Sentence examples for intermediate rock from inspiring English sources

Ten novices in rock climbing and five intermediate rock climbers were observed climbing an icefall.

Epidote is a hydroxylated Ca-Al-silicate commonly observed in a variety of high-pressure rocks, from basaltic eclogites, to metagabbros and rodingites of the metamorphosed oceanic crust, then to intermediate rock compositions representative of slices of the continental crust involved in high-pressure processes at subduction zones.

Felsic rocks are commonly oversaturated and contain free quartz (SiO2), intermediate rocks contain little or no quartz or feldspathoids (undersaturated minerals), and mafic rocks may contain abundant feldspathoids.

The early-stage intermediate rocks have relatively high MgO contents (2.71 to 4.84%) and Mg# values (46 to 60), but low Sr/Y and LaN/YbN ratios, which were likely derived from a hybrid mantle metasomatized by melts from foundered eclogitic lower continental crust and subsequent fractional crystallization.

The Matterhorn can be scaled with intermediate rock-climbing skills, but Kathy warned that if unexpected bad weather blows up, it tends to come from the back, or Italian, side.

The high-activity clays are predominantly smectitic on basic and intermediate rocks, e.g. basalt and andesite, and vermiculitic on more siliceous rocks such as granite, gneiss and schist.

Zircons of an Ivisârtoq supracrustal belt ∼3075 Ma intermediate volcanic rock have initial ɛHf values of +2 to +5 thus are juvenile crustal additions.

Association of acidic (rhyolite) and intermediate (trachyte) rock, often considered differentiates of the Deccan trap basaltic magma.

At intermediate elevations, rock fall protection declines slightly by 2080 in the scenarios based on more severe climate change, such as Growth and convergence (A1) and Regional centers (A2) which is illustrated by the aggregated indicator in Figure 4. Figure 5 Spatially explicit provision of rock fall protection.

In contrast, soils stemming from ultrabasic, basic and intermediate igneous rocks and sandstones show no significant correlation.

Sanidine (alkali feldspar) is a common high temperature mineral and often dominates the phenocryst assemblage in silicic to intermediate volcanic rocks.