Meteoroid Etoiles Filantes 08102011 2...
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Photo panoramique par dieter kik EXPERT MAESTRO Pris 19:48, 08/10/2011 - Views loading...


Meteoroid Etoiles Filantes 08102011 2148h Odet Quimper 3333

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it was the best time but I have seen no falling star
Photo of a part of the sky during a meteor shower over an extended exposure time. The meteors have actually occurred several seconds to several minutes apart.
A Perseid meteor (light streak somewhat to right of center of photo) and Milky Way
A meteoroid is a sand- to boulder-sized particle of debris in the Solar System. The visible path of a meteoroid that enters Earth's (or another body's) atmosphere is called a meteor, or colloquially a shooting star or falling star. If a meteoroid reaches the ground and survives impact, then it is called a meteorite. Many meteors appearing seconds or minutes apart are called a meteor shower. The root word meteor comes from the Greek meteo¯ros, meaning "high in the air". The Minor Planet Center does not use the term "meteoroid".
As of 2011 the International Astronomical Union officially defines a meteoroid as "a solid object moving in interplanetary space, of a size considerably smaller than an asteroid and considerably larger than an atom".[1][2] Beech and Steel, writing in Quarterly Journal of the Royal Astronomical Society, proposed a new definition where a meteoroid is between 100 µm and 10 m across.[3] The NEO definition includes larger objects, up to 50 m in diameter, in this category. Very small meteoroids are known as micrometeoroids (see also interplanetary dust).
The composition of meteoroids can be determined as they pass through Earth's atmosphere from their trajectories and the light spectra of the resulting meteor. Their effects on radio signals also give information, especially useful for daytime meteors which are otherwise very difficult to observe. From these trajectory measurements, meteoroids have been found to have many different orbits, some clustering in streams (see Meteor showers) often associated with a parent comet, others apparently sporadic. Debris from meteoroid streams may eventually be scattered into other orbits. The light spectra, combined with trajectory and light curve measurements, have yielded various compositions and densities, ranging from fragile snowball-like objects with density about a quarter that of ice,[4] to nickel-iron rich dense rocks.
Meteoroids travel around the Sun in a variety of orbits and at various velocities. The fastest ones move at about 26 miles per second (42 kilometers per second) through space in the vicinity of Earth's orbit. The Earth travels at about 18 miles per second (29 kilometers per second). Thus, when meteoroids meet the Earth's atmosphere head-on (which would only occur if the meteors were in a retrograde orbit), the combined speed may reach about 44 miles per second (71 kilometers per second). Meteoroids moving through the earth's orbital space at about 20 km/sec.[5]
A meteor is the visible path of a meteoroid that has entered the Earth's atmosphere. Meteors typically occur in the mesosphere, and most range in altitude from 75 km to 100 km.[6] Millions of meteors occur in the Earth's atmosphere every day. Most meteoroids that cause meteors are about the size of a pebble. They become visible between about 40 and 75 miles (65 and 120 kilometers) above the Earth. They disintegrate at altitudes of 30 to 60 miles (50 to 95 kilometers). Meteors have roughly a fifty percent chance of a daylight (or near daylight) collision with the Earth. Most meteors are, however, observed at night as low light conditions allow fainter meteors to be observed.
For bodies with a size scale larger than the atmospheric mean free path (10 cm to several metres)[clarification needed] the visibility is due to the atmospheric ram pressure (not friction) that heats the meteoroid so that it glows and creates a shining trail of gases and melted meteoroid particles. The gases include vaporized meteoroid material and atmospheric gases that heat up when the meteoroid passes through the atmosphere. Most meteors glow for about a second. A relatively small percentage of meteoroids hit the Earth's atmosphere and then pass out again: these are termed Earth-grazing fireballs (for example The Great Daylight 1972 Fireball).
Meteors may occur in showers, which arise when the Earth passes through a trail of debris left by a comet, or as "random" or "sporadic" meteors, not associated with a specific single cause. A number of specific meteors have been observed, largely by members of the public and largely by accident, but with enough detail that orbits of the meteoroids producing the meteors have been calculated. All of the orbits passed through the asteroid belt.[7]
A fireball is a brighter-than-usual meteor. The International Astronomical Union defines a fireball as "a meteor brighter than any of the planets" (magnitude −4 or greater).[8] The International Meteor Organization (an amateur organization that studies meteors) has a more rigid definition. It defines a fireball as a meteor that would have a magnitude of −3 or brighter if seen at zenith. This definition corrects for the greater distance between an observer and a meteor near the horizon. For example, a meteor of magnitude −1 at 5 degrees above the horizon would be classified as a fireball because if the observer had been directly below the meteor it would have appeared as magnitude −6.
The word bolide comes from the Greek βολίς (bolis) [2] which can mean a missile or to flash. The IAU has no official definition of "bolide", and generally considers the term synonymous with "fireball". The term generally applies to fireballs reaching magnitude −14 or brighter.[10] Astronomers tend to use "bolide" to identify an exceptionally bright fireball, particularly one that explodes (sometimes called a detonating fireball). It may also be used to mean a fireball which creates audible sounds.
Geologists use the term "bolide" more often than astronomers do: in geology it indicates a very large impactor. For example, the USGS uses the term to mean a generic large crater-forming projectile "to imply that we do not know the precise nature of the impacting body ... whether it is a rocky or metallic asteroid, or an icy comet, for example".
If the magnitude of a bolide reaches −17 or brighter it is known as a superbolide.
Main article: meteorite
A meteorite is a portion of a meteoroid or asteroid that survives its passage through the atmosphere and impact with the ground without being destroyed.[13] Meteorites are sometimes, but not always, found in association with hypervelocity impact craters; during energetic collisions, the entire impactor may be vaporized, leaving no meteorites.
Molten terrestrial material "splashed" from a meteorite impact crater can cool and solidify into an object known as a tektite. These are often mistaken for meteorites.
Meteoric dust
Most meteoroids burn up when they enter the atmosphere. The left-over debris is called meteoric dust or just meteor dust. Meteor dust particles can persist in the atmosphere for up to several months. These particles might affect climate, both by scattering electromagnetic radiation and by catalyzing chemical reactions in the upper atmosphere.
 Ionization trails
During the entry of a meteoroid or asteroid into the upper atmosphere, an ionization trail is created, where the molecules in the upper atmosphere are ionized by the passage of the meteor. Such ionization trails can last up to 45 minutes at a time. Small, sand-grain sized meteoroids are entering the atmosphere constantly, essentially every few seconds in any given region of the atmosphere,and thus ionization trails can be found in the upper atmosphere more or less continuously. When radio waves are bounced off these trails, it is called meteor burst communications.
Meteor radars can measure atmospheric density and winds by measuring the decay rate and Doppler shift of a meteor trail.
The visible light produced by a meteor may take on various hues, depending on the chemical composition of the meteoroid, and its speed through the atmosphere. As layers of the meteoroid are stripped off and ionized, the color of the light emitted may change according to the layering of minerals. Some of the possible colors and the compounds responsible for them are: orange/yellow (sodium); yellow (iron); blue/green (copper); purple (potassium); and red (silicate).
Any sound generated by a meteor in the upper atmosphere, such as a sonic boom, should not be heard until many seconds after the meteor disappeared. However, in certain instances, for example during the Leonid meteor shower of 2001, several people reported sounds described as "crackling", "swishing", or "hissing"[15] occurring at the same instant as a meteor flare. Similar sounds have also been reported during intense displays of Earth's auroras.
Sound recordings made under controlled conditions in Mongolia in 1998 by a team led by Slaven Garaj, a physicist at the Swiss Federal Institute of Technology at Lausanne, support the contention that the sounds are real.
How these sounds could be generated, assuming they are in fact real, remains something of a mystery. It has been hypothesized by some scientists at NASA as that the turbulent ionized wake of a meteor interacts with the magnetic field of the Earth, generating pulses of radio waves. As the trail dissipates, megawatts of electromagnetic energy could be released, with a peak in the power spectrum at audio frequencies. Physical vibrations induced by the electromagnetic impulses would then be heard if they are powerful enough to make grasses, plants, eyeglass frames, and other conductive materials vibrate.[21][22][23][24] This proposed mechanism, although proven to be plausible by laboratory work, remains unsupported by corresponding measurements in the field.
 Frequency of large meteors
See also: Planet Earth collision probability with near-Earth objects
The biggest asteroid to hit Earth on any given day is likely to be about 40 centimeters, in a given year about 4 meters, and in a given century about 20 meters. These statistics are obtained by the following:
Over at least the range from 5 centimeters (2 inches) to roughly 300 meters (1,000 feet), the rate at which Earth receives meteors obeys a power-law distribution as follows:
    N(>D) = 37 D^{-2.7}\
where N(>D) is the expected number of objects larger than a diameter of D meters to hit Earth in a year.[25] This is based on observations of bright meteors seen from the ground and space, combined with surveys of near Earth asteroids. Above 300 meters in diameter, the predicted rate is somewhat higher, with a two-kilometer asteroid (one million-megaton TNT equivalent) every couple of million years — about 10 times as often as the power-law extrapolation would predict.
Seasonal variation in frequency of fireball sightings
The frequency of fireball sightings increases by about 10-30% during the weeks of vernal equinox.[26] Even meteorite falls are more common during the spring season. Although this phenomenon has been known for quite some time, the reason behind the anomaly is not fully understood by scientists. Some researchers attribute this to an intrinsic variation in the meteoroid population along Earth's orbit, with a peak in big fireball-producing debris around spring and early summer. Research is in progress for mapping the orbits of the meteors in order to gain a better understanding of the phenemenon.
Notable meteors
See also: Near-Earth object#Historic impacts
Perhaps the best-known meteor/meteorite fall is the Peekskill Meteorite, filmed on October 9, 1992 by at least 16 independent videographers.
Eyewitness accounts indicate the fireball entry of the Peekskill meteorite started over West Virginia at 23:48 UT (±1 min). The fireball, which traveled in a northeasterly direction had a pronounced greenish color, and attained an estimated peak visual magnitude of −13. During a luminous flight time that exceeded 40 seconds the fireball covered a ground path of some 700 to 800 km.
One meteorite recovered at Peekskill, New York, for which the event and object gained its name, had a mass of 12.4 kg (27 lb) and was subsequently identified as an H6 monomict breccia meteorite.[30] The video record suggests that the Peekskill meteorite had several companions over a wide area. The companions are unlikely to be recovered in the harsh terrain in the vicinity of Peekskill.
2008 TC3 was discovered on 6 October 2008 and entered the Earth's atmosphere the next day, striking a remote area of northern Sudan. It was the first time a meteoroid had been observed in space and tracked prior to impacting Earth.
A large fireball was observed in the skies near Bone, Indonesia on October 8, 2009. This was thought to be caused by an asteroid approximately 10 meters in diameter. The fireball contained an estimated energy of 50 kilotons of TNT, or about twice the Nagasaki atomic bomb. No injuries were reported.
A large bolide was reported on 18 November 2009 over southeastern California, northern Arizona, Utah, Wyoming, Idaho and Colorado. At 12:07 a.m., a security camera at the high altitude W. L. Eccles Observatory (9600 ft above sea level) recorded a movie of the passage of the object to the north.[32][33] Of particular note in this video is the spherical "ghost" image slightly trailing the main object (this is likely a lens reflection of the intense fireball), and the bright fireball explosion associated with the breakup of a substantial fraction of the object. An object trail can be seen to continue northward after the bright fireball event. The shock from the final breakup triggered seven seismological stations in northern Utah; a timing fit to the seismic data yielded a terminal location of the object at 40.286 N, -113.191 W, altitude 27 km.[34] This is above the Dugway Proving Grounds, a closed Army testing base.
Although meteors have been known since ancient times, they were not known to be an astronomical phenomenon until early in the 19th century. Prior to that, they were seen in the West as an atmospheric phenomenon, like lightning, and were not connected with strange stories of rocks falling from the sky. Thomas Jefferson wrote "I would more easily believe that (a) Yankee professor would lie than that stones would fall from heaven."[35] He was referring to Yale chemistry professor Benjamin Silliman's investigation of an 1807 meteorite that fell in Weston, Connecticut.[35] Silliman believed the meteor had a cosmic origin, but meteors did not attract much attention from astronomers until the spectacular meteor storm of November 1833.[36] People all across the eastern United States saw thousands of meteors, radiating from a single point in the sky. Astute observers noticed that the radiant, as the point is now called, moved with the stars, staying in the constellation Leo.
The astronomer Denison Olmsted made an extensive study of this storm, and concluded it had a cosmic origin. After reviewing historical records, Heinrich Wilhelm Matthias Olbers predicted its return in 1867, which drew the attention of other astronomers. Hubert A. Newton's more thorough historical work led to a refined prediction of 1866, which proved to be correct.[36] With Giovanni Schiaparelli's success in connecting the Leonids (as they are now called) with comet Tempel-Tuttle, the cosmic origin of meteors was now firmly established. Still, they remain an atmospheric phenomenon, and retain their name "meteor" from the Greek word for "atmospheric".
Earth moves at about 30 km/s in its orbit.[39] Meteoroids also have significant orbital speeds. The differences in velocities where these orbits intersect combined with the gravitational attraction of Earth result in the velocities observed for meteors.

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Ce panorama é été pris à Cornouaille

Ceci est un aperçu de Cornouaille


Un article de Wikipédia, l'encyclopédie libre.

Capitale historique Quimper

Langue(s) Français - Breton

Religion Catholique

Superficie 5 979 Km²

Population 456 307 (1999)

Gwenn ha du.svg Portail de la Bretagne

La Cornouaille (Kernev, Bro Gernev en breton) est un pays de Bretagne (à ne pas confondre avec la Cornouailles britannique, dont le nom s'écrit avec un "s").

Le gentilé de la Cornouaille bretonne est cornouaillais  e (le gentilé de la Cornouailles britannique est cornique).


Cornouaille se dit Kerne, Kernev ou Bro Gerne en breton, et Cornugallia en latin, parfois « Cornubia ».

* Il est possible que ce nom lui ait été donné en référence à cette région de Cornouailles (Kernow), tout comme l'actuel Devon (ancienne Dumnonia) a donné son nom à la Domnonée qui désignait la côte Nord de la Bretagne au Haut Moyen Âge.

* Selon une autre hypothèse qui a eu longtemps cours, le nom serait d'origine anglo-saxonne et signifierait « Le pays des étrangers » en référence au cantonnement des Celtes d'Outre-Manche par les envahisseurs angles, saxons, jutes et frisons.

* Une troisième hypothèse, basée sur la traduction latine cornugallia, est invoquée par certains auteurs : cornugallia signifierait le coin de la Gaule, relativement à la situation géographique de la Cornouaille bretonne.

Antiquité tardive

Les deux Cornouaille(s) trouvent plus vraisemblablement leur origine commune à la fin du IIIe siècle : les incursions de pirates saxons, frisons et scots, associées aux pillages des bagaudes, contraignent les villes armoricaines (entre autres) à s'entourer en urgence de murailles dont les restes se voient encore à Alet, Brest, Nantes, Rennes et Vannes. Devant l'incurie de l'empire romain, le responsable de la défense des côtes, le ménapien Carausius (puis son successeur Allectus) établit entre 288 et 296 un empire séparé sur les côtes nord et sud de la Manche pour les garantir des invasions.

L'empereur Constance Chlore les vainc en 293 et 296 et, ayant rétabli l'unité de l'empire de ce côté, organise la défense côtière en transférant des Bretons en Armorique à partir de 296-297. Ces Bretons sont des Cornovii, peuple sans doute fidèle à Rome et choisi pour ce motif. Le chef-lieu de leur cité est à Viroconium Cornoviorum (l'actuelle Wroxeter) et ils occupent plus au nord le port de Deva (Chester). Les Cornovii étant chargés du contrôle militaire des pointes occidentales de la Bretagne et de l'Armorique, c’est-à-dire de l'ouest de la Manche, leur nom se serait conservé en ces lieux. Il ne s'agit donc pas d'une colonisation massive comme cela arrivera au VIe siècle, mais d'une occupation militaire.

Le Tractus armoricanus et nervicanus (administration militaire chargée du contrôle de toutes les côtes de Boulogne à la Gironde), et son bras armé, la Classis armoricana (Flotte armoricaine), ne sont créés proprement qu'en 370, sous le règne de l'empereur Valentinien Ier.

Haut Moyen Âge

D'autres princes sont dits avoir régné sur les côtes nord et sud de la Manche occidentale, comme le roi de Cornouaille Daniel Drem Rud au VIe siècle, et le fameux comte Conomor assimilé au roi Marc de la Cornouailles britannique (Marcus Cunomorus).

Entre 815 et 839, Egbert annexe le royaume breton de Cornouaille.

La Cornouaille armoricaine est mentionnée pour la première fois et indirectement entre 852 et 857 quand « l'évêque de Saint-Corentin », Anaweten, est qualifié de Cornugallensis (adj. latin dérivé de Cornugallia).

L'existence d'une commune d'Anjou dénommée « La Cornuaille » a suscité une hypothèse qui en ferait une appellation géographique ou militaire couvrant toute la Bretagne du Sud et faisant pendant à la Domnonée sur le rivage Nord au VIe siècle ou VIIe siècle.

Formation de la Bretagne

Au IXe siècle, il semble que le nom de Poher (pour Pou-Caer = Pays de la Ville ou Pays du Château ou Pays de Carhaix) se soit substitué à celui de Cornouaille. Par la suite, il fut réservé à la vallée de l'Aulne, dont la capitale était Carhaix.

À la fin du IXe siècle, le comté féodal de Cornouaille reprend le nom de l'ancien royaume. Sa dynastie accède au trône ducal, il passa à l'évêque de Quimper qui devient comte-évêque de Cornouaille jusqu'au XIe siècle où deux frères s'en répartissent les dignités.

La Cornouaille de nos jours

Composée de 218 communes (sur la base des communes actuelles), la Cornouaille comptait - au dernier recensement de 1999 - 456 307 habitants pour une superficie totale de 5 979 km².

Le nom a été repris officiellement en 2001 pour sa partie au sud d'une ligne Châteaulin-Scaër pour la circonscription de programmation « Pays de Cornouaille » composée de 112 communes (loi Voynet, 1999)

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