Skip to main content

Home/ JJP Website Review/ Group items matching "material" in title, tags, annotations or url

Group items matching
in title, tags, annotations or url

Sort By: Relevance | Date Filter: All | Bookmarks | Topics Simple Middle
Jilliane Velazco

Digital Sales Not Enough to Save Music Industry, says JupiterResearch | Tekrati Research News - 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,”
  • ...2 more annotations...
  • 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.
  •  
    apple is the most popular device/music player and it is hard for other companies to compete with apple and itunes
Stephania D

Water Pollution - 0 views

  • According to the American College Dictionary, pollution is defined as:  �to make foul or unclean; dirty.
  • When it is unfit for its intended use, water is considered polluted.
  • Point sources of pollution occur when harmful substances are emitted directly into a body of water.
  • ...10 more annotations...
  • A nonpoint source delivers pollutants indirectly through environmental changes.
  • Nonpoint sources are much more difficult to control.
  • Pollution arising from nonpoint sources accounts for a majority of the contaminants in streams and lakes.  
  • Many causes of pollution including sewage and fertilizers contain nutrients such as nitrates and phosphates.  In excess levels, nutrients over stimulate the growth of aquatic plants and algae.  Excessive growth of these types of organisms consequently clogs our waterways, use up dissolved oxygen as they decompose, and block light to deeper waters.
  • Pollution in the form of organic material enters waterways in many different forms as sewage, as leaves and grass clippings, or as runoff from livestock feedlots and pastures.
  •     Pathogens are another type of pollution that prove very harmful.
  • Three last forms of water pollution exist in the forms of petroleum, radioactive substances, and heat.
  •      Ninety-five percent of all fresh water on earth is ground water
  • Ground water is found in natural rock formations.
  • These formations, called aquifers, are a vital natural resource with many uses.  Nationally, 53% of the population relies on ground water as a source of drinking water.  In rural areas this figure is even higher.  Eighty one percent of community water is dependent on ground water.  Although the 1992 Section 305(b) State Water Quality Reports indicate that, overall, the Nation�s ground water quality is good to excellent, many local areas have experienced significant ground water contamination. Some examples are leaking underground storage tanks and municipal landfills.
  •  
    Full description of water pollution, etc.
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.
  • ...20 more annotations...
  • 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.
Harry W

www.driverssuit.com authentic race used race worn drivers suits uniforms firesuits sheetmetal sheet metal helmets crew shirts - 0 views

  • The suit is made out of either Proban or the same Nomex material that lines the inside of the driver's helmet.
cory delacruz

Cretaceous-Tertiary extinction event - Wikipedia, the free encyclopedia - 0 views

  • More has been published about the extinction of dinosaurs at the K-T boundary than any other group of organisms. Excluding a few controversial claims, it is agreed that all non-avian dinosaurs went extinct at the K-T boundary. The dinosaur fossil record has been interpreted to show both a decline in diversity and no decline in diversity during the last few million years of the Cretaceous, and it may be that the quality of the dinosaur fossil record is simply not good enough to permit researchers to distinguish between the choices.[54] Since there is no evidence that late Maastrichtian nonavian dinosaurs could burrow, swim or dive, they were unable to shelter themselves from the worst parts of any environmental stress that occurred at the K-T boundary. It is possible that small dinosaurs (other than birds) did survive, but they would have been deprived of food as both herbivorous dinosaurs would have found plant material scarce, and carnivores would have quickly found prey to be in short supply.[35] The growing consensus about the endothermy of dinosaurs (see dinosaur physiology) helps to understand their full extinction in contrast with their close relatives, the crocodilians. Cold-blooded crocodiles have very limited needs of food (they can survive several months without eating) while warm-blooded animals of similar size need much more food in order to sustain their faster metabolism. Thus, under the circumstancies of food chain disruption above mentioned, non-avian dinosaurs died [55] while some crocodiles survived. In this context, the survival of other endothermic animals, such as some birds and mammals, could be due, among other
Bibin John

Aircraft - Wikipedia, the free encyclopedia - 0 views

  • An aircraft is a vehicle which is able to fly through the Earth's atmosphere or through any other atmosphere. Rocket vehicles are not aircraft if they are not supported by the surrounding air. All the human activity which surrounds aircraft is called aviation.
  • Heavier-than-air aircraft must find some way to push air or gas downwards, so that a reaction occurs (by Newton's laws of motion) to push the aircraft upwards. This dynamic movement through the air is the origin of the term aerodyne. There are two ways to produce dynamic upthrust: aerodynamic lift, and powered lift in the form of engine thrust. Aerodynamic lift is the most common, with aeroplanes being kept in the air by the forward movement of wings, and rotorcraft by spinning wing-shaped rotors sometimes called rotary wings. A wing is a flat, horizontal surface, usually shaped in cross-section as an aerofoil. To fly, the wing must move forwards through the air; this movement of air over the aerofoil shape deflects air downward to create an equal and opposite upward force, called lift, according to Newton's third law of motion. A flexible wing is a wing made of fabric or thin sheet material, often stretched over a rigid frame. A kite is tethered to the ground and relies on the speed of the wind over its wings, which may be flexible or rigid, fixed or rotary. With powered lift, the aircraft directs its engine thrust vertically downwards. The initialism VTOL (vertical take off and landing) is applied to aircraft that can take off and land vertically. Most are rotorcraft. Others, such as the Hawker Siddeley Harrier, take off and land vertically using powered lift and transfer to aerodynamic lift in steady flight. Similarly, STOL stands for short take off and landing. Some VTOL aircraft often operate in a short take off/vertical landing regime known as STOVL. A pure rocket is not usually regarded as an aerodyne, because it does not depend on the air for its lift (and can even fly into space), however many aerodynamic lift vehicles have been powered or assisted by rocket motors. Rocket-powered missiles which obtain aerodynamic lift at very high speed due to airflow over their bodies, are a marginal case.
  • The forerunner of the aeroplane is the kite
  • ...1 more annotation...
  • Number of planes - Monoplane, biplane, etc. Wing support - Braced or cantilever, rigid or flexible. Wing planform - including aspect ratio, angle of sweep and any variations along the span. Includes the important class of delta wings. Location of the horizontal stabiliser, if any. Dihedral angle - positive, zero or negative (anhedral). A variable geometry aircraft can change its wing configuration during flight. A flying wing has no fuselage, though it may have small blisters or pods. The opposite of this is a lifting body which has no wings, though it may have small stabilising and control surfaces.
  •  
    Tells all about different kinds of aircrafts.
Sara Espinosa

Biggest Cities | Galleries | Allianz Knowledge - 0 views

  • 1. Tokyo, Japan Metropolitan area: 34 million people City: 12.5 million people Tokyo is by far the largest urban region in the world. Despite its size and complexity, Tokyo has a very efficient public transportation, which accounts for almost 80 percent of all daily journeys in Tokyo.
  • 1. Tokyo, Japan Metropolitan area: 34 million people City: 12.5 million people Tokyo is by far the largest urban region in the world. Despite its size and complexity, Tokyo has a very efficient public transportation, which accounts for almost 80 percent of all daily journeys in Tokyo. Urban Detail: Tokyo Bay has been gradually filled up to create more space for housing and offices. Odaiba, an island entirely created out of waste material, became one of Tokyo’s most interesting tourist spots with futuristic architecture, shopping, and entertainment centers. (Photo: Miki Yokoyama)
  •  
    tokyo
robert meeker

Skydiving-Guide.com - History of skydiving - 0 views

    • robert meeker
       
      best site yet!!!!!!
    • robert meeker
       
      very good web site
  • Eventhough parachutes seem to have been used in China since the 1100s and that Leonardo da Vinci of Italy had invented devices similar to parachutes nowadays, worldwide skydivers state that the French inventor André-Jacques Garnerin is the one to make the first parachute. In 1797 he jumped from a balloon over Paris using a parachute and kept on making other jumps in France and also in England.
  • In World War I , that is between 1914 and 1918, the military began using parachutes in their missions
  • ...6 more annotations...
  • Barnstormers, who were in fact aerial showmen, fired the imagination of aviators and skydivers after World War I. The barnstormers showed airborne performances and parachute jumps and travelled every year throughout the United States. Competitions began as a result of the increase of parachuting awareness. The first contest of accuracy landing was held in 1930 in the Union of Soviet Socialist Republics (USSR).
  • The military used paratroopers in World War II , that is between 1939 and 1945. The paratroopers were parachute-equipped soldiers and had the most famous use on D-Day, the invasion of Normandy (Normandie), France, on June 6, 1944
  • The surplus of nylon parachute equipment after World War II and the fact that the U.S. Army had started the first military sport parachuting clubs, set the grounds of skydiving in the United Dtates, as a pleasant and relaxing activity. The same thing happened in many other countries, and thus , the first parachuting world championships were organized in 1951 in Yugoslavia.
  • Little by little, in the mid 1960, systems specially made for sport parachutes took the place of the military surplus systems. Parachutists started to call this activity skydiving and calling themselves skydivers. In order to improve the opening characteristics and to make them more maneuverable, there were a few sport modifications to military parachutes. A French Canadian kite builder, Domina Jalbert, developed in 1964 the the ram-air design, that has set the tendencies for parachutes in skydiving from then on.
  • Sport skydivers constantly tested new and revolutionary designs and materials. Apart from sport uses , there have also been designed sport-generated designs like military HAHO (high altitude, high opening) designs, smoke jumping designs and many types of equipment for two-person and four-person tandem jumping. The military HAHO designs allowed soldiers to silently fly over large areas. The smoke jumping designs aimed to put firefighters into remote forest fires from low altitude.
  • Skydiving has kept on becoming more and more popular after the late 1980s, and this is because the equipment, that is reliable, lightweight, and easy-to-operate, picture this sport as accesible to many people. The U.S. president George H. W. Bush also jumped , thus increasing the popularity of skydiving.
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.
  • ...10 more annotations...
  • 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!!!!!!
1 - 12 of 12
Showing 20 items per page