Bing

it means when some thing explodes

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It could mean that the engine is backfiring, perhaps due to timing error. It could mean that an exhaust valve is not opening, perhaps due to a bent pushrod, causing release of the combustion cycle back into the intake manifold.

No. Too many people, including myself, have had WAY to many problems with them. Wish I would never have bought it. One Big NIGHTMARE!

answer

Kia Sedona for 2011 can conveniently accommodate seven people in its interior.

This comes with a traditional V-6 drive-train and is available in traditional LX and upgraded EX trim levels.

Anyways, competitors of this vehicle are Dodge Grand Caravan, Toyota Sienna, and Honda Odyssey.

A small bell attached to a motorcycle, believed by some bikers to scare off road gremlins. Gremlin bells should be given as a gift to assure maximum effectiveness.

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Mostly just a decorative item.

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Road Gremlins:

There are motorcycle gremlins (AKA: Evil Road Spirits) that LOVE to ride, but they are also mischievous little devils and they cause all sorts of problems for you while you are riding. Road gremlins leave obstacles in your path- old mufflers, pieces of rubber, boxes and things like that. Some say they are responsible for that old lady in the minivan not seeing you and cutting you off in traffic. Or, you may be having trouble shifting smoothly, your battery goes dead, your turn signal suddenly refuses to work, an oil spill appears out of nowhere, etc - you get the idea. Those little gremlins look for trouble and try to steer your bike towards it. Road gremlins hope to make a biker crash so they can rejoice over their little acts of evil.

Once you get a bell on your scoot - it wards off these attacks from the little gremlins, not allowing any more to get onto your bike. If you already have some gremlins riding with you, they will get trapped in the hollow of the bell, and the constant ringing will drive them insane - causing them to lose their grip and fall to the roadway.

When you purchase a motorcycle bell and place it on your bike, it offers protection. If you receive the gremlin bell as a gift - the powerful magic of the bell is doubled. When you place it on your bike, you want it to be low to the ground, but not so low it will catch on obstacles and come off. Place it as forward as possible, so that the road gremlins will jump away when they first see you.

Motorcycles bells come in all types, small angel bells, patriotic bells, dealers specific bells, POW bells, etc. No matter if you believe in road gremlins or not, a road bell and regular preventive maintenance goes a long way to keep you feeling safe and secure.

The Progressive Insurance Company believes in road gremlins and has caught them in action in their commercial, Gremlins-Kickstand. (Find it on YouTube to see what a road gremlin looks like).

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LEGEND OF THE BELL

Many years ago, on a cold December night a crusty old biker was returning from a trip to Mexico with his saddlebags filled with toys and other assorted trinkets for the kids at a group home, near where he worked.

As he rode along that night thinking how lucky he had been in life, having a loving riding partner that understood his need to roam the highways and to his trusty old pan that hadn't let him down once in the many years they shared the road together.

Well about 40 miles north of the border, in the high desert lurked a small group of those notorious little critters known as road gremlins, you know the ones that always leave little obstacles like, one shoe, boards, pieces of old tires, and dig the dreaded pot holes for bikers to run over and crash thus giving the road gremlins a chance to rejoice over their acts of evil.

Well as the lone wolf of a biker rounded a curve that moonlit night the gremlins ambushed him, causing him to crash to the asphalt and skid for always before coming to a stop, next to one of his saddlebags that had broken free. As he lay there, unable to move, the road gremlins made their move towards him. Well this biker not being one to give up started throwing things at the gremlins as they approached him. Finally with nothing else to throw but a bell he started ringing it, in hopes to scare off the dirty little gremlins.

About a half a mile away camped in the desert, were two bikers sitting around the camp fire talking about their days ride, and the freedom of the wind blowing in their faces as they rode across this vast country. In the stillness of the night air, they heard what sounded to them like church bells ringing and upon investigating, found the old biker lying along the roadside with the gremlins about to get him. Needless to say, being part of the biker brotherhood they preceded to ward off the gremlins until the last of gremlins ran off into the night.

Being grateful to the two bikers the old road dog offered to pay them for their help, but as all true bikers do, they refused to accept any type of payment from him. Not being one to let a good deed go unnoticed, the old biker cut two pieces of leather from his saddle bags tassels and tied a bell to each one, then slowly placed them on each of the bikers motorcycles, as near to the ground as possible. The tired, old road warrior, then told the two travelers that with those bells placed on their bikes they would be protected from the road gremlins and that if ever in trouble, just ring the bell and a fellow biker will come to their aid.

So when ever you see a biker with a bell you'll know that he has been blessed with the most important thing in life -- friendship from a fellow biker.

It will not cost you any money to view your own video clip on YouTube. You should not, however, repeatedly watch your videos in order to game the monetization system since this is against the rules of YouTube.

i dotn know

bing means because its not Google

Bing Maps Platform was created in 2005.

I am having this problem too. So far, the most possible answer is about the GFW, great/government firewall, if you are live in mainland you must be farmiliar with it. China bans google, youtube, facebook, twitter... and maybe this time, they banned bing rewards.

Microsoft Headquarters, Right next to their new anti-apple gadgets... I just love Microsoft.

A company in california that controls the entire network, pays Bing per click. Also when you search something then you click on the site, that site pays bing for a person clicking on their site through Bing.

probally around the web,and other place,s.

Bing was pretty much Google, so there basically the same thing anyways.

Just different ways of showing it.

I think google is just making improvments.

Bing was created to allow you to search the internet for websites of interest.

A ton of people go on bing because maybe the pictures or because of 'hotmail'. I would estimate around 10 trillion people visit bing per day. Welcome :P.

Google

No, it is completely free to use.

P-waves are type of elastic wave, also called seismic waves, that can travel through gasses (such as sounds), elastic solids and liquids, including the Earth. P-waves can be produced by earthquakes and recorded by seismometers. The name P-wave stands for primary wave, as the P-wave is the fastest among the elastic waves, compared to the S-waves. In isotropic and homogeneous solids, the polarization of a P-wave is always longitudinal; thus, the particles in the solid have vibrations along or parallel to the travel direction of the wave energy. In isotropic and homogeneous solids, the polarization of P-waves is always longitudinal. This means that the particles in the body have vibrations along or parallel to the direction of travel of the wave energy. Earthquake advance warning is possible by detecting the non-destructive primary waves that travel more quickly through the earth's crust than do the destructive secondary and Rayleigh waves. The amount of advance warning depends on the delay between the arrival of the P-wave and other destructive waves, generally on the order of seconds up to about a minute maximum for deep, distant, large quakes. The effectiveness of advance warning depends on accurate detection of the P-waves and compensation for ground vibrations caused by local activity (such as trucks or construction work). Almost all the information available on the structure of the Earth's deep interior is derived from observations of the travel times, reflections, refractions and phase transitions of seismic body waves, or normal modes. Body waves travel through the fluid layers of the Earth's interior, but P-waves are refracted slightly when they pass through the transition between the semisolid mantle and the liquid outer core. As a result, there is a P-wave "shadow zone" between 104° and 140°, where the initial P-waves are not registered on seismometers. In contrast, S-waves do not travel through liquids, rather, they are attenuated.A type of seismic wave, the S-wave, secondary wave, or shear wave (sometimes called an elastic S-wave) is one of the two main types of elastic body waves, so named because they move through the body of an object, unlike surface waves. The S-wave move as a shear or transverse wave, so motion is perpendicular to the direction of wave propagation: S-waves, like waves in a rope, as opposed to waves moving through a slinky, the P-wave. The wave moves through elastic media, and the main restoring force comes from shear effects. These waves are divergenceless and obey the continuity equation for incompressible media: Its name, S for secondary, comes from the fact that it is the second direct arrival on an earthquake seismogram, after the compressional primary wave, or P-wave. Unlike the P-wave, the S-wave cannot travel through the molten outer core of the Earth, and this causes a shadow zone for S-waves opposite to where they originate. They can still appear in the solid inner core: when a P-wave strikes the boundary of molten and solid cores, called the Lehmann discontinuity, S-waves will then propagate in the solid medium. And when the S-waves hit the boundary again they will in turn create P-waves. In fact, this property allows seismologists to determine the nature of the inner core. The velocity of an S-wave in an isotropic medium can be described by the shear modulus μ and density ρ. As transverse waves, S-waves exhibit properties, such as polarization and birefringence, much like other transverse waves. S-waves polarized in the horizontal plane are classified as SH-waves. If polarized in the vertical plane, they are classified as SV-waves. When an S- or P-wave strikes an interface at an angle other than 90 degrees, a phenomenon known as mode conversion occurs. As described above, if the interface is between a solid and liquid, S becomes P or vice versa. However, even if the interface is between two solid media, mode conversion results. If a P-wave strikes an interface, four propagation modes may result: reflected and transmitted P and reflected and transmitted SV. Similarly, if an SV-wave strikes an interface, the same four modes occur in different proportions. The exact amplitudes of all these waves are described by the Zoeppritz equations, which in turn are solutions to the wave equation. In elastodynamics, Love waves are essentially horizontally polarized shear waves (SH waves) guided by an elastic layer, which is "welded" to an elastic half space on one side while bordering a vacuum on the other side. In seismology, Love waves (also named Q waves (Quer: German for lateral)) are surface seismic waves that cause horizontal shifting of the earth during an earthquake. A.E.H. Love predicted the existence of Love waves mathematically in 1911; the name comes from him (Chapter 11 from Love's book "Some problems of geodynamics", first published in 1911). They form a distinct class, different from other types of seismic waves, such as P-waves and S-waves (both body waves), or Rayleigh waves (another type of surface wave). Love waves travel with a slower velocity than P- or S- waves, but faster than Rayleigh waves. The particle motion of a Love wave forms a horizontal circle or ellipse moving in the direction of propagation. Moving deeper into the material, motion decreases to a "node" and then alternately increases and decreases as one examines deeper layers of particles. The amplitude, or maximum particle motion, decreases rapidly as one examines deeper layers of particles. Since Love waves travel on the Earth's surface, the strength (or amplitude) of the waves decrease exponentially with the depth of an earthquake. However, given their confinement to the surface, their amplitude decays only as, where r represents the distance the wave has traveled from the earthquake. Surface waves therefore decay more slowly with distance than do body waves, which travel in three dimensions. Large earthquakes may generate Love waves that travel around the Earth several times before dissipating. Love waves take a long time to dissipate due to the huge amount of energy that they contain. For this reason, they are most destructive within the immediate area of the focus or epicentre of an earthquake. They are what most people feel directly during an earthquake. In the past, it was often thought that animals like cats and dogs could predict an earthquake before it happened. However, they are simply more sensitive to ground vibrations than humans and able to detect the subtler waves that precede Love waves, like the P-waves and the S-waves.

5 million feet long 5 million feet long

The name of the girl is Melisa De Carlo and she is from Argentina.