Sentence examples for most recent lava from inspiring English sources
Haleakala's most recent lava flow formed La Perouse Bay and the Ahihi-Kinau Natural Area Reserve, (808) 587-0063, in south Maui.
The lava domes in the younger stage are distributed in the region between the profile and the most recent lava dome, as shown in Fig. 3.
During these field campaigns, we also mapped the edges of the most recent lava flows and made measurements of lava flow thicknesses (Figs. 2, 3 and 4).
The results showed fish community structure strongly related to measured environmental variables, of which depth, width of the island shelf, age of the lava flow and distance to the most recent lava flow were the most influential.
The most recent lava flows from the flanks of Aragats include Tirinkatar, which is separated into two individual trachybasalt flows Tirinkatar-1 and Tirinkatar-2, and the Ashtarak lava flow.
It also proposed some hypotheses on the mechanisms of selection and speciation of endemic species of the southwestern Indian Ocean region, particularly diversified on the most recent lava flows of the Piton de la Fournaise, and provided a model of distribution of environmental and fish assemblage variables in four homogeneous patterns of colonization (landscapes) retained within the study area.
Considering the most recent lavas of the TSP complex, young Holocene dacites, Costa et al. (2004) constrained pre-eruptive conditions as 200 ± 50 MPa, 850 ± 10 °C, and 4.5 5.5 wt% H2O in the melt.
In the late 18th century Cinder Cone had its most recent eruption and lava flow.
The third and most recent eruption produced another lava flow that was largely erupted above glacial ice, but was probably constrained on its northern margin by a small glacier.
The most recent graft scandal — known as Operação Lava Jato, or Operation Car Wash — has proved even bigger, with billions of dollars in bribes directed to political parties from the national oil company, Petrobras.
Post-caldera lava domes, the most recent eruptive products of Akagi, are the most felsic but the most isotopically depleted (Kobayashi and Nakamura 2001), suggesting that production of mantle-derived magmas decreased, and they no longer interacted with crustal materials.
