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Christina T

ABC-CLIO: World Geography: Japan - 0 views

  • Etiquette and good manners are extremely important to the Japanese people.
  • On entering a Japanese home, temple, or shrine, shoes are removed.
  • Business cards are extremely important in Japan.
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  • Japanese people give gifts for certain holidays, and bring gifts to family and friends when they return from vacation.
  • sticking chopsticks into a bowl of rice is considered bad manners
  • Part of the marriage ceremony involves ritual purification and the drinking of sake (rice wine)
  • choose to be married in Christian ceremonies
  • most funerals are Buddhist. The body is cremated, and while that is happening, the family eats the first meal of the day.
  • on the first day of spring and fall, and during the summer Obon (Festival of Lanterns), a Buddhist festival signifying the reunion of the living with the spirits of the dead.
Carlen Hodgson

Bodybuilding.com - Mauro Di Pasquale - Cardio Training Guidelines For Basketball Players! - 0 views

  • is crucial in order to build a solid base of conditioning. This type of training should be executed 3-4 days per week and can involve activities such as running, biking, hiking and swimming.
  • Running is extremely effective, but it is also extremely stressful if done over long periods and distances. Cross-Training is an effective method to use in order to get results with little risk to your body
  • . The stresses that the body encounters doing a variety of activities is more beneficial to the athlete than the stresses encountered by doing the same old, tired routine. Also, the risk of injury is greater if you only take part in one activity.
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  • Exercise Bike - 30-45 minutes. Jogging - 30 minutes. Stairmaster - 30 minutes. Aerobics Class - 30 minutes. Water Exercise - 30 minutes. Versa Climber - 30 minute
Patrick Wan

Extreme Crew - 0 views

shared by Patrick Wan on 08 Dec 08 - Cached
Stephania D

Oil Remains - 0 views

  • largest and most productive estuaries in North America.  
  • However, in 1993 the EVOS Trustee Council funded an additional survey that estimated 7 km of shoreline were still contaminated with subsurface oil.
  • Because a significant survey of Prince William Sound had not been conducted since 1993 and the cumulative extent of the remaining oil was unknown, concerns were generated by the public and scientific communities about the oil’s possible continuing effects on humans and fauna potentially exposed to the oil directly or indirectly.
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  • Without an accurate assessment of the extent of the remaining oil, subsistence food-gatherers, consumers of commercial fish products from the area, and tourists have used mostly anecdotal evidence as the basis for economic decisions regarding resource utilization in the affected area.
  • Consequently, the Auke Bay Laboratory (ABL) with funding from the EVOS Trustee Council, took on the task of assessing the remaining oil along the shorelines of Prince William Sound during the summer of 2001
  • The primary objective of the project was to measure the amount of oil remaining in the intertidal zone of Prince William Sound.  Secondary objectives include determining the rate of decline of oil on these beaches, estimating the persistence of the remaining oil, and correlating the remaining oil with geomorphological features.
  • heavily and moderately oiled
  • The 2001 survey adopted a stratified random/adaptive sampling (SRAS) design. Two random pits were excavated to a depth of 0.5 m (1.6 feet) in every stratified block (0.5-m verticle drop in tide height) within a grid system established at each site. If subsurface oil was discovered in any of the randomly stratified origin pits, then additional adaptive pits were excavated above, below, to the right, and to the left of the origin pit until the extent of the oil patch was determined.
  • Buried or subsurface oil is of greater concern than surface oil.
  • Subsurface oil can remain dormant for many years before being dispersed and is more liquid, still toxic, and may become biologically available.
  • A disturbance event such as burrowing animals or a severe storm reworks the beach and can reintroduce unweathered oil into the water.
  • The toxic components of this type of surface oil are not as readily available to biota, although some softer forms do cause sheens in tide pools.
  • 1) Surface oil was determined to be not a good indicator of subsurface oil. 2) Twenty subsurface pits were classified as heavily oiled.  Oil saturated all of the interstitial spaces and was extremely repugnant. These “worst case” pits exhibited an oil mixture that resembled oil encountered in 1989 a few weeks after the spill - highly odiferous, lightly weathered, and very fluid. 3) Subsurface oil was also found at a lower tide height than expected (between 0 and 6 feet), in contrast to the surface oil, which was found mostly at the highest levels of the beach (Table 3).  This is significant, because the pits with the most oil were found low in the intertidal zone, closest to the zone of biological production, and indicate that our estimates are conservative at best.
  • The possibility of continuing low level chronic effects of the Exxon Valdez oil spill seem very real now, although measurable population effects would be very difficult to detect in wild populations.
  •  Sea otters and harlequin ducks fall into this category
  • such as sea otters, harlequin ducks, and their intertidal prey.
  • The last beach assessment was completed in September 2001. Supporting chemical analyses will be completed in fall 2002, and a final report with statistical analyses and conclusions will be completed by April 2002.
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    Exxon Valdez
Christina T

Student Research Center - powered by EBSCOhost: Early Japan -- The Yayoi Period - 0 views

  • Japan entered into its second major prehistoric period, a civilized era known as the Yayoi period.
  • he name Yayoi is derived from an area Tokyo known as Yayoi, where the first documented pottery from this period was discovered in an archaeological excavation in 1884.
  • ron and bronze materials are believed to have been exchanged with Japanese envoys either for token tributes or prisoners of war.
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  • early all of the country's inhabitants belong to the same ethnic group and share the same racial background and cultural characteristics.
  • Within the villages, households consist of large families. This usually includes a farmer, his wife and children, grandparents, and grown sons and their families.
  • Yayoi culture originally developed in northern Kyushu, the western and southernmost of Japan's main islands.
  • Japanese city life is much more Westernized than that of the countryside.
  • ayoi culture spread into Honshu (Japan's largest island) and present-day Tokyo in the Middle (100 BC-100 AD) to Late Yayoi (100-300AD) period.
  • Modern entertainment is also active in the cities of Japan.
  • The Japanese celebrate many holidays and practice many customs throughout the year.
  • On May 5 Kodomo-no-Hi (Children's Day) is celebrated. This is a day set aside to honor all children.
  • Perhaps the most important development of the Yayoi period was the cultivation of rice, probably introduced from the area near the Yangtze River delta in southern China.
  • November 23 marks Kansha-no-Hi (Labor-Thanksgiving Day). On this day, the Japanese give thanks to laborers and for a successful harvest.
  • apanese men and women did not choose their marriage partners based on love. Instead, marriage was arranged by families who paired couples based on their social and economic status.
  • At the end of the day a large bathtub is filled with hot water. Then, each family member, in turn washes and rinses thoroughly before getting into the tub.
  • In addition to pottery and iron and bronze tools, archaeologists have depended largely on burial remains to uncover Yayoi culture.
  • For years, the Japanese have taken great pride in their performing arts. Dance and theater are essential parts of Japanese culture.
  • n northeastern Japan, secondary burials were conducted in which the bones of the dead were exhumed, painted decoratively, and placed in ornamental clay jars.
  • "No plays" are other types of theatrical performances common in Japan.
  • The gagaku, for example, is classical music that was introduced into Japan from China in the 8th century A.D.
  • Western music is also popular in Japan.
  • For many years the Japanese style of dress consisted of long, flowing robes called kimonos.
  • The climate of Japan varies a great deal from heavy snows and extreme cold along the west coast to warm and humid summers in the rest of the country.
anonymous

The Wrong Way to Win - 0 views

  • The Wrong Way to Win › Introduction to The Wrong Way to Win › Why Do Athletes Use Performance-enhancing Drugs? › Masking Pain and Managing Weight and Stress › Detecting Drugs Why Do Athletes Use Performance-enhancing Drugs?
  • An athlete may want to: Build mass and strength of muscles and/or bones Increase delivery of oxygen to exercising tissues Mask pain Stimulate the body Hide use of other drugs
  • Many drugs are banned outright in Olympic competitions. However, some drugs, such as cortisone and local anesthetics, are merely restricted because they have legitimate clinical uses. Athletes may also misuse drugs to reduce weight, relax, cope with stress or boost their own confidence. Whatever the reason, doping has many unsafe if not deadly side effects.
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  • Another method for improving oxygen concentration is blood doping -- infusing whole blood into an athlete. An athlete who infuses his own blood may cause infection or cardiovascular problems because of the increased blood volume (high blood pressure, blood clots, heart failure and stroke). An athlete who uses someone else's blood runs the risk of acquiring viral infections such as HIV/AIDS. These are huge risks for a result that can also be achieved by training at high altitudes.
  • In addition to taking drugs that build mass and strength, some athletes take drugs and engage in practices that increase the amount of oxygen in tissues. Endurance athletes, like cyclists or cross-country skiers, may use Erythropoietin (EPO). EPO can increase an athlete's oxygen supply by as much as seven to 10 percent. As mentioned earlier, EPO is extremely dangerous, if not deadly in some cases. The increased red cell density caused by EPO can thicken the blood. The thickened blood -- which is more like honey than water -- cannot flow through the blood vessels well. To pump the thickened blood, the heart must work harder. This increases the chances of heart attack and stroke.
  • Athletes looking to build mass may also abuse Human Growth Hormone (hGH). Excessive hGH levels increase muscle mass by stimulating protein synthesis, strengthen bones by stimulating bone growth and reduce body fat by stimulating the breakdown of fat cells. Use of hGH has become increasingly popular because it is difficult to detect. Side effects include overgrowth of hands, feet, and face (known as acromegaly), enlarged internal organs, especially heart, kidneys, tongue and liver and heart problems.
  • Athletes use anabolic steroids to increase muscle strength. Anabolic steroids, which can be injected or taken as pills, allow the athlete to train harder and longer at any given period. The possible and well-known side effects of anabolic steroid use include jaundice and liver damage, mood swings, depression and aggression. Men may also suffer from baldness, infertility and breast development. Females may grow excessive hair on the face and body and suffer from infertility. The substances Human Chorionic Gonadotropin (hCG), Luteinizing Hormone (LH) may also produce the same side effects.
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    use it
  •  
    Use this site for information
Carlen Hodgson

Suggestions for Physical Training on the Off-Season for the Basketball Player - 0 views

  • Basketball may be the most demanding of all sports. Basketball is a game of quickness: fast starts, sharp cuts and turns, acceleration and deceleration, and jumping. The heart of the game is running. Some coaches estimated that a starting high school player will run a total of 3 to 5 miles in a 32-minute game.
  • During the off-season prepare yourself by putting into practice good training principles. This will help you to maintain your fitness at a high level. Therefore, you can better bring out the best in your athletic potential.
  • Off-season training for competitive basketball requires self- discipline, dedication, and sacrifice. Also, you must have a good working knowledge of athletic training principles.
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  • It's for this reason that the off-season is used to follow a training program to develop endurance, strength, speed, coordination, and agility. In order to be successful
  • Warm-up 5 to 10 minutes to increase blood flow and lubricate the joints.Flexibility exercises to slowly stretch muscles and tendons that cross and surround the joints.Strength development to increase muscular power and force.Endurance work to increase and maintain a high level of cardiovascular conditioning and interval workouts to increase speed and stamina.A cool-down period of 5 to 10 minutes after the exercise has finished to let the heart rate return to normal and facilitate the return of blood from the extremities.Post-exercise flexibility exercises of 5 to 10 minutes to prevent muscles from shortening.
  • The Warm-UpAll exercise should be preceded by a short warm-up period of 5 to 10 minutes. The purpose of this is to prepare your body for more strenuous activity to follow. An excellent warm-up is rope skipping with little or no resistance. Once your body starts to lightly perspire, you are probably sufficiently warmed up. Rope jumping will greatly increase the flow of blood to the muscle tissues and lubricate the joints. This allows you to bend, stretch, jump, and run to the maximum of your ability without fear of injury. Exercise without a proper warm-up is very taxing to the muscles, tendons, ligaments, and joints. Failure to warm-up may lead to injury. Flexibility: Stretching Exercises
  • Prepare to be a WinnerA high level of personal motivation is critical to the success of anything that you do in life. No matter how much or how little basketball talent you have, if you are motivated enough to follow the program set forth here, you will get in shape. Therefore, you will be better able to achieve your goals. All the many hours that you put into your conditioning program will eventually yield results. In the final minutes of a game when your team is desperately looking for someone to score, grab a rebound, or block a shot, it is you who will come through. Why? Because you are in shape and, even in the waning minutes when everyone else is tired, you can still perform at a high competitive level. With the base built from your preseason training program, you are the one who still has the mental toughness, the strength, the power, and the motivation to get the job done. Although you may never have all the tools to be the most talented basketball player, by working hard and following this preseason program, you will become a well conditioned athlete, able to maximize all your basketball talents. In the end this will enable you to come as close as possible to achieving your basketball dreams.
Aloysius Utomo

Panda - Enchanted Learning Software - 0 views

    • Aloysius Utomo
       
      Size of pandas
  • Chinese people call the panda "Da xiong mao,"
  • "giant bear cat"
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  • symbol of peace in China
  • Female pandas are called sows
  • males are called boars
  • young are called cubs
  • Most bears' eyes have round pupils
  • giant panda, whose pupils are vertical slits
  • Pandas have very good eyesight
  • largest pandas grow to be about 250 pounds
  • 5.25 to 6 feet (1.6 to 1.8 m) long
  • weighs about 220 pounds
  • 40 pounds (18 kg) of food each day
  • Bamboo is very low in nutrition
  • cannot digest it very well
  • 12 hours every day
  • throat and stomach have extra-tough linings to protect them from the tough food
  • captivity (zoos and breeding centers), pandas eat bamboo, rice cereal, carrots, apples, and sweet potatoes
  • usually eat while sitting in an upright positio
  • strong teeth and jaws are very important to a panda's survival
  • Giant pandas have large molars (flat teeth used for crushing food)
  • few sharp teeth which they use to bite tough bamboo stalks
  • Pandas have 42 teeth
  • very thick, oily, woolly fur
  • two types of hairs
  • long, thick, coarse hairs
  • fur is waterproof
  • shorter, fine, dense underfur
  • endangered species
  • roughly 1,000-1,500 pandas living in the wild (in China)
  • 120 living in zoos and breeding centers around the world
  • extremely vulnerable to extinction because of humans
  • mostly shy, solitary animals
  • mostly silent, but they can bleat!
  • 11 different calls, four of which are only used during mating
  • live longer in captivity than in the wild
  • Unlike many other bears, pandas cannot walk on their hind legs
  • do not hibernate since their food is available all year long
  • During the cold winter months, giant pandas go to lower altitudes where it is a bit warmer
  • don't seem to have permanent dens
  • very slow reproductive rate
  • mate in the spring
  • give birth between 95 and 160 days after mating
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    lota facts
Patrick Wan

Physicx - Wikipedia, the free encyclopedia - 0 views

  • Physicx
  • HyoKeun Kim
  • his signature move, the "waistbreaker," or the "hollowback swing"
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  • Physicx has developed and popularized several breakdance techniques and moves, many of which are considered extremely technical and difficult. Below is a list of moves pioneered by Physicx:
cory delacruz

Blue Sky - Why is the Sky Blue? - 0 views

  • end of the spectrum are the reds and oranges. These gradually shade into yellow, green, blue, indigo and violet. The colors have different wavelengths, frequencies, and energies. Violet has the shortest wavelength in the visible spectrum. That means it has the highest frequency and energy. Red has the longest wavelength, and lowest frequency and energy. LIGHT IN THE AIR Light travels through space in a straight line as long as nothing disturbs it. As light moves through the atmosphere, it continues to go straight until it bumps into a bit of dust or a gas molecule. Then what happens to the light depends on its wave length and the size of the thing it hits. Dust particles and water droplets are much larger than the wavelength of visible light. When light hits these large particles, it gets reflected, or bounced off, in different directions. The different colors of light are all reflected by the particle in the same way. The reflected light appears white because it still contains all of the same colors. Gas molecules are smaller than the wavelength of visible light. If light bumps into them, it acts differently. When light hits a gas molecule, some of it may get absorbed. After awhile, the molecule radiates (releases, or gives off) the light in a different direction. The color that is radiated is the same color that was absorbed. The different colors of light are affected differently. All of the co
  • d after Lord John Rayleigh, an English physicist, who first described it in the 1870's.) WHY IS THE SKY BLUE? The blue color of the sky is due to Rayleigh scattering. As light moves through the atmosphere, most of the longer wavelengths pass straight through. Little of the red, orange and yellow light is affected by t
  • As you look closer to the horizon, the sky appears much paler in color. To reach you, the scattered blue light must pass through more air. Some of it gets scattered away again in other directions. Less blue light reaches your eyes. The color of the sky near the horizon appears paler or white.
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  • THE BLACK SKY AND WHITE SUN On Earth, the sun appears yellow. If you were out in space, or on the moon, the sun would look white. In space, there is no atmosphere to scatter the sun's light. On Earth, some of the shorter wavelength light (the blues and violets) are removed from the direct rays of the sun by scattering. The remaining colors together appear yellow. Also, out in space, the sky looks dark and black, instead of blue. This is because there is no atmosphere. There is no scattered light to reach your eyes. WHY IS THE SUNSET RED? As the sun begins to set, the light must travel farther through the atmosphere before it gets to you. More of the light is reflected and scattered. As less reaches you directly, the sun appears less
  • The sky around the setting sun may take on many colors. The most spectacular shows occur when the air contains many small particles of dust or water. These particles reflect light in all directions. Then, as some of the light heads towards you, different amounts of the shorter wavelength colors are scattered out. You see the longer wavelengths, and the sky appears red, pink or orange.
  • RE ABOUT:THE ATMOSPHERE WHAT IS THE ATMOSPHERE? The atmosphere is the mixture of gases and other materials that surround the Earth in a thin, mostly transparent shell. It is held in place by the Earth's gravity. The main components are nitrogen (78.09%), oxygen (20.95%), argon (0.93%), and carbon dioxide (0.03%). The atmosphere also contains small amounts, or traces, of water (in local concentrations ranging from 0% to 4%), solid particles, neon, helium, methane, krypton, hydrogen, xenon and ozone. The study of the atmosphere is called meteorology. Life on Earth would not be possible without the atmosphere.
  • d increases with increasing altitude. The increase is caused by the absorption of UV radiation by the oxygen and ozone. · The temperature increase with altitude results in a layering effect. It creates a global "inversion layer", and reduces vertical convection. Mesosphere - Extends out to about 100 km (65 miles) · Temperature decreases rapidly with increasing altitude. Thermosphere - Extends out to about 400 km ( 250 miles)
  • hes the Earth, 30% is reflected back into space by clouds and the Earth's surface. The atmosphere absorbs 19%. Only 51% is absorbed by the Earth's surface. We are not normally aware of it but air does have weight. The column of air above us exerts pressure on us. This pressure at sea level is defined as one atmosphere. Other equivalent measurements you may hear used are 1,013 millibars, 760 mm Hg (mercury), 29.92 inches of Hg, or 14.7 pounds/square inch (psi). Atmospheric pressure decreases rapidly with height. Pressure drops by a factor of 10 for every 16 km (10 miles) increase in altitude. This means that the pressure is 1 atmosphere at sea level, but 0.1 atmosphere at 16 km and only 0.01 atmosphere at 32 km. The density of the lower atmosphere is about 1 kg/cubic meter (1 oz./cubic foot). There are approximately 300 billion billion (3 x 10**20, or a 3 followed by 20 zeros) molecules per cubic inch (16.4 cubic ce
  • ers). At ground level, each molecule is moving at about 1600 km/hr (1000 miles/hr), and collides with other molecules 5 billion times per second. The density of air also decreases rapidly with altitude. At 3 km (2 miles) air density has decreased by 30%. People who normally live closer to sea level experience temporary breathing difficulties when traveling to these altitudes. The highest permanent human settlements are at about 4 km (3 miles). LAYERS OF THE ATMOSPHERE The atmosphere is divided into layers based on temperature, composition and electrical properties. These layers are approximate and the boundaries vary, depending on the seasons and latitude. (The boundaries also depend on which "authority" is defining them.) LAYERS BASED ON COMPOSITION Homosphere
  • LAYERS BASED ON TEMPERATURE Troposphere - Height depends on the seasons and latitude. It extends from ground level up to about 16 km (10 miles) at the equator, and to 9 km (5 miles) at the North and South Poles. · The prefix "tropo" means change. Changing conditions in the Troposphere result in our weather. · Temperature decreases with increasing altitude. Warm air rises, then cools and falls back to Earth. This process is called convection, and results in huge movements of air. Winds in this layer are mostly vertical. · Contains more air molecules than
  • · The air is very thin. · The prefix "strato" is related to layers, or stratification. · The bottom of this layer is calm. Jet planes often fly in the lower Stratosphere to avoid bad weather in the Troposphere. · The upper part of the Stratosphere holds the high winds known as the jet streams. These blow horizontally at speeds up to 480 km/hour (300 miles/hour) · Contains the "ozone layer" located
  • gen we need to breath. But it also serves other important functions. It moderates the planet's temperature, reducing the extremes that occur on airless worlds. For example, temperatures on the moon range from 120 °C (about 250 °F) in the day to -170 °C (about -275 °F) at night. The atmosphere
    • cory delacruz
       
      sounds good, by the way am i annoying you with my sticky note??? well, TOO BAD!!!!!!
Katie M

Global Warming Effects, Global Warming Causes, Causes of Global Warming, Effects of Global Warming - 0 views

  • Many scientists have specified various reasons for global warming effects on the environment and for human life. It is not easy to point one reason for global warming effects, but recently you might have saw many change in global climate. Global warming effects have various consequences such as glacier volume decreasing, rise in sea levels, shrinkage of Arctic and altered fashion of doing agriculture have been named as direct effects on global warming. Secondary global warming effects are extreme weather events, increase in tropical diseases, changes in the timing of seasonal patterns in ecosystems, and drastic economic impact.
  • Before many times back, many scientist and researchers were hopping that a positive effect of global warming would be increased agricultural yields(outputs), because of the role of carbon dioxide in photosynthesis which might behave in positive manner, but now it resulting in destructions of several crops. In the area of Iceland, due the rising temperatures which have made possible the widespread sowing of barley easily in an effective manner, which was not possible twenty years from now. The net result is expected to be that 33% less maize—the country's staple crop—will be grown. The reduction in rainfall has turned millions of land into deserts.
  • Insurance industry has been affected very badly with the risk of insurance; the number of major natural disasters has been increased to 300% since 1960s, and insured losses increased fifteenfold in real terms. According to Choi and Fisher (2003) each 1% increase in annual precipitation could enlarge catastrophe loss by as much as 2.8%.
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  • All major Transportation sources such as Roads, airport runways, railway lines and pipelines, always require time to time maintenance and renewal as they become subject to greater temperature variation. Regions already adversely affected include areas of permafrost, which are subject to high levels of subsidence, resulting in buckling roads, sunken foundations, severely cracked runways and many other related problems.
  • Most of the low-lying countries such as Bangladesh, Indonesia, Netherlands and many other small islands have been affected by sea level rise, in terms of floods or the cost of preventing them. In most of the poorest low-plain countries, land is the only available space, or fertile agricultural land which is livelihood for them. But due to flood they are finding problem now to perform their activities.
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    effects of global warming
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