funwithfire:

Cliff exposure of the distral fringe of the Devonian clastic wedge on the north coast of Banks Island, Canadian Arctic.

funwithfire:

Cliff exposure of the distral fringe of the Devonian clastic wedge on the north coast of Banks Island, Canadian Arctic.

kateoplis:

Scorched Earth by Michael Wells

kateoplis:

Scorched Earth by Michael Wells

L’encavalcament de Vallfogona vol marxa!

Un terratrèmol de 3,1  graus a l’escala de Richter es deixa sentir al Ripollès
Ensurt al Ripollès. Un sisme de 3,1 graus a l’escala de Richter s’ha sentit a la comarca. El terratrèmol ha tingut l’epicentre a cinc quilòmetres al nord de Ripoll i a 2.000 metres de profunditat. La tremolor s’ha notat a municipis com Sant Pau de Segúries, Vallfogona o Sant Joan de les Abadesses. De moment, no es té constància de danys materials ni personals.

L’encavalcament de Vallfogona vol marxa!

Un terratrèmol de 3,1 graus a l’escala de Richter es deixa sentir al Ripollès

Ensurt al Ripollès. Un sisme de 3,1 graus a l’escala de Richter s’ha sentit a la comarca. El terratrèmol ha tingut l’epicentre a cinc quilòmetres al nord de Ripoll i a 2.000 metres de profunditat. La tremolor s’ha notat a municipis com Sant Pau de Segúries, Vallfogona o Sant Joan de les Abadesses. De moment, no es té constància de danys materials ni personals.

Eu eu que flipo con Castellfollit de la Roca…
(via reddit)

Eu eu que flipo con Castellfollit de la Roca

(via reddit)

(via Bucknell University)

The 7.0 magnitude earthquake that rocked Haiti Tuesday afternoon registered hundreds of miles away at Bucknell University’s seismic station. According to Brad Jordan, lab director of geology, the quake was close to two major plate boundaries, the North American Plate and the Caribbean Plate.  “It appears that most of the energy was released in a side-to-side motion, which would not result in a large vertical displacement of the ocean water, which is likely the reason there was no significant tsunami associated with this quake,” said Jordan. Bucknell’s seismograph is located in the basement of the Carnegie Hall.

(via Bucknell University)

The 7.0 magnitude earthquake that rocked Haiti Tuesday afternoon registered hundreds of miles away at Bucknell University’s seismic station. According to Brad Jordan, lab director of geology, the quake was close to two major plate boundaries, the North American Plate and the Caribbean Plate.  “It appears that most of the energy was released in a side-to-side motion, which would not result in a large vertical displacement of the ocean water, which is likely the reason there was no significant tsunami associated with this quake,” said Jordan. Bucknell’s seismograph is located in the basement of the Carnegie Hall.

sojamo:

The geometry of geology
by Vincente Guallart, via BLDGBLOG, alvin

sojamo:

The geometry of geology

by Vincente Guallart, via BLDGBLOG, alvin