SHS Earth and Life Quarter 1 Module 4.pdfryannable1
油
This document provides information about metamorphism and igneous rocks. It defines metamorphism as the change of minerals or texture in rocks without melting due to heat, pressure, or fluids. It describes different types of metamorphism including burial, regional, contact, and dynamic. It also defines igneous rocks as those formed from cooling magma and describes intrusive and extrusive varieties and examples like granite, basalt, and pumice.
The document discusses several key geologic cycles and processes:
1) There are endogenic systems within the Earth driven by heat and radioactive decay, and exogenic systems external to the Earth driven by solar energy and gravity. These systems interact in geologic cycles that shape the Earth's surface over millions of years.
2) The rock cycle occurs at plate boundaries where igneous rocks are transformed into sedimentary and metamorphic rocks via weathering, erosion, deposition, and subduction.
3) Plate tectonics involves the fragmentation of crust into plates that move at boundaries, creating volcanism from magma at divergent boundaries and subduction at convergent boundaries, building mountains 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.
The document summarizes key information about the structure and composition of the Earth. It describes the four major layers from the center out - the inner core, outer core, mantle, and crust. The crust is divided into tectonic plates that move via three processes at their boundaries: convergent, divergent, and sliding. Earthquakes and volcanoes occur as results of this plate tectonic activity and the movement of molten rock within the Earth.
3.Introduction to Geology and Geological Investigation.docxAzazAlamKhan
油
The document provides an overview of geology and geological investigation methods. It discusses the internal structure of Earth, including the crust, mantle, and core. It also describes the three main types of rocks: igneous, sedimentary, and metamorphic rocks. Finally, it introduces common structural features in rocks, such as bedding, folds, faults, joints, cleavage, and veins. The lesson aims to teach students about the origin and components of Earth through examination of rocks and geological techniques.
Plate tectonics and the movement of tectonic plates cause dynamic earth processes like earthquakes and volcanic activity. Evidence from seafloor topography, paleomagnetism, and earthquake patterns provided evidence for plate tectonics and Alfred Wegener's hypothesis of continental drift. There are three types of plate boundaries - divergent where plates pull apart, convergent where they push together, and transform where they slide past each other like the San Andreas fault. Earthquakes are usually caused by the sudden release of built up energy at plate boundaries, and can be used to determine the structure of the Earth's interior. Volcanic eruptions are powered by movement of magma from deep in the lithosphere along
The document provides information about the three main types of rocks: igneous, sedimentary, and metamorphic. It explains that igneous rocks form from magma and contain crystals. Sedimentary rocks form from layers of sediment cemented together over time and can contain fossils. Metamorphic rocks form from existing rocks undergoing heat and pressure, changing their structure and forming new layers. The document also discusses the rock cycle and how rocks continuously change forms through geological processes.
hope it can help ya! i and my groupmates work hard just to present a simple but eye pleasing presentation just to make our classmates and teacher satisfied
The document summarizes key concepts in geology, including:
1) The formation of the solar system from a nebula of dust and gas around 4.5 billion years ago, which led to the formation of the Sun and planets through gravitational attraction and other processes.
2) Methods for determining the age of the Earth including absolute radiometric dating techniques that measure radioactive decay and relative dating principles like superposition and cross-cutting relationships.
3) The use of fossils to provide temporal and paleoecological information about Earth's history and environmental conditions of different periods. Index fossils in particular help date and classify rock layers.
Geology is the study of the solid Earth, including the rocks and processes that change them. The Earth has layered structure based on both chemical composition and physical properties. The layers from outer to inner are: crust, mantle, outer core, and inner core. The crust and upper mantle make up rigid tectonic plates that move and interact at plate boundaries, resulting in phenomena like earthquakes, volcanoes, and mountain building.
This document provides an introduction to geotourism and geology. It summarizes key concepts in 3 sentences or less:
Geotourism involves traveling to discover Earth's landscapes and geological phenomena, which tell the history of our planet. The basics of plate tectonics theory explain large-scale geological processes like diverging plates forming new crust at ocean ridges or converging plates causing subduction and mountain building. Rocks form through sedimentary, igneous, and metamorphic processes and can be classified based on their composition and origin, with sedimentary rocks containing important clues in their fossils.
SHS Earth and Life Quarter 1 Module 2.pdfryannable1
油
The document provides information about a module on minerals, rocks, and exogenic processes for an Earth and Life Science course. It includes details about the module such as the topics covered in each lesson, the learning objectives, and assessment questions. The module is intended to help students understand the three main categories of rocks based on their origin, how minerals and rocks are formed, and exogenic processes like weathering and erosion.
Rocks are composed of minerals and come in three main types: igneous, sedimentary, and metamorphic. Igneous rocks form from solidified magma or lava. Sedimentary rocks form from compressed sediment. Metamorphic rocks form from changes to existing rocks by heat, pressure, and chemical reactions. These three rock types are continuously transforming into one another through geological processes in the rock cycle.
This document provides an overview of structural geomorphology and the key surface and subsurface processes that shape the Earth's landscapes. It discusses global geomorphology and the intersection between climatic, hydrologic, and biologic surface processes with underlying geologic processes. Specific topics covered include plate tectonics and the different landforms that form at divergent, convergent and transform plate boundaries. The document also discusses weathering processes, the factors that influence them, and characteristic landforms formed by weathering such as exfoliation domes and rock basins. Finally, it covers slope stability and the different types of landslides that can occur based on material type and movement.
Earthquakes are caused by the release of elastic strain energy stored in rocks along faults. The Earth's surface consists of tectonic plates that are constantly moving due to convection currents in the mantle. Where the plates meet, they can collide, move apart, or move past each other, building up stress. If the stress becomes too great, the rocks suddenly slip along a fault, releasing energy in waves called seismic waves. There are two main types of earthquakes - interplate quakes at plate boundaries and intraplate quakes within plates. Fault slip during quakes can be vertical, horizontal, or lateral.
ROCKS and minerals of science into the reportRaymond Mortel
油
Rocks are naturally occurring consolidated substances that are made up of minerals, other rock pieces, and fossil materials. Rocks form through various geological processes on Earth's surface and underground, or in space from meteorites.
There are three main types of rocks - sedimentary, igneous, and metamorphic - but other types include deformation rocks from Earth movements, meteorites, and impact rocks from meteorite strikes.
The rock cycle describes how rocks are recycled at Earth's surface through weathering, erosion into sediments, burial and heating within the Earth to form new rocks or melt into magma. Igneous rocks form from cooling magma, sedimentary rocks form from compressed sediments, and metamorphic
The document discusses the scientific study of landforms and the processes that shape them, known as geomorphology. It is a composite science that studies landforms and investigates the processes that cause and alter them. Geomorphology is practiced within several related fields. Some key processes discussed include weathering, erosion, transportation, deposition, and mass movement. Both exogenous processes from outside forces like the sun, wind and water, as well as endogenous processes from inside the earth like earthquakes, volcanism, and tectonic activity can shape landforms. Remote sensing techniques are also used to study landforms from satellites and aircraft.
The document discusses geochemical cycles. It begins by defining geochemical cycles as the natural movement and redistribution of elements on Earth through various geological processes like melting, crystallization, erosion and precipitation.
It then explains that the lithosphere geochemical cycle involves the crystallization of magma, surface weathering of igneous rock into sediment, sediment lithification and metamorphism, and eventual melting to form new magma.
The cycle can be interrupted and different elements are affected differently as the cycle progresses. For example, during rock weathering, elements like iron and magnesium are dissolved while quartz and feldspar remain as sediment. The summary concludes by noting the cycle includes both deep geological and surface processes
Plate tectonics involves the large rigid plates that make up the Earth's crust and upper mantle. These plates constantly move and interact with each other at their boundaries. There are three main types of plate boundaries: divergent where plates move apart and new crust is formed, convergent where plates collide and oceanic plates are subducted, and transform where plates slide past each other causing earthquakes. The movement of tectonic plates leads to volcanic activity and mountain building at convergent boundaries, and the formation of new seafloor at divergent boundaries.
This document provides an introduction to different types of rocks and their formation processes. It discusses igneous rocks such as granite and basalt that form from the cooling of magma, sedimentary rocks like sandstone and limestone that form through the compaction and cementation of sediments, and metamorphic rocks that form from the alteration of existing rocks through heat and pressure. It also introduces the rock cycle concept whereby rocks continuously transform between igneous, sedimentary and metamorphic types through geological processes over long periods of time.
hope it can help ya! i and my groupmates work hard just to present a simple but eye pleasing presentation just to make our classmates and teacher satisfied
The document summarizes key concepts in geology, including:
1) The formation of the solar system from a nebula of dust and gas around 4.5 billion years ago, which led to the formation of the Sun and planets through gravitational attraction and other processes.
2) Methods for determining the age of the Earth including absolute radiometric dating techniques that measure radioactive decay and relative dating principles like superposition and cross-cutting relationships.
3) The use of fossils to provide temporal and paleoecological information about Earth's history and environmental conditions of different periods. Index fossils in particular help date and classify rock layers.
Geology is the study of the solid Earth, including the rocks and processes that change them. The Earth has layered structure based on both chemical composition and physical properties. The layers from outer to inner are: crust, mantle, outer core, and inner core. The crust and upper mantle make up rigid tectonic plates that move and interact at plate boundaries, resulting in phenomena like earthquakes, volcanoes, and mountain building.
This document provides an introduction to geotourism and geology. It summarizes key concepts in 3 sentences or less:
Geotourism involves traveling to discover Earth's landscapes and geological phenomena, which tell the history of our planet. The basics of plate tectonics theory explain large-scale geological processes like diverging plates forming new crust at ocean ridges or converging plates causing subduction and mountain building. Rocks form through sedimentary, igneous, and metamorphic processes and can be classified based on their composition and origin, with sedimentary rocks containing important clues in their fossils.
SHS Earth and Life Quarter 1 Module 2.pdfryannable1
油
The document provides information about a module on minerals, rocks, and exogenic processes for an Earth and Life Science course. It includes details about the module such as the topics covered in each lesson, the learning objectives, and assessment questions. The module is intended to help students understand the three main categories of rocks based on their origin, how minerals and rocks are formed, and exogenic processes like weathering and erosion.
Rocks are composed of minerals and come in three main types: igneous, sedimentary, and metamorphic. Igneous rocks form from solidified magma or lava. Sedimentary rocks form from compressed sediment. Metamorphic rocks form from changes to existing rocks by heat, pressure, and chemical reactions. These three rock types are continuously transforming into one another through geological processes in the rock cycle.
This document provides an overview of structural geomorphology and the key surface and subsurface processes that shape the Earth's landscapes. It discusses global geomorphology and the intersection between climatic, hydrologic, and biologic surface processes with underlying geologic processes. Specific topics covered include plate tectonics and the different landforms that form at divergent, convergent and transform plate boundaries. The document also discusses weathering processes, the factors that influence them, and characteristic landforms formed by weathering such as exfoliation domes and rock basins. Finally, it covers slope stability and the different types of landslides that can occur based on material type and movement.
Earthquakes are caused by the release of elastic strain energy stored in rocks along faults. The Earth's surface consists of tectonic plates that are constantly moving due to convection currents in the mantle. Where the plates meet, they can collide, move apart, or move past each other, building up stress. If the stress becomes too great, the rocks suddenly slip along a fault, releasing energy in waves called seismic waves. There are two main types of earthquakes - interplate quakes at plate boundaries and intraplate quakes within plates. Fault slip during quakes can be vertical, horizontal, or lateral.
ROCKS and minerals of science into the reportRaymond Mortel
油
Rocks are naturally occurring consolidated substances that are made up of minerals, other rock pieces, and fossil materials. Rocks form through various geological processes on Earth's surface and underground, or in space from meteorites.
There are three main types of rocks - sedimentary, igneous, and metamorphic - but other types include deformation rocks from Earth movements, meteorites, and impact rocks from meteorite strikes.
The rock cycle describes how rocks are recycled at Earth's surface through weathering, erosion into sediments, burial and heating within the Earth to form new rocks or melt into magma. Igneous rocks form from cooling magma, sedimentary rocks form from compressed sediments, and metamorphic
The document discusses the scientific study of landforms and the processes that shape them, known as geomorphology. It is a composite science that studies landforms and investigates the processes that cause and alter them. Geomorphology is practiced within several related fields. Some key processes discussed include weathering, erosion, transportation, deposition, and mass movement. Both exogenous processes from outside forces like the sun, wind and water, as well as endogenous processes from inside the earth like earthquakes, volcanism, and tectonic activity can shape landforms. Remote sensing techniques are also used to study landforms from satellites and aircraft.
The document discusses geochemical cycles. It begins by defining geochemical cycles as the natural movement and redistribution of elements on Earth through various geological processes like melting, crystallization, erosion and precipitation.
It then explains that the lithosphere geochemical cycle involves the crystallization of magma, surface weathering of igneous rock into sediment, sediment lithification and metamorphism, and eventual melting to form new magma.
The cycle can be interrupted and different elements are affected differently as the cycle progresses. For example, during rock weathering, elements like iron and magnesium are dissolved while quartz and feldspar remain as sediment. The summary concludes by noting the cycle includes both deep geological and surface processes
Plate tectonics involves the large rigid plates that make up the Earth's crust and upper mantle. These plates constantly move and interact with each other at their boundaries. There are three main types of plate boundaries: divergent where plates move apart and new crust is formed, convergent where plates collide and oceanic plates are subducted, and transform where plates slide past each other causing earthquakes. The movement of tectonic plates leads to volcanic activity and mountain building at convergent boundaries, and the formation of new seafloor at divergent boundaries.
This document provides an introduction to different types of rocks and their formation processes. It discusses igneous rocks such as granite and basalt that form from the cooling of magma, sedimentary rocks like sandstone and limestone that form through the compaction and cementation of sediments, and metamorphic rocks that form from the alteration of existing rocks through heat and pressure. It also introduces the rock cycle concept whereby rocks continuously transform between igneous, sedimentary and metamorphic types through geological processes over long periods of time.
How to create security group category in Odoo 17Celine George
油
This slide will represent the creation of security group category in odoo 17. Security groups are essential for managing user access and permissions across different modules. Creating a security group category helps to organize related user groups and streamline permission settings within a specific module or functionality.
AI and Academic Writing, Short Term Course in Academic Writing and Publication, UGC-MMTTC, MANUU, 25/02/2025, Prof. (Dr.) Vinod Kumar Kanvaria, University of Delhi, vinodpr111@gmail.com
How to Configure Proforma Invoice in Odoo 18 SalesCeline George
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In this slide, well discuss on how to configure proforma invoice in Odoo 18 Sales module. A proforma invoice is a preliminary invoice that serves as a commercial document issued by a seller to a buyer.
Unit 1 Computer Hardware for Educational Computing.pptxRomaSmart1
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Computers have revolutionized various sectors, including education, by enhancing learning experiences and making information more accessible. This presentation, "Computer Hardware for Educational Computing," introduces the fundamental aspects of computers, including their definition, characteristics, classification, and significance in the educational domain. Understanding these concepts helps educators and students leverage technology for more effective learning.
One Click RFQ Cancellation in Odoo 18 - Odoo 際際滷sCeline George
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In this slide, well discuss the one click RFQ Cancellation in odoo 18. One-Click RFQ Cancellation in Odoo 18 is a feature that allows users to quickly and easily cancel Request for Quotations (RFQs) with a single click.
Effective Product Variant Management in Odoo 18Celine George
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In this slide well discuss on the effective product variant management in Odoo 18. Odoo concentrates on managing product variations and offers a distinct area for doing so. Product variants provide unique characteristics like size and color to single products, which can be managed at the product template level for all attributes and variants or at the variant level for individual variants.
Mastering Soft Tissue Therapy & Sports Taping: Pathway to Sports Medicine Excellence
This presentation was delivered in Colombo, Sri Lanka, at the Institute of Sports Medicine to an audience of sports physiotherapists, exercise scientists, athletic trainers, and healthcare professionals. Led by Kusal Goonewardena (PhD Candidate - Muscle Fatigue, APA Titled Sports & Exercise Physiotherapist) and Gayath Jayasinghe (Sports Scientist), the session provided comprehensive training on soft tissue assessment, treatment techniques, and essential sports taping methods.
Key topics covered:
Soft Tissue Therapy The science behind muscle, fascia, and joint assessment for optimal treatment outcomes.
Sports Taping Techniques Practical applications for injury prevention and rehabilitation, including ankle, knee, shoulder, thoracic, and cervical spine taping.
Sports Trainer Level 1 Course by Sports Medicine Australia A gateway to professional development, career opportunities, and working in Australia.
This training mirrors the Elite Akademy Sports Medicine standards, ensuring evidence-based approaches to injury management and athlete care.
If you are a sports professional looking to enhance your clinical skills and open doors to global opportunities, this presentation is for you.
Azure Data Engineer Interview Questions By ScholarHatScholarhat
油
Earth-and-Life-Science-Reporting-Topics.pptx
1. GROUP 1: Exogenic
Processes
Describe how rocks undergo
weathering
Explain how the products of weathering
are carried away by erosion and
deposited elsewhere
2. GROUP 2: Endogenic Processes
(Geologic Processes that occur within
the Earth)
Describe where the Earths internal heat
comes from
Describe how magma is formed
(Magmatism)
3. GROUP 3: Endogenic Processes
(The folding and faulting of rocks)
Describe what happens after the magma
is formed (Plutonism and Volcanism)
Describe the changes in mineral
components and texture of rocks due to
changes in pressure and temperature
(Metamorphism)
4. GROUP 4: Deformation of the
Crust (Plate Tectonics)
Explain how the continents drift
Explain how the movement of plates
leads to the formation of folds and faults
Explain how the seafloor spreads
Describe the structure and evolution of
ocean basins
5. GROUP 5: History of the
Earth
Describe how layers of rocks (stratified rocks)
are formed
Describe the different methods (relative and
absolute dating) to determine the age of stratified
rocks
Explain how relative and absolute dating were
used to determine the subdivisions of geologic
time.
6. GROUP 6: Geologic
Processes and Hazards
Describe the various hazards that
may happen in the event of
earthquakes, volcanic eruptions,
and landslides