The Faults from within Earth
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This document discusses faults and earthquakes. It describes how faults are fractures in the Earth's crust where earthquakes occur. There are different types of stresses that can cause faults, such as tensional, compressional, and shear stresses. Active faults have generated earthquakes within the last 10,000 years and may continue to do so, while inactive faults are not likely to produce future quakes. When rocks break along a fault, stored elastic energy is released as seismic energy in the form of seismic waves, causing earthquakes. Earthquakes are recorded by modern seismographs that detect seismic waves and produce seismograms. Earthquake preparedness is important, as described in the final section.
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This document discusses sexuality and how it is an integral part of personality. It defines sexuality as including gender, gender roles, body image, and how one expresses emotions and communicates with others. Sexuality is influenced by culture, media, peers and significant individuals. The document also outlines primary and secondary sex characteristics that develop in males and females during puberty, influenced by hormones like estrogen and testosterone. It prompts the reader to complete an activity reflecting on changes during this stage of life.
Redefining Sexuality
This document discusses sexuality and its influences on teenagers. It defines sexuality as involving more than just sex, and encompassing aspects of masculinity and femininity. Sex is defined as a person's capacity for sexual feelings and attraction to a particular sex. The document outlines some negative effects of pornography, premarital sex, and vulgar conversation/lewd acts on teenagers, including feelings of guilt, weakened self-esteem, unwanted pregnancy, sexually transmitted diseases, emotional issues, and negative impacts on work and relationships.
Building relationship through Effective Communication
This document discusses effective communication and provides tips for improving communication. It defines communication as sharing ideas and feelings with others. Some key tips for effective communication include being a reliable source, encoding messages clearly, choosing the best communication channel, and accurately decoding messages. The document also outlines different types of communication like verbal, nonverbal, and written. It describes various levels of communication from phatic to evaluate to gut-level to peak communication. Finally, it discusses potential barriers to communication such as language, lack of understanding, inadequate feedback, emotional interference, cultural differences, and poor listening skills.
My Relationship with others
Friends provide encouragement and support during difficult times, helping to build self-esteem and confidence. They can also encourage you to try new activities and experiences outside your comfort zone. The values and behaviors of your friends can influence you, so surrounding yourself with generous, family-oriented and ambitious friends can help develop those qualities in yourself. To nurture friendships, make time for quality conversations, end one-sided relationships, communicate regularly but also in-person, and be generous with praise but cautious with criticism. Loyalty during both good and bad times is essential, and acts of kindness can deepen any friendship.
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dtubbenhauer@gmail.com
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equations sourced by a topological defect, i.e. a singularity of a very specific form, the result is a localized gravitational
field capable of driving flat rotation (i.e. Keplerian circular orbits at a constant speed for all radii) of test masses on a thin
spherical shell without any underlying mass. Moreover, a large-scale structure which exploits this solution by assembling
concentrically a number of such topological defects can establish a flat stellar or galactic rotation curve, and can also deflect
light in the same manner as an equipotential (isothermal) sphere. Thus, the need for dark matter or modified gravity theory is
mitigated, at least in part.
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The binding of cosmological structures by massless topological defects
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The Faults from within Earth
- 1. THE FAULTS FROM WITHIN EARTH Prepared by: JM Ramos
- 2. LAYERS OF THE EARTH
- 3. FAULTS •Fracture or break in Earth’s crust where earthquakes are most likely to occur repeatedly
- 5. STRESS •The force applied to rock
- 6. TYPES OF THE STRESS 1. Tensional Stress - Rocks stretched away from each other
- 7. TYPES OF THE STRESS 2. Compressional Stress - Rocks are pushed toward each other
- 8. TYPES OF THE STRESS 3. Shear Stress -push toward each other but not in the same axis
- 9. TYPES OF THE STRESS
- 10. TYPES OF THE STRESS
- 11. TYPES OF THE STRESS
- 12. TYPES OF THE STRESS
- 13. ACTIVE AND INACTIVE FAULTS ACTIVE FAULTS - Known to have recently generated earthquakes within the last 10, 000 years, which may still continue to generate earthquakes
- 14. ACTIVE AND INACTIVE FAULTS ACTIVE FAULTS - Known to have recently generated earthquakes within the last 10, 000 years, which may still continue to generate earthquakes
- 15. FAULTS GENERATE EARTQUAKES When an earthquake occurs strong enough for you to feel it, you recognize it as the shaking that affects anyone and anything that stands on the ground WHAT IS THE RELATIONSHIP BETWEEN FAULTS AND EARTHQUAKES ?
- 16. FAULTS GENERATE EARTQUAKES •When a material is compressed or stretched, the ______ energy is stored in the materials
- 19. FAULTS GENERATE EARTQUAKES •When the rocks break along a fault, the stored elastic energy is released as a special type if kinetic energy called seismic energy
- 20. FAULTS GENERATE EARTQUAKES •Seismic energy passes through rocks as seismic waves
- 21. ANATOMY OF AN EARTHQUAKE
- 22. EARTHQUAKES OCCUR UNDERWATER •A large volume of water is pushed to the surface, creating a huge wave referred to as tsunamis
- 23. How are earthquakes recorded?
- 24. RECORDING EARTHQUAKES •Seismograph was invented in 1875 by an Italian by the name of Filippo Cecchi who was a physicist and priest
- 26. RECORDING EARTHQUAKES • Seismometers - modern seismographs, record earthquakes electronically - data recorded by it are presented as a seismogram
- 27. INFORMATION FROM EARTHQUAKES • P – waves • Primary waves • Arrived first • Can pass through the solid and liquid layers of the Earth’s interior
- 28. INFORMATION FROM EARTHQUAKES • S – waves • Secondary waves • Arrived after P- waves • Can only pass through the solid layers of Earth’s interior
- 29. INTESITY • Tells how much a certain area was shaken where the earthquake reach the area • Intensity I - X
- 30. MAGNITUDE • Describes the total amount of energy that was released by the earthquakes at the focus • Magnitude less than 2.0 – 10.0 and greater
- 31. QUESTION: How does one prepare for an Earthquake?
- 36. THE END!
Editor's Notes
- Crust cannot be bend nor stretch because it is brittle Fault zones
- Crust cannot be bend nor stretch because it is brittle Fault zones
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