Sedimentary rock notes09
•Download as PPT, PDF•
3 likes•1,172 views
There are three main types of sedimentary rocks: clastic or terrigenous rocks which are formed from weathered and eroded fragments and can be deposited in continental, shoreline, or marine environments; biogenic rocks which are usually carbonate sediments classified by mineral composition and formed through biological processes in limited depositional locations; and chemical rocks which form from precipitation of salts from solution in both marine and non-marine environments, such as gypsum and halite.
Report
Share
Report
Share
Recommended
Sedimentary bhupesh ppt
This document discusses sedimentary petrology and the formation of sedimentary rocks. It defines sediments as materials formed by weathering and erosion of pre-existing rocks. Sediments are classified based on particle size, ranging from boulders and pebbles to clay. Sedimentary rocks form through the processes of sediment generation, transportation, deposition, compaction and cementation. The roundness of sediment particles provides clues about the distance of sediment transportation prior to deposition and lithification into sedimentary rock. Major rock types include clastic rocks derived from eroded particles or clasts, and non-clastic rocks formed by chemical or organic processes.
Lime stone and sandstone
This document provides information about the classification and characteristics of limestone and sandstone. It begins by defining limestone as a sedimentary rock composed mainly of calcium carbonate in the form of calcite and aragonite. It describes the microscopic components of limestone including skeletal fragments, ooids, peloids, and lime mud. It explains that limestone forms most readily in warm, shallow marine environments. The document then discusses various types of limestone based on composition and texture. It concludes by outlining some of the major uses of limestone, particularly in construction as a crushed stone for concrete, cement production, and road base. The document also provides definitions of quartz arenites, feldspathic arenites, and lith
Sedimentary Rocks
This document provides a lesson about sedimentary rocks. It begins with a quiz to assess prior knowledge about sedimentary rocks. The lesson then explains that sedimentary rocks are formed from pieces of eroded earth that are pushed together by water and wind near bodies of water. Examples of sedimentary rocks include conglomerate, sandstone, siltstone, shale, and limestone. Specific uses of each rock type are also outlined.
Earth science 2.3 : Sedimentary Rock
Sedimentary rock forms through the deposition and lithification of sediment. It is categorized based on its composition and origin into clastic, chemical, and organic types. Clastic sedimentary rock like sandstone and shale form from cemented rock fragments. Chemical sedimentary rock like halite forms from crystallized mineral deposits. Organic sedimentary rock like coal forms from the remains of plants and animals. Sedimentary rock exhibits layers and other structures that indicate its formation history, such as ripple marks, mud cracks, and raindrop impressions preserved in the strata.
Report on sand
Sand is a naturally occurring granular material composed of finely divided rock and mineral particles. It is formed through the weathering and erosion of rocks and transported by wind and water. Sand is commonly divided into subcategories based on grain size, and its composition varies depending on the local rock sources. The most common type of sand found in coastal and continental areas is silica sand, usually in the form of quartz, which is very resistant to weathering. Sand has many uses including in construction, industrial applications like glassmaking, and recreational activities.
Economic geology - Sedimentary ore deposits
This document summarizes sedimentary ore deposits, specifically banded iron formations (BIF). It discusses the processes that form different types of BIF, including Algoma and Superior types, as well as their geologic time distribution. The document also explains the role of microbial communities in the deposition of iron minerals and formation of BIF layers through anoxic iron redox cycling, including phototrophic Fe(II) oxidation and nitrate-dependent Fe(II) oxidation mediated by bacteria. Overall, the document provides an overview of the genesis and microbial influences on the formation of important economic BIF deposits in sedimentary environments.
Soil classification
The document discusses soil texture and grain size distribution. It defines different soil types based on particle size, including gravel, sand, silt and clay. Various classification systems are used to categorize soils based on predominant particle sizes. The size of particles in a soil can range widely, from boulders larger than 60mm to clay particles smaller than 2 micrometers. The grain size distribution of a soil, including metrics like D10, D30 and D60, impact its engineering properties such as permeability and compressibility.
Sedimentary rocks bs 1st year
Sedimentary rocks form from the compaction and cementation of sediments. There are three main types: detrital (clastic) rocks that form from lithified rock fragments and minerals, chemical rocks that precipitate directly from solution, and organic rocks that accumulate from biological debris. Sedimentary rocks provide clues about past environments and climates based on their composition, structures like cross-bedding and ripples, and any fossil content. Important resources like coal and oil are also found within sedimentary basins.
Recommended
Sedimentary bhupesh ppt
This document discusses sedimentary petrology and the formation of sedimentary rocks. It defines sediments as materials formed by weathering and erosion of pre-existing rocks. Sediments are classified based on particle size, ranging from boulders and pebbles to clay. Sedimentary rocks form through the processes of sediment generation, transportation, deposition, compaction and cementation. The roundness of sediment particles provides clues about the distance of sediment transportation prior to deposition and lithification into sedimentary rock. Major rock types include clastic rocks derived from eroded particles or clasts, and non-clastic rocks formed by chemical or organic processes.
Lime stone and sandstone
This document provides information about the classification and characteristics of limestone and sandstone. It begins by defining limestone as a sedimentary rock composed mainly of calcium carbonate in the form of calcite and aragonite. It describes the microscopic components of limestone including skeletal fragments, ooids, peloids, and lime mud. It explains that limestone forms most readily in warm, shallow marine environments. The document then discusses various types of limestone based on composition and texture. It concludes by outlining some of the major uses of limestone, particularly in construction as a crushed stone for concrete, cement production, and road base. The document also provides definitions of quartz arenites, feldspathic arenites, and lith
Sedimentary Rocks
This document provides a lesson about sedimentary rocks. It begins with a quiz to assess prior knowledge about sedimentary rocks. The lesson then explains that sedimentary rocks are formed from pieces of eroded earth that are pushed together by water and wind near bodies of water. Examples of sedimentary rocks include conglomerate, sandstone, siltstone, shale, and limestone. Specific uses of each rock type are also outlined.
Earth science 2.3 : Sedimentary Rock
Sedimentary rock forms through the deposition and lithification of sediment. It is categorized based on its composition and origin into clastic, chemical, and organic types. Clastic sedimentary rock like sandstone and shale form from cemented rock fragments. Chemical sedimentary rock like halite forms from crystallized mineral deposits. Organic sedimentary rock like coal forms from the remains of plants and animals. Sedimentary rock exhibits layers and other structures that indicate its formation history, such as ripple marks, mud cracks, and raindrop impressions preserved in the strata.
Report on sand
Sand is a naturally occurring granular material composed of finely divided rock and mineral particles. It is formed through the weathering and erosion of rocks and transported by wind and water. Sand is commonly divided into subcategories based on grain size, and its composition varies depending on the local rock sources. The most common type of sand found in coastal and continental areas is silica sand, usually in the form of quartz, which is very resistant to weathering. Sand has many uses including in construction, industrial applications like glassmaking, and recreational activities.
Economic geology - Sedimentary ore deposits
This document summarizes sedimentary ore deposits, specifically banded iron formations (BIF). It discusses the processes that form different types of BIF, including Algoma and Superior types, as well as their geologic time distribution. The document also explains the role of microbial communities in the deposition of iron minerals and formation of BIF layers through anoxic iron redox cycling, including phototrophic Fe(II) oxidation and nitrate-dependent Fe(II) oxidation mediated by bacteria. Overall, the document provides an overview of the genesis and microbial influences on the formation of important economic BIF deposits in sedimentary environments.
Soil classification
The document discusses soil texture and grain size distribution. It defines different soil types based on particle size, including gravel, sand, silt and clay. Various classification systems are used to categorize soils based on predominant particle sizes. The size of particles in a soil can range widely, from boulders larger than 60mm to clay particles smaller than 2 micrometers. The grain size distribution of a soil, including metrics like D10, D30 and D60, impact its engineering properties such as permeability and compressibility.
Sedimentary rocks bs 1st year
Sedimentary rocks form from the compaction and cementation of sediments. There are three main types: detrital (clastic) rocks that form from lithified rock fragments and minerals, chemical rocks that precipitate directly from solution, and organic rocks that accumulate from biological debris. Sedimentary rocks provide clues about past environments and climates based on their composition, structures like cross-bedding and ripples, and any fossil content. Important resources like coal and oil are also found within sedimentary basins.
Sediementary
1. Sedimentary rock forms through the compaction and cementation of sediments like sand and mud. Sediments are materials eroded from source rocks by weathering and transported via water, wind, or ice.
2. Sedimentary rocks are classified based on their composition and include clastic rocks like sandstone and conglomerate formed from fragments, and non-clastic rocks like limestone formed from minerals precipitated from solution.
3. Important sedimentary rocks and minerals discussed include various sandstones, conglomerates, limestones, dolomite, chalk, gypsum, anhydrite, halite, and evaporites. Characteristics like grain size, sorting, and cementation determine the
Classaification of sediments
Sediments are classified based on their particle size. There are four main categories of siliciclastic sedimentary particles: major minerals, accessory minerals, rock fragments, and chemical sediments. Sediments are named based on whether they are loose or consolidated into rock. Loose sediments include boulder, cobble, pebble, sand, silt, and clay depending on their size range. The corresponding consolidated rocks are conglomerate/breccia, gravel, sandstone, siltstone, and claystone/mudstone/shale. Carbonate sediments are comprised of minerals like aragonite, calcite, and dolomite. They generally form limestone when lithified, but can also form dolom
23.3.d sedimentary rocks ppt.ppt
The document discusses sedimentary rocks, describing their formation from weathering and erosion of pre-existing rocks. Sediment is transported via water or wind and sorted by size into gravel, sand, silt, or clay. Sediment is then deposited and may undergo lithification into sedimentary rock through compaction and cementation. The main types of sedimentary rocks are clastic (formed from fragments), chemical (formed from precipitation), and biochemical (containing organic material). Sedimentary structures provide clues about the environment of deposition, and the interpretation of these rocks can reveal information about past plate tectonic settings and conditions. Sedimentary rocks are an important source of non-metallic and energy resources.
sedimentaryrocks-190716154658.pdf
Sedimentary rocks form through the compaction and cementation of sediments. There are two main types - clastic sedimentary rocks, which form from eroded fragments of pre-existing rocks, and chemical sedimentary rocks, which form through precipitation or biochemical processes. Sedimentary rocks are classified based on their mineral composition, grain size, sorting, and rounding. Sedimentary structures within the rocks provide clues about the depositional environment.
Sedimentary rocks
Sedimentary rocks are formed by the lithification of sediments and include clastic sedimentary rocks such as sandstone and shale that are formed from fragments of pre-existing rocks transported by water, wind or ice. They also include chemical sedimentary rocks such as limestone that are formed via precipitation from solution. Sedimentary structures within these rocks provide clues about the depositional environment, and sedimentary rocks are classified based on their mineral composition, grain size, sorting and rounding. Common sedimentary rocks used in construction include sandstone, limestone and shale.
Sedimentary rocks
Sedimentary rocks are formed by the lithification of sediments and include clastic rocks from weathered rock fragments, chemical rocks from mineral precipitation, and organic rocks from accumulated biological matter. Sedimentary rocks provide clues to past environments through their composition and structures, and often contain fossils that reveal the history of life. Important resources like coal and oil are found within sedimentary layers.
1111111111456.pdf
Sedimentary rocks form from the consolidation of sediments and are divided into clastic, chemical, and biochemical types. Clastic rocks like sandstone and shale form from weathered fragments transported by wind, water, or ice. Chemical rocks like limestone precipitate directly from solution. Biochemical rocks such as coal form from the remains of living organisms. Sedimentary structures and fossils within rocks provide clues about depositional environments. Sedimentary rocks are economically important resources for construction materials, energy, and industrial minerals.
Petrologi 9-klastika
This document provides information about a petrology course for the 2008-2009 semester. The course includes 2 credits of theory and 1 credit of practical work. It is taught by Hill Gendoet Hartono on Mondays from 9:50-10:40 and 10:45-11:35. The document then provides detailed information about sedimentary rocks, including descriptions of different types of clastic rocks like breccias, conglomerates, sandstones and shales. It also discusses carbonate sedimentary rocks, chemical sedimentary rocks, and the environments and processes involved in forming different sedimentary rocks.
Petrologi 8-sedimen
This document provides an overview of a semester 2 course on petrology from 2007-2008 taught by Hill Gendoet Hartono. The course covers sedimentary rocks, sediments, the rock cycle, types of sedimentary rocks including clastic rocks like sandstones and shales, and chemical rocks like limestones. It discusses the processes of weathering, erosion, transport, deposition, and lithification that form sedimentary rocks. Key concepts covered are sedimentary environments, plate tectonics settings, and the economic importance of sedimentary rocks.
Sedimentary Rocks/EPCC/LM5 A
This document discusses different types of sedimentary rocks including clastic sedimentary rocks like breccia, conglomerate, sandstone, siltstone and shale formed from weathered debris. It also discusses chemical sedimentary rocks like limestone, evaporites including rock salt and gypsum, chert and coal. Finally, it mentions several sedimentary structures including cross bedded sandstone, graded bedding, mud cracks, ripple marks and trace fossils.
Sedimentary rocks
This slide will give you complete information about formation, classification, textures, structures and engineering importance of Sedimentary rocks.
Lect6 ppt of G2
This document provides a summary of common sedimentary rock types. It describes clastic sedimentary rocks such as sandstones, conglomerates, and shales which form from weathered rock and mineral particles. Sandstones are classified based on their composition and texture. Carbonate sedimentary rocks like limestones form from calcium carbonate and can have grain, micrite, or sparry textures. Siliceous sedimentary rocks like chert predominantly contain silica minerals that form from the shells of organisms like diatoms and radiolaria.
Characteristics of sedimentary rocks
The document provides information about sedimentary rocks, including their formation, classification, characteristics, and types. It discusses how sedimentary rocks form through the compaction and cementation of sediments. It classifies sedimentary rocks based on the nature of sediments (mechanically, chemically, or organically formed) and transporting agents (aqueous, aeolian, glacial). It provides details on specific sedimentary rock types like sandstones, conglomerates, limestone, and their properties. The document also covers concepts like bedding, stratification, unconformities in sedimentary rocks.
Petroleum geology lab 1
Rocks are a combination of minerals that are bonded together in some way.
All rocks are made of minerals
Monomineralic- contain one mineral
Polymineralic- contain more than one mineral
Rocks are classified into three groups by how they are formed
Igneous Rocks
Sedimentary rock
Metamorphic rock
The Bed Rocks
Sedimentary rocks represent materials deposited from ancient environments. There are two main types - clastic rocks formed from solid grains and chemical rocks formed from mineral precipitation. Sedimentary rocks provide information about past earth environments and contain important natural resources. They are found in depositional environments like continental, nearshore, and deep marine settings. Sedimentary rock characteristics like texture, structures, and fossils can provide clues about the depositional environment.
Sand
This document discusses different types and properties of sand. It describes sand as a mixture of small rock and mineral particles between 0.06 mm and 2 mm in size. The main components of sand are quartz and feldspar. Sand comes in different colors depending on its mineral composition, and there are various types including river sand, sea sand, volcanic sand, and heavy mineral sand. Sand is classified based on particle size, with very fine, fine, medium, and coarse categories.
Clastic sedimentary rockssmall
This document provides information on clastic/detrital sedimentary rocks, including their characteristics, classification, particle sizes, rock groups, terminology, and examples. It describes the key properties of sedimentary rocks formed from eroded fragments such as conglomerate, breccia, sandstone, siltstone, mudstone, shale, and discusses the environments in which they form.
Sedimentary Rock Classification
This document provides an overview of sedimentary rocks and the processes involved in their formation. Sedimentary rocks are formed from the deposition of materials at the Earth's surface or within bodies of water. They provide information about past environmental conditions and geological history. The key processes involved in sedimentary rock formation are weathering, erosion, transportation, deposition, and diagenesis, which is the chemical and physical changes that occur after deposition. Sedimentary rocks can be divided into clastic sediments like sandstone, chemical sediments like limestone formed by precipitation from solution, and biochemical sediments like coal formed from organic material.
Clastic and Non-Clastic Sediments
This PPT about Sedimentary Rock Classification of Clastic and Non-Clastic Rocks; Its tells about the origin and Types...
Stratified Rocks.pptx
The document describes different types of sedimentary rocks including sandstone, shale, conglomerate, siltstone, limestone, chert, rock salt, chalk, coal. It provides details on their composition, texture, color and formation. Sandstone is composed of sand particles and matrix deposited in water. Shale is a laminated rock made of silt and clay. Conglomerate contains rounded rock fragments over 2mm. Siltstone contains fine grains and can form layers. Limestone forms from marine life shells. Chert is made of microcrystalline quartz. Rock salt consists of sodium chloride crystals. Chalk forms from marine organisms. Coal accumulates from preserved plant materials.
South African Journal of Science: Writing with integrity workshop (2024)
South African Journal of Science: Writing with integrity workshop (2024)Academy of Science of South Africa
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Natural birth techniques - Mrs.Akanksha Trivedi Rama UniversityAkanksha trivedi rama nursing college kanpur.
Natural birth techniques are various type such as/ water birth , alexender method, hypnosis, bradley method, lamaze method etcMore Related Content
Similar to Sedimentary rock notes09
Sediementary
1. Sedimentary rock forms through the compaction and cementation of sediments like sand and mud. Sediments are materials eroded from source rocks by weathering and transported via water, wind, or ice.
2. Sedimentary rocks are classified based on their composition and include clastic rocks like sandstone and conglomerate formed from fragments, and non-clastic rocks like limestone formed from minerals precipitated from solution.
3. Important sedimentary rocks and minerals discussed include various sandstones, conglomerates, limestones, dolomite, chalk, gypsum, anhydrite, halite, and evaporites. Characteristics like grain size, sorting, and cementation determine the
Classaification of sediments
Sediments are classified based on their particle size. There are four main categories of siliciclastic sedimentary particles: major minerals, accessory minerals, rock fragments, and chemical sediments. Sediments are named based on whether they are loose or consolidated into rock. Loose sediments include boulder, cobble, pebble, sand, silt, and clay depending on their size range. The corresponding consolidated rocks are conglomerate/breccia, gravel, sandstone, siltstone, and claystone/mudstone/shale. Carbonate sediments are comprised of minerals like aragonite, calcite, and dolomite. They generally form limestone when lithified, but can also form dolom
23.3.d sedimentary rocks ppt.ppt
The document discusses sedimentary rocks, describing their formation from weathering and erosion of pre-existing rocks. Sediment is transported via water or wind and sorted by size into gravel, sand, silt, or clay. Sediment is then deposited and may undergo lithification into sedimentary rock through compaction and cementation. The main types of sedimentary rocks are clastic (formed from fragments), chemical (formed from precipitation), and biochemical (containing organic material). Sedimentary structures provide clues about the environment of deposition, and the interpretation of these rocks can reveal information about past plate tectonic settings and conditions. Sedimentary rocks are an important source of non-metallic and energy resources.
sedimentaryrocks-190716154658.pdf
Sedimentary rocks form through the compaction and cementation of sediments. There are two main types - clastic sedimentary rocks, which form from eroded fragments of pre-existing rocks, and chemical sedimentary rocks, which form through precipitation or biochemical processes. Sedimentary rocks are classified based on their mineral composition, grain size, sorting, and rounding. Sedimentary structures within the rocks provide clues about the depositional environment.
Sedimentary rocks
Sedimentary rocks are formed by the lithification of sediments and include clastic sedimentary rocks such as sandstone and shale that are formed from fragments of pre-existing rocks transported by water, wind or ice. They also include chemical sedimentary rocks such as limestone that are formed via precipitation from solution. Sedimentary structures within these rocks provide clues about the depositional environment, and sedimentary rocks are classified based on their mineral composition, grain size, sorting and rounding. Common sedimentary rocks used in construction include sandstone, limestone and shale.
Sedimentary rocks
Sedimentary rocks are formed by the lithification of sediments and include clastic rocks from weathered rock fragments, chemical rocks from mineral precipitation, and organic rocks from accumulated biological matter. Sedimentary rocks provide clues to past environments through their composition and structures, and often contain fossils that reveal the history of life. Important resources like coal and oil are found within sedimentary layers.
1111111111456.pdf
Sedimentary rocks form from the consolidation of sediments and are divided into clastic, chemical, and biochemical types. Clastic rocks like sandstone and shale form from weathered fragments transported by wind, water, or ice. Chemical rocks like limestone precipitate directly from solution. Biochemical rocks such as coal form from the remains of living organisms. Sedimentary structures and fossils within rocks provide clues about depositional environments. Sedimentary rocks are economically important resources for construction materials, energy, and industrial minerals.
Petrologi 9-klastika
This document provides information about a petrology course for the 2008-2009 semester. The course includes 2 credits of theory and 1 credit of practical work. It is taught by Hill Gendoet Hartono on Mondays from 9:50-10:40 and 10:45-11:35. The document then provides detailed information about sedimentary rocks, including descriptions of different types of clastic rocks like breccias, conglomerates, sandstones and shales. It also discusses carbonate sedimentary rocks, chemical sedimentary rocks, and the environments and processes involved in forming different sedimentary rocks.
Petrologi 8-sedimen
This document provides an overview of a semester 2 course on petrology from 2007-2008 taught by Hill Gendoet Hartono. The course covers sedimentary rocks, sediments, the rock cycle, types of sedimentary rocks including clastic rocks like sandstones and shales, and chemical rocks like limestones. It discusses the processes of weathering, erosion, transport, deposition, and lithification that form sedimentary rocks. Key concepts covered are sedimentary environments, plate tectonics settings, and the economic importance of sedimentary rocks.
Sedimentary Rocks/EPCC/LM5 A
This document discusses different types of sedimentary rocks including clastic sedimentary rocks like breccia, conglomerate, sandstone, siltstone and shale formed from weathered debris. It also discusses chemical sedimentary rocks like limestone, evaporites including rock salt and gypsum, chert and coal. Finally, it mentions several sedimentary structures including cross bedded sandstone, graded bedding, mud cracks, ripple marks and trace fossils.
Sedimentary rocks
This slide will give you complete information about formation, classification, textures, structures and engineering importance of Sedimentary rocks.
Lect6 ppt of G2
This document provides a summary of common sedimentary rock types. It describes clastic sedimentary rocks such as sandstones, conglomerates, and shales which form from weathered rock and mineral particles. Sandstones are classified based on their composition and texture. Carbonate sedimentary rocks like limestones form from calcium carbonate and can have grain, micrite, or sparry textures. Siliceous sedimentary rocks like chert predominantly contain silica minerals that form from the shells of organisms like diatoms and radiolaria.
Characteristics of sedimentary rocks
The document provides information about sedimentary rocks, including their formation, classification, characteristics, and types. It discusses how sedimentary rocks form through the compaction and cementation of sediments. It classifies sedimentary rocks based on the nature of sediments (mechanically, chemically, or organically formed) and transporting agents (aqueous, aeolian, glacial). It provides details on specific sedimentary rock types like sandstones, conglomerates, limestone, and their properties. The document also covers concepts like bedding, stratification, unconformities in sedimentary rocks.
Petroleum geology lab 1
Rocks are a combination of minerals that are bonded together in some way.
All rocks are made of minerals
Monomineralic- contain one mineral
Polymineralic- contain more than one mineral
Rocks are classified into three groups by how they are formed
Igneous Rocks
Sedimentary rock
Metamorphic rock
The Bed Rocks
Sedimentary rocks represent materials deposited from ancient environments. There are two main types - clastic rocks formed from solid grains and chemical rocks formed from mineral precipitation. Sedimentary rocks provide information about past earth environments and contain important natural resources. They are found in depositional environments like continental, nearshore, and deep marine settings. Sedimentary rock characteristics like texture, structures, and fossils can provide clues about the depositional environment.
Sand
This document discusses different types and properties of sand. It describes sand as a mixture of small rock and mineral particles between 0.06 mm and 2 mm in size. The main components of sand are quartz and feldspar. Sand comes in different colors depending on its mineral composition, and there are various types including river sand, sea sand, volcanic sand, and heavy mineral sand. Sand is classified based on particle size, with very fine, fine, medium, and coarse categories.
Clastic sedimentary rockssmall
This document provides information on clastic/detrital sedimentary rocks, including their characteristics, classification, particle sizes, rock groups, terminology, and examples. It describes the key properties of sedimentary rocks formed from eroded fragments such as conglomerate, breccia, sandstone, siltstone, mudstone, shale, and discusses the environments in which they form.
Sedimentary Rock Classification
This document provides an overview of sedimentary rocks and the processes involved in their formation. Sedimentary rocks are formed from the deposition of materials at the Earth's surface or within bodies of water. They provide information about past environmental conditions and geological history. The key processes involved in sedimentary rock formation are weathering, erosion, transportation, deposition, and diagenesis, which is the chemical and physical changes that occur after deposition. Sedimentary rocks can be divided into clastic sediments like sandstone, chemical sediments like limestone formed by precipitation from solution, and biochemical sediments like coal formed from organic material.
Clastic and Non-Clastic Sediments
This PPT about Sedimentary Rock Classification of Clastic and Non-Clastic Rocks; Its tells about the origin and Types...
Stratified Rocks.pptx
The document describes different types of sedimentary rocks including sandstone, shale, conglomerate, siltstone, limestone, chert, rock salt, chalk, coal. It provides details on their composition, texture, color and formation. Sandstone is composed of sand particles and matrix deposited in water. Shale is a laminated rock made of silt and clay. Conglomerate contains rounded rock fragments over 2mm. Siltstone contains fine grains and can form layers. Limestone forms from marine life shells. Chert is made of microcrystalline quartz. Rock salt consists of sodium chloride crystals. Chalk forms from marine organisms. Coal accumulates from preserved plant materials.
Similar to Sedimentary rock notes09 (20)
Recently uploaded
South African Journal of Science: Writing with integrity workshop (2024)
South African Journal of Science: Writing with integrity workshop (2024)Academy of Science of South Africa
A workshop hosted by the South African Journal of Science aimed at postgraduate students and early career researchers with little or no experience in writing and publishing journal articles.Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Natural birth techniques - Mrs.Akanksha Trivedi Rama UniversityAkanksha trivedi rama nursing college kanpur.
Natural birth techniques are various type such as/ water birth , alexender method, hypnosis, bradley method, lamaze method etcRHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
Physical pharmaceutics notes for B.pharm students
How to Create a More Engaging and Human Online Learning Experience
How to Create a More Engaging and Human Online Learning Experience Wahiba Chair Training & Consulting
Wahiba Chair's Talk at the 2024 Learning Ideas Conference. PCOS corelations and management through Ayurveda.
This presentation includes basic of PCOS their pathology and treatment and also Ayurveda correlation of PCOS and Ayurvedic line of treatment mentioned in classics.
How to Build a Module in Odoo 17 Using the Scaffold Method
Odoo provides an option for creating a module by using a single line command. By using this command the user can make a whole structure of a module. It is very easy for a beginner to make a module. There is no need to make each file manually. This slide will show how to create a module using the scaffold method.
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.
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.)
How to Setup Warehouse & Location in Odoo 17 Inventory
In this slide, we'll explore how to set up warehouses and locations in Odoo 17 Inventory. This will help us manage our stock effectively, track inventory levels, and streamline warehouse operations.
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
বাংলাদেশের অর্থনৈতিক সমীক্ষা ২০২৪ [Bangladesh Economic Review 2024 Bangla.pdf] কম্পিউটার , ট্যাব ও স্মার্ট ফোন ভার্সন সহ সম্পূর্ণ বাংলা ই-বুক বা pdf বই " সুচিপত্র ...বুকমার্ক মেনু 🔖 ও হাইপার লিংক মেনু 📝👆 যুক্ত ..
আমাদের সবার জন্য খুব খুব গুরুত্বপূর্ণ একটি বই ..বিসিএস, ব্যাংক, ইউনিভার্সিটি ভর্তি ও যে কোন প্রতিযোগিতা মূলক পরীক্ষার জন্য এর খুব ইম্পরট্যান্ট একটি বিষয় ...তাছাড়া বাংলাদেশের সাম্প্রতিক যে কোন ডাটা বা তথ্য এই বইতে পাবেন ...
তাই একজন নাগরিক হিসাবে এই তথ্য গুলো আপনার জানা প্রয়োজন ...।
বিসিএস ও ব্যাংক এর লিখিত পরীক্ষা ...+এছাড়া মাধ্যমিক ও উচ্চমাধ্যমিকের স্টুডেন্টদের জন্য অনেক কাজে আসবে ...
BÀI TẬP BỔ TRỢ TIẾNG ANH 8 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2023-2024 (CÓ FI...
BÀI TẬP BỔ TRỢ TIẾNG ANH 8 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2023-2024 (CÓ FI...Nguyen Thanh Tu Collection
https://app.box.com/s/y977uz6bpd3af4qsebv7r9b7s21935vdBBR 2024 Summer Sessions Interview Training
Qualitative research interview training by Professor Katrina Pritchard and Dr Helen Williams
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
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/tacvl9ekroe9hqupdnjruiypvm9rdaneWhat is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Aberdeen
How to deliver Powerpoint Presentations.pptx
"How to make and deliver dynamic presentations by making it more interactive to captivate your audience attention"
Recently uploaded (20)
South African Journal of Science: Writing with integrity workshop (2024)
South African Journal of Science: Writing with integrity workshop (2024)
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
Natural birth techniques - Mrs.Akanksha Trivedi Rama University
RHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
RHEOLOGY Physical pharmaceutics-II notes for B.pharm 4th sem students
How to Create a More Engaging and Human Online Learning Experience
How to Create a More Engaging and Human Online Learning Experience
How to Build a Module in Odoo 17 Using the Scaffold Method
How to Build a Module in Odoo 17 Using the Scaffold Method
Leveraging Generative AI to Drive Nonprofit Innovation
Leveraging Generative AI to Drive Nonprofit Innovation
Film vocab for eal 3 students: Australia the movie
Film vocab for eal 3 students: Australia the movie
How to Setup Warehouse & Location in Odoo 17 Inventory
How to Setup Warehouse & Location in Odoo 17 Inventory
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
বাংলাদেশ অর্থনৈতিক সমীক্ষা (Economic Review) ২০২৪ UJS App.pdf
BÀI TẬP BỔ TRỢ TIẾNG ANH 8 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2023-2024 (CÓ FI...
BÀI TẬP BỔ TRỢ TIẾNG ANH 8 CẢ NĂM - GLOBAL SUCCESS - NĂM HỌC 2023-2024 (CÓ FI...
Chapter wise All Notes of First year Basic Civil Engineering.pptx
Chapter wise All Notes of First year Basic Civil Engineering.pptx
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 - ...
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
What is Digital Literacy? A guest blog from Andy McLaughlin, University of Ab...
Sedimentary rock notes09
- 2. What are they? 3 types: Clastic or Terrigenous Biogenic Chemical
- 3. Clastic or Terrigenous sedimentary rocks WEDCC Many depositional locations: Continental Shoreline Marine
- 4. Grain Size Name of Particle Size Range Loose Sediment Consolidated Rock Boulder >256 mm Gravel Conglomerate or Breccia (depends on rounding) Cobble 64 - 256 mm Gravel Pebble 2 - 64 mm Gravel Sand 1/16 - 2mm Sand Sandstone Silt 1/256 - 1/16 mm Silt Siltstone Clay <1/256 mm Clay Claystone, mudstone, and shale
- 5. Texture Sorting- how uniform the particle size is Rounding- angular to rounded
- 6. Sedimentary structures Bedding (stratification) Cross-bedding Ripples Fossils
- 7. Biogenic sedimentary rocks Usually carbonate sediments Classified by mineral composition Created through biological processes Limited depositional location
- 8. Chemical sedimentary rocks precipitation of salts from solution Marine or non-marine Gypsum Halite