This document discusses a rock found in Hanford, California. The author examines the rock's physical properties and performs tests to determine it is basalt, an igneous rock. Basalt is common in the Lovejoy Basalt formation near the location it was found. The author believes the rock may have originated from that geological area.
The document describes Jacqueline Alvarez's journey to Los Gatos Road in Coalinga, CA where she observed various geological formations and features. She saw anticlines in the mountains that indicate the area's rich history of petroleum. She examined rocks like vaqueros sandstone, granite, conglomerate, and snail fossils. The document discusses how the local geology and biology have evolved over millions of years, from an ancient seabed to the present landscape, and shares pictures and references to support the observations.
California offers a variety of rock types due to its complex geological history. The document describes the author's process of collecting and identifying different rock samples from locations in California such as Yosemite National Park. Through online research of geological maps and the scientific method of questioning, hypothesizing and testing, the author was able to determine they had collected examples of igneous rocks such as granite and andesite, metamorphic rocks such as gneiss and phyllite, and sedimentary rocks including conglomerate and siltstone.
The author conducted field research at three locations, observing rocks, trees, plants, and animals. At the third location, a hike near Heavenly, the author found most of the samples and learned more about their surroundings. Samples included mafic diorite and brown chert rocks, Jeffrey pine trees containing ant nests, Collomia linearis and Penstemon newberryi plants, and tree borers on a fallen log. The author documented principles of geology observed like weathering, erosion, inclusions and unconformities.
The document describes the process of identifying different types of rocks found in California. It discusses going to geological maps and researching the local area to find igneous, metamorphic, and sedimentary rocks. Samples were collected from places like Yosemite National Park and analyzed using a scientific process to determine their classifications. Key details like appearance, texture, and location helped identify the rocks as granite, andesite, gneiss, phyllite, conglomerate, and siltstone.
This document is a thesis submitted by Claire Marie Showalter to Miami University in fulfillment of requirements for University Honors with Distinction. The thesis examines the historical and contemporary meanings of stone and glass as building materials. It will include timelines detailing the factual background and uses of each material. The text will be accompanied by original drawings and photos to illustrate key points. The thesis will conclude with a reflective essay summarizing the analysis and explaining formatting choices. The thesis analyzes how the meanings of stone and glass have changed over time and in different contexts.
The document describes a student's field and lab assignment where they identified and described various rocks and geological features they encountered. It includes descriptions of igneous, metamorphic, and sedimentary rocks the student found on hiking trips. The student also provides pictures showing examples of geological structures and processes like faults, mass wasting, weathering, sedimentary environments, erosion events, and how geology is applied in infrastructure.
The document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and provides details about their characteristics, formation processes, and common uses. Igneous rocks such as basalt form from cooling magma. Sedimentary rocks like sandstone are formed through deposition and cementation of sediments. Metamorphic rocks like slate form from existing rocks undergoing changes due to heat and pressure.
Year 11 Powerpoint about 3 main types of rock and their characteristics. Looks at their distribution in the UK. Brief intoduction about Granite (in more detail)
The document describes Jacqueline Alvarez's journey to Los Gatos Road in Coalinga, CA where she observed various geological formations and features. She saw anticlines in the mountains that indicate the area's rich history of petroleum. She examined rocks like vaqueros sandstone, granite, conglomerate, and snail fossils. The document discusses how the local geology and biology have evolved over millions of years, from an ancient seabed to the present landscape, and shares pictures and references to support the observations.
California offers a variety of rock types due to its complex geological history. The document describes the author's process of collecting and identifying different rock samples from locations in California such as Yosemite National Park. Through online research of geological maps and the scientific method of questioning, hypothesizing and testing, the author was able to determine they had collected examples of igneous rocks such as granite and andesite, metamorphic rocks such as gneiss and phyllite, and sedimentary rocks including conglomerate and siltstone.
The author conducted field research at three locations, observing rocks, trees, plants, and animals. At the third location, a hike near Heavenly, the author found most of the samples and learned more about their surroundings. Samples included mafic diorite and brown chert rocks, Jeffrey pine trees containing ant nests, Collomia linearis and Penstemon newberryi plants, and tree borers on a fallen log. The author documented principles of geology observed like weathering, erosion, inclusions and unconformities.
The document describes the process of identifying different types of rocks found in California. It discusses going to geological maps and researching the local area to find igneous, metamorphic, and sedimentary rocks. Samples were collected from places like Yosemite National Park and analyzed using a scientific process to determine their classifications. Key details like appearance, texture, and location helped identify the rocks as granite, andesite, gneiss, phyllite, conglomerate, and siltstone.
This document is a thesis submitted by Claire Marie Showalter to Miami University in fulfillment of requirements for University Honors with Distinction. The thesis examines the historical and contemporary meanings of stone and glass as building materials. It will include timelines detailing the factual background and uses of each material. The text will be accompanied by original drawings and photos to illustrate key points. The thesis will conclude with a reflective essay summarizing the analysis and explaining formatting choices. The thesis analyzes how the meanings of stone and glass have changed over time and in different contexts.
The document describes a student's field and lab assignment where they identified and described various rocks and geological features they encountered. It includes descriptions of igneous, metamorphic, and sedimentary rocks the student found on hiking trips. The student also provides pictures showing examples of geological structures and processes like faults, mass wasting, weathering, sedimentary environments, erosion events, and how geology is applied in infrastructure.
The document describes the three main types of rocks - igneous, sedimentary, and metamorphic - and provides details about their characteristics, formation processes, and common uses. Igneous rocks such as basalt form from cooling magma. Sedimentary rocks like sandstone are formed through deposition and cementation of sediments. Metamorphic rocks like slate form from existing rocks undergoing changes due to heat and pressure.
Year 11 Powerpoint about 3 main types of rock and their characteristics. Looks at their distribution in the UK. Brief intoduction about Granite (in more detail)
This document summarizes Sara Huckabey's geology project examining three rock types: igneous, metamorphic, and sedimentary rocks. For each rock type, Sara describes examples she found in different locations, provides pictures and her analysis of each rock, and identifies the type of rock based on its characteristics. She believes one igneous rock is feldspar found in a creek bed near Bakersfield. Her metamorphic rocks include possible slate found at Morro Bay beach and quartzite from a creek in Coalinga. The sedimentary rocks are likely sandstone from Pyramid Lake and limestone from caves at Pismo Beach.
Brennan Dowling visited the American River Parkway several times to photograph examples of living things and geological features. The parkway is located where mountain sediment from the Sierra Nevada mountains settled. Dowling found examples that showed geological changes over time, including a snake skeleton, deer, and blackberry bushes. Rock samples were collected from creek beds that appeared to be metamorphic rocks such as marble, schist, and hornfels. A photograph showed an old engine sticking out of sediment layers, demonstrating Steno's principle of superposition. A creek bed wall also featured a disconformity between sediment layers.
This document provides a summary of a field assignment to document the animal and plant life, rock types, and geological features of Signal Hill and San Pedro, California. The assignment involved taking photographs of these elements in both locations to analyze and draw conclusions. Signal Hill is at a higher elevation closer to water, while San Pedro is on the coast with some hills and cliffs. Common rocks in San Pedro include basalt from volcanic activity. Several species found in the areas are described, including the invasive purple fountain grass, native bush sunflower, gray bird grasshopper, and various rock samples like sandstone, andesite, and shale.
The Lake Tahoe Basin formed over millions of years through the movement of tectonic plates and glacial activity. Approximately 670 million years ago, the area was a shallow sea. As the plates collided and pushed against each other over 130 million years, lava plumes rose and granite formed. Around 10 million years ago, faults caused the Sierra Nevada to rise, creating the valley where Lake Tahoe now sits. The last ice age, ending 10,000 years ago, shaped features like Emerald Bay through glacial activity. Today, the area is surrounded by granite peaks and contains diverse plant and animal life.
This document summarizes a geology student's rock sample collection and analysis from two locations in Washington state. At Rosario Beach, the student found two sedimentary rocks - chert and shale. At Fall City along the Snoqualmie River, the student discovered three igneous rocks - granite, andesite, and one metamorphic rock, hornfels. The student provided details on the appearance and characteristics that led to the identification of each rock sample.
1) The document describes a geology student collecting and analyzing 5 rock samples near some railroad tracks in Firebaugh, California.
2) The first sample is identified as granite, an igneous rock that forms when magma cools underground.
3) The second sample is marble, a metamorphic rock formed from limestone.
4) The third sample is scoria, a volcanic rock with gas bubbles indicating it cooled quickly.
1) The document summarizes the author's observations from hiking trails near Simi Valley, California. The author observed various plants and animals, including black mustard, mallards, squirrels, and lizards. The author also examined and classified various rocks found on the trails.
2) The author discusses the evolution of mallards, black mustard, and the three rock types identified: shale, sandstone, and granite. Principles of stratigraphy, including the principle of inclusions and unconformities are also explained.
3) References are provided for information on the plants, animals, and geology discussed in the report. Photos taken by the author are included to illustrate observations.
1. The document describes a sedimentary sandstone rock found in Sequoia Park. It is gray and black with tiny black crystal dots and grass growing in parts of it.
2. A metamorphic hornfels rock is described as dark gray to black, hard, and breaking into sharp angular pieces. It formed under heat and pressure near magma or intrusions.
3. A siltstone rock is pale colored with small holes and black dots. It was found near a small lake in Santa Cruz Boardwalk.
This document contains a student's lab assignment consisting of three parts: descriptions of rocks found in different environments, descriptions of geological features and processes, and examples of practical uses of geology. The student provides summaries of sedimentary rocks found near lakes and rivers based on their location and physical characteristics. Descriptions of an igneous rock found at a waste water treatment plant and a metamorphic rock seen in Yosemite are also given. The second part discusses the San Andreas fault and examples of weathering. The third part gives examples of different sedimentary environments and practical applications of geology such as in construction.
The document discusses various rocks, geological formations, and wildlife found near the Yuba River in the Tahoe National Forest. Samples of quartzite, basalt, and granite rocks were collected and identified based on their characteristics. An angular unconformity sample showed tilted igneous rock overlaid by sedimentary deposits. An inclusion sample showed an older lighter rock within a darker surrounding rock. Other observations included a blackberry bush, signs of brown bears, and details about the formation of the Yuba River over millions of years.
The document discusses geological changes that have occurred around Lake Tahoe over time. It notes that the Lake Tahoe basin was formed 3-5 million years ago by rising mountains on both sides, and the lake took shape from faulting, volcanic activity, and glaciation. Lava flows formed dams that allowed rivers and streams to fill the basin. The document also provides details on the present features of Lake Tahoe such as its depth and location along the California-Nevada border.
This document contains descriptions of various geological features and samples observed in the field, including:
1) A sandstone rock sample found in Sequoia Park that is gray and black with tiny black crystals and lines.
2) A hornfels rock sample also found in Sequoia Park that is almost black with some light blue and green cracks.
3) A siltstone rock sample found at the Santa Cruz Boardwalk that has a pale color with small holes and black dots.
This document contains descriptions of various geological features and samples observed in the field, including:
1) A sandstone rock sample found in Sequoia Park described as gray and black with tiny black crystals and grass growing in parts.
2) A hornfels rock sample found in Sequoia Park described as almost black with light blue and green colors and small cracks.
3) A siltstone rock sample found at the Santa Cruz Boardwalk described as pale colored with small holes and black dots.
4) A rhyolite rock sample found in the author's backyard described as light brown in color and located in a muddy area with cracks.
5) An amphibolite rock
Enrique Lomeli collected 5 rock samples for a geology field lab. The first was a metamorphic gneiss rock found in Avocado Lake, California. The second was a metamorphic slate rock found in San Miguel, California. The third was an igneous granite rock found in Bear Creek near Merced River in Fresno County. The fourth was a sedimentary limestone rock also found near Avocado Lake. The fifth and final sample was a sedimentary sandstone rock found in Parkfield, California near the San Andreas Fault.
This document provides descriptions and background information for several rock samples collected from locations in California. It describes obsidian collected in Bishop, granite from Raymond, "cross rocks" from Chowchilla, a sedimentary rock also from Chowchilla, and a metamorphic rock near a slough in Chowchilla. For each rock, it provides details on appearance, composition and formation, as well as context about the sampling locations.
This document contains descriptions and background information about several rock samples collected from locations in California. It includes details about obsidian collected in Bishop, granite from Raymond, staurolite "cross rocks" from Chowchilla, a sedimentary rock with embedded rocks from Chowchilla, and a metamorphic rock near a slough in Chowchilla. For each rock, it provides information on physical characteristics, how it was identified, and geological context of where it was found.
The document describes the student's field trip to Morro Bay in California. They found various rocks during their exploration, including igneous rocks like dacite which forms Morro Rock, sedimentary rocks like marble, and metamorphic rocks like granite. They also observed different geological features and processes along the shoreline such as faults, weathering, erosion, and more. The student documented their findings through pictures and descriptions to complete their field project.
This document provides examples and descriptions of different types of rocks, including sedimentary (shale, sandstone, limestone), igneous (basalt, granite), and metamorphic (marble). The sedimentary rocks were described as being formed from layers of sand and mud 130-150 million years ago in Napa, CA. The igneous basalt was seen in Hawaii near a volcano and is estimated to be 23,000 years old. Granite was observed in Stanislaus National Forest with a coarse texture. Tennessee marble found in city hall was formed 4600 million years ago from bryozoan accumulations. Limestone in Hayward, CA city hall is 450 million years old Kasota stone
The document describes 5 different rock samples collected by Roberto Vargas. The first sample is basalt, an extrusive igneous rock found near Parkfield, California. The second is a metamorphic rock called gneiss that has undergone regional metamorphism giving it a layered appearance. The third is an intrusive igneous rock, granite, found near Slack Canyon with quartz and feldspar. The fourth is a sedimentary limestone sample near a creek. The fifth sample is another extrusive basalt rock found on Parkfield Road, larger than expected.
The document summarizes the geology of the San Joaquin Valley in California. It describes how the valley formed 65 million years ago between two mountain ranges. Sediment from the Sierra Nevada filled the basin. The document also discusses the evolution of pill bugs from sea creatures with gills to land-dwelling crustaceans. Spider plants are described as having adapted from South African origins to survive drought conditions through a tuberous root system. Samples of igneous granite, metamorphic slate, and sedimentary shale rocks found in Fresno are presented along with their identifying characteristics.
This document summarizes Sara Huckabey's geology project examining three rock types: igneous, metamorphic, and sedimentary rocks. For each rock type, Sara describes examples she found in different locations, provides pictures and her analysis of each rock, and identifies the type of rock based on its characteristics. She believes one igneous rock is feldspar found in a creek bed near Bakersfield. Her metamorphic rocks include possible slate found at Morro Bay beach and quartzite from a creek in Coalinga. The sedimentary rocks are likely sandstone from Pyramid Lake and limestone from caves at Pismo Beach.
Brennan Dowling visited the American River Parkway several times to photograph examples of living things and geological features. The parkway is located where mountain sediment from the Sierra Nevada mountains settled. Dowling found examples that showed geological changes over time, including a snake skeleton, deer, and blackberry bushes. Rock samples were collected from creek beds that appeared to be metamorphic rocks such as marble, schist, and hornfels. A photograph showed an old engine sticking out of sediment layers, demonstrating Steno's principle of superposition. A creek bed wall also featured a disconformity between sediment layers.
This document provides a summary of a field assignment to document the animal and plant life, rock types, and geological features of Signal Hill and San Pedro, California. The assignment involved taking photographs of these elements in both locations to analyze and draw conclusions. Signal Hill is at a higher elevation closer to water, while San Pedro is on the coast with some hills and cliffs. Common rocks in San Pedro include basalt from volcanic activity. Several species found in the areas are described, including the invasive purple fountain grass, native bush sunflower, gray bird grasshopper, and various rock samples like sandstone, andesite, and shale.
The Lake Tahoe Basin formed over millions of years through the movement of tectonic plates and glacial activity. Approximately 670 million years ago, the area was a shallow sea. As the plates collided and pushed against each other over 130 million years, lava plumes rose and granite formed. Around 10 million years ago, faults caused the Sierra Nevada to rise, creating the valley where Lake Tahoe now sits. The last ice age, ending 10,000 years ago, shaped features like Emerald Bay through glacial activity. Today, the area is surrounded by granite peaks and contains diverse plant and animal life.
This document summarizes a geology student's rock sample collection and analysis from two locations in Washington state. At Rosario Beach, the student found two sedimentary rocks - chert and shale. At Fall City along the Snoqualmie River, the student discovered three igneous rocks - granite, andesite, and one metamorphic rock, hornfels. The student provided details on the appearance and characteristics that led to the identification of each rock sample.
1) The document describes a geology student collecting and analyzing 5 rock samples near some railroad tracks in Firebaugh, California.
2) The first sample is identified as granite, an igneous rock that forms when magma cools underground.
3) The second sample is marble, a metamorphic rock formed from limestone.
4) The third sample is scoria, a volcanic rock with gas bubbles indicating it cooled quickly.
1) The document summarizes the author's observations from hiking trails near Simi Valley, California. The author observed various plants and animals, including black mustard, mallards, squirrels, and lizards. The author also examined and classified various rocks found on the trails.
2) The author discusses the evolution of mallards, black mustard, and the three rock types identified: shale, sandstone, and granite. Principles of stratigraphy, including the principle of inclusions and unconformities are also explained.
3) References are provided for information on the plants, animals, and geology discussed in the report. Photos taken by the author are included to illustrate observations.
1. The document describes a sedimentary sandstone rock found in Sequoia Park. It is gray and black with tiny black crystal dots and grass growing in parts of it.
2. A metamorphic hornfels rock is described as dark gray to black, hard, and breaking into sharp angular pieces. It formed under heat and pressure near magma or intrusions.
3. A siltstone rock is pale colored with small holes and black dots. It was found near a small lake in Santa Cruz Boardwalk.
This document contains a student's lab assignment consisting of three parts: descriptions of rocks found in different environments, descriptions of geological features and processes, and examples of practical uses of geology. The student provides summaries of sedimentary rocks found near lakes and rivers based on their location and physical characteristics. Descriptions of an igneous rock found at a waste water treatment plant and a metamorphic rock seen in Yosemite are also given. The second part discusses the San Andreas fault and examples of weathering. The third part gives examples of different sedimentary environments and practical applications of geology such as in construction.
The document discusses various rocks, geological formations, and wildlife found near the Yuba River in the Tahoe National Forest. Samples of quartzite, basalt, and granite rocks were collected and identified based on their characteristics. An angular unconformity sample showed tilted igneous rock overlaid by sedimentary deposits. An inclusion sample showed an older lighter rock within a darker surrounding rock. Other observations included a blackberry bush, signs of brown bears, and details about the formation of the Yuba River over millions of years.
The document discusses geological changes that have occurred around Lake Tahoe over time. It notes that the Lake Tahoe basin was formed 3-5 million years ago by rising mountains on both sides, and the lake took shape from faulting, volcanic activity, and glaciation. Lava flows formed dams that allowed rivers and streams to fill the basin. The document also provides details on the present features of Lake Tahoe such as its depth and location along the California-Nevada border.
This document contains descriptions of various geological features and samples observed in the field, including:
1) A sandstone rock sample found in Sequoia Park that is gray and black with tiny black crystals and lines.
2) A hornfels rock sample also found in Sequoia Park that is almost black with some light blue and green cracks.
3) A siltstone rock sample found at the Santa Cruz Boardwalk that has a pale color with small holes and black dots.
This document contains descriptions of various geological features and samples observed in the field, including:
1) A sandstone rock sample found in Sequoia Park described as gray and black with tiny black crystals and grass growing in parts.
2) A hornfels rock sample found in Sequoia Park described as almost black with light blue and green colors and small cracks.
3) A siltstone rock sample found at the Santa Cruz Boardwalk described as pale colored with small holes and black dots.
4) A rhyolite rock sample found in the author's backyard described as light brown in color and located in a muddy area with cracks.
5) An amphibolite rock
Enrique Lomeli collected 5 rock samples for a geology field lab. The first was a metamorphic gneiss rock found in Avocado Lake, California. The second was a metamorphic slate rock found in San Miguel, California. The third was an igneous granite rock found in Bear Creek near Merced River in Fresno County. The fourth was a sedimentary limestone rock also found near Avocado Lake. The fifth and final sample was a sedimentary sandstone rock found in Parkfield, California near the San Andreas Fault.
This document provides descriptions and background information for several rock samples collected from locations in California. It describes obsidian collected in Bishop, granite from Raymond, "cross rocks" from Chowchilla, a sedimentary rock also from Chowchilla, and a metamorphic rock near a slough in Chowchilla. For each rock, it provides details on appearance, composition and formation, as well as context about the sampling locations.
This document contains descriptions and background information about several rock samples collected from locations in California. It includes details about obsidian collected in Bishop, granite from Raymond, staurolite "cross rocks" from Chowchilla, a sedimentary rock with embedded rocks from Chowchilla, and a metamorphic rock near a slough in Chowchilla. For each rock, it provides information on physical characteristics, how it was identified, and geological context of where it was found.
The document describes the student's field trip to Morro Bay in California. They found various rocks during their exploration, including igneous rocks like dacite which forms Morro Rock, sedimentary rocks like marble, and metamorphic rocks like granite. They also observed different geological features and processes along the shoreline such as faults, weathering, erosion, and more. The student documented their findings through pictures and descriptions to complete their field project.
This document provides examples and descriptions of different types of rocks, including sedimentary (shale, sandstone, limestone), igneous (basalt, granite), and metamorphic (marble). The sedimentary rocks were described as being formed from layers of sand and mud 130-150 million years ago in Napa, CA. The igneous basalt was seen in Hawaii near a volcano and is estimated to be 23,000 years old. Granite was observed in Stanislaus National Forest with a coarse texture. Tennessee marble found in city hall was formed 4600 million years ago from bryozoan accumulations. Limestone in Hayward, CA city hall is 450 million years old Kasota stone
The document describes 5 different rock samples collected by Roberto Vargas. The first sample is basalt, an extrusive igneous rock found near Parkfield, California. The second is a metamorphic rock called gneiss that has undergone regional metamorphism giving it a layered appearance. The third is an intrusive igneous rock, granite, found near Slack Canyon with quartz and feldspar. The fourth is a sedimentary limestone sample near a creek. The fifth sample is another extrusive basalt rock found on Parkfield Road, larger than expected.
The document summarizes the geology of the San Joaquin Valley in California. It describes how the valley formed 65 million years ago between two mountain ranges. Sediment from the Sierra Nevada filled the basin. The document also discusses the evolution of pill bugs from sea creatures with gills to land-dwelling crustaceans. Spider plants are described as having adapted from South African origins to survive drought conditions through a tuberous root system. Samples of igneous granite, metamorphic slate, and sedimentary shale rocks found in Fresno are presented along with their identifying characteristics.
How to Make a Field Mandatory in Odoo 17Celine George
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.
Strategies for Effective Upskilling is a presentation by Chinwendu Peace in a Your Skill Boost Masterclass organisation by the Excellence Foundation for South Sudan on 08th and 09th June 2024 from 1 PM to 3 PM on each day.
Chapter wise All Notes of First year Basic Civil Engineering.pptxDenish Jangid
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
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 ...
ISO/IEC 27001, ISO/IEC 42001, and GDPR: Best Practices for Implementation and...PECB
Denis is a dynamic and results-driven Chief Information Officer (CIO) with a distinguished career spanning information systems analysis and technical project management. With a proven track record of spearheading the design and delivery of cutting-edge Information Management solutions, he has consistently elevated business operations, streamlined reporting functions, and maximized process efficiency.
Certified as an ISO/IEC 27001: Information Security Management Systems (ISMS) Lead Implementer, Data Protection Officer, and Cyber Risks Analyst, Denis brings a heightened focus on data security, privacy, and cyber resilience to every endeavor.
His expertise extends across a diverse spectrum of reporting, database, and web development applications, underpinned by an exceptional grasp of data storage and virtualization technologies. His proficiency in application testing, database administration, and data cleansing ensures seamless execution of complex projects.
What sets Denis apart is his comprehensive understanding of Business and Systems Analysis technologies, honed through involvement in all phases of the Software Development Lifecycle (SDLC). From meticulous requirements gathering to precise analysis, innovative design, rigorous development, thorough testing, and successful implementation, he has consistently delivered exceptional results.
Throughout his career, he has taken on multifaceted roles, from leading technical project management teams to owning solutions that drive operational excellence. His conscientious and proactive approach is unwavering, whether he is working independently or collaboratively within a team. His ability to connect with colleagues on a personal level underscores his commitment to fostering a harmonious and productive workplace environment.
Date: May 29, 2024
Tags: Information Security, ISO/IEC 27001, ISO/IEC 42001, Artificial Intelligence, GDPR
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2. •This is an igneous rock. I was fairly sure this rock was granite,
•Granite is cooled intrusively (beneath but decided to break it open with a
the surface of the Earth). hammer and see the inside to be sure.
•The composition of granite is Sialic Once broken, I could see the signature
with coarse grains and flecks of quartz salt-and-pepper look of granite along
and potassium feldspar. with the shimmery flecks of quartz
and potassium feldspar!
3. I found this chunk of granite rock in a field in
Hanford, California, near my workplace. There are
many fields around the area and a variety of rocks can
be found there. Yosemite National Park’s bedrock is
formed mostly of granite. There are many formations
(El Capitan, Cathedral Rocks, etc.) that are formed
from this granite (Time). This chunk of granite is
fairly large and I believe most likely came down from
the Yosemite area.
4. I first identified this rock as a Studying this rock in low light,
sedimentary rock, identified by its one can see the few shimmery
several strata from compressed layers flecks in the surface of the rock.
of sediment and brownish-gray color.
The texture of the rock is not
gritty, like the sedimentary rock
It is also very smooth in texture, most sandstone, but instead is
likely from water. Further identified, I extremely smooth. I assumed
believe this rock may be basalt. this may be either from long
exposure to wind or water. Some
of the layers in the rock look like
they are etched in and possibly
disintegrating. This leads me to
the conclusion that some layers
of the sediment were not held
together as strongly as the others
due to the material they are
made up of.
5. This rock is extremely hard and would
not break with a hammer. I had to use a
sledge hammer to break it open. Once
broken open, the layers that were so
apparent on the outside of the rock
became almost non-existent on the
inside. The entire rock is extremely fine-
grained and the inside is a dark grey and
very shimmery. Because the shimmers
are so many and so tiny, I would guess
that they may be flecks of mica. There
are flecks of mica in basalt. I also did the
scratch test with this rock, and was not
able to scratch it with a nail. Using a
knife, I was able to scratch thin, shallow
lines into the surface of the rock. Further Outward appearance, this rock looks
testing with vinegar, I dropped a couple sedimentary, but the inside makes
of drops onto the exterior surface, as well
as the inside, and nothing happened. me think metamorphic. Due to the
This is common for basalt rocks, unless physical properties and the tests that
there are patches or bands of calcite, I did on this rock, I concluded that
which there weren’t in my rock.
this rock is the igneous rock, basalt.
6. I found this intriguing and perplexing rock on a
country road in Hanford, California while out taking
photographs. If I correctly identified this rock as
basalt, then it may be from the Lovejoy basalt, the
largest eruptive unit in California. The Lovejoy flowed
to the Sacramento Valley, which is very near to our
Central Valley, where Hanford, California is located (A
Mantle Plume).
7. This rock is white with semi- I deduced that this rock
translucent high-shine flecks in it. In
this piece, there are a small amount of was marble due to the
gray streaks and many medium-sized color, shape, shining
crystals that glitter when light is flecks, and scratch and
shined on it. I scratched this rock vinegar tests. Marble is a
with a knife and white powder came metamorphic rock that was
off easily. I also tried the white
vinegar test, which produced slight once limestone. Limestone
bubbling. is a sedimentary rock, but
once exposed to high heat
and pressure underground,
it morphs into marble
(Neighborhood Rocks:
White Marble).
8. I found this chunk of marble in another field between
my house and work in Hanford, California. It really is
a beautiful rock and it stood out in the field because of
its stark white color and reflective flecks throughout
the rock. I deduced that this rock probably came from
someone’s garden/landscaping project because, after
researching, I found that there aren’t any large marble
areas around here. Marble chips are sold at home
improvement stores and nurseries and are commonly
found in landscaping.
9. Kingdom: Animalia (animals)
Phylum: Anthropoda (crustaceans,
spiders, insects, and relatives)
Class: Arachnida (arachnids)
Order: Solpugida ( solpugids and sun
spiders) (ADW)
10. Sun spiders are otherwise known as
camel spiders or wind scorpions.
The names come from the color,
humped back, or speed of the
spider-like insect. These creatures
are commonly found in the desert
but they do not like the sun. It looks
like a scorpion mixed with a spider,
but it is not a spider. It uses its front
legs (which are sticky) to grab its
prey and pull it towards its pincers,
which work like tiny saws to liquefy
it before consuming it. They are not
venomous and usually go near
humans merely to stand in the
This sun spider was found in Hanford, shade of their shadow (Cranshaw).
CA, in a home improvement store.
Since these insects are desert dwellers,
I’m guessing this guy hitched a ride
from one of the seamen that came back
from Navy business in Fallon, CA.
12. The California Poppy is the
state flower for California
and grows wild throughout
the state. They flourish on
hillsides and in grassy,
sandy, or rocky areas that
are dry. They grow
primarily in Southern
California, but are also
This poppy is growing in Hanford, common up the coast
CA, located in the Central Valley, through Oregon and into
which is a very dry area. Washington, as well as in
Nevada, New Mexico, and
the northern part of Baja,
Mexico (Biogeography).
13. The Kings River that runs
through Kings County, Fresno
County, and Kings Canyon
National Park in California
begins in the Sierra Nevada.
Some parts of the river are
dammed and much of the river
is utilized for its
agricultural/irrigation
purposes. It has also carved
one of the deepest canyons in
North America, beginning in
the Sierra Nevada and
dropping more than 13,000ft to
the upper limit to the Pine Flat
Reservoir! (Friends of the
River)
14. This is a picture of what the
part of Kings River looks
like that runs near
Lemoore, Ca. It is
commonly utilized during
the warmer months for
rafting, floating, boating,
and fishing. This part of
the river is far from the
Middle and North Forks
that are more commonly
known for its rafting
opportunities.
15.
16. References
A mantle plume beneath California? The mid-Miocene Lovejoy flood basalt, northern California . (n.d.). Geological Society of America Special
Papers . Retrieved November 15, 2011, from http://specialpapers.gsapubs.org/content/438/551.abstract
ADW: Eremobatidae: Classification. (n.d.). Animal Diversity Web. Retrieved November 18, 2011, from
http://animaldiversity.ummz.umich.edu/site/accounts/classification/path/Eremobatidae.html#Eremobatidae
Biogeography of the California Poppy. (n.d.). redirect. Retrieved November 18, from
http://bss.sfsu.edu/holzman/courses/Fall02%20projects/calpoppy.html
Cranshaw, W. (n.d.). Sunspiders (Windscorpions). Colorado State University Extension. Retrieved November 18, 2011, from
http://www.ext.colostate.edu/pubs/insect/05589.html
Friends of the River: California Rivers - Kings River. (n.d.). Friends of the River: Home Preserve Restore Sustain California Rivers. Retrieved
November 18, 2011, from http://www.friendsoftheriver.org/site/PageServer?pagename=FORCalRiversKingsRiver
Neighborhood Rocks: Gray Slate. (n.d.). Salt the Sandbox: Home Page. Retrieved November 18, 2011, from
http://saltthesandbox.org/rocks/grayslate.htm
Neighborhood Rocks: Scoria Basalt. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from
http://saltthesandbox.org/rocks/basalt.htm
Neighborhood Rocks: White Marble. (n.d.). Salt the Sandbox: Home Page. Retrieved November 12, 2011, from
http://saltthesandbox.org/rocks/whitemarble.htm#HowFormed
claystone (geology) -- Britannica Online Encyclopedia. (n.d.). Encyclopedia - Britannica Online Encyclopedia. Retrieved December 1, 2011, from
http://www.britannica.com/EBchecked/topic/120751/claystone
time, m. C., & ago, a. f. (n.d.). CVO Menu - America's Volcanic Past - Yosemite. USGS Cascades Volcano Observatory (CVO). Retrieved December 1,
2011, from http://vulcan.wr.usgs.gov/LivingWith/VolcanicPast/Places/volcanic_past_yosemite.html