This document discusses crustal deformation and geologic structures. It describes the different types of stresses that cause deformation, including compressional, tensional, and shear stresses associated with convergent, divergent, and transform plate boundaries. It also explains how rocks deform through folding, faulting, and fracturing in response to these stresses. Specific structures covered include folds like anticlines and synclines, as well as normal, reverse, thrust, and strike-slip faults. The document concludes by discussing how geologists measure and map the orientation of rock layers and faults.
Faults occur along planes of weakness in the Earth's crust where displacement has taken place due to tectonic forces. There are three main types of faults - normal faults caused by tension, reverse faults caused by compression, and strike-slip faults caused by horizontal shear. Faults lead to different types of mountain formation, such as folded mountains from crustal compression, fault-block mountains from vertical movement along fault planes, and volcanic mountains from magma erupting at divergent boundaries.
The document defines and provides examples of different types of geological folds including anticlines, synclines, monoclines, recumbent folds, overturned folds, plunging folds, ptygmatic folds, chevron folds, and drag folds. Examples show the folded rock strata, describing the plate tectonics settings and rock types involved. Different terminology is introduced for upwardly arched anticlines versus downwardly arched synclines and other specialized fold patterns.
Folding occurs when layers of rock in the crust buckle due to collisions between tectonic plates. There are two main types of folds: anticlines, where the rock layers buckle upwards in an inverted U-shape, and synclines, where layers buckle downwards in a U-shape. Different kinds of folds form depending on the direction and amount of compressional forces, including symmetrical, asymmetrical, overfolded, recumbent, and overthrust folds. Folding of layers can result in the formation of fold mountains over geologic timescales.
Geological structures folds faults joints types of folds jointsAmjad Ali Soomro
This document discusses different types of geological structures including folds, faults, and joints. It defines key terms related to these structures and provides examples. Specifically, it describes:
1) Different types of folds such as anticlines, synclines, symmetrical, asymmetrical, overturned, and recumbent folds.
2) Fault types including normal, reverse, strike-slip, oblique-slip, and blind faults. It explains the movement and features of each.
3) Joints as fractures with no displacement that form due to stresses and rock movements, and classifies them as tension or shear joints.
Structural Geology for petroleum Egineering GeologyKamal Abdurahman
Structural geology is the study of geological structures like faults, folds, and joints. It provides important information for fields like engineering geology, economic geology, and plate tectonics. Folds form when rock layers bend under pressure and heat. The limbs of folds dip inward or outward forming anticlines and synclines. Faults form when rocks break under stress, producing displacement along a fracture. The hanging wall moves relative to the footwall. Joints are fractures without displacement that form to relieve stress. Unconformities represent gaps in the geological record due to erosion. They provide evidence about past environmental conditions. Structural features must be considered for engineering projects due to their effects on rock strength and fluid flow. Plate t
Structural geology is the study of the architecture and geometry of the Earth's crust and the processes that have shaped it. It involves analyzing how rock bodies deform in response to tectonic stresses. Structural analysis generally involves descriptive, kinematic, and dynamic analysis. Descriptive analysis describes rock structures like folds and faults. Kinematic analysis evaluates strain and changes in shape and orientation of rocks. Dynamic analysis reconstructs the stresses that caused rock deformation and failure. Stresses in rocks can be tensile, compressive, or shear stresses. Stress is analyzed using concepts like the stress tensor, Mohr's circle diagrams, and the orientation of maximum shear stresses. The main sources of stress that drive deformation are the motions of tectonic
The document discusses faults in terms of geology. It begins by defining a fault as a fracture between rock blocks that have moved relative to each other parallel to the fracture plane. It then discusses different types of faults including normal faults, strike-slip faults, and oblique slip faults. It provides examples of key features associated with different fault types, such as horsts and grabens associated with normal faults, and flower structures associated with strike-slip faults. The document also discusses methods for recognizing faults based on geological, fault plane, and physiographic evidence observed in the field.
Fault is a fracture discontinuity along which the rocks on either side have moved past each other . It describes about the parts and types of fault an also the various field evidences for the occurrence of a fault .
This document discusses various structural geology concepts including folds, faults, joints, strike and dip. It defines key terms like anticline, syncline, and provides classifications of different fold types such as symmetrical vs. asymmetrical. Faults are described as fractures with displacement, and classified by displacement type. Joints are fractures that do not involve displacement. The effects of joints on rock competence and permeability are also noted.
Normal faults occur when rocks pull apart, causing the rock on one side of the fault to move down relative to the other side. Reverse faults occur when rocks are pushed together, causing the rock on one side to move up. Transform faults cause horizontal movement between blocks of rock on either side. Oblique faults involve a combination of these movements. Faults represent zones of weakness where future earthquakes and surface rupturing are most likely to occur. Infrastructure like buildings and transportation corridors in fault zones faces damage during seismic activity.
The document discusses various geological structures including outcrops, rock deformation, folds, faults, and joints. It defines key terms like strike and dip which are used to describe the orientation of deformed rocks. It explains different types of folds such as anticlines, synclines, overturned folds, and plunging folds. It also describes various types of faults including normal faults, thrust faults, strike-slip faults, and transform faults. Additionally, it discusses joints as fractures in rocks where there is no relative displacement and classifies joints based on their orientation. In summary, the document provides an overview of structural geology and the terminology used to describe deformed rocks and geological structures.
The document discusses endogenetic forces that cause folding and faulting within the Earth's crust. It describes several types of folds that occur due to compression, such as anticlines where rock layers bend upwards and synclines where they bend downwards. It also details different fault types like normal faults where rocks move apart and reverse faults where they move together. In total, the document outlines seven fold types and five fault types that shape the Earth's surface over millions of years through horizontal and vertical crustal movements.
This document provides an overview of structural geology concepts including folds, faults, strike, dip, and fold classification. It discusses that structural geology studies secondary rock structures like folds and faults, and defines key terms like outcrop, strike, and dip. It also categorizes and describes various types of folds such as anticlines, synclines, symmetrical/asymmetrical, plunging/non-plunging, open/closed, and domes and basins. The causes of folding from tectonic forces and effects on erosion are summarized. Faults are described as unfavorable for construction.
This document defines and describes the key elements of faults in geology. It discusses fault plane, fault line, strike, dip, hanging wall, footwall, throw, heave, net slip, rake, and hade. Elements such as strike and dip are used to characterize the orientation of the fault plane. Hanging wall and footwall refer to the rock blocks separated by the fault. Throw, heave and net slip describe the displacement components. Understanding these fault elements aids in field study and identification of fault types.
Faults are fractures where there is movement parallel to the fault plane. They can range in length from hundreds of meters to a few centimeters. The key parts of a fault include the fault plane, hanging wall, and footwall. The fault plane is the surface where movement occurs, and dip and strike are measured here. The hanging wall is the rock mass above the fault plane, while the footwall is below. Faults can be classified based on their movement as dip-slip faults, like normal and reverse faults where movement is parallel to dip, or strike-slip faults where movement is parallel to strike. Normal faults involve the hanging wall dropping down, while reverse faults involve it moving up.
Structural geology is the study of rock structures and deformations within the Earth's crust. There are several types of rock structures that provide evidence of past deformation, including folds, faults, joints, and foliations. Folds occur when rock layers are bent, and there are different types such as anticlines, synclines, tight folds, overfolds, recumbent folds, and nappe folds. Understanding rock structures provides insight into the stress fields and tectonic processes that shaped the geological past.
1) Rock bursts occur due to the violent release of strain energy stored in rock mass in underground excavations under high stress. They can be caused by stress redistribution around excavations or reactivation of geological discontinuities.
2) There are several types of rock bursts including strain bursts caused by buckling near excavation boundaries, pillar bursts due to pillar failure, and fault slips or shear ruptures related to geological structures.
3) Damage from rock bursts can range from limited ejection of small rock pieces to severe damage over a large area from higher energy events involving faults or shear ruptures. Prevention methods aim to reduce rock stiffness, dissipate strain energy, or modify excavation layouts and shapes to
This document discusses different types of landforming processes caused by stress and strain on rocks. It describes three main types of deformation - folding, faulting, and fracturing. Folds form from compressional stress causing rocks to buckle into arches (anticlines) or sinks (synclines). Faults form when rocks fracture from strain, with one side displaced relative to the other along the fault plane. The main types of faults are normal, reverse, thrust, transform, and oblique-slip faults, which result from different types of differential stress.
Faults and rock deformation occur due to stress placed on rock layers from tectonic forces. There are three main types of rock response to stress: brittle, elastic, and plastic. Brittle response results in fracturing and faulting, elastic response allows the rock to return to its original shape, and plastic response involves permanent folding and flowing of the rock. Different rock types have different strengths and responses to compression, tension and shear stresses. Folds form from plastic rock deformation and include anticlines, synclines, domes and basins. Brittle deformation results in joints and faults, with normal, reverse, thrust, and strike-slip faults recognized based on the direction of displacement. Fault movement and folding can create
Earthquakes are caused by the sudden release of energy from faulting or breaking of rocks deep within the earth. The majority of earthquakes occur along plate boundaries where tectonic plates are converging, diverging, or sliding past one another. Earthquakes generate seismic waves that radiate out from the hypocenter or focus, including P waves, S waves, and surface waves. The location and magnitude of earthquakes can be determined through analysis of seismic wave arrival times recorded by seismographs. Larger earthquakes pose significant hazards through ground shaking and can potentially trigger destructive tsunamis.
Mountain building occurs through various geological processes including volcanic activity, tectonic activity like folding and faulting of rocks. The key factors that influence rock deformation are temperature, pressure, rock type, and time. Different types of stresses like compression, tension, and shear can cause rocks to deform through folding or fracturing. Major mountain ranges form at convergent plate boundaries through compression of colliding plates.
Geologic structures form due to stresses deforming rocks over time. There are three main types of structures: folds, faults, and fractures. Folds are bent layers caused by compression, and include anticlines and synclines. Faults are fractures with displacement, and can be normal, reverse, strike-slip, or oblique. Fractures include joints with no displacement and faults. Geologic structures are important because they can trap oil and gas, act as pathways for groundwater and minerals, and help date the geologic timescale.
This document discusses various geological processes that shape Earth's surface over long periods of time. It describes how stress and strain lead to folding and faulting in the crust. It also explains how volcanic activity, earthquakes, and plate tectonics result in mountain building and other surface features. Key points include how the principle of uniformity helps us understand slow, gradual changes versus sudden catastrophic events, and how different rock types respond to stress depending on temperature, pressure, and time.
Faults are fractures along which the rock masses on either side have moved relative to each other. A fault occurs when movement happens along a discontinuity due to brittle deformation from stress. Faults can be classified in different ways, including based on the apparent movement, dip angle, pattern of faults, and more. Common fault types include normal faults, reverse faults, strike-slip faults, and oblique slip faults. Normal faults occur when the hanging wall block moves downward relative to the footwall, while reverse faults occur when the hanging wall moves upward.
The document discusses how mountains are formed through crustal deformation processes. It describes how isostatic adjustments occur as the crust seeks equilibrium between downward pressure from overlying rock and upward pressure from the mantle. When forces exceed rocks' ability to deform through folding, faults form through brittle failure. There are four main types of faults. Mountains are often formed at plate boundaries through collision and compression of crust. The main types are folded mountains, fault-block mountains, volcanic mountains, and dome mountains, each involving different deformation mechanisms.
Deformation of the crust occurs along tectonic plate margins and produces geologic structures like folds and faults. Folds form as bent layers of rock in response to compressional forces, and the main types are anticlines, synclines, and monoclines. Faults form when stresses exceed a rock's strength, causing fractures. The main types of faults are normal, reverse, strike-slip, and oblique-slip faults. Evidence for seafloor spreading includes drilling samples from the ocean floor that show the oldest rocks farthest from mid-ocean ridges and the youngest rocks closest.
The document discusses plate tectonic theory and the three types of plate boundaries: divergent boundaries, convergent boundaries, and transform boundaries. At divergent boundaries, tension causes plates to move apart and seafloor spreading occurs. At convergent boundaries, compression causes plates to collide, leading to subduction zones, volcanoes, and mountain building. Transform boundaries involve shear stress as plates slide past each other horizontally.
MOVEMENT OF PLATES AND FORMATION OF FOLDS AND.pptxmarionboyka
This document discusses various types of rock deformation processes including metamorphism, plate tectonics, folds, faults, and joints. It describes contact and regional metamorphism, the four main types of stresses that cause rock deformation, and plate tectonic theory including the three types of plate boundaries. The document also defines common geological structures such as anticlines, synclines, monoclines and the four basic types of folds. Finally, it explains joints, faults, and the four main fault types.
This document discusses various types of rock deformation processes including metamorphism, plate tectonics, folds, faults, and joints. It describes contact and regional metamorphism, the four main types of stresses that cause rock deformation, and plate tectonic theory including the three types of plate boundaries. The document also defines common geological structures such as anticlines, synclines, and the four basic types of folds. Finally, it explains joints, faults, and the four main fault types.
Rocks can deform when stresses exceed their strength. The three main types of deformation are elastic, ductile and brittle. Stress leads to strain, with tension causing stretching, compression causing thickening, and shear causing blocks to move past each other. How rocks deform depends on factors like temperature, pressure, strain rate and mineral composition. Deformation results in structures like faults, folds, joints and breccias providing evidence of past stresses. Mountains form through processes like folding, faulting and uplift associated with plate tectonics.
GEOHAZARDS03 - Earthquakes Causes and Measurements.pdfraincabcaban
This document discusses earthquakes, their causes, and how they are measured. It begins by explaining that most earthquakes occur along faults in the earth's crust where tectonic forces cause deformation. It then describes how rocks deform under stress, the different types of stresses that can occur, and how materials respond as either brittle or ductile. Evidence of past deformation is discussed, including how the orientation of inclined rock layers is defined and measured. The document concludes by describing the different types of faults like normal, reverse, strike-slip and transform faults, and explains that earthquakes are caused by a sudden release of elastic strain energy built up along fault zones.
Joints, parts, varieties and clssification madan lal
Joints are fractures in rocks where the rock has broken, creating two free surfaces. Joints form due to contraction from cooling, consolidation, or tectonic stresses. Joints are classified based on their formation process or geometry. Tectonic joints form from differential stress and may indicate past stress orientations. Unloading joints form from uplift and erosion reducing compressive loads. Cooling joints commonly form vertically in cooling lava.
The document discusses the theory of plate tectonics, including what plates are, how they move, and the three types of plate boundaries. The three types of boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; and transform boundaries, where plates move past each other laterally. Each boundary type results in different geologic features and events due to the stresses caused by the ways plates are pulled, pushed, or sheared at their edges.
The document discusses the theory of plate tectonics, including what plates are, how they move, and the three types of plate boundaries. The three types of boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates move towards each other; and transform boundaries, where plates move past each other laterally. Each boundary type results in different geologic features and events due to the stresses caused by the ways plates are pulled, pushed, or sheared at their edges.
Similar to Ch10 structuralgeologyfall2007-140429091340-phpapp02 (20)
This document discusses suffixes and terminology used in medicine. It begins by listing common combining forms used to build medical terms and their meanings. It then defines several noun, adjective, and shorter suffixes and provides their meanings. Examples are given of medical terms built using combining forms and suffixes. The document also examines specific medical concepts in more depth, such as hernias, blood cells, acromegaly, splenomegaly, and laparoscopy.
The document is a chapter from a medical textbook that discusses anatomical terminology pertaining to the body as a whole. It defines the structural organization of the body from cells to tissues to organs to systems. It also describes the body cavities and identifies the major organs contained within each cavity, as well as anatomical divisions of the abdomen and back.
This document is from a textbook on medical terminology. It discusses the basic structure of medical words and how they are built from prefixes, suffixes, and combining forms. Some key points:
- Medical terms are made up of elements including roots, suffixes, prefixes, and combining vowels. Understanding these elements is important for analyzing terms.
- Common prefixes include hypo-, epi-, and cis-. Common suffixes include -itis, -algia, and -ectomy.
- Dozens of combining forms are provided, such as gastro- meaning stomach, cardi- meaning heart, and aden- meaning gland.
- Rules are provided for analyzing terms, such as reading from the suffix backward and dropping combining vowels before suffixes starting with vowels
This document is the copyright information for Chapter 25 on Cancer from the 6th edition of the textbook Molecular Cell Biology published in 2008 by W. H. Freeman and Company. The chapter was authored by a team that includes Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This document is the copyright information for Chapter 24 on Immunology from the 6th edition of the textbook Molecular Cell Biology published in 2008 by W. H. Freeman and Company. The chapter was authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
Nerve cells, also known as neurons, are highly specialized cells that process and transmit information through electrical and chemical signals. This chapter discusses the structure and function of neurons, how they communicate with each other via synapses, and how signals are propagated along neurons through changes in their membrane potentials. Neurons play a vital role in the nervous system by allowing organisms to process information and coordinate their responses.
This document is the copyright information for Chapter 22 from the 6th edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "The Molecular Cell Biology of Development" and is authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This document is the copyright information for Chapter 21 from the sixth edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Cell Birth, Lineage, and Death" and is authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This document is the copyright page for Chapter 20 from the 6th edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Regulating the Eukaryotic Cell Cycle" and is authored by a group of scientists including Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This document is the copyright information for Chapter 19 from the 6th edition textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Integrating Cells into Tissues" and is authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This chapter discusses microtubules and intermediate filaments, which are types of cytoskeletal filaments that help organize and move cellular components. Microtubules are involved in processes like cell division and intracellular transport, while intermediate filaments provide mechanical strength and help integrate the nucleus with the cytoplasm. Together, these filaments play important structural and functional roles in eukaryotic cells.
This chapter discusses microfilaments, which are one of the three main types of cytoskeletal filaments found in eukaryotic cells. Microfilaments are composed of actin filaments and play important roles in cell motility, structure, and intracellular transport. They allow cells to change shape and to move by contracting or extending parts of the cell surface.
This document is the copyright page for Chapter 16 from the 6th edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Signaling Pathways that Control Gene Activity" and is authored by a group of scientists including Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh and Matsudaira.
This document is the copyright page for Chapter 15 of the 6th edition textbook "Molecular Cell Biology" by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira. It provides the chapter title "Cell Signaling I: Signal Transduction and Short-Term Cellular Responses" and notes the copyright is held by W. H. Freeman and Company in 2008.
This document is the copyright page for Chapter 14 from the 6th edition textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Vesicular Traffic, Secretion, and Endocytosis" and is authored by a group of scientists including Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh and Matsudaira.
This chapter discusses how proteins are transported into membranes and organelles within cells. Proteins destined for membranes or organelles have targeting signals that are recognized by transport systems. The transport systems then direct the proteins to their proper destinations, such as inserting membrane proteins into membranes or delivering soluble proteins into organelles.
This document is the copyright information for Chapter 12 from the sixth edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Cellular Energetics" and is authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
This chapter discusses the transmembrane transport of ions and small molecules across cell membranes. It covers topics such as passive transport through membrane channels and pumps, as well as active transport using ATP. The chapter is from the 6th edition of the textbook Molecular Cell Biology and is copyrighted by W. H. Freeman and Company in 2008.
This document is the copyright information for Chapter 10, titled "Biomembrane Structure", from the sixth edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter was written by a team of authors including Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh and Matsudaira.
This document is the copyright information for Chapter 9 from the 6th edition of the textbook "Molecular Cell Biology" published in 2008 by W. H. Freeman and Company. The chapter is titled "Visualizing, Fractionating, and Culturing Cells" and is authored by Lodish, Berk, Kaiser, Krieger, Scott, Bretscher, Ploegh, and Matsudaira.
Beyond the Advance Presentation for By the Book 9John Rodzvilla
In June 2020, L.L. McKinney, a Black author of young adult novels, began the #publishingpaidme hashtag to create a discussion on how the publishing industry treats Black authors: “what they’re paid. What the marketing is. How the books are treated. How one Black book not reaching its parameters casts a shadow on all Black books and all Black authors, and that’s not the same for our white counterparts.” (Grady 2020) McKinney’s call resulted in an online discussion across 65,000 tweets between authors of all races and the creation of a Google spreadsheet that collected information on over 2,000 titles.
While the conversation was originally meant to discuss the ethical value of book publishing, it became an economic assessment by authors of how publishers treated authors of color and women authors without a full analysis of the data collected. This paper would present the data collected from relevant tweets and the Google database to show not only the range of advances among participating authors split out by their race, gender, sexual orientation and the genre of their work, but also the publishers’ treatment of their titles in terms of deal announcements and pre-pub attention in industry publications. The paper is based on a multi-year project of cleaning and evaluating the collected data to assess what it reveals about the habits and strategies of American publishers in acquiring and promoting titles from a diverse group of authors across the literary, non-fiction, children’s, mystery, romance, and SFF genres.
Is Email Marketing Really Effective In 2024?Rakesh Jalan
Slide 1
Is Email Marketing Really Effective in 2024?
Yes, Email Marketing is still a great method for direct marketing.
Slide 2
In this article we will cover:
- What is Email Marketing?
- Pros and cons of Email Marketing.
- Tools available for Email Marketing.
- Ways to make Email Marketing effective.
Slide 3
What Is Email Marketing?
Using email to contact customers is called Email Marketing. It's a quiet and effective communication method. Mastering it can significantly boost business. In digital marketing, two long-term assets are your website and your email list. Social media apps may change, but your website and email list remain constant.
Slide 4
Types of Email Marketing:
1. Welcome Emails
2. Information Emails
3. Transactional Emails
4. Newsletter Emails
5. Lead Nurturing Emails
6. Sponsorship Emails
7. Sales Letter Emails
8. Re-Engagement Emails
9. Brand Story Emails
10. Review Request Emails
Slide 5
Advantages Of Email Marketing
1. Cost-Effective: Cheaper than other methods.
2. Easy: Simple to learn and use.
3. Targeted Audience: Reach your exact audience.
4. Detailed Messages: Convey clear, detailed messages.
5. Non-Disturbing: Less intrusive than social media.
6. Non-Irritating: Customers are less likely to get annoyed.
7. Long Format: Use detailed text, photos, and videos.
8. Easy to Unsubscribe: Customers can easily opt out.
9. Easy Tracking: Track delivery, open rates, and clicks.
10. Professional: Seen as more professional; customers read carefully.
Slide 6
Disadvantages Of Email Marketing:
1. Irrelevant Emails: Costs can rise with irrelevant emails.
2. Poor Content: Boring emails can lead to disengagement.
3. Easy Unsubscribe: Customers can easily leave your list.
Slide 7
Email Marketing Tools
Choosing a good tool involves considering:
1. Deliverability: Email delivery rate.
2. Inbox Placement: Reaching inbox, not spam or promotions.
3. Ease of Use: Simplicity of use.
4. Cost: Affordability.
5. List Maintenance: Keeping the list clean.
6. Features: Regular features like Broadcast and Sequence.
7. Automation: Better with automation.
Slide 8
Top 5 Email Marketing Tools:
1. ConvertKit
2. Get Response
3. Mailchimp
4. Active Campaign
5. Aweber
Slide 9
Email Marketing Strategy
To get good results, consider:
1. Build your own list.
2. Never buy leads.
3. Respect your customers.
4. Always provide value.
5. Don’t email just to sell.
6. Write heartfelt emails.
7. Stick to a schedule.
8. Use photos and videos.
9. Segment your list.
10. Personalize emails.
11. Ensure mobile-friendliness.
12. Optimize timing.
13. Keep designs clean.
14. Remove cold leads.
Slide 10
Uses of Email Marketing:
1. Affiliate Marketing
2. Blogging
3. Customer Relationship Management (CRM)
4. Newsletter Circulation
5. Transaction Notifications
6. Information Dissemination
7. Gathering Feedback
8. Selling Courses
9. Selling Products/Services
Read Full Article:
https://digitalsamaaj.com/is-email-marketing-effective-in-2024/
Front Desk Management in the Odoo 17 ERPCeline George
Front desk officers are responsible for taking care of guests and customers. Their work mainly involves interacting with customers and business partners, either in person or through phone calls.
Join educators from the US and worldwide at this year’s conference, themed “Strategies for Proficiency & Acquisition,” to learn from top experts in world language teaching.
No, it's not a robot: prompt writing for investigative journalismPaul Bradshaw
How to use generative AI tools like ChatGPT and Gemini to generate story ideas for investigations, identify potential sources, and help with coding and writing.
A talk from the Centre for Investigative Journalism Summer School, July 2024
Split Shifts From Gantt View in the Odoo 17Celine George
Odoo allows users to split long shifts into multiple segments directly from the Gantt view.Each segment retains details of the original shift, such as employee assignment, start time, end time, and specific tasks or descriptions.
Credit limit improvement system in odoo 17Celine George
In Odoo 17, confirmed and uninvoiced sales orders are now factored into a partner's total receivables. As a result, the credit limit warning system now considers this updated calculation, leading to more accurate and effective credit management.
Beginner's Guide to Bypassing Falco Container Runtime Security in Kubernetes ...anjaliinfosec
This presentation, crafted for the Kubernetes Village at BSides Bangalore 2024, delves into the essentials of bypassing Falco, a leading container runtime security solution in Kubernetes. Tailored for beginners, it covers fundamental concepts, practical techniques, and real-world examples to help you understand and navigate Falco's security mechanisms effectively. Ideal for developers, security professionals, and tech enthusiasts eager to enhance their expertise in Kubernetes security and container runtime defenses.
How to Add Colour Kanban Records in Odoo 17 NotebookCeline George
In Odoo 17, you can enhance the visual appearance of your Kanban view by adding color-coded records using the Notebook feature. This allows you to categorize and distinguish between different types of records based on specific criteria. By adding colors, you can quickly identify and prioritize tasks or items, improving organization and efficiency within your workflow.
AI Risk Management: ISO/IEC 42001, the EU AI Act, and ISO/IEC 23894PECB
As artificial intelligence continues to evolve, understanding the complexities and regulations regarding AI risk management is more crucial than ever.
Amongst others, the webinar covers:
• ISO/IEC 42001 standard, which provides guidelines for establishing, implementing, maintaining, and continually improving AI management systems within organizations
• insights into the European Union's landmark legislative proposal aimed at regulating AI
• framework and methodologies prescribed by ISO/IEC 23894 for identifying, assessing, and mitigating risks associated with AI systems
Presenters:
Miriama Podskubova - Attorney at Law
Miriama is a seasoned lawyer with over a decade of experience. She specializes in commercial law, focusing on transactions, venture capital investments, IT, digital law, and cybersecurity, areas she was drawn to through her legal practice. Alongside preparing contract and project documentation, she ensures the correct interpretation and application of European legal regulations in these fields. Beyond client projects, she frequently speaks at conferences on cybersecurity, online privacy protection, and the increasingly pertinent topic of AI regulation. As a registered advocate of Slovak bar, certified data privacy professional in the European Union (CIPP/e) and a member of the international association ELA, she helps both tech-focused startups and entrepreneurs, as well as international chains, to properly set up their business operations.
Callum Wright - Founder and Lead Consultant Founder and Lead Consultant
Callum Wright is a seasoned cybersecurity, privacy and AI governance expert. With over a decade of experience, he has dedicated his career to protecting digital assets, ensuring data privacy, and establishing ethical AI governance frameworks. His diverse background includes significant roles in security architecture, AI governance, risk consulting, and privacy management across various industries, 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: June 26, 2024
Tags: ISO/IEC 42001, Artificial Intelligence, EU AI Act, ISO/IEC 23894
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Training: ISO/IEC 42001 Artificial Intelligence Management System - EN | PECB
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2. Deformation
• Deformation involves:
– Stress – the amount of force applied to
a given area.
– Types of Stress:
–Confining Stress – stress applied
equally in all directions.
–Differential Stress – stress applied
unequally in different directions.
3. Deformational Stress
• Types of Differential Stress:
(1) Compressional Stress – shortens and thickens a
rock body (associated with convergent plate
boundaries).
(2) Tensional Stress – tends to elongate and thin or
pull apart a rock unit (associated with divergent
plate boundaries).
(3) Shear Stress – produces a
motion similar to slippage that
occurs between individual
playing cards when the top of
the stack is moved relative to
the bottom (associated with
transform plate boundaries).
5. Deformation
• Differential stress applied to rocks during
tectonic activity causes rocks to respond via
deformation.
• Strain – changes in the shape or size of a rock
body caused by stress.
• Strained rock bodies do not retain their original
configuration during deformation.
6. How Do Rocks Deform?
• Rocks subjected to stresses greater than
their own strength begin to deform
usually by folding, flowing, or
fracturing.
– General Characteristics of Rock
Deformation:
• Elastic deformation – the rock returns to
nearly its original size and shape when the
stress is removed.
• Once the elastic limit (strength) of a rock is
surpassed, it either flows (ductile deformation)
or fractures (brittle deformation).
7. • Factors that influence the strength
of a rock and how it will deform:
• Depth
• Temperature
• Confining Pressure
• Rock Type
• Availability of Fluids
• Time
How Do Rocks Deform?
8. • Rocks near the surface, where confining pressures and
temperatures are low, will behave as a brittle solid and
fracture once their strength is exceeded.
• Rocks at depth, where confining pressures and
temperatures are high, will exhibit ductile behavior or
solid-state flow, in which changes occur without
fracturing.
How Do Rocks Deform?
9. Crustal Structures
• Folds – During crustal deformation rocks
are often bent into a series of wave-like
undulations.
– Anticlines and Synclines
– Domes and Basins
– Monoclines
• Characteristics of Folds:
• Most folds result from compressional
stresses which shorten and thicken the crust.
• Most of them occur in a series.
10. Anatomy of a Fold
• Limbs – Refers to the two sides of a fold.
• Axis (or Hinge) – A line drawn down the
points of maximum curvature of each
layer.• Axial Plane – An
imaginary surface
that divides a fold
symmetrically.
• Plunge – In
complex folding,
the axis is often
inclined at an angle
called plunge.
12. Common Types of Folds
• Anticline – upfolded
or arched rock
layers.
• Syncline –
downfolds or
troughs of rock
layers.
Photo courtesy of J. T. Daniels
http://disc.gsfc.nasa.gov/geomorphology/GEO_2/GEO_PLATE_T-42.shtml
Photo courtesy of Brennan T. Jordan, Department of Earth Sciences,
University of South Dakota
http://www.usd.edu/~Brennan.Jordan/
13. Common Types of Folds
• Depending on their orientation, anticlines and
synclines can be described as…
• Symmetrical, asymmetrical, overturned, recumbent
(a type of overturned fold – “lying on its side”), or
plunging.
19. Other Types of Folds
• Monoclines
• Large, step-like folds in otherwise horizontal sedimentary strata.
• Closely associated with faulting.
20. Other Types of Folds
• Dome
• Upwarped displacement of rocks.
• Circular or slightly elongated structure.
• Oldest rocks in center, younger rocks on the flanks.
21. Other Types of Folds
• Basin
• Circular or slightly elongated structure.
• Downwarped displacement of rocks.
• Youngest rocks are found near the center, oldest
rocks on the flanks.
22. Crustal Structures
• Faults – Fractures in rocks along which appreciable
displacement has taken place.
• Fault Zone – Displacements along multiple interconnected
faults.
• Sudden movements along faults are the cause of most
earthquakes.
23. Types of Faults
• Classified by their relative movement
which can be Horizontal, Vertical, or
Oblique.
24. Summary of Fault Types
• Dip-Slip Faults:
• Normal (gravity) – associated with divergent plate
boundaries.
• Reverse and Thrust – associated with convergent
plate boundaries.
• Strike-Slip Faults:
• Lateral (right and left) – associated with transform
plate boundaries.
25. Dip-Slip Faults
• Movement is
mainly parallel to
the dip of the
fault surface.
• Parts of a dip-slip
fault include the
hanging wall
(rock surface
above the fault)
and the footwall
(rock surface
below the fault).
26. Dip-Slip Faults
• Normal Fault (gravity)
Dip-Slip Faults
– Hanging wall block moves
down relative to the footwall
block.
– Tensional stress
– Accommodate lengthening or
extension and thinning of the
crust.
– Associated with divergent plate
boundaries.
– Most are small with
displacements of a meter or so.
– Larger scale normal faults are
associated with structures
called fault-block mountains
(Teton Range in Wyoming,
Basin and Range Province in
Nevada).
28. Normal Faulting – Fault Block Mountains
• Fault-Block Mountains – Basin and Range Province
in Nevada – topography generated by a system of
roughly north to south trending normal faults.
• Movements along these faults have
produced alternating uplifted blocks
called horsts (form elevated ranges)
and down-dropped blocks called
grabens (form basins).
• Half-Grabens – a tilted fault block in
which the higher side forms
mountainous topography and the
lower side forms a basin that fills
with sediment.
• Detachment Fault – nearly horizontal
fault extending up to hundreds of
kilometers into the subsurface.
Smaller faults are connected to this
larger fault. Boundary between
ductile and brittle deformation.
29. Dip-Slip Faults
• Reverse and Thrust Dip-Slip Faults
– Hanging wall block moves up relative to the
footwall block.
– Reverse faults have dips greater than 45o
– Thrust faults have dips less than 45o
.
• Strong compressional stress.
• Accommodate shortening
and thickening of the crust.
• Associated with convergent
plate boundaries.
32. Strike-Slip Faults
• Dominant displacement is horizontal
and parallel to the strike of the fault.
• May produce broad zones of roughly
parallel fractures up too several
kilometers in width.
• Shear stress.
• Associated with transform plate
boundaries.
34. Types of Strike-Slip Faults
• Right-Lateral – as you face the fault, the
opposite side of the fault moves to the right.
• Left-Lateral – as you face the fault, the
opposite side of the fault moves to the left.
http://www.pbs.org/wnet/savageearth/animations/
Animations:
Right-Lateral
Strike-Slip Fault
35. Types of Strike-Slip Faults
• Transform Fault
– Large strike-slip
fault that cuts
through
accommodates
motion between
two large crustal
plates.
– Example: San
Andreas Fault
System
43. Mapping Geologic Structures
• Geologists measure the orientation or
attitude of a rock layers or
fault/fracture surfaces in order to
describe and map geologic structures
that result from deformation.
44. Mapping Geologic Structures
– Strike (Trend)
• The compass direction of the line produced by the
intersection of an inclined rock layer or fault with a
horizontal plane.
• Generally
expressed an an
angle relative to
north.
• Example: N10ºE
45. Mapping Geologic Structures
– Dip (Inclination)
• The angle of inclination of the surface of a rock unit
or fault measured from a horizontal plane.
• Includes both an
inclination and a
direction toward
which the rock is
inclined.
• Example: 30ºSE
46. A Geologic Map Showing
Strike and Dip of Structures
By knowing the strike and dip, geologists can predict the nature of
rock structures hidden beneath the surface.