Sentence examples for edifice surface from inspiring English sources

Exact(1)

As a mere example, decreasing of the equivalent thermal resistance Rb applied to a small edifice (surface ~ 150 m2, for which ~ 200 linear meters of borehole are needed) can entail a total borehole length reduction on the order of 30 40 m (ca. 15 20%).

Similar(59)

A second later, he pushes off from the building, flying off the window's surface, rounding the corner of that huge edifice — whoosh!

Taken all together, these data support the suggestion that porous ZnS edifices, when formed at the UV-irradiated surface of primordial Earth, could photoreduce CO2 and other chemical compounds.

When magma approaches the ground surface, the temperature of the volcanic edifice increases by hot volcanic fluid being exsolved from the magma or by the heat of the magma itself.

Other examples observed in Japan are shown in Sasaki et al. (2016); further, the 1980 eruption of Mt. St. Helens (Brantley and Myers 2000) and the 1926 eruption of Tokachi-dake (Uesawa 2014) indicate significant contributions of water from the edifice to lahar generation, even though water from the surface glacier and snow also contributed.

"Much like the hotly anticipated Apple HQ, the Central & Wolfe project will replace an unsightly set of sprawling cookie-cutter buildings and their surface parking lots with a curvy modern edifice surrounded by greenery". The campus will consist of three main buildings with four floors each.

One concludes that Russians think not in terms of consent and opportunity, but of empires and enforced unions with barely suppressed discontents roiling just beneath the surface that any moment can threaten the entire edifice.

The geophysical observations collected in volcanic areas are the surface expressions of processes that occur deeply within the volcanic edifice.

These ZnS edifices should have been accessible to solar UV radiation at the surface of continents and in shallow waters surrounding them (see Fig. 1).

Earthquake surface ruptures appeared along these faults and on the Aso volcanic edifice, which in turn generated landslides.

Surtla's phreatomagmatic jets breached the ocean surface from less than a metre's depth (Fig. 1C 2, but the edifice was never observed above water, and its activity had ceased by 6 January 1964.

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