Personal Experience Taking A Look At The Police Department

While making copies the morning of November 3rd, I commented to another teacher in the copy room that it was weird that some of the central office staff was in the building this early. It was 6:40. I should have put the pieces together that the crisis team was assembled. I walked back to my room to start prepping for the day with my co-teacher and student intern. Another math teacher came in at 7:15 and asked me if I had heard. Not knowing what she was talking about, she showed me a text message she had received from another teacher in the district, which indicated the passing of one of my students. Not 30 seconds went by and the phone rings. The secretary asked me to come to the Principal’s Conference Room for an important meeting.†¦show more content†¦Both last year and this year, I have suggested the need to add a teacher to the team (it doesn’t need to be me but someone who is a problem solver). While I understand that everyone involved has a specific role, I think a teacher would help with how to communicate to students and staff. I think there was a lack of a unified message to staff on how to handle this at the beginning of the school day. Students started taking about it when they began arriving at 6:55. The school counselors opened a classroom for group counseling. Additionally, some used the offices and small conference meeting rooms in the guidance suite for a smaller setting. One counselor followed the student’s class schedule and did group counseling at the beginning of every period. I thought this was extremely beneficial, since I hadn’t had time to process the information I was given. After teaching and quizzing 1st block, 2nd block I covered a PPT as the administrator for our Principal and then helped out in the office afterwards. This small class has individuals from all sides of the situation are enrolled in my class, the victim, best friends, friends of the suspect, and a first responders. I was so glad th at the school counselor came up and talked with my kids for about a 20 minutes and then checked back in periodically the remainder of the period. At the end of theShow MoreRelatedPolice Officers And The Police Vehicles1429 Words   |  6 Pagessaying that police officers use, and it is on the police vehicles. They take pride to serve our community, take pride to protect our community, and take pride of wearing the badge on their uniforms. Our community wouldn’t be the same if we didn’t have the protection from them; if so there will be some disasters like some today. But yet, they get accused, getting name, and getting threaten for the things that happen consequently. When I was growing up, I hear all these sayings that â€Å"police officers areRead MorePolice Suicide And Its Effects1720 Words   |  7 Pagesterm paper is to talk about police suicide and whether or not it is preventable. While police suicide is an huge issue, the public do not hear much about it nor have enough information. Therefore, it is important to let the public know that it is an issue by spreading awareness and creating prevention methods. Important questions that should be asked are : What is suicide? Why are police officers committing suicide? How many police officers are committing suicide? Can police suicide be prevented? HaveRead MoreThe Police Department Of Whittier850 Words   |  4 PagesThe police department of Whittier began in April 1917 and their primary objective is to maintain the upkeep and protect the community. In 2001, Chief David M. Singer took oath to take upon the leadership of the department. 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The fear of crime and even the people who commit crime, there is always a chance that you could get robbed, caught up in physical altercation, or even happen to be in the wrong place at the wrong time. People in general approach these situations differently and prepare for these situations in different waysRead MorePolice Gangs Of Americ Policing Gangs872 Words   |  4 PagesAmerica This book primarily focused on ways police reacted to gang presence, problems, and illegal activity, based on the way America views gangs. Gangs are described differently by people based on geography, class, age, race, and personal agenda’s. Statistic’s based on research, help grasp the whole situation and soak in the problems for society and also police. Police forces may change up tactics to respond to a certain gang compared to a different police force and different gangs. After reading this

The Challenges Of Math And Science Classes Essay - 968 Words

Creativity is in all of us often we failed to see it. We think art, design, and marketing are creative. However, creativity lies in every field that you are curious in. There is no definite space that creativity exists in. Obviously, this idea struck me later. I also thought a creative person was the one who could compose rhyming poems and stories, who could draw beautiful pictures, or who could sing and dance effortlessly and I also wanted these skills, but it was impossible. Later, I found out, I was creative too. I enjoyed the challenges problems in math and science classes. And thinking to solve a problem in various ways is also being a creative. Hence, creativity can be learned in the fields that you are curious in and not from sitting in a lecture, but by learning and applying creative thinking processes. Children are more creative than adults. I too was creative when I was young. In Nepal, we rarely wrote creative pieces. Most of our English syllabus included short/long questions answers from the chapters. The first creative writing I recall is the one from third grade. We were given the assignment to describe our home. I went little overboard and described that I had the magical tree whose leaves taste like candies and had four peacocks that would dance in the backyard. I will always remember this unique writing. If I got the assignment like this now, it would be boring as I will focus on the rules and regulations. I will try my best to be inside the margin whichShow MoreRelatedThe Challenges Of Math And Science Classes Essay1169 Words   |  5 Pagespictures, or who could sing and dance effortlessly. I attempted to be creative several times. They were dull and lifeless. I now recognize my creativity is in STEM fields rather than in arts and humanities. I have enjoyed the challenge s problems in math and science classes. And thinking to solve a problem in various ways is also being a creative. 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Introduction Chapter Free Essays

Key Terms and Concepts (1-24) 1. Denudation is the total effect of all actions (weathering, mass wasting, and erosion) that lower the surface of the continents. 2. We will write a custom essay sample on Introduction Chapter or any similar topic only for you Order Now Weathering- the physical and chemical disintegration of rock that is exposed to the atmosphere. Mass-wasting- the short-distance down slope movement of weathered rock under the direct influence of gravity; also called mass movement. Erosion- detachment, removal, and transportation of fragmented rock material. 3. Openings in the surface and near- urface bedrock are frequently microscopic, but they may also be large enough to be conspicuous and are sometimes huge. In any case, they occur in vast numbers and provide avenues along which weathering agents can attack the bedrock and break it apart. Subsurface weathering is initiated along these openings, which can be penetrated by such weathering agents such as water, air, and plant roots. As time passes, the weathering effects spread from the immediate vicinity of the openings into the denser rock beyond. . Joints are cracks that develop in bedrock due to tress, but in which there is no appreciable movement parallel to the walls of the joint. Faults are breaks in bedrock along which there is relative displacement of the walls of the crack. 5. Master Joints are Joints that run for great distances through a bedrock structure. Master Joints play a role in topographic development by functioning as a plane of weakness, a plane more susceptible to weat hering and erosion than the rock around it. 6. Mechanical weathering is the physical disintegration of rock material without any change in its chemical composition; also alled physical weathering. Chemical weathering is the chemical decomposition of rock by the alteration of rock-forming minerals. 7. Frost wedging is the fragmentation of rock due to expansion of water that freezes into ice within rock openings. 8. Salt wedging is the rock disintegration caused by the crystallization of salts from evaporating water. 9. Exfoliation is the weathering process in which curved layers peel off bedrock in sheets. This process commonly occurs in granite and related intrusive rocks after overlying rock has been removed, allowing the body to expand slightly. An exfoliation dome is a large rock mass with a surface confguration that consists of imperfect curves punctured by several partially fractured shells of the surface layers (due to exfoliation). 10. Oxidation is the chemical union of oxygen atoms with atoms from various metallic elements to form new products, which are usually more voluminous, softer, and more easily eroded than the original compounds. When iron-bearing minerals react with oxygen (become oxidized), iron oxide is produced. This reaction, probably the most common oxidation in the lithosphere, is called rusting. 1 . Hydrolysis- a chemical union of water with another substance to produce a new compound that is nearly always softer and weaker than the original. Carbonation- a process in which carbon dioxide in water reacts with carbonate rocks to produce a very soluble product (calcium bicarbonate), which can readily be removed by runoff or percolation, and which can also be deposited in crystalline from if the water is evaporated. 2. Biological weathering is rock biological weathering is lichens. Lichens are primitive organisms that consist of algae and fungi living as a single unit. Typically they live on bare rock, bare soil, or tree bark. They draw minerals from the rock by ion exchange, and this leaching can weaken the rock. 13. Differential weathering is the process whereby different rocks or parts of the same roc k weather and/or erode at different rates. 14. The steepest angle that can be assumed by loose fragments on a slope without downslope movement is called the angle of repose. This angle, which varies with the nature and internal cohesion of the material, represents a fine balance between the pull of gravity and the cohesion and friction of the rock material. If additional material ccumulates on a debris pile lying on a slope that is near the angle of repose, the newly added material may upset the balance and may cause all of part of the material to slide downward. 15. Rockfall (fall) is the mass wasting process in which weathered rock drops to the foot ofa cliff or steep slope. 16. Talus (scree) are pieces of weathered rock, of various sizes, that fall directly downslope. Sometimes the fragments accumulate relatively uniformly along the base of the slope, in which case the resultant landform is called a talus slope or talus apron. 17. A talus cone is a sloping, cone-shaped heap of dislodged talus. This cone pattern is commonplace because most steep bedrock slopes and cliffs are seamed by vertical ravines and gullies that funnel the falling rock fragments into piles directly beneath the ravines, usually producing a series of talus cones side by side along the base of the slope or cliff. 18. A rock glacier is an accumulated talus mass that moves slowly but distinctly downslope under its own weight. 9. Landslides do not require the lubricating effects of water or clay, although the presence of water may contribute to the action; many slides are triggered by rains that add weight to already overloaded slopes. Landslides may be activated by other stimuli as well, most notably by earthquakes. 20. A slump is different from other kinds of landslides because i t is a slope collapse slide with rotation along a curved sliding plane. 21. A landslide is a general term for a type of slope failure involving an instantaneous collapse of a slope and movement along a generally flat sliding plane. A mudflow is a rapid, downslope movement of a dense mixture of weathered rock and water through or within a valley. 22. Earthflow is the mass wasting process in which a portion of a water- saturated slope moves a short distance downhill. A debris flow is a stream-like flow of dense, muddy water heavily laden with sediments of various sizes; a mudflow containing large boulders. 23. A soil creep is the slowest and least perceptible form of mass wasting, which consists of a very gradual downhill movement of soil and regolith. Soil creeps happen slower than a snail can move, and they usually can be prevented if falling towards a house/building. 24. Solifluction is a special form of soil creep in tundra areas; associated with summer thawing of the near-surface portion of permafrost, causing the wet, heavy surface material to sag slowly downslope. Study Questions (1-5) 1. It is possible for weathering to take place beneath the surface of bedrock because of things such as Joints within the rock. If the Joints are deep enough, the weathering will take place underneath certain parts of the rock. There are many types of a whole, not Just the surface. 2. Chemical weathering is more effective in humid climates than in arid climates because arid climates do not have water. Humid climates have higher amounts of water and higher temperatures so chemical weathering happens faster. 3. There is a direct relationship between gravity and ass wasting. Any mass moves in the direction of the vector sum of all the forces acting on it, with acceleration numerically equal to the magnitude of the sum of the forces divided by its mass. On or near the Earth’s surface, gravity is always one of the forces. 4. Clay reacts to water by expanding, and when it dries, it contracts. Some clay does it so small that it’s barely noticeable, some clay does it so much that you can very easily see it happen right in front of your eyes. If these clays are in a crack between rock, or in a layer beneath rock, or basically any place that the clay is omehow packed between two hard rocks, and it gets wet, then it will expand, and put force on the two rock layers. Then it will dry, and â€Å"pull† the layer or Joint into a weaker state. If this happens over a long enough time, then it will break the rock that is in the weaker position. 5. Rainfall can expedite mass wasting because when there is more water in the objects that are falling, the objects (falling rocks) become heavier, therefore the process is speeded up. The more rainfall there is, the more water will be accumulated and the heavier the falling rocks will be. 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