How to use in-sentence of “tectonic”:
– This means that there are two tectonic plates that come together underneath the city.
– Volcanoes are usually not found where two tectonic plates slide past one another.
– Hotspots may be far from tectonic plate boundaries.
– It takes place when two tectonic plates come together.
– The island was formed by two tectonic plates meeting and forcing each other upwards.
– A mid-ocean ridge marks the boundary between two tectonic plates which are moving apart.
Example sentences of “tectonic”:
– Ophiolites have always played a central role in plate tectonic theory and the interpretation of ancient mountain belts.
– Because the Pacific plate is the largest of all the tectonic plates on Earth, crustal material at its western edge has had up to 170 million years to compact and become very dense; hence its great height-difference relative to the higher-riding Mariana Plate, at the point where the Pacific Plate crust is subducted.
– The Pacific plate is a tectonic plate beneath parts of the Pacific Ocean.
– The island was formed mainly by tectonic uplift during the early AlpsAlpine orogeny towards the end of the Cretaceous.
– Mandalay is on a tectonic fault.
– Some geographygeographers say Eurasia is one continent, because Europe and Asia are mostly on the same tectonic plate and do not have a sea between them.
– The sudden release of tension in the tectonic plates sends waves of energy that travel through the Earth.
– The African Great Lakes are a series of lakes formed by the action of the tectonic East African Rift on the continent of Africa.
– The ridge runs directly through the populated Reykjavik and Thingvellir historic areas, and the tectonic activity of these plates separating is the source of the abundant geothermal energy in the region.
- Ophiolites have always played a central role in plate tectonic theory and the interpretation of ancient mountain belts.
- Because the Pacific plate is the largest of all the tectonic plates on Earth, crustal material at its western edge has had up to 170 million years to compact and become very dense; hence its great height-difference relative to the higher-riding Mariana Plate, at the point where the Pacific Plate crust is subducted.
– Horizontal tectonic movements such as the collision of continents create orogenic belts.
– The South American plate is a major tectonic plate which includes the continent of South America.
– This high level of endemism is explained by the continent’s long geographic isolation and its tectonic stability.
– Volcanoes are made when two tectonic plates come together.
– It is an assembly of smaller tectonic plates which merged early in the Archaean era.
– At first the crust was very thin, and was probably changed often as the tectonic plates shifted around a lot more than they do now.
More in-sentence examples of “tectonic”:
– The lithosphere is divided into tectonic plates, which move gradually relative to one another.
– Terrestrial planets can have canyons, Impact cratercraters, mountains, volcanoes, and other surface structures, depending on the presence of water and tectonic activity.
– The Molucca Sea Plate, the tectonic plate named after the sea, goes further north.
– This is a list of the biggest tectonic plates on Earth.
– The correct technical name is Tectonic Pit, due to the presence of a fault along the foot of the Central Volcanic Sierra, which is evidenced by the existence of thermo-mineral sources.
– The Earth’s crust has 17 major, rigid tectonic plates.
– The North American plate is a large tectonic plate.
– A lot of earthquakes happen on tectonic faults.
– The orbit is not circular, and this sets up the stresses which cause the tectonic activity.
– In geology, a rift is caused by tectonic plates in the Earth’s lithosphere moving apart.
– The volcanos were caused by the Pacific oceanic tectonic plate moving over a hotspot.
– The Variscan collage and orogeny and the tectonic definition of the Armorica microplate: a review.
– Although it forms under the surface of the Earth, there are many places where it has been forced upwards by tectonic movement.
– Implications of plate tectonics for the Cenozoic tectonic evolution of western North America.
– The Malay Archipelago is the place where two large tectonic plates meet, and is an area where orogeny and volcanoes are common.
– It is the Earth’s second largest tectonic plate, behind the Pacific Plate.
– Recently, two of these sunken islands were found to the west of Perth, Western Australia.Sunken islands could cause tectonic shift in Gondwana story.
– The rocks in the Rocky Mountains were formed before the mountains were raised by tectonic forces.
– A number of tectonic plates began to slide under the North American plate.
– The crustal portions of oceanic tectonic plates are made mostly of basalt, produced from upwelling mantle below mid-ocean ridges.
– They formed because of the collision between the Australian and the Asian tectonic plates.
– At the point where two tectonic plates collide, the Lesser Sunda Islands are some of the most geologically complex and active regions in the world.
– The African Plate is a major tectonic plate.
– Wind and water can create sediment from rocks, and movement of one tectonic plate against another creates enormous heat and pressure which affects rocks greatly.
– The lake was formed as a result of tectonic activity and is the largest freshwater lake in Asia.
– Since then, further tectonic activity and erosion by glaciers has sculpted the Rockies into dramatic peaks and valleys.
– One theory is that these bands suggest plate tectonicsplate tectonic activity on Mars four billion years ago, before the planetary dynamo stopped working and the planet’s magnetic field faded.
– Rocks of the Lewisian complex were caught up in the Caledonian orogeny, appearing in the hanging walls of many of the thrust Fault faults formed during the late stages of this tectonic event.
– Around 40 million years ago, the Indo-Australian PlateIndo-Australian tectonic plate began to split apart from the ancient supercontinent Gondwana.
– They happen when two tectonic plates shift underground.
– Iceland, though considered to be a European country, sits partly in North America since it straddles the Mid-Atlantic Ridge which marks the boundary between the Eurasian and North American tectonic plates.
– These volcanoes are the result of subduction of the Juan de Fuca tectonic plate: the plates meet just seaward of the west coast of Vancouver Island.
– They are almost all near or in continental Rift rift-related tectonic settings.
– Tuzo Wilson suggested in 1963 that volcanic chains like the Hawaiian Islands result from the slow movement of a tectonic plate across a fixed hot spot deep beneath the surface of the planet.
– The Western half sits in North America, while the Eastern half sits on the European tectonic plate.
– The bend shows how a tectonic plate can shift direction suddenly.
– Fold mountains are formed when two tectonic plates move together.
– Iceland sits on the European – North American tectonic plates.
– Fluvial terrace is divided into Rock terrace and Gravel terrace according to structure materials, and it is also classified as Tectonic terrace and Climate terrace according to causes of formation.
– There are two types of tectonic plates: oceanic and continental.
– An island on lake is the most eastern tectonic part of Finland and the European Union.
– This marks the subduction of the African tectonic plate underneath the Aegean part of the Eurasian tectonic plate, at a rate of up to 5cm per year in a northeasterly direction.
– The park is in an area with a lot of tectonic activity.
– After surviving cycles of merging and rifting of continents, cratons are usually found in the interiors of tectonic plates.
– When large tectonic plates collided about 100 million years, magma escaped between these plates and solidified between other rocks.
– Geologically, they are on the same tectonic plate.
– Seafloor spreading happens at the bottom of an ocean as tectonic plates move apart.
- The lithosphere is divided into tectonic plates, which move gradually relative to one another.
- Terrestrial planets can have canyons, Impact cratercraters, mountains, volcanoes, and other surface structures, depending on the presence of water and tectonic activity.