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Carlen Hodgson

12 Surefire Basketball Tips for the Off Season - What Should Players Do Between Seasons? - 0 views

  • The season is winding down. Routines change, friendships have grown, priorities change. As a player, what should you do now? When practice time comes and there is no practice, what do you do? When there are no games to prepare for, what do you do with your time? Here are a just a few thoughts I had as to how to recover and prepare for the next season. 1. Take 3 - 4 weeks to relax. It has been a long, physically and mentally draining season. If you want to improve, you have to give yourself a chance to recover. 2. Catch up and get ahead of your schoolwork. 3. Talk to your coach and evaluate your season. Talk about what you did well and what you did not. Determine the areas you need to improve on. Discuss the things you would like to do and how to accomplish them. 4. After taking a month off, start on your off-season workout program. The program should be about 75% skill work and 25% play. 5. Develop your shooting stroke. If you want to become a GREAT shooter and raise your percentage, it MUST happen during the off season. It's just TOO difficult to develop these skills and improve during the season. It must be done during the off season! 6. Start a strength training program. Your objective should be to gain strength from now until the end of the summer. 7. As you enter the summer, add more play to your workout. You should be at about 50% skill work, 50% play. Don't neglect your weight work. Great strength gains can be made during this period. 8. Go to camp. Learn form other coaches, play against different players. The more diverse your summer experience, the better player you will become. 9. When the summer is over, your routine changes. GET AHEAD in the classroom. Once the season starts, it is easy for your schoolwork to slip. 10. Change your workout routine to 25% skill, 75% play. 11. Switch you strength training routine to an endurance and strength maintenance routine. 12. A week before the season, take some time off. Get ready to go.
Catherine A.

Child development - Wikipedia, the free encyclopedia - 0 views

    • Catherine A.
       
      Now I understand why my new baby cousin sometimes cry when i carry her
  • The capacity to learn, remember, and symbolize information, and to solve problems, exists at a simple level in young infants, who can perform cognitive tasks such as discriminating animate and inanimate beings or recognizing small numbers of objects
  • Abilities for physical movement change through childhood from the largely reflexive (unlearned,involuntary) movement patterns of the young infant to the highly skilled voluntary movements characteristic of later childhood and adolescence
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  • Physical growth in stature and weight occurs over the 15-20 years following birth, as the individual changes from the average weight of 7 1/2 pounds and length of 20" at full-term birth to full adult size. As stature and weight increase, the individual's proportions also change, from the relatively large head and small torso and limbs of the neonate, to the adult's relatively small head and long torso and limbs.
  • Newborn infants do not seem to experience fear or have preferences for contact with any specific people.By about 8-10 months, they go through a fairly rapid change and become fearful of perceived threats; they also begin to prefer familiar people and show anxiety and distress when separated from them or approached by strangers
  • Dyslexia is a significant topic in child development as it affects approximately 5% of the population (in the western world). Essentially it is a disorder whereby children fail to attain the language skills of reading, writing and spelling commensurate with their intellectual abilities.
Jesse Lavine

Student Research Center - powered by EBSCOhost: Longer, straighter and sweeter - 0 views

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    equipment changes in golf
Kate L

Types of Alternative Fuels - Moving Away From Oil - 0 views

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    Changing from oil to alternative fuels
karen ponce

Encyclopedia Smithsonian: Thanksgiving in North America: From Local Harvests to Nationa... - 0 views

shared by karen ponce on 05 Dec 08 - Cached
  • Thanksgiving Feast of 1621, but few realize that it was not the first festival of its kind in North America. Long before Europeans set foot in the Americas, native peoples sought to insure a good harvest with dances and rituals such as the Green Corn Dance of the Cherokees.
  • The first Thanksgiving service known to be held by Europeans in North America occurred on May 27, 1578 in Newfoundland, although earlier Church-type services were probably held by Spaniards in La Florida. However, for British New England, some historians believe that the Popham Colony in Maine conducted a Thanksgiving service in 1607 (see Sources: Greif, 208-209; Gould, and Hatch). In the same year, Jamestown colonists gave thanks for their safe arrival, and another service was held in 1610 when a supply ship arrived after a harsh winter. Berkley Hundred settlers held a Thanksgiving service in accordance with their charter which stated that the day of their arrival in Virginia should be observed yearly as a day of Thanksgiving, but within a few years an Indian uprising ended further services (Dabney). Thus British colonists held several Thanksgiving services in America before the Pilgrim's celebration in 1621.
  • In 1623, the Pilgrims at Plymouth Plantation, Massachusetts, held another day of Thanksgiving. As a drought was destroying their crops, colonists prayed and fasted for relief; the rains came a few days later. And not long after, Captain Miles Standish arrived with staples and news that a Dutch supply ship was on its way. Because of all this good fortune, colonists held a day of Thanksgiving and prayer on June 30. This 1623 festival appears to have been the origin of our Thanksgiving Day because it combined a religious and social celebration.
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  • estivals of Thanksgiving were observed sporadically on a local level for more than 150 years. They tended to be autumn harvest celebrations. But in 1789, Elias Boudinot, Massachusetts, member of the House of Representatives, moved that a day of Thanksgiving be held to thank God for giving the American people the opportunity to create a Constitution to preserve their hard won freedoms. A Congressional Joint Committee approved the motion, and informed President George Washington. On October 3, 1789, the President proclaimed that the people of the United States observe "a day of public thanksgiving and prayer" on Thursday, the 26th of November. The next three Presidents proclaimed, at most, two days of thanksgiving sometime during their terms of office, either on their own initiative or at the request of a joint Resolution of Congress. One exception was Thomas Jefferson, who believed it was a conflict of church and state to require the American people hold a day of prayer and thanksgiving. President James Madison proclaimed a day of Thanksgiving to be held on April 13, 1815, the last such proclamation issued by a President until Abraham Lincoln did so in 1862.
  • Thanksgiving holiday may be given to Sarah Josepha Hale. Editor of Ladies Magazine and Godey's Lady's Book, she began to agitate for such a day in 1827 by printing articles in the magazines. She also published stories and recipes, and wrote scores of letters to governors, senators, and presidents. After 36 years of crusading, she won her battle. On October 3, 1863, buoyed by the Union victory at Gettysburg, President Lincoln proclaimed that November 26, would be a national Thanksgiving Day, to be observed every year on the fourth Thursday of November. Only twice has a president changed the day of observation. President Franklin D. Roosevelt, in order to give depression-era merchants more selling days before Christmas, assigned the third Thursday to be Thanksgiving Day in 1939 and 1940. But he was met with popular resistance, largely because the change required rescheduling Thanksgiving Day events such as football games and parades. In 1941, a Congressional Joint Resolution officially set the fourth Thursday of November as a national holiday for Thanksgiving.
cory delacruz

Why Did All Dinosaurs Become Extinct? | Scholastic.com - 0 views

  • Adapted from Dinosaurs: The Very Latest Information and Hands-On Activities From the Museum of the Rockies, by Liza Charlesworth and Bonnie Sachatello-Sawyer. A Scholastic Professional Book. The last dinosaurs died approximately 65 million years ago. Although the cause of their extinction is still a mystery, climatic change, diseases, changing plant communities, and geologic events could all have played a role. Lately, dinosaur extinction theories have been the subject of much debate and controversy. A recent explanation, supported by many scientists, suggests that dinosaurs died out soon after a huge meteorite crashed to Earth near the Gulf of Mexico. A giant meteorite, they reason, could have landed with an impact that kicked up enough dust and debris to block out sunlight for a long time — leading to a deadly chain of events. Without the sun, all the plants died; without the plants, all the plant-eaters died; and without the plant-eaters, all the meat-eaters died. Sounds reasonable. But there is one problem with this theory: Paleontologists have not yet been able to find dinosaur skeletons in rocks dating to the period of impact. Some evidence even seems to indicate that all the dinosaurs had died before the meteorite hit. What is the answer? As paleontologists search for clues to support their theories, they agree to disagree.
    • cory delacruz
       
      sounds interseting so i could use this to learn.........................................................................................................................................................................................................
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    I can use this to give a general idea of what exactly made the dinosaurs extinct.
Stephania D

Coral Reefs - 0 views

  • A third of reef-building corals worldwide are threatened with extinction due to climate change and water pollution, according to the first global assessment on the marine creature by 39 scientists.
  • Destructive fishing and the degradation
  • "When corals die off, so do the other plants and animals that depend on coral reefs for food and shelter, and this can lead to the collapse of entire ecosystems," he added.
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  • "We either reduce our CO2 emission now or many corals will be lost forever," warned Julia Marton-Lefevre, IUCN Director General.
  • According to the study, the Caribbean region has the highest number of highly threatened corals.
  • As they are home to over 25 percent of marine species -- including fish stocks -- loss of reefs could also impact coastal fishing communities.
  • depend on coral reefs for their livelihoods,
  • reef-building corals in particular were "most vulnerable to the effects of climate change".
  • Sea temperature rises bleach and weaken the algae that give the underwater sea life its vibrant color, and make it more susceptible to diseases.
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    Coral reef dangers
Haley Herebia

Polar Bear - Defenders of Wildlife - 0 views

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    threats, protection and help them climate change and the effect it has on the ice, their habit
Katie M

Global warming, photography, pictures, photos, climate change, impact, science, weather... - 0 views

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    pictures!!
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 Glo... - 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
Jilliane Velazco

PowerSearch  Document - 0 views

  • 51 per cent of its earnings over the past year came from digital sales.
  • falling CD sales and illegal downloading.
  • "Some fans only want to buy the physical disc, some only want to buy a ringtone and a T-shirt, others just want a concert ticket, others want to buy a digital album.
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  • worldwide sales of digital music grew by 40 per cent last year
  • CDs would continue to narrow.
  • "Record labels are continually diversifying and moving away from CDs because they know that fans have completely changed the way they are buying music.''
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    fans buy different things of music: physical discs, ringtones and a t-shirt, a concert ticket, or a digital album; worldwide sales of digital music grew by 40% last year
Jilliane Velazco

Digital Sales Not Enough to Save Music Industry, says JupiterResearch | Tekrati Researc... - 0 views

  • Digital music was a $1.3 billion business in 2007, but it still only comprised 10 percent of consumer music spending
  • compete with Apple and the future of music CD sales.
  • “The challenge remains for the industry to find new ways to compete with Apple, who remains the dominant player for portable media devices,”
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  • it will become even more critical to find new devices paradigms to capture consumer attention and new business models to sell content and services on those devices
  • iTunes and other online music retailers are also changing the way music is purchased. Hot and popular are now giving way to Independent artists who are just as likely and able to make their material available on iTunes and other internet resources.
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    apple is the most popular device/music player and it is hard for other companies to compete with apple and itunes
Tucker Haydon

Koala info. 3 - 0 views

shared by Tucker Haydon on 03 Dec 08 - Cached
  • The word koala comes from Dharuk gula. Although the vowel /u/ was originally written in the Latin alphabet as "oo" (in spellings such as coola or koolah), it was changed to "oa" possibly due to an error.[3] The word is erroneously said to mean "doesn't drink"
  • The scientific name of the Koala's genus, Phascolarctos, is derived from Greek phaskolos "pouch" and arktos "bear". Its species name, cinereus, is Latin and means "ash-coloured"
Stephania D

Discovery News : Discovery Channel - 0 views

  • To make or mitigate rain, target clouds are injected with chemicals such as silver iodide, which has a crystalline structure almost identical to ice, or with dry ice, which changes the clouds' structure.
Stephania D

China - 0 views

  • Though it sounds like a classroom assignment from Hogwarts School of Witchcraft and Wizardry, weather modification programs have been around for more than 50 years.
  • The problem is there are too many factors that affect the weather, making naturally occurring phenomena difficult to separate from man-made triggers.
  • "There was no strong scientific base for changing the weather."
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  • Determined to prevent rain from dampening the spirits -- not to mention the crowds -- on opening day ceremonies, the government plans to seed any threatening clouds with chemicals to dispel, or at least delay, rainfall.
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    Pollution, prevention
Kate L

What types of alternative fuels are being explored or used in automobiles today? How ef... - 0 views

  • The primary fuels now used in automobiles, namely gasoline and diesel, are essentially derived from crude oil (petroleum)
  • properties as natural gas, coal and other carbonaceous fuels
  • as Fischer-Tropsch Diesel, a mixture of hydrogen and carbon monoxide
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  • not require a major shift from current automobile design.
  • address this question, we will assume that "alternative" refers to those fuels that are produced from a nonfossil source or to those fuels (fossil or otherwise) that would require substantial changes in automotive design or in the distribution and marketing infrastructure.
  • proposed a number of compounds--including methanol, ethanol, hydrogen, compressed natural gas (CNG), liquefied petroleum gas (LPG), so-called biodiesel and hydrogen--
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    Types of alternative fuels
Carlen Hodgson

Basketball Tip, Basketball Tips, Basketball Shooting Tips, Free Basketball Tips - 0 views

  • One of the keys to getting the most out of your training program is to work outside of your comfort zone.
  • I can't argue that you're doing something to stay in shape and work on your game. But you're not really pushing yourself, and you shouldn't really expect those types of workouts to pay huge dividends.
  • Change your approach. Push yourself harder than you normally do, and you'll start to see results. Instead of shooting 30 or 40 random, lazy jump shots, create a plan for yourself. Shoot from 4 or 5 spots on the floor until you've made 30 or 40 shots from each spot (or some number that you set as a goal for yourself). Get in the triple-threat position, head-fake, take a quick dribble to one side or the other, get good lift on your shot (really getting off the ground), and concentrate on your follow-through. Push yourself to move quicker than you normally do, and to jump higher than you normally do.
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  • Or when you go to the track, create a plan to really work on your stamina and quickness. Run 2 laps at a good pace to warm up. Then do some interval training where you sprint at top speed for 40 or 50 yards, then walk for 30 or 45 seconds to get your wind back. When you first start doing interval training, you'll probably only be able to do 4 or 5 repetitions, but you'll get in better shape over time and the numbers will increase. As you get into better shape, you'll work your way up to longer distances, shorter breaks in between sprints, and more repetitions. Follow-up your sprints with 4 or 5 hard minutes of jumping rope. Mix in some longer distance training during the week and you're on your way to really improving your stamina and quickness.
Kate L

Solar Energy As A Sustainable Source Of European Economic Growth - 0 views

  • Scientists from leading European research institutions in the field of solar-to-fuel energy conversion call for unified action and substantial support for novel clean fuel technologies as well as a paradigm change in Europe’s current energy policy
  • crucial if Europe is to maintain its environmental stability and economic development.
emily jackson

Greenberg Millennial Survey: How Generation WE Are Taking Over America and Changing... ... - 0 views

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    this website is kinda ragging on the milennial
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