs through food chains and webs.
2. As energy moves up trophic levels from producers to primary, secondary, and tertiary consumers, 90% less energy is available at each level. Marine ecosystems tend to have more microscopic autotrophs while terrestrial ecosystems rely more on plant autotrophs and large herbivores.
3. Key biogeochemical cycles like carbon, nitrogen, and phosphorus are outlined as well as how pollutants can biomagnify up food chains. Biodiversity and human impacts
This document provides an overview of ecology and ecological organization. It discusses key terms like biotic and abiotic factors, and describes different levels of ecological organization from the biosphere down to species, populations, communities, and ecosystems. Relationships between organisms like competition, cooperation, predation, and symbiosis are also summarized. Adaptations and behaviors that help organisms survive, like structural adaptations, innate behaviors, and learned behaviors, are briefly covered.
How to Show Sample Data in Tree and Kanban View in Odoo 17Celine George
In Odoo 17, sample data serves as a valuable resource for users seeking to familiarize themselves with the functionalities and capabilities of the software prior to integrating their own information. In this slide we are going to discuss about how to show sample data to a tree view and a kanban view.
The Jewish Trinity : Sabbath,Shekinah and Sanctuary 4.pdfJackieSparrow3
we may assume that God created the cosmos to be his great temple, in which he rested after his creative work. Nevertheless, his special revelatory presence did not fill the entire earth yet, since it was his intention that his human vice-regent, whom he installed in the garden sanctuary, would extend worldwide the boundaries of that sanctuary and of God’s presence. Adam, of course, disobeyed this mandate, so that humanity no longer enjoyed God’s presence in the little localized garden. Consequently, the entire earth became infected with sin and idolatry in a way it had not been previously before the fall, while yet in its still imperfect newly created state. Therefore, the various expressions about God being unable to inhabit earthly structures are best understood, at least in part, by realizing that the old order and sanctuary have been tainted with sin and must be cleansed and recreated before God’s Shekinah presence, formerly limited to heaven and the holy of holies, can dwell universally throughout creation
Understanding and Interpreting Teachers’ TPACK for Teaching Multimodalities i...Neny Isharyanti
Presented as a plenary session in iTELL 2024 in Salatiga on 4 July 2024.
The plenary focuses on understanding and intepreting relevant TPACK competence for teachers to be adept in teaching multimodality in the digital age. It juxtaposes the results of research on multimodality with its contextual implementation in the teaching of English subject in the Indonesian Emancipated Curriculum.
Beginner's Guide to Bypassing Falco Container Runtime Security in Kubernetes ...anjaliinfosec
This presentation, crafted for the Kubernetes Village at BSides Bangalore 2024, delves into the essentials of bypassing Falco, a leading container runtime security solution in Kubernetes. Tailored for beginners, it covers fundamental concepts, practical techniques, and real-world examples to help you understand and navigate Falco's security mechanisms effectively. Ideal for developers, security professionals, and tech enthusiasts eager to enhance their expertise in Kubernetes security and container runtime defenses.
How to Configure Time Off Types in Odoo 17Celine George
Now we can take look into how to configure time off types in odoo 17 through this slide. Time-off types are used to grant or request different types of leave. Only then the authorities will have a clear view or a clear understanding of what kind of leave the employee is taking.
Ardra Nakshatra (आर्द्रा): Understanding its Effects and RemediesAstro Pathshala
Ardra Nakshatra, the sixth Nakshatra in Vedic astrology, spans from 6°40' to 20° in the Gemini zodiac sign. Governed by Rahu, the north lunar node, Ardra translates to "the moist one" or "the star of sorrow." Symbolized by a teardrop, it represents the transformational power of storms, bringing both destruction and renewal.
About Astro Pathshala
Astro Pathshala is a renowned astrology institute offering comprehensive astrology courses and personalized astrological consultations for over 20 years. Founded by Gurudev Sunil Vashist ji, Astro Pathshala has been a beacon of knowledge and guidance in the field of Vedic astrology. With a team of experienced astrologers, the institute provides in-depth courses that cover various aspects of astrology, including Nakshatras, planetary influences, and remedies. Whether you are a beginner seeking to learn astrology or someone looking for expert astrological advice, Astro Pathshala is dedicated to helping you navigate life's challenges and unlock your full potential through the ancient wisdom of Vedic astrology.
For more information about their courses and consultations, visit Astro Pathshala.
Views in Odoo - Advanced Views - Pivot View in Odoo 17Celine George
In Odoo, the pivot view is a graphical representation of data that allows users to analyze and summarize large datasets quickly. It's a powerful tool for generating insights from your business data.
The pivot view in Odoo is a valuable tool for analyzing and summarizing large datasets, helping you gain insights into your business operations.
Beyond the Advance Presentation for By the Book 9John Rodzvilla
In June 2020, L.L. McKinney, a Black author of young adult novels, began the #publishingpaidme hashtag to create a discussion on how the publishing industry treats Black authors: “what they’re paid. What the marketing is. How the books are treated. How one Black book not reaching its parameters casts a shadow on all Black books and all Black authors, and that’s not the same for our white counterparts.” (Grady 2020) McKinney’s call resulted in an online discussion across 65,000 tweets between authors of all races and the creation of a Google spreadsheet that collected information on over 2,000 titles.
While the conversation was originally meant to discuss the ethical value of book publishing, it became an economic assessment by authors of how publishers treated authors of color and women authors without a full analysis of the data collected. This paper would present the data collected from relevant tweets and the Google database to show not only the range of advances among participating authors split out by their race, gender, sexual orientation and the genre of their work, but also the publishers’ treatment of their titles in terms of deal announcements and pre-pub attention in industry publications. The paper is based on a multi-year project of cleaning and evaluating the collected data to assess what it reveals about the habits and strategies of American publishers in acquiring and promoting titles from a diverse group of authors across the literary, non-fiction, children’s, mystery, romance, and SFF genres.
Is Email Marketing Really Effective In 2024?Rakesh Jalan
Slide 1
Is Email Marketing Really Effective in 2024?
Yes, Email Marketing is still a great method for direct marketing.
Slide 2
In this article we will cover:
- What is Email Marketing?
- Pros and cons of Email Marketing.
- Tools available for Email Marketing.
- Ways to make Email Marketing effective.
Slide 3
What Is Email Marketing?
Using email to contact customers is called Email Marketing. It's a quiet and effective communication method. Mastering it can significantly boost business. In digital marketing, two long-term assets are your website and your email list. Social media apps may change, but your website and email list remain constant.
Slide 4
Types of Email Marketing:
1. Welcome Emails
2. Information Emails
3. Transactional Emails
4. Newsletter Emails
5. Lead Nurturing Emails
6. Sponsorship Emails
7. Sales Letter Emails
8. Re-Engagement Emails
9. Brand Story Emails
10. Review Request Emails
Slide 5
Advantages Of Email Marketing
1. Cost-Effective: Cheaper than other methods.
2. Easy: Simple to learn and use.
3. Targeted Audience: Reach your exact audience.
4. Detailed Messages: Convey clear, detailed messages.
5. Non-Disturbing: Less intrusive than social media.
6. Non-Irritating: Customers are less likely to get annoyed.
7. Long Format: Use detailed text, photos, and videos.
8. Easy to Unsubscribe: Customers can easily opt out.
9. Easy Tracking: Track delivery, open rates, and clicks.
10. Professional: Seen as more professional; customers read carefully.
Slide 6
Disadvantages Of Email Marketing:
1. Irrelevant Emails: Costs can rise with irrelevant emails.
2. Poor Content: Boring emails can lead to disengagement.
3. Easy Unsubscribe: Customers can easily leave your list.
Slide 7
Email Marketing Tools
Choosing a good tool involves considering:
1. Deliverability: Email delivery rate.
2. Inbox Placement: Reaching inbox, not spam or promotions.
3. Ease of Use: Simplicity of use.
4. Cost: Affordability.
5. List Maintenance: Keeping the list clean.
6. Features: Regular features like Broadcast and Sequence.
7. Automation: Better with automation.
Slide 8
Top 5 Email Marketing Tools:
1. ConvertKit
2. Get Response
3. Mailchimp
4. Active Campaign
5. Aweber
Slide 9
Email Marketing Strategy
To get good results, consider:
1. Build your own list.
2. Never buy leads.
3. Respect your customers.
4. Always provide value.
5. Don’t email just to sell.
6. Write heartfelt emails.
7. Stick to a schedule.
8. Use photos and videos.
9. Segment your list.
10. Personalize emails.
11. Ensure mobile-friendliness.
12. Optimize timing.
13. Keep designs clean.
14. Remove cold leads.
Slide 10
Uses of Email Marketing:
1. Affiliate Marketing
2. Blogging
3. Customer Relationship Management (CRM)
4. Newsletter Circulation
5. Transaction Notifications
6. Information Dissemination
7. Gathering Feedback
8. Selling Courses
9. Selling Products/Services
Read Full Article:
https://digitalsamaaj.com/is-email-marketing-effective-in-2024/
Front Desk Management in the Odoo 17 ERPCeline George
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The membership Module in the Odoo 17 ERPCeline George
Some business organizations give membership to their customers to ensure the long term relationship with those customers. If the customer is a member of the business then they get special offers and other benefits. The membership module in odoo 17 is helpful to manage everything related to the membership of multiple customers.
3. Continental Drift:
1912 Alfred Wegner proposed the idea that the
continents were moving away from one another,
breaking from one giant protocontinent he named
(Pangaea); he but didn’t know why.
Today we know that the Earth’s plates float upon
the semi-liquid mantle and move due to:
The Lithosphere moves & changes.
7. The plates move slowly on the upper mantle
(asthenosphere)
http://kids.britannica.com/comptons/art-156130/A-diagram-shows-the-relationship-
between-volcanic-activity-and-Earths
8. Movement is caused by mantle convection inside
the Earth
• Hot, less dense fluids go up while cold,
more dense ones go down
9. ridge push: sliding plate force; occurs at mid-
ocean ridges; caused by gravitational force
• spreading happens at the hot magma exit;
less dense
= greater volume
= higher elevation than the
cooler ocean floor beside it
• As plate moves from the boundary, it also
cools, condenses & sinks, creating a SLOPE
• lithosphere slides down
• the PUSH is applied to the tectonic plate due
to gravity
10. slab pull: part of the tectonic process caused by
subduction
• weight of cold, dense oceanic plate dropping
under another plate
• PULLS the oceanic plate down into the
mantle
13. Correlation of rocks & minerals
Coastal regions of different continents have the
same rocks & minerals
EXAMPLE:
Rocks in the Uwharries of NC near Albemarle are
of the same rhyolite found on the western coast
of Africa
EVIDENCE:
14. Correlation of fossils
Coastal regions of different continents have the
same fossils
EXAMPLE:
fossils of
ancient
species
crossing
continents
EVIDENCE:
15. Finding fossils in unusual locations
If we find fossils of a species unable to live in that
location today, the plates must have moved
EXAMPLE:
whale &
marine
fossils
found in
Andes
mountains
EVIDENCE:
17. Ocean Floor Evidence
• Age of rocks get older away from the divergent
boundary
• Magnetic Reversals recorded in ocean floor
match on
opposite sides
of the divergent
boundary
EVIDENCE:
20. • Two Types of Crust
• Float on the asthenosphere
Oceanic Crust
Density: 2.7 g/cm3
-Cooler
-Sinks below
continental crust
Continental Crust
Density: 3.0 g/cm3
-Warmer
GRANITE
BASALT
21. Convergent boundaries- plate boundaries where
the force of compression pushes two plates
together
Divergent boundaries- plate boundaries where
the tension pulls plates away from one another
Transform boundaries- plate boundaries where
one plate slides past another plate through
shearing
Which subducts?
Continental vs. Oceanic
What happens in the space?
What happens at
these faults?
27. Folded Mountains
http://freddoty.com/folded-mountains
Near the Sullivan
River in the Canadian
Rockies The Cape Fold Belt
Mountains, S Africa
http://www.geocaching.com/geocache/GC2CEJP_steytlerville-arch?guid=ff36205a-b979-422c-8266-f7f83ec4d884
FORCE:
compression
35. Earthquakes: tension builds up at plate
boundaries until the plates slip & tension is
released- we feel earthquakes
36. • Pressure builds within the crust at the focus
and suddenly breaks along a fault
• The sudden release of energy causes seismic
waves that make the ground shake
• epicenter: place on the surface above the
focus
37. Seismograph- strength of an earthquake is
measured with this tool that records the
vibrations from sensors placed in the earth
http://sydney.edu.au/science/uniserve_science/school/Seismograph/menu.html
http://sydney.edu.au/science/uniserve_science/school/Seismograph/menu.html
39. Seismic waves: waves of
energy are radiated from an
earthquake as both body &
surface waves;
2 kinds:
BODY WAVES travel through
earth’s inner layers; faster;
arrive first
1. P-wave- primary wave;
compressional wave;
FIRST WAVE: fastest
40. BODY WAVE
2. S-wave- SECOND WAVES
slower; can only move
through solid rock
(not liquid)
(this is why scientists
deduce the earth’s outer
core is liquid)
• moves particles up and
down or side to side
perpendicular to the
direction the wave is
traveling
41. SURFACE WAVES travel only through the crust;
• lower frequency; seismographs pick up
• damaging waves, sending movement in any
direction on the surface; tearing apart structures
• deeper earthquakes are less destructive
42. Shadow zones- places on Earth’s surface that will
not receive seismic waves because of density of
material
• S-waves are absorbed by the liquid outer core
• P-waves care refracted by the liquid outer core
ANIMATION
44. • Closer a seismic station is to the epicenter
1. The sooner the P-wave will arrive
2. The smaller the difference between P & S
waves
Determining distance from the Epicenter
45. Measure the distance between the first p wave
and the first s wave for each station.
1. Which is the closest station?
CLOSEST
2nd CLOSEST
FARTHEST
46. Earthquake Monitoring
• National Earthquake Information Center- US
(NEIC) determines size & location of
significant earthquakes worldwide & sends
information out, & maintains a database
• Global Seismographic Network (GSN)
worldwide seismic network
48. Locating the epicenter
Determining the location requires distances
from three stations.
• This will determine the location on a circle
with the radius being the distance from that
station to the epicenter.
• Using data from 3 stations, scientists can
triangulate where the epicenter is:
• Where the 3 circles intersect
= epicenter
49. Deadly Hazards
• Shaking ground causes buildings, roads and
bridges to shake, roofs cave in
• Poorly constructed buildings in
underdeveloped countries, especially
devastating
Haiti Earthquake
2010
Magnitude 7.2
230,000 died
50. 15,900 + died
Japan Earthquake Pictures, Video (9 min)
Tohoku Earthquake, Japan
2011
Magnitude 9.1
51. Causes of Earthquakes:
1. natural pressure buildup
2. groundwater extraction
3. wastewater injection
Destruction dependent upon:
1. Intensity & duration of the vibrations
2. Nature of the material where a structure is
built
3. Design of the structure
53. IN HOME: seek cover against an interior wall;
protect head; avoid mirrors/windows & tall
furniture
54. Tsunami: when an
earthquake or volcanic
eruption happens under
the ocean
1. Initiation: under-ocean
earthquake
2. Split: created wave
splits: one moving
towards ocean, one
towards shore
3. Amplification: front of
wave gets taller as it
moves toward shore
55. Deadly Hazards
• Speeds faster than a jet liner
• Heights rise 40 feet or more before crashing
on shore
• 50,000+ people killed this century
• 1998 Paupa New Guinea earthquake: 2,200
killed
56. • On shore, a person would see the water
receding from shoreline as it gathers with the
upcoming tidal wave.
57. • Pacific Tsunami Warning Center- 1948; collects
seismic data from 26 member countries; keeps
watch for suspicious shaking that might trigger
tsunamis;
• Palmer, Alaska- warning center that monitors
coasts specific to British Columbia, Washington,
Oregon, & California
• When an earthquake of 7/5 magnitude or greater
near/under the ocean occurs, these warning
centers send out initial alerts to all local
authorities within 3 hours of tsunami travel time
• Local authorities decide on evacuation plans
63. Pressure under the crust becomes great within a
magma chamber & must come out… volcanoes
Volcanoes: cracks in the crust where lava flows
1. shield volcanoes
2. cinder cone volcanoes
3. composite volcanoes
64. Mauna Kea, Hawaii
(shield volcano)
http://www.uhh.hawaii.edu/~csav/gallery/decker/hawaii_mauna_kea.php
http://www.the-vu.com/2010/05/mauna-kea-in-hawaii-driving-to-the-
summit-of-this-grand-volcano/
Shield volcano: layers of lava released from non-
explosive eruptions
Hawaiian islands are on a hot spot in
the center of the Pacific plate
66. Mt. Fuji
Mount St . Helens
ruby.colorado.edu/.../Volcanix/Volc
anix.html
Composite volcano:
pyroclastic explosions
followed by slower, longer
flowing-lava (Mt. St.
Helens
67. Caldera: large,
semicircular pit
that forms when
the chamber
supplying
magma to a
volcano partially
empties, then
the roof
collapses; sinks
the ground
thinkgeoenergy.com/archives/747
69. Ring of Fire
Major area in Pacific Ocean basin where many
earthquakes and volcanic eruptions occur
70. Yellowstone Volcano, Wyoming
Enormous caldera & super-volcano under the surface
• 40 mile crater
• last eruption: 640,000 ya
• 1000-2000 earthquakes a year
(most below 3 magnitude)
• an eruption would be 1000X
more powerful than Mt St.
Helen’s in 1980
• hydrothermal water features
are evidence it is still active
• most scientists believe that
weeks of warning signs will
alert us; 1/700,000 chance a
year it will erupt
CURRENT
CONDITIONS LINK:
71. Yellowstone Hotspot
hotspot- thermally expanded buoyant mantle that
lifts an overlying plate
-used to track motion of tectonic plates: hot plate
stays put as plate moves across it
72. Craters of the Moon National Monument, Idaho
-final stage of the Yellowstone hotspot volcanism
-result of volcanic flow and a rift valley (62 miles in
the park)
83. • Scientists study and monitor seismic activity
at a volcanic hot zone
• In scientific observatories & through field
work, scientists look for warning signs of an
eruption
• small earthquakes
• inflation/swelling of the land
• increased emission of heat/gas from
vents
Kilauea Observatory,
HI
84. Official Volcano Warnings
• color codes & alert levels
• specific for each volcano
• warning systems are based on probability of
eruption
85. Safety After a Volcano
• cover mouth &nose
• wear goggles/protect eyes
• cover skin
• clear roofs from heavy ash