We use a kinematic GPS and laser range finder survey of a 200 m-long section of the Muliwai a Pele lava channel (Mauna Ulu, Kilauea) to examine the construction processes and flow dynamics responsible for the channel–levee structure. The levees comprise three packages. The basal package comprises an 80–150 m wide ′a′a flow in which a ∼2 m deep and ∼11 m wide channel became centred. This is capped by a second package of thin (<45 cm thick) sheets of pahoehoe extending no more than 50 m from the channel. The upper-most package comprises localised ′a′a overflows. The channel itself contains two blockages located 130 m apart and composed of levee chunks veneered with overflow lava. The channel was emplaced over 50 h, spanning 30 May–2 June, 197...
We present the evolution over 3 months of a 2016–2017 pāhoehoe flow at Kīlauea as it changed from a ...
Etna’s 2001 basaltic lava flow provided a good example of the distal flow segment between the flow f...
co-auteur étrangerInternational audienceIn this study, we examine the channel-fed ‘a‘ā lava flow sys...
We use a kinematic GPS and laser range finder survey of a 200 m-long section of the Muliwai a Pele l...
Channelized lava flows are commonly produced during the early stages of basaltic eruptions. These ch...
Lava flows are common at volcanoes around the world and on other terrestrial planets, but their beha...
During long-lived basaltic eruptions, overflows from lava channels and breaching of channel levées a...
An open channel lava flow on Mt. Etna (Sicily) was observed during May 30–31, 2001. Data collected ...
International audienceThe stabilized channel is a crucial element of an `a`ā flow system, delivering...
International audienceThe Muliwai a Pele lava channel was emplaced during the final stage of Mauna U...
The evolution of lava flows emplaced on Mount Etna (Italy) in September 2004 is examined in detail t...
Factors which control lava flow length are still not fully understood. The assumption that flow leng...
We present the evolution over 3 months of a 2016–2017 pāhoehoe flow at Kīlauea as it changed from a ...
Etna’s 2001 basaltic lava flow provided a good example of the distal flow segment between the flow f...
co-auteur étrangerInternational audienceIn this study, we examine the channel-fed ‘a‘ā lava flow sys...
We use a kinematic GPS and laser range finder survey of a 200 m-long section of the Muliwai a Pele l...
Channelized lava flows are commonly produced during the early stages of basaltic eruptions. These ch...
Lava flows are common at volcanoes around the world and on other terrestrial planets, but their beha...
During long-lived basaltic eruptions, overflows from lava channels and breaching of channel levées a...
An open channel lava flow on Mt. Etna (Sicily) was observed during May 30–31, 2001. Data collected ...
International audienceThe stabilized channel is a crucial element of an `a`ā flow system, delivering...
International audienceThe Muliwai a Pele lava channel was emplaced during the final stage of Mauna U...
The evolution of lava flows emplaced on Mount Etna (Italy) in September 2004 is examined in detail t...
Factors which control lava flow length are still not fully understood. The assumption that flow leng...
We present the evolution over 3 months of a 2016–2017 pāhoehoe flow at Kīlauea as it changed from a ...
Etna’s 2001 basaltic lava flow provided a good example of the distal flow segment between the flow f...
co-auteur étrangerInternational audienceIn this study, we examine the channel-fed ‘a‘ā lava flow sys...