Examples of using Tectonic processes in English and their translations into Bulgarian
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Tectonic processes on Earth.
However, erosion can also affect tectonic processes.
Tectonic processes control rates and distributions of erosion at the Earth's surface.
If we get too warm, plate tectonic processes help us cool off.
Active tectonic processes, historical earthquakes, the degree of seismic activity in the region;
The earthquake is the tremors caused by tectonic processes occurring inside the Earth, this oscillation t….
Scientists believed the features might be deep cracks,caused by crustal rifting or tectonic processes.
According to recent research, the tectonic processes in this part of Bulgaria have a positive tendency.
Researchers have proposed the theory that the cause of the accumulation of oxygen steel tectonic processes, not biological.
It was formed as a result of turbulent tectonic processes on the floor of a sedimentary lake that existed here.
These tectonic processes played important role in the disappearance of the ancient continent known as Lemuria to western scholars.
Scientists believe the Alps reached their greatest heights millions of years ago andthat they're no longer growing as a result of tectonic processes.
It seems that these tectonic processes are not yet completed because the control of“PST Group” has not changed.
Around 3 billion years ago, cooling of the mantle allowed much larger plates to form andthis set in motion plate tectonic processes that disperse and reassemble continental masses.
They can form from tectonic processes such as continental collisions, which cause horizontal pressure, friction and distortion.
An international study led by researchers at Macquarie University has uncovered the ways in which giant meteorite impacts may have helped to kick-start our planet's global tectonic processes and magnetic field.
They can be formed by tectonic processes such as continental collisions which cause horizontal pressure, friction and distortion.
They have been little affected by tectonic events following the end of the Precambrian, and are relatively flat regions where mountain building,faulting, and other tectonic processes are greatly diminished compared with the activity that occurs at the margins of the shields and the boundaries between tectonic plates.
Because tectonic processes are driven by gradients in the stress field developed in the crust, this unloading can in turn cause tectonic or isostatic uplift in the region.
They can be originally emplaced in a horizontal orientation, although tectonic processes may cause subsequent rotation of horizontal sills into near vertical orientations.
The tectonic processes that took place at the beginning of the Paleoproterozoic era(about 2.4 billion years ago) led to the appearance of supercratons- large temporal geological structures consisting of ancient platforms(cratons).
The granite rocks, called Precariously Balanced Rocks, or PBRs,form when tectonic processes allow a big chunk of rock, tattooed with patterns of fractures, to ascend from beneath the surface of the Earth.
But during intensive tectonic processes such as orogenesis, metamorphism, emergences and erosion of the land, these contrasting elements found each other and crystallised out to make one of our most beautiful gemstones.
The formation of an orogen can be accomplished by the tectonic processes such as oceanic subduction(where a continent rides forcefully over an oceanic plate for accretionary orogeny) or continental subduction convergence of two or more continents for collisional orogeny.
By and large, what the world is facing today is a systemic crisis, a tectonic process of global transformation.
Tectonic landforms are created primarily by processes contributing to the rising and falling of the earth's crust.
Is novel, however, as it highlights the potential of caves and their deposits to quantitatively constrain mountain evolution on a timescale of millions of years andfurther shows how the interplay of tectonic and climatic processes can be understood.
Mountain ranges are in a constant interplay between climatically controlled weathering processes on the one hand and the tectonic forces that cause folding and thrusting and thus thickening of the Earth's crust on the other hand.
Beginning of the Mesozoic era coincided with the end of varistsiyskih orogenic processes of, it ended with the beginning of the last powerful tectonic revolution- Alpine folding.
The processes of physical and chemical weathering have led to the formation of an entrance a widened tectonic fissure in the base of which there are several small terraces.
