Baixem o Destinator 9 em: http://www.gpspoint.com.br/index.php/igo/42-destinator/60-destinatordescompacte e coloque a pasta Destinator no cartao de memoria.Apos baixado o Destinator 9, basta copiar este arquivo, e colar por cima do que ja esta no cartao de memoria do GPShttp://www.megaupload.com/?d=XY3Q8CJMso nao esquecam de colocar o Destinator no cartao tambem srsrsrOBS: e normal o Destinator ficar com alguns bug's de cores ou ate mesmo de BMP, pois narealidade, ele e feito para rodar em WIN CE 5.0mais o mapa e a navegacao fica normal ( um pouco lerdo apenas ) Bem... vamos la.copiem o LK8000 e coloquem em seu cartao de memoria ( apos descompacta-lo ) http://parapente-arrabida.blogspot.com/2009/10/lk8000-112b.htmlDepois copie no novo menu.. ( copie, descompacte e cola em sima do existente )http://www.megaupload.com/?d=KECW5G2Hretire os arquivos executaveis do LK8000 excepto os que tem informacao de PNA ( ficarao apenas 2 )O = LK8000-PNA.exe e o LK8000SIM.exe.Reinicie o GPS.Abra o LK8000 e siga as intrucoes de configuracao de porta.pressionar no planador ou no parapente no canto inferior direito, pressionar duas vezes em Config > Setup System> em Device A e B por a seguinte configuracao: GENERIC, PORT: COM1, 57600.Porem, o meu esta funcionando na COM7.... veja qual porta o seu vai funcionar e bons voos. During a volcanic eruption, lava, tephra (ash, lapilli, volcanic bombs and blocks), and various gases are expelled from a volcanic vent or fissure. Several types of volcanic eruptions have been distinguished by volcanologists. These are often named after famous volcanoes where that type of behavior has been observed. Some volcanoes may exhibit only one characteristic type of eruption during a period of activity, while others may display an entire sequence of types all in one eruptive series.There are three different metatypes of eruptions. The most well-observed are magmatic eruptions, which involve the decompression of gas within magma that propels it forward. Phreatomagmatic eruptions are another type of volcanic eruption, driven by the compression of gas within magma, the direct opposite of the process powering magmatic activity. The last eruptive metatype is thePhreatic eruption, which is driven by the superheating of steam via contact with magma; these eruptive types often exhibit no magmatic release, instead causing the granulation of existing rock.Volcanic eruptions arise through three main mechanisms:Within these wide-defining eruptive types are several subtypes. The weakest are Hawaiian andsubmarine, then Strombolian, followed by Vulcanian and Surtseyan. The stronger eruptive types are Pelean eruptions, followed by Plinian eruptions; the strongest eruptions are called "Ultra Plinian." Subglacial and Phreatic eruptions are defined by their eruptive mechanism, and vary in strength. An important measure of eruptive strength is Volcanic Explosivity Index (VEI), magnitud scale ranging from 0 to 8 that often correlates to eruptive types. Loose snow avalanches an avalanche formed in snow with little internal cohesion among individual snow crystals. Usually very few fatalities occur from loose snow avalanches, as the avalanches have a tendency to break beneath the person and are usually small even having a path as small as a few centimeters, and as a result are sometimes called "harmless sloughs" that usually at most cause the person to merely fall. However based on the terrain