Tectonics Dingbats
•Download as PPTX, PDF•
1 like•1,189 views
The document is a quiz called "Tectonics Dingbats" that tests knowledge of 14 key terms related to tectonics. It awards 1 point for correctly identifying each term and 2 points for providing a correct definition. The terms covered include core, crust, lapilli, magma, sial, subduction, asthenosphere, horst, pahoehoe, paleomagnetism, pyroclastic flow, batholith, Kilauea, and basaltic. Answers defining each term are provided at the end.
Report
Share
Report
Share
Recommended
EART4002 Lect2 Ore classification reporting.ppt
This document discusses ore deposit classification and the JORC code for reporting mineral resources and ore reserves. It begins with an introduction to the JORC code, emphasizing the principles of transparency, materiality, and competence in public reporting. Key aspects of the JORC code include definitions of mineral resources and ore reserves based on the level of geological confidence. The document then covers various types of ore deposit classifications including their host rock types, structures at different scales, and examples of alteration textures and fluid inclusions that provide insight into ore-forming processes.
Pre cambrain deposits
The document summarizes the Cambrian deposits found in extra-peninsular India. It discusses the Cambrian system, which covers the period between 570-500 million years ago. Three major locations of Cambrian deposits in India are highlighted: the Salt Range in northwest Punjab, the Spiti Valley, and Kashmir. The Salt Range contains a thick series of marine fossiliferous rocks from the Cambrian period, including salt pseudomorph shales, magnesium sandstones, Neobolus beds, and purple sandstones. Trilobites, brachiopods, and hyoliths found in the strata indicate a Lower Cambrian age.
Singhbhum Craton by AD.pptx
The document summarizes the stratigraphy and geological succession of the Singhbhum Craton located in eastern India. It describes the various rock groups that make up the craton in chronological order from oldest to youngest. The oldest is the Older Metamorphic Group composed of gneisses and schists. Unconformably above this lies the economically important Banded Iron Formation of the Iron Ore Group. Intruding all the older rock is the Singhbhum Granite batholith. Younger sedimentary successions include the Singhbhum Group, overlain by volcanic Dhanjori Group lavas and the Gangpur Group sediments. The stratigraphy represents the geological evolution of the Singhbhum Crat
Geology mcq
The document contains questions about general geology, geotectonics, physical geology, geomorphology, crystallography, mineralogy, and optical mineralogy. It includes multiple choice questions testing knowledge of topics like the speed of light, planetary characteristics, geological structures, weathering processes, crystal systems, mineral properties, and optical properties of minerals under polarized light. The questions cover a wide range of foundational topics in earth sciences.
Banded iron formations formed rapidly
And now for something very different:
Evidence that banded iron formations formed very rapidly
and a proposed YE correlation.
Enjoy the food for thought in this extraordinary period we are all experiencing!
PALAEOZOIC SUCCESSION OF SPITI.pptx
1. The Palaeozoic succession of Spiti, India contains a complete record of marine sedimentary rocks ranging in age from Cambrian to Permian.
2. The succession includes the Haimanta Group (Cambrian), Thango Formation (Ordovician), Takche Formation (Silurian), Muth Formation (Devonian), Kanawar Group (Carboniferous), and Kuling Group (Permian).
3. These sedimentary rocks comprise limestones, dolomites, shales, quartzites, and sandstones that provide a rich fossil record documenting the evolution of life during the Palaeozoic era in the region.
UNFC concept & teminology.ppt
This document provides an overview of the United Nations Framework Classification (UNFC) system for classifying mineral resources. It discusses how UNFC improved on previous classification systems by incorporating economic feasibility criteria in addition to geological factors. UNFC uses a three-axis system considering economic, feasibility, and geological characteristics to categorize resources from inferred to proved reserves. The document outlines the different levels and codes within each axis to classify resources and reserves according to UNFC terminology.
Carbonate Depositional Systems
This document provides information on carbonate systems, including their formation processes, modern and ancient settings, controlling factors, and sedimentary facies. Carbonate sediment is formed through biological processes controlled by factors like temperature, salinity, and clastic sediment influx. Modern carbonates are found in warm-water, cool-water, and pelagic settings. Ancient carbonates developed on flooded continental shelves during high sea levels. Carbonate platforms, ramps, reefs, and other depositional environments are described.
Recommended
EART4002 Lect2 Ore classification reporting.ppt
This document discusses ore deposit classification and the JORC code for reporting mineral resources and ore reserves. It begins with an introduction to the JORC code, emphasizing the principles of transparency, materiality, and competence in public reporting. Key aspects of the JORC code include definitions of mineral resources and ore reserves based on the level of geological confidence. The document then covers various types of ore deposit classifications including their host rock types, structures at different scales, and examples of alteration textures and fluid inclusions that provide insight into ore-forming processes.
Pre cambrain deposits
The document summarizes the Cambrian deposits found in extra-peninsular India. It discusses the Cambrian system, which covers the period between 570-500 million years ago. Three major locations of Cambrian deposits in India are highlighted: the Salt Range in northwest Punjab, the Spiti Valley, and Kashmir. The Salt Range contains a thick series of marine fossiliferous rocks from the Cambrian period, including salt pseudomorph shales, magnesium sandstones, Neobolus beds, and purple sandstones. Trilobites, brachiopods, and hyoliths found in the strata indicate a Lower Cambrian age.
Singhbhum Craton by AD.pptx
The document summarizes the stratigraphy and geological succession of the Singhbhum Craton located in eastern India. It describes the various rock groups that make up the craton in chronological order from oldest to youngest. The oldest is the Older Metamorphic Group composed of gneisses and schists. Unconformably above this lies the economically important Banded Iron Formation of the Iron Ore Group. Intruding all the older rock is the Singhbhum Granite batholith. Younger sedimentary successions include the Singhbhum Group, overlain by volcanic Dhanjori Group lavas and the Gangpur Group sediments. The stratigraphy represents the geological evolution of the Singhbhum Crat
Geology mcq
The document contains questions about general geology, geotectonics, physical geology, geomorphology, crystallography, mineralogy, and optical mineralogy. It includes multiple choice questions testing knowledge of topics like the speed of light, planetary characteristics, geological structures, weathering processes, crystal systems, mineral properties, and optical properties of minerals under polarized light. The questions cover a wide range of foundational topics in earth sciences.
Banded iron formations formed rapidly
And now for something very different:
Evidence that banded iron formations formed very rapidly
and a proposed YE correlation.
Enjoy the food for thought in this extraordinary period we are all experiencing!
PALAEOZOIC SUCCESSION OF SPITI.pptx
1. The Palaeozoic succession of Spiti, India contains a complete record of marine sedimentary rocks ranging in age from Cambrian to Permian.
2. The succession includes the Haimanta Group (Cambrian), Thango Formation (Ordovician), Takche Formation (Silurian), Muth Formation (Devonian), Kanawar Group (Carboniferous), and Kuling Group (Permian).
3. These sedimentary rocks comprise limestones, dolomites, shales, quartzites, and sandstones that provide a rich fossil record documenting the evolution of life during the Palaeozoic era in the region.
UNFC concept & teminology.ppt
This document provides an overview of the United Nations Framework Classification (UNFC) system for classifying mineral resources. It discusses how UNFC improved on previous classification systems by incorporating economic feasibility criteria in addition to geological factors. UNFC uses a three-axis system considering economic, feasibility, and geological characteristics to categorize resources from inferred to proved reserves. The document outlines the different levels and codes within each axis to classify resources and reserves according to UNFC terminology.
Carbonate Depositional Systems
This document provides information on carbonate systems, including their formation processes, modern and ancient settings, controlling factors, and sedimentary facies. Carbonate sediment is formed through biological processes controlled by factors like temperature, salinity, and clastic sediment influx. Modern carbonates are found in warm-water, cool-water, and pelagic settings. Ancient carbonates developed on flooded continental shelves during high sea levels. Carbonate platforms, ramps, reefs, and other depositional environments are described.
Chemostratigraphy
Chemostratigraphy is the study of chemical variations in sedimentary rocks to determine stratigraphic relationships. It uses inorganic geochemical data like carbon and oxygen isotopes to correlate rock layers. Oxygen isotopes fractionate with temperature changes and are measured in marine organism shells to create records for paleoclimate analysis. Carbon also has stable isotopes that provide information about past climate, evolution, and atmospheric CO2 levels. Chemostratigraphy has advantages over other correlation techniques as it can be used on any aged sediments regardless of lithology or environment. It has been applied successfully at major geologic boundaries and in unconventional reservoirs. Recent studies have also used sulfur and strontium isotopes to better understand changes around the Ordov
Introduction on mineral processing_01.pptx
This document provides an introduction to mineral processing. It discusses what minerals are, how they form, and how they are classified. It then describes how ores containing metals are found in nature and how they are concentrated and processed to extract the valuable metals. Physical and chemical processing methods used in mineral concentration are outlined, including crushing, grinding, gravity separation, flotation, magnetic separation, and leaching. The importance of mineral liberation during comminution and the goals of concentration to produce high grade concentrates and tailings are also summarized.
Geomorfologi jawa timur zona tengah
Dokumen tersebut memberikan ringkasan tentang geologi dan geomorfologi sebagian pulau Jawa. Terdapat beberapa zona utama yaitu zona utara, tengah, dan selatan dengan karakteristik berbeda. Juga dijelaskan beberapa kompleks gunung api seperti Gunung Merapi, Lawu, Wilis, Arjuno, Tengger, Iyang, dan Ijen beserta ciri geologi masing-masing.
Traps anticlinal
Most of the world's oil deposits are found trapped in upward folds in rock called anticlines. Oil accumulates in these structures when impermeable rock above traps oil and gas that has migrated upward from its source rock. The document describes various geological processes that can form anticlines, such as igneous intrusions, settling of sediments, salt tectonics, and deposition along an uneven seafloor. It then analyzes several major oil fields around the world defined by anticline traps, including Ghawar in Saudi Arabia, the largest oil field, and Burgan in Kuwait, once the highest producing field.
Sedimentary basins
Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
Sedimentary structures smallas
Sedimentary structures provide important information about depositional environments and allow the orientation of sedimentary beds to be determined. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding showing current direction, sole structures like flute casts formed by erosion on sediment surfaces, and trace fossils providing evidence of organism behavior and helping determine the correct vertical orientation of strata. Together, an understanding of these sedimentary structures is essential for interpreting the depositional history preserved in sedimentary rocks.
FASIES & LINGKUNGAN PENGENDAPAN BATUAN KARBONAT FORMASI WONOSARI-LOKASI GOA P...
membahas mengenai fasies & lingkungan pengendapan batuan karbonat formasi wonosari dengan lokasi studi kasus pada goa pindul yogyakarta
Limitation Of Walthers Law
Walther's law states that sedimentary rock layers are deposited continuously without major breaks in the order they were deposited. However, the document discusses limitations of Walther's law observed in Chandipur, India. Barrier bar and swamp facies were found deposited out of order, with sand deposited on top of mud. This is because sand is non-cohesive and can be transported more easily than cohesive mud, leading to differential migration rates between sand and mud bodies. While most conditions of Walther's law were satisfied, the observation of eroded mud layers beneath sand shows it is not always perfectly followed.
Diagenesis of clay minerals
Diagenesis refers to the physical, chemical, and biological changes that sediments undergo after deposition to form sedimentary rock. It can include compaction, cementation, replacement of minerals, and formation of new minerals. There are three main stages of diagenesis: syndiagenesis during sedimentation, anadiagenesis involving compaction and maturation, and epidigenesis during emergence before erosion. Common diagenetic processes in mudrocks include mechanical and chemical compaction, which reduce porosity, and the formation of authigenic minerals like calcite, illite, and kaolinite via replacement or precipitation. Clay minerals are important indicators in hydrocarbon exploration as they can provide information about tectonics, hydrocarbon generation
Meteorites and its composition.pptx
Meteorites originate from outer space objects like asteroids and comets. There are three main types of meteorites: iron, stony, and stony-iron. Iron meteorites are composed primarily of nickel and iron, and are thought to originate from asteroid cores. Stony meteorites are rock-like and can be chondrites containing chondrules, or achondrites from larger bodies. Stony-iron meteorites have a mix of stone and metal, and two subtypes are pallasites with distinctive olivine crystals, and rarer mesosiderites from violent collisions. Studying meteorites provides insights into the early solar system's formation and history of impacts.
Chemostratigraphy Presentation.pptx
Chemostratigraphy is the study of chemical variations in rock sequences based on elemental or isotopic composition. It provides a useful tool for unconventional resource exploration. Some chemical signatures in rocks, like stable isotopes, can be used as accurate stratigraphic markers because they record global environmental changes over thousands of years. Common tools in chemostratigraphy include oxygen, carbon, and strontium isotope analysis, with strontium isotopes widely used for correlation due to long ocean residence times allowing identification of major shifts in the isotopic curve.
Sٍedimentary manganes and iron ore deposits
MANGANESE ORE DEPOSITS, Sedimentary Manganese Deposits, Types of Sedimentary Manganese, Classification, Manganese Nodules, EGYPTIAN MANGANESE ORE DEPOSITS , IRON ORE DEPOSITS, Cycle of Iron , Ironstone (Sedimentary iron) Ore Deposits, Bog Iron Ore Deposits, Principal iron-bearing minerals, Geochemical stability of iron-rich minerals, World Resources Iron Deposit, EGYPTIAN IRON ORE DEPOSITS, Iron ore deposit of sedimentary nature, Sinai: Gabal Halal iron ore deposit, Aswan iron Ore Deposits, Bahariya iron Ore Deposits
aravalli craton.pptx
The Aravalli Craton in western India is divided into eight elements based on geology and age. It contains ancient gneiss and supracrustal rocks from the Archean era, followed by sedimentary and volcanic sequences from the Paleoproterozoic and Mesoproterozoic. Notable features include large lead-zinc deposits, stromatolitic phosphorites, and the large felsic Malani Igneous Suite from the Neoproterozoic. The oldest rocks date to 3300 million years ago, and the craton has undergone multiple periods of tectonism, magmatism, and basin formation.
National mineral exploration policy(nmep)basepaper
India’s mineral sector can best be characterized as one of immense potential that is waiting to be tapped. Exploration to uncover this potential is crucial. For this, a sound and comprehensive strategy is required to be framed which can be implemented in a coordinated, systematic and consistent manner.
The National mineral exploration policy must address undermentioned considerations
(i) establishes priorities, in terms of mineral commodities, areas, mining technology etc;
(ii) identifies and defines roles for the groups of key players in the sector viz., government, the exploration industry, research and academic bodies, and financiers;
(iii)recognizes that coordinated activity amongst all these players is vital to success in exploration, and, therefore, creates the institutional mechanisms necessary for this purpose;
(iv)outlines the changes in the enabling framework (legal, regulatory, financial, fiscal etc.) required for obtaining the best possible results in exploration; and
(v) estimates the resources required, in terms of funds, human capital and technology, and the means of harnessing these to the tasks ahead.
Palaeobiogeographical provinces
This PPT give us information about Palaeobiogeographical provinces it is helpful for our study. This PPT made up by me because of this ia my presentation topic. And i also share on this platform for many students have been helpful for her study.
Kuliah 6 unit biostratigrafi
The document discusses different types of biostratigraphic units used in classifying rock layers based on their fossil content. It defines key terms like biostratigraphy, biostratigraphic zone, biohorizon, and provides examples of different kinds of biostratigraphic units including taxon range zones, concurrent range zones, interval zones, lineage zones, assemblage zones, and abundance zones. The types of units are distinguished based on whether they represent the range of a single taxon, concurrence of taxa, intervals bounded by horizons, segments of an evolutionary lineage, distinctive fossil associations, or zones of maximum development of a taxon.
Paired metamorphic belts
Paired metamorphic belts occur where zones of high-pressure low-temperature metamorphism are parallel to zones of low-pressure high-temperature metamorphism. They were first recognized in Japan and form due to subduction of oceanic crust beneath continental crust. Paired metamorphic belts support the theory of plate tectonics, as the contrasting pressure-temperature conditions in the two parallel belts can be explained by ocean-continent convergence. Examples of paired metamorphic belts are found throughout the basement rocks of the former Gondwanaland supercontinent.
Subduction related igneous activity.pptx
1) Island arcs form as a result of subduction between two oceanic tectonic plates, resulting in a chain of volcanic islands.
2) Volcanic activity in island arcs produces both tholeiitic and calc-alkaline magmas. The proportions of these magma types can vary spatially along the arc and temporally as the arc evolves.
3) Island arc magmas are generated by melting of the subducting oceanic crust and mantle due to heat and fluids released by dehydration reactions during subduction at depths between 50-150km.
Dingbats (Countries)
The document appears to be a geography quiz containing 15 countries represented by symbols. Each country is associated with a number from 1 to 15. The countries included in the quiz are Argentina, Canada, Sudan, Finland, Japan, Turkey, India, Thailand, Angola, China, Philippines, Denmark, Sweden, Norway, and Benin.
Dingbats (Uk Towns & Cities)
This document contains a list of 20 UK towns and cities represented through geography-themed pictographs. Each entry uses symbols like mountains, rivers, coastlines to depict a location rather than spelling it out directly. The list covers several well-known places across the UK in a pictorial format that requires decoding their geographic clues.
More Related Content
What's hot
Chemostratigraphy
Chemostratigraphy is the study of chemical variations in sedimentary rocks to determine stratigraphic relationships. It uses inorganic geochemical data like carbon and oxygen isotopes to correlate rock layers. Oxygen isotopes fractionate with temperature changes and are measured in marine organism shells to create records for paleoclimate analysis. Carbon also has stable isotopes that provide information about past climate, evolution, and atmospheric CO2 levels. Chemostratigraphy has advantages over other correlation techniques as it can be used on any aged sediments regardless of lithology or environment. It has been applied successfully at major geologic boundaries and in unconventional reservoirs. Recent studies have also used sulfur and strontium isotopes to better understand changes around the Ordov
Introduction on mineral processing_01.pptx
This document provides an introduction to mineral processing. It discusses what minerals are, how they form, and how they are classified. It then describes how ores containing metals are found in nature and how they are concentrated and processed to extract the valuable metals. Physical and chemical processing methods used in mineral concentration are outlined, including crushing, grinding, gravity separation, flotation, magnetic separation, and leaching. The importance of mineral liberation during comminution and the goals of concentration to produce high grade concentrates and tailings are also summarized.
Geomorfologi jawa timur zona tengah
Dokumen tersebut memberikan ringkasan tentang geologi dan geomorfologi sebagian pulau Jawa. Terdapat beberapa zona utama yaitu zona utara, tengah, dan selatan dengan karakteristik berbeda. Juga dijelaskan beberapa kompleks gunung api seperti Gunung Merapi, Lawu, Wilis, Arjuno, Tengger, Iyang, dan Ijen beserta ciri geologi masing-masing.
Traps anticlinal
Most of the world's oil deposits are found trapped in upward folds in rock called anticlines. Oil accumulates in these structures when impermeable rock above traps oil and gas that has migrated upward from its source rock. The document describes various geological processes that can form anticlines, such as igneous intrusions, settling of sediments, salt tectonics, and deposition along an uneven seafloor. It then analyzes several major oil fields around the world defined by anticline traps, including Ghawar in Saudi Arabia, the largest oil field, and Burgan in Kuwait, once the highest producing field.
Sedimentary basins
Sedimentary basins are the depressions in the earth's crust where loose particles accumulate and finally lithified to form sedimentary rocks. Basins are particularly attractive to geoscientists from time immemorial due to the wealth hidden here in the form of oil, gas, coal etc. In this document you will find the types of basins, basin-fill types, methods of basin analysis and so on.
Sedimentary structures smallas
Sedimentary structures provide important information about depositional environments and allow the orientation of sedimentary beds to be determined. Key structures discussed include beds and bedding planes, laminations, graded bedding indicating changes in grain size over time, cross-bedding showing current direction, sole structures like flute casts formed by erosion on sediment surfaces, and trace fossils providing evidence of organism behavior and helping determine the correct vertical orientation of strata. Together, an understanding of these sedimentary structures is essential for interpreting the depositional history preserved in sedimentary rocks.
FASIES & LINGKUNGAN PENGENDAPAN BATUAN KARBONAT FORMASI WONOSARI-LOKASI GOA P...
membahas mengenai fasies & lingkungan pengendapan batuan karbonat formasi wonosari dengan lokasi studi kasus pada goa pindul yogyakarta
Limitation Of Walthers Law
Walther's law states that sedimentary rock layers are deposited continuously without major breaks in the order they were deposited. However, the document discusses limitations of Walther's law observed in Chandipur, India. Barrier bar and swamp facies were found deposited out of order, with sand deposited on top of mud. This is because sand is non-cohesive and can be transported more easily than cohesive mud, leading to differential migration rates between sand and mud bodies. While most conditions of Walther's law were satisfied, the observation of eroded mud layers beneath sand shows it is not always perfectly followed.
Diagenesis of clay minerals
Diagenesis refers to the physical, chemical, and biological changes that sediments undergo after deposition to form sedimentary rock. It can include compaction, cementation, replacement of minerals, and formation of new minerals. There are three main stages of diagenesis: syndiagenesis during sedimentation, anadiagenesis involving compaction and maturation, and epidigenesis during emergence before erosion. Common diagenetic processes in mudrocks include mechanical and chemical compaction, which reduce porosity, and the formation of authigenic minerals like calcite, illite, and kaolinite via replacement or precipitation. Clay minerals are important indicators in hydrocarbon exploration as they can provide information about tectonics, hydrocarbon generation
Meteorites and its composition.pptx
Meteorites originate from outer space objects like asteroids and comets. There are three main types of meteorites: iron, stony, and stony-iron. Iron meteorites are composed primarily of nickel and iron, and are thought to originate from asteroid cores. Stony meteorites are rock-like and can be chondrites containing chondrules, or achondrites from larger bodies. Stony-iron meteorites have a mix of stone and metal, and two subtypes are pallasites with distinctive olivine crystals, and rarer mesosiderites from violent collisions. Studying meteorites provides insights into the early solar system's formation and history of impacts.
Chemostratigraphy Presentation.pptx
Chemostratigraphy is the study of chemical variations in rock sequences based on elemental or isotopic composition. It provides a useful tool for unconventional resource exploration. Some chemical signatures in rocks, like stable isotopes, can be used as accurate stratigraphic markers because they record global environmental changes over thousands of years. Common tools in chemostratigraphy include oxygen, carbon, and strontium isotope analysis, with strontium isotopes widely used for correlation due to long ocean residence times allowing identification of major shifts in the isotopic curve.
Sٍedimentary manganes and iron ore deposits
MANGANESE ORE DEPOSITS, Sedimentary Manganese Deposits, Types of Sedimentary Manganese, Classification, Manganese Nodules, EGYPTIAN MANGANESE ORE DEPOSITS , IRON ORE DEPOSITS, Cycle of Iron , Ironstone (Sedimentary iron) Ore Deposits, Bog Iron Ore Deposits, Principal iron-bearing minerals, Geochemical stability of iron-rich minerals, World Resources Iron Deposit, EGYPTIAN IRON ORE DEPOSITS, Iron ore deposit of sedimentary nature, Sinai: Gabal Halal iron ore deposit, Aswan iron Ore Deposits, Bahariya iron Ore Deposits
aravalli craton.pptx
The Aravalli Craton in western India is divided into eight elements based on geology and age. It contains ancient gneiss and supracrustal rocks from the Archean era, followed by sedimentary and volcanic sequences from the Paleoproterozoic and Mesoproterozoic. Notable features include large lead-zinc deposits, stromatolitic phosphorites, and the large felsic Malani Igneous Suite from the Neoproterozoic. The oldest rocks date to 3300 million years ago, and the craton has undergone multiple periods of tectonism, magmatism, and basin formation.
National mineral exploration policy(nmep)basepaper
India’s mineral sector can best be characterized as one of immense potential that is waiting to be tapped. Exploration to uncover this potential is crucial. For this, a sound and comprehensive strategy is required to be framed which can be implemented in a coordinated, systematic and consistent manner.
The National mineral exploration policy must address undermentioned considerations
(i) establishes priorities, in terms of mineral commodities, areas, mining technology etc;
(ii) identifies and defines roles for the groups of key players in the sector viz., government, the exploration industry, research and academic bodies, and financiers;
(iii)recognizes that coordinated activity amongst all these players is vital to success in exploration, and, therefore, creates the institutional mechanisms necessary for this purpose;
(iv)outlines the changes in the enabling framework (legal, regulatory, financial, fiscal etc.) required for obtaining the best possible results in exploration; and
(v) estimates the resources required, in terms of funds, human capital and technology, and the means of harnessing these to the tasks ahead.
Palaeobiogeographical provinces
This PPT give us information about Palaeobiogeographical provinces it is helpful for our study. This PPT made up by me because of this ia my presentation topic. And i also share on this platform for many students have been helpful for her study.
Kuliah 6 unit biostratigrafi
The document discusses different types of biostratigraphic units used in classifying rock layers based on their fossil content. It defines key terms like biostratigraphy, biostratigraphic zone, biohorizon, and provides examples of different kinds of biostratigraphic units including taxon range zones, concurrent range zones, interval zones, lineage zones, assemblage zones, and abundance zones. The types of units are distinguished based on whether they represent the range of a single taxon, concurrence of taxa, intervals bounded by horizons, segments of an evolutionary lineage, distinctive fossil associations, or zones of maximum development of a taxon.
Paired metamorphic belts
Paired metamorphic belts occur where zones of high-pressure low-temperature metamorphism are parallel to zones of low-pressure high-temperature metamorphism. They were first recognized in Japan and form due to subduction of oceanic crust beneath continental crust. Paired metamorphic belts support the theory of plate tectonics, as the contrasting pressure-temperature conditions in the two parallel belts can be explained by ocean-continent convergence. Examples of paired metamorphic belts are found throughout the basement rocks of the former Gondwanaland supercontinent.
Subduction related igneous activity.pptx
1) Island arcs form as a result of subduction between two oceanic tectonic plates, resulting in a chain of volcanic islands.
2) Volcanic activity in island arcs produces both tholeiitic and calc-alkaline magmas. The proportions of these magma types can vary spatially along the arc and temporally as the arc evolves.
3) Island arc magmas are generated by melting of the subducting oceanic crust and mantle due to heat and fluids released by dehydration reactions during subduction at depths between 50-150km.
What's hot (20)
FASIES & LINGKUNGAN PENGENDAPAN BATUAN KARBONAT FORMASI WONOSARI-LOKASI GOA P...
FASIES & LINGKUNGAN PENGENDAPAN BATUAN KARBONAT FORMASI WONOSARI-LOKASI GOA P...
National mineral exploration policy(nmep)basepaper
National mineral exploration policy(nmep)basepaper
Viewers also liked
Dingbats (Countries)
The document appears to be a geography quiz containing 15 countries represented by symbols. Each country is associated with a number from 1 to 15. The countries included in the quiz are Argentina, Canada, Sudan, Finland, Japan, Turkey, India, Thailand, Angola, China, Philippines, Denmark, Sweden, Norway, and Benin.
Dingbats (Uk Towns & Cities)
This document contains a list of 20 UK towns and cities represented through geography-themed pictographs. Each entry uses symbols like mountains, rivers, coastlines to depict a location rather than spelling it out directly. The list covers several well-known places across the UK in a pictorial format that requires decoding their geographic clues.
What On Earth 04
The Yangtze River is about 6,380 km long and flows through China. Camel racing in the UAE is being transformed with the use of robot jockeys instead of child jockeys. The Grand Canyon Skywalk in Arizona exceeds the height of the world's tallest skyscrapers.
Dingbats PowerPoint
The document contains a list of phrases and terms without context. It includes various idioms, movie and book titles, and weather-related terms that do not form a coherent story or provide any clear meaning on their own in just 3 short sentences.
Case Studies
Take Me Out is a dating game show that airs on ITV in the UK. Contestants are single men who try to win a date with one of 30 single women by going through a series of rounds. Paddy McGuinness hosts the show, which aims to match couples but has seen declining success in recent years. There are no prizes besides a date for the contestants.
Viewers also liked (7)
Similar to Tectonics Dingbats
Ohsm science1 q2 module5
This document provides an overview of a module on plate tectonics that includes the following:
1) The module covers topics on evidence of plate tectonics and managing effects of natural phenomena associated with plate tectonics through 4 lessons on the structure of Earth, formation of continents, earthquakes, and volcanoes.
2) Students will complete a pre-assessment on their understanding of the structure of Earth, movement of tectonic plates, earthquakes, and volcanoes from elementary science.
3) The module will help students develop a better understanding of plate tectonics to inform decisions on managing effects of natural phenomena through acquiring scientific knowledge from the lessons and activities.
Changing earth
The document provides information over 12 days about changing Earth and plate tectonics. Day 1 introduces the four layers of the Earth - crust, mantle, outer core and inner core. Day 2 reviews the layers and their characteristics. Day 3 discusses Alfred Wegener's theory of continental drift and how plate tectonics explains the movement of continents. It also introduces the concept of Pangaea. Day 4 identifies the three types of plate boundaries - divergent, convergent and transform. Later days discuss earthquakes, volcanoes, and how volcanic activity forms new land and islands.
Plate tectonics Basic (KS3)
1. The document describes the structure of the Earth, which is divided into four main layers - the crust, mantle, outer core, and inner core.
2. The crust and upper mantle make up tectonic plates that slowly move and interact with each other, influencing volcanic and earthquake activity.
3. Tectonic plates are driven by convection currents in the hot, liquid mantle and influence volcanoes and earthquakes through processes like plate collisions and divergent boundaries.
layers of the earth
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.
Unit 1 - Inside the Earth and Plate Tectonics (2017/2018)
1) Earth is unique in our solar system for having liquid water, oxygen in its atmosphere, and supporting life.
2) Earth has three main compositional zones - a crust, mantle, and core. As depth increases, pressure, density, and temperature all rise.
3) Plate tectonics theory explains how large tectonic plates slowly move and interact at plate boundaries, causing geologic events like volcanoes and earthquakes. There are three main types of plate boundaries.
Module-1-LITHOSPHERE1 (GRADE 10 SCIENCE FIRST QUARTER MODULE )1upload.pptx
The document discusses the layers of the Earth's lithosphere. It describes the lithosphere as the cool, rigid outer layer of the Earth made up of crust and upper mantle. The lithosphere is divided into tectonic plates that float on the asthenosphere. There are two types of plates - continental plates composed of less dense rocks found under land, and oceanic plates made of denser rocks under oceans. The boundaries between plates experience geological events like earthquakes and volcanoes.
Interior Of Earth
The document discusses what lies within Earth's interior based on indirect evidence from seismic waves. [1] Seismic waves provide information about Earth's layered structure as the waves refract and reflect differently depending on density changes. [2] Earth has a crust, mantle, outer core, and inner core, with increasing temperatures and pressures toward the center. [3] The core generates Earth's magnetic field through its spinning liquid outer layer.
Lesson 3_Science 10- Q1W3_ Plate Movement.pptx
The Earth is divided into three main layers - the crust, mantle, and core - based on their composition. The crust is the outermost solid layer and is divided into continental and oceanic crust. Below the crust is the mantle, which is divided into the upper and lower mantle. The innermost layer is the core, consisting of a solid inner core surrounded by a liquid outer core. These layers move and interact through plate tectonics.
Livingwithearthquakesandvolcanoes 101001170840-phpapp02
The document describes an earthquake that struck the Iranian city of Bam in 2003. The earthquake, measured at 6.6 on the Richter scale, was caused by the pushing together of the Iranian and Arabian tectonic plates. Over 20,000 people were killed when the earthquake destroyed thousands of homes in Bam. Emergency services struggled to help those injured and trapped in the rubble due to damaged roads and collapsed buildings. The earthquake devastated the historic structures in Bam, including the famous 2,000-year-old citadel.
PPT_Geography_Lecture_1_Geomorphology_I_Dated_09th_May_2022.pdf
The document contains 17 multiple choice questions regarding geology and the structure of the Earth. The questions cover topics such as the composition of the continental and oceanic crust, earthquake waves, rock types, plate tectonics, and sources of information about Earth's interior. Correct explanations are provided for each answer.
Layers of the Earth.pptx
This document discusses the layers of the Earth, including the crust, mantle, outer core, and inner core. It describes the composition and properties of each layer. The crust is the outermost solid layer, varying in thickness between continents and oceans. The mantle, made largely of silicate rocks, flows slowly due to heat and pressure. Beneath the lithosphere lies the asthenosphere, facilitating plate tectonics. The outer core is liquid, while the inner core is solid due to extreme pressure despite temperatures over 5000°C. Together, the cores generate Earth's magnetic field.
Layers of the Earth (Application)
The document is a quiz about the layers of the Earth. It asks questions about which layer we live on (crust), the layer below the crust composed of solid and melted rocks (mantle), the deepest portion of the Earth (core), the boundary between the crust and mantle (Mohorovicic Discontinuity), the topmost solid part (lithosphere), the boundary between the mantle and core (Gutenberg Discontinuity), the hottest layer (inner core), the thickest layer making up 80% of the volume (mantle), and the scientists who study the layers (geologists). It also provides the average temperature of the inner core (5,000°C).
Plate Tectonics
Plate tectonics involves the slow movement of sections of Earth's crust called tectonic plates. Plates move due to convection currents in the underlying mantle. Where plates meet, they can cause earthquakes, volcanoes, and mountains as the plates push together, slide past each other, or move apart. The movement of plates over time has resulted in continents joining together in a supercontinent called Pangea and breaking apart again.
Plate layers convection distribution_movement
1. The document discusses natural hazards and tectonic plate movement. It defines a natural hazard as a natural event that threatens lives and property. Examples given are earthquakes, volcanic eruptions, and tsunamis.
2. It describes the internal structure of the Earth, including the lithosphere which comprises the crust and upper mantle, and tectonic plates which are pieces of the lithosphere that move in relation to one another.
3. The causes of tectonic plate movements are explained as being due to convection currents in the mantle driven by heat from the Earth's core, and the slab-pull force exerted by subducting plates pulling the other plates along.
ramosearthscience.pptx
The document describes the different layers that make up the Earth. It discusses three main layers - the crust, mantle, and core. The crust is the topmost layer and is broken into tectonic plates. Below the crust is the mantle, made of hot dense rock that flows slowly due to convection currents. The core is at the center and has a solid inner core surrounded by a liquid outer core made of iron and nickel.
9/21 and 9/22
This document discusses tectonic plate boundaries and their effects on the Earth's surface. It begins with questions to activate students' prior knowledge about boundaries, earthquakes, and volcanoes. The text then defines the four types of boundaries - divergent, convergent, transform, and subduction - and has students learn about each through reading groups. Each boundary type is characterized by how the plates move at the boundary and the resulting geologic effects, such as new crust being formed at divergent boundaries and mountains resulting from convergent boundaries. In summary, the document aims to teach students about the four types of tectonic plate boundaries and how they change the Earth's shape through volcanic and earthquake activity.
All About Earth (Core to Crust; Includes Facts; Q/A & much more)
This presentation is made in power point 2016.with lots of exciting transitions and animation. With loads of information and pictures.Helpful for students in classes 8,9,10 in social studies (SSC syllabus)
Kuliah GL-3 (Plate Tec).ppt
Earth's surface is divided into tectonic plates that move over time. Heat from radioactive decay in Earth's interior drives convection currents in the mantle, providing the force that pushes plates together or pulls them apart at boundaries. Evidence from seismic waves, the distribution of ocean sediments and magnetic patterns on the seafloor have confirmed plate tectonic theory and helped explain features like mid-ocean ridges, volcanoes, and earthquake zones. Plate tectonics unifies many fields of geology by explaining the formation of continents, oceans, and mountain ranges over billions of years.
Layers of the Earth and its Composition.pptx
The document describes the three main layers of the Earth - crust, mantle, and core. It explains that the crust is the thinnest layer and is divided into tectonic plates that move due to convection currents in the mantle. The mantle, which is the largest layer, flows slowly due to these convection currents caused by hot material rising and cool material sinking. Temperature, density and pressure all increase with depth in the Earth. The core is the center-most layer and has a solid inner core surrounded by a liquid outer core.
Similar to Tectonics Dingbats (20)
Unit 1 - Inside the Earth and Plate Tectonics (2017/2018)
Unit 1 - Inside the Earth and Plate Tectonics (2017/2018)
Module-1-LITHOSPHERE1 (GRADE 10 SCIENCE FIRST QUARTER MODULE )1upload.pptx
Module-1-LITHOSPHERE1 (GRADE 10 SCIENCE FIRST QUARTER MODULE )1upload.pptx
Livingwithearthquakesandvolcanoes 101001170840-phpapp02
Livingwithearthquakesandvolcanoes 101001170840-phpapp02
PPT_Geography_Lecture_1_Geomorphology_I_Dated_09th_May_2022.pdf
PPT_Geography_Lecture_1_Geomorphology_I_Dated_09th_May_2022.pdf
All About Earth (Core to Crust; Includes Facts; Q/A & much more)
All About Earth (Core to Crust; Includes Facts; Q/A & much more)
Recently uploaded
Bed Making ( Introduction, Purpose, Types, Articles, Scientific principles, N...
Topic : Bed making
Subject : Nursing Foundation
Solutons Maths Escape Room Spatial .pptx
Solutions of Puzzles of Mathematics Escape Room Game in Spatial.io
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
(𝐓𝐋𝐄 𝟏𝟎𝟎) (𝐋𝐞𝐬𝐬𝐨𝐧 𝟏)-𝐏𝐫𝐞𝐥𝐢𝐦𝐬
𝐃𝐢𝐬𝐜𝐮𝐬𝐬 𝐭𝐡𝐞 𝐄𝐏𝐏 𝐂𝐮𝐫𝐫𝐢𝐜𝐮𝐥𝐮𝐦 𝐢𝐧 𝐭𝐡𝐞 𝐏𝐡𝐢𝐥𝐢𝐩𝐩𝐢𝐧𝐞𝐬:
- Understand the goals and objectives of the Edukasyong Pantahanan at Pangkabuhayan (EPP) curriculum, recognizing its importance in fostering practical life skills and values among students. Students will also be able to identify the key components and subjects covered, such as agriculture, home economics, industrial arts, and information and communication technology.
𝐄𝐱𝐩𝐥𝐚𝐢𝐧 𝐭𝐡𝐞 𝐍𝐚𝐭𝐮𝐫𝐞 𝐚𝐧𝐝 𝐒𝐜𝐨𝐩𝐞 𝐨𝐟 𝐚𝐧 𝐄𝐧𝐭𝐫𝐞𝐩𝐫𝐞𝐧𝐞𝐮𝐫:
-Define entrepreneurship, distinguishing it from general business activities by emphasizing its focus on innovation, risk-taking, and value creation. Students will describe the characteristics and traits of successful entrepreneurs, including their roles and responsibilities, and discuss the broader economic and social impacts of entrepreneurial activities on both local and global scales.
Leveraging Generative AI to Drive Nonprofit Innovation
In this webinar, participants learned how to utilize Generative AI to streamline operations and elevate member engagement. Amazon Web Service experts provided a customer specific use cases and dived into low/no-code tools that are quick and easy to deploy through Amazon Web Service (AWS.)
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...Nguyen Thanh Tu Collection
https://app.box.com/s/tacvl9ekroe9hqupdnjruiypvm9rdaneGender and Mental Health - Counselling and Family Therapy Applications and In...
A proprietary approach developed by bringing together the best of learning theories from Psychology, design principles from the world of visualization, and pedagogical methods from over a decade of training experience, that enables you to: Learn better, faster!
Chapter wise All Notes of First year Basic Civil Engineering.pptx
Chapter wise All Notes of First year Basic Civil Engineering
Syllabus
Chapter-1
Introduction to objective, scope and outcome the subject
Chapter 2
Introduction: Scope and Specialization of Civil Engineering, Role of civil Engineer in Society, Impact of infrastructural development on economy of country.
Chapter 3
Surveying: Object Principles & Types of Surveying; Site Plans, Plans & Maps; Scales & Unit of different Measurements.
Linear Measurements: Instruments used. Linear Measurement by Tape, Ranging out Survey Lines and overcoming Obstructions; Measurements on sloping ground; Tape corrections, conventional symbols. Angular Measurements: Instruments used; Introduction to Compass Surveying, Bearings and Longitude & Latitude of a Line, Introduction to total station.
Levelling: Instrument used Object of levelling, Methods of levelling in brief, and Contour maps.
Chapter 4
Buildings: Selection of site for Buildings, Layout of Building Plan, Types of buildings, Plinth area, carpet area, floor space index, Introduction to building byelaws, concept of sun light & ventilation. Components of Buildings & their functions, Basic concept of R.C.C., Introduction to types of foundation
Chapter 5
Transportation: Introduction to Transportation Engineering; Traffic and Road Safety: Types and Characteristics of Various Modes of Transportation; Various Road Traffic Signs, Causes of Accidents and Road Safety Measures.
Chapter 6
Environmental Engineering: Environmental Pollution, Environmental Acts and Regulations, Functional Concepts of Ecology, Basics of Species, Biodiversity, Ecosystem, Hydrological Cycle; Chemical Cycles: Carbon, Nitrogen & Phosphorus; Energy Flow in Ecosystems.
Water Pollution: Water Quality standards, Introduction to Treatment & Disposal of Waste Water. Reuse and Saving of Water, Rain Water Harvesting. Solid Waste Management: Classification of Solid Waste, Collection, Transportation and Disposal of Solid. Recycling of Solid Waste: Energy Recovery, Sanitary Landfill, On-Site Sanitation. Air & Noise Pollution: Primary and Secondary air pollutants, Harmful effects of Air Pollution, Control of Air Pollution. . Noise Pollution Harmful Effects of noise pollution, control of noise pollution, Global warming & Climate Change, Ozone depletion, Greenhouse effect
Text Books:
1. Palancharmy, Basic Civil Engineering, McGraw Hill publishers.
2. Satheesh Gopi, Basic Civil Engineering, Pearson Publishers.
3. Ketki Rangwala Dalal, Essentials of Civil Engineering, Charotar Publishing House.
4. BCP, Surveying volume 1
ANATOMY AND BIOMECHANICS OF HIP JOINT.pdf
it describes the bony anatomy including the femoral head , acetabulum, labrum . also discusses the capsule , ligaments . muscle that act on the hip joint and the range of motion are outlined. factors affecting hip joint stability and weight transmission through the joint are summarized.
Mule event processing models | MuleSoft Mysore Meetup #47
Mule event processing models | MuleSoft Mysore Meetup #47
Event Link:- https://meetups.mulesoft.com/events/details/mulesoft-mysore-presents-mule-event-processing-models/
Agenda
● What is event processing in MuleSoft?
● Types of event processing models in Mule 4
● Distinction between the reactive, parallel, blocking & non-blocking processing
For Upcoming Meetups Join Mysore Meetup Group - https://meetups.mulesoft.com/mysore/YouTube:- youtube.com/@mulesoftmysore
Mysore WhatsApp group:- https://chat.whatsapp.com/EhqtHtCC75vCAX7gaO842N
Speaker:-
Shivani Yasaswi - https://www.linkedin.com/in/shivaniyasaswi/
Organizers:-
Shubham Chaurasia - https://www.linkedin.com/in/shubhamchaurasia1/
Giridhar Meka - https://www.linkedin.com/in/giridharmeka
Priya Shaw - https://www.linkedin.com/in/priya-shaw
How to Make a Field Mandatory in Odoo 17
In Odoo, making a field required can be done through both Python code and XML views. When you set the required attribute to True in Python code, it makes the field required across all views where it's used. Conversely, when you set the required attribute in XML views, it makes the field required only in the context of that particular view.
Walmart Business+ and Spark Good for Nonprofits.pdf
"Learn about all the ways Walmart supports nonprofit organizations.
You will hear from Liz Willett, the Head of Nonprofits, and hear about what Walmart is doing to help nonprofits, including Walmart Business and Spark Good. Walmart Business+ is a new offer for nonprofits that offers discounts and also streamlines nonprofits order and expense tracking, saving time and money.
The webinar may also give some examples on how nonprofits can best leverage Walmart Business+.
The event will cover the following::
Walmart Business + (https://business.walmart.com/plus) is a new shopping experience for nonprofits, schools, and local business customers that connects an exclusive online shopping experience to stores. Benefits include free delivery and shipping, a 'Spend Analytics” feature, special discounts, deals and tax-exempt shopping.
Special TechSoup offer for a free 180 days membership, and up to $150 in discounts on eligible orders.
Spark Good (walmart.com/sparkgood) is a charitable platform that enables nonprofits to receive donations directly from customers and associates.
Answers about how you can do more with Walmart!"
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.
Recently uploaded (20)
Bed Making ( Introduction, Purpose, Types, Articles, Scientific principles, N...
Bed Making ( Introduction, Purpose, Types, Articles, Scientific principles, N...
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
Philippine Edukasyong Pantahanan at Pangkabuhayan (EPP) Curriculum
Film vocab for eal 3 students: Australia the movie
Film vocab for eal 3 students: Australia the movie
NEWSPAPERS - QUESTION 1 - REVISION POWERPOINT.pptx
NEWSPAPERS - QUESTION 1 - REVISION POWERPOINT.pptx
Leveraging Generative AI to Drive Nonprofit Innovation
Leveraging Generative AI to Drive Nonprofit Innovation
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
BÀI TẬP BỔ TRỢ TIẾNG ANH LỚP 9 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2024-2025 - ...
Liberal Approach to the Study of Indian Politics.pdf
Liberal Approach to the Study of Indian Politics.pdf
Gender and Mental Health - Counselling and Family Therapy Applications and In...
Gender and Mental Health - Counselling and Family Therapy Applications and In...
Chapter wise All Notes of First year Basic Civil Engineering.pptx
Chapter wise All Notes of First year Basic Civil Engineering.pptx
Mule event processing models | MuleSoft Mysore Meetup #47
Mule event processing models | MuleSoft Mysore Meetup #47
Walmart Business+ and Spark Good for Nonprofits.pdf
Walmart Business+ and Spark Good for Nonprofits.pdf
Tectonics Dingbats
- 1. Tectonics Dingbats! 1 How many key words can you remember? • 1 point for correctly identifying each word • 2 points for each correct definition
- 15. Answers 1. Core – centre and hottest part of earth (>5000C) 2. Crust – hard rigid surface layer of Earth 3. Lapilli – small tephra 2 – 64mm diamter 4. Magma – molten rock inside earth 5. Sial – continental crust (slica and aluminium) 6. Subduction – one plate moves under another in2 mantle 7. Asthenosphere – upper mantle 8. Horst – block pushed up by faulting e.g. at a rift valley 9. Pahoehoe – ropy, basaltic lave 10. Paleomagnetism – study of changes in earth’s magnetic field 11. Pyroclastic Flow – flow of hot gas and tephra 12. Batholith – igneous intrusion 13. Kilauea – active volcano, Hawaii 14. Basaltic – runny type of lava
Editor's Notes
- (how does she look rather than who is she)
- 15 mins