Al principio esta es la primera toma pensaba  
que era bomba del volcán ....

Luego pensé si que va lejos y aquí dio media vuelta cambiando el sentido

pero llevo dias sin leer nada de rios de lava de ahi mi sospecha que se este llenando el crater.de todas formas esa lava que se ve ahora por la webcam parece bastante liquida o esa impresion me da a mi

Cita de: Caminero en Miércoles 28 Abril 2010 00:47:51 AM
Que va El_Buho... sigue sobrevolando el volcan... no sé que será pero tiene mucha velocidad y maniobrabilidad... quizás sea un caza??? no sé pero ahí sigue

Aquí otra vista desde otra cam 5 minutos despues

Si mirais esta imagen de esta web cam en directo,fijaros bien en las luces que se ven mas al fondolas casas o lo que sea, pues bien, yo obsevo este volcan desde que entro en erupcion y los primeros dias,las luces de lava que se veian por la noche eran perpendiculares a las luces del fondo que nombre anteriormente,y aora si os fijais la lava sale mas a la izquierda de la imagen???
http://eldgos.mila.is/eyjafjallajokull-fra-thorolfsfelli/

otra mas aquí parada un ratito, claro que con el refresco de la camara

Son bombas de lava.

pues yo diria que es un ODFNI 

No enserio yo e estado presente cuando ocurría y a mi parecer son bombas ya que salían del cráter, lo malo que no capture esa imagen 

Curiosamente el Instituto de Ciencias de la Tierra hoy no han publicado el resumen de ayer y que posteo cada día.

Current events
Assessment - 27 April 2010 22:40

Overall assessment: Plume elevations and magma discharge levels remain similar to the preceding four days of activity. Lava continues to flow north from the eruption site toward the head of the Gígjökull glacier. Despite light ash-fall occurring up to 45 km west of the eruption site, today's explosive activity and ash production represents a fraction of conditions during the height of the eruption (14?17 April). There are no measurable indications that the eruption is about to end.

Seismic tremor: Intensity comparable to the preceding four days of eruptive activity.Earthquakes: No locatable seismicity has been recorded today beneath Eyjafjallajökull.

GPS deformation: Horizontal displacement towards the centre of the volcano, in addition to vertical subsidence. These observations are consistent with deflation of a magma reservoir beneath Eyjafjallajökull.

Magma flow: No measurements possible today; however, the intensity of the eruption suggests that the discharge level is similar to the preceding four days (i.e. 20?40 tonnes s?1).

Meltwater: Continuing discharge of water from Gígjökull due to ice-melt at the eruption site. Discharge at the old Markarfljót bridge, 18 km from Gígjökull, is estimated at ~100 m3 s?1, of which ~30 m3 s?1 is baseflow.

Other remarks: No measurable geophysical changes within the Katla volcano.

Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; information from local police; and aerial observations over the eruption site.

The above is based on status report issued collectively by IMO and the Institute of Earth Sciences at 19:00 this evening.

por cierto..
os presento al eyjafjalla:

Como veis.. esta poniendo mala cara....















Y ESTAS de ayer:

Cita de: Sondebueu en Miércoles 28 Abril 2010 08:04:40 AM
Current events
Assessment - 27 April 2010 22:40

Overall assessment: Plume elevations and magma discharge levels remain similar to the preceding four days of activity. Lava continues to flow north from the eruption site toward the head of the Gígjökull glacier. Despite light ash-fall occurring up to 45 km west of the eruption site, today's explosive activity and ash production represents a fraction of conditions during the height of the eruption (14?17 April). There are no measurable indications that the eruption is about to end.

Seismic tremor: Intensity comparable to the preceding four days of eruptive activity.Earthquakes: No locatable seismicity has been recorded today beneath Eyjafjallajökull.

GPS deformation: Horizontal displacement towards the centre of the volcano, in addition to vertical subsidence. These observations are consistent with deflation of a magma reservoir beneath Eyjafjallajökull.

Magma flow: No measurements possible today; however, the intensity of the eruption suggests that the discharge level is similar to the preceding four days (i.e. 20?40 tonnes s?1).

Meltwater: Continuing discharge of water from Gígjökull due to ice-melt at the eruption site. Discharge at the old Markarfljót bridge, 18 km from Gígjökull, is estimated at ~100 m3 s?1, of which ~30 m3 s?1 is baseflow.

Other remarks: No measurable geophysical changes within the Katla volcano.

Based on: IMO seismic monitoring; IES-IMO GPS monitoring; IMO river gauges; information from local police; and aerial observations over the eruption site.

The above is based on status report issued collectively by IMO and the Institute of Earth Sciences at 19:00 this evening.

por cierto..
os presento al eyjafjalla:

Hola, buenos días

Puedes pasarnos el enlace de esa información. Muchas gracias.

Por cierto, a los interesados: os comento un poco la última predicción en este enlace.

Buenas 

Vuelven a subir bastante los tremores de las estaciones GOD y HVO. Bastante además en esta última 

Tremores

La webcam muestra hoy toda la cima blanca de nuevo  y la columna de ceniza parece diferente , parece como que sale de más atrás 

WEBCAM


La webcam del "Katla" no sé que muestra CAM Katla   Cenizas del "Eyfjafja" , que esté nevando... 

Pongo la animación del enlace de Vigi



Como comenté ayer vamos a volver a tener problemas con el tráfico aéreo.