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10 Sentences With "areally"

How to use areally in a sentence? Find typical usage patterns (collocations)/phrases/context for "areally" and check conjugation/comparative form for "areally". Mastering all the usages of "areally" from sentence examples published by news publications.

THEIR MORTGAGE PRACTICESWERE LESS DECEPTIVE, THEY HAD LESS FAILURE, THEY WERE GENERALLY THOUGHT OF AS AREALLY RESPONSIBLE BANK.
The definite article spread areally among the Central Semitic languages and it would seem that Proto-Arabic lacked any overt marking of definiteness.
The Arctic is likely to be especially affected by climate change because of the high projected rate of regional warming and associated impacts. Temperature projections for the Arctic region were assessed by Anisimov et al. (2007). These suggested areally averaged warming of about 2 °C to 9 °C by the year 2100. The range reflects different projections made by different climate models, run with different forcing scenarios.
"The Gorans, who are also Muslim, have a separate identity. The Goran dialects used to be classed with Serbian, but have more recently been assigned to Macedonian, and Gorans themselves recognize that their dialects are closer to Macedonian than to Serbian." Gorani speech has numerous loan words, being greatly influenced by Turkish and Arabic due to the influence of Islam, as well as Albanian areally.
The mineralizing fluids are conducted upwards within sedimentary units toward basin-bounding faults. The fluids move upwards due to thermal ascent and pressure of the underlying reservoir. Faults which host the hydrothermal flow can show evidence of this flow due to development of massive sulfide veins, hydrothermal breccias, quartz and carbonate veining and pervasive ankerite- siderite-chlorite-sericite alteration. Fluids eventually discharge onto the seafloor, forming areally extensive, stratiform deposits of chemical precipitates.
The oldest material and features in the Victoria quadrangle are the intercrater plains material and areally associated, severely degraded basins. No craters are clearly older than intercrater plains material, and the relative ages of the cl basins are ambiguous. Numerous large craters are superposed on intercrater plains material; by analogy with lunar and martian history these craters most likely date from more than about 4 b.y. ago. The available evidence suggests a relatively long history of plains formation.
On the other hand, contamination from nonpoint sources, such as agricultural activities, may be areally extensive with minimal effect on the use of the groundwater for drinking-water supply or other purposes. Point-source prevention programs are almost entirely established as regulatory programs and are administered primarily by ADEQ. Most nonpoint sources are related to agriculture and other land-use activities and commonly are addressed by joint efforts of several agencies, with lead oversight relegated to the ANRC. Despite the threat to groundwater resources, no Federal or State statute comprehensively addresses groundwater protection.
For superposition, the grid generated for the subsurface domain is mirrored areally for the surface flow nodes, with surface flow node elevations corresponding to the top elevation of the topmost active layer of the subsurface grid. Note that surface flow node elevations may vary substantially to conform with topography. However, the assumptions of small slope inherent in the diffusion-wave equation will not allow for modeling of inertial effects. The discretized surface equation is coupled with the 3-D subsurface flow equation via superposition (common node approach) or via leakage through a surficial skin layer (dual node approach).
The Lower Floridan aquifer is generally less permeable than the Upper Floridan aquifer and the water produced can be highly mineralized and/or saline; however, the Lower Floridan aquifer is relatively fresh water to the base of the system in central Florida and in updip areas of central and southern Georgia and Alabama. A new basal permeable zone is mapped throughout the Florida peninsula, and slightly into southeastern Georgia, that incorporates the previously established Boulder Zone and Fernandina permeable zone; this more extensive unit is called the Oldsmar permeable zone. The Oldsmar permeable zone appears to have higher permeability, far greater than the cavernous areas of the Boulder and Fernandina permeable zones, and contains freshwater in the central peninsula area. This newly delineated areally extensive basal unit containing freshwater may influence the movement of freshwater water through the deepest part of the aquifer system toward the discharge areas.
It is famous for being the highly-resistant mostly-horizontal unit above the 1,000 my (1 by), Great Unconformity expressed areally in the Grand Canyon of Arizona; also in other areas of Arizona and adjacent Nevada. The Tapeats Sandstone is the highly erosion-resistant unit laid upon the Vishnu Basement Rocks in the central, parts of east, and parts of west Grand Canyon, Arizona. The unit comprises the 'base horizontal unit' of the platform around Granite Gorge (Inner Gorge) on the Colorado River, and because of its hardness, creates the Tonto Platform upon which the slope-forming, Bright Angel Shale, (extensive, and distinctively soft drab-greenish), and above it low cliff-forming cliff of Muav Limestone lie. The Tapeats Sandstone and the Tonto Platform follow the Colorado River, and surrounding tributary canyons, creeks, watercourses, or washes, in a dendritic fashion, much like the branches of a tree.

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