The Arteara rock avalanche is developed in the Fataga Group which is related to the first volcanic stage in the Gran Canaria Island (8.6–13.3 Ma). The materials of the avalanche are mainly phonolitic ignimbrites and lava flows. We have investigated the geotechnical quality of the five lithotypes distinguished in the area: (a) phonolitic lava, (b) phonolitic agglomerate breccia, (c) reddish non-welded ignimbrite, (d) welded fiamme-bearing ignimbrite, and (e) pumice tuff with lithics. The weak geotechnical properties of the reddish non-welded ignimbrite, the pumice tuff with lithics and the agglomerate breccia, and their location at the middle of the slope suggest that these lithotypes can be regarded as potential sliding surfaces of the aval...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...
The Roque Nublo non-welded, lithic rich, ignimbrites are the most characteristic deposits of the sec...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...
In Arteara (Canary Island), a Holocene rock avalanche comprises accumulation of large reddish blocks...
The geological and geomechanical characterizations of the volcanic rock mass succession affected by ...
We studied a large debris-avalanche deposit of Pleistocene age in the Tenteniguada Basin, Gran Canar...
The island of Gran Canaria (Canary Islands, Spain) is characterized by a large variability of volcan...
Large landslides are common processes during the evolution of volcanoes and individual events can ex...
This work provides geological observations that support the existence of several large rock slides i...
A detailed morphometric analysis was performed on the 24 Holocene eruptions of Gran Canaria, a nearl...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...
The Roque Nublo non-welded, lithic rich, ignimbrites are the most characteristic deposits of the sec...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...
In Arteara (Canary Island), a Holocene rock avalanche comprises accumulation of large reddish blocks...
The geological and geomechanical characterizations of the volcanic rock mass succession affected by ...
We studied a large debris-avalanche deposit of Pleistocene age in the Tenteniguada Basin, Gran Canar...
The island of Gran Canaria (Canary Islands, Spain) is characterized by a large variability of volcan...
Large landslides are common processes during the evolution of volcanoes and individual events can ex...
This work provides geological observations that support the existence of several large rock slides i...
A detailed morphometric analysis was performed on the 24 Holocene eruptions of Gran Canaria, a nearl...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The huge volcanic debris avalanche occurred at 4.5Â ka is a major event in the evolution of the Coto...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...
The Roque Nublo non-welded, lithic rich, ignimbrites are the most characteristic deposits of the sec...
The volcanic stones, especially basalts, phonolites and tuffs, are the most common material used in ...