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Convergent boundaries are responsible for creating mountain ranges. When two tectonic plates collide, the land is forced upwards, creating intense pressure that results in the formation of mountain ranges. Examples of mountain ranges formed by convergent boundaries include the Himalayas and the Andes.

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Divergent boundaries form ocean ridges.

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Divergent boundaries are tectonic plate boundaries where two plates move away from each other. This movement results in the upwelling of magma from the mantle, creating new crust. Divergent boundaries are typically found along mid-ocean ridges.

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Both divergent boundaries and transform boundaries involve horizontal movement of Earth's tectonic plates. At divergent boundaries, plates move apart, creating new crust, while at transform boundaries, plates slide horizontally past each other. Both types of boundaries contribute to the overall movement and rearrangement of Earth's lithosphere.

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Both divergent and transform boundaries involve the movement of tectonic plates, but in different ways. At divergent boundaries, plates move away from each other, creating new crust as magma rises to the surface. At transform boundaries, plates slide past each other horizontally, without creating or destroying crust. Both types of boundaries contribute to the overall movement of Earth's tectonic plates.

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Hot spots are not directly associated with plate boundaries. Hot spots are areas of intense volcanic activity that are thought to be caused by mantle plumes rising from deep within the Earth's mantle, creating a hotspot of magma beneath the Earth's crust. These hotspots can occur in the middle of a tectonic plate and are responsible for creating volcanic island chains, such as the Hawaiian Islands.

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  1. Convergent plate boundaries: Where two tectonic plates collide, one plate is forced beneath the other, creating intense heat and pressure that leads to volcanic activity.
  2. Divergent plate boundaries: Where two tectonic plates move apart, magma rises to fill the gap, creating new volcanic activity along the boundary.
  3. Hot spots: Areas where magma plumes rise from deep within the mantle, creating isolated volcanic activity away from tectonic plate boundaries, such as the Hawaiian Islands.

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The margin of a continent is determined by the location of its tectonic plate boundaries. Convergent boundaries create subduction zones or mountain ranges, while divergent boundaries form rift valleys or mid-ocean ridges along the margins. Transform boundaries can also influence the shape of a continent's margin by creating strike-slip faults.

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Geographical boundaries of a watershed can be identified by tracing the high points or ridgelines surrounding a particular area. Water within these boundaries will flow towards a common outlet, such as a river or lake, creating a distinct drainage basin. Maps and topographical features can help determine the boundaries of a watershed.

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The motto of White Violet Center for Eco-Justice is 'Breaking boundaries, creating hope.'.

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Sisters of Providence of Saint Mary-of-the-Woods's motto is 'Breaking boundaries, creating hope.'.

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Divergent boundaries are areas where continental or oceanic plates are moving away from each other and creating new crust. Examples would be the Mid-Oceanic Ridge and the East African Rift Zone.

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The process that occurs at convergent boundaries is called subduction. This is when one tectonic plate moves under another, creating deep ocean trenches and often leading to volcanic activity and earthquakes.

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Tall mountains form at converging boundaries because the tectonic plates collide and push against each other, causing the crust to fold and uplift. At diverging boundaries, mountains can form due to the upwelling of magma creating volcanic mountain ranges. In contrast, at sliding boundaries (transform boundaries), the plates slide past each other horizontally, leading to earthquakes but not significant mountain building.

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Volcanoes are often located at plate boundaries due to the movement and interaction of tectonic plates. At convergent boundaries, one plate is forced beneath another in a process called subduction, leading to the formation of volcanic arcs. At divergent boundaries, magma rises to the surface, creating new crust and volcanic activity. Transform boundaries can also have volcanic activity associated with them, although it is less common.

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Different landforms result at convergent boundaries because the tectonic plates are colliding, causing one plate to be pushed beneath the other (subduction) or creating mountains. Divergent boundaries result in landforms like rift valleys and mid-ocean ridges because the plates are separating, allowing magma to rise and create new crust.

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The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.

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Mountains are typically formed by tectonic plate movements, where one plate is pushed up over another, creating uplifted landforms. The boundaries where tectonic plates meet, such as convergent or collision boundaries, often lead to the formation of mountain ranges through processes like folding, faulting, and volcanic activity. These boundaries can also experience intense seismic activity, leading to the further formation and growth of mountains over time.

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Yes, earthquakes and volcanoes commonly occur at plate boundaries due to the movement and interaction of tectonic plates. At convergent boundaries, one plate is forced below the other, leading to earthquakes and volcanic activity. At divergent boundaries, plates move apart, creating fissures where magma can rise to the surface. Transform boundaries, where plates slide past each other, can also produce earthquakes.

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Convergent boundaries can impact the biosphere by creating volcanic arcs and mountain ranges, which can change local climates and habitats for plants and animals. On the other hand, convergent boundaries can also affect the atmosphere by releasing gases and ash during volcanic eruptions, which can impact air quality and climate patterns.

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At diverging plate boundaries, new oceanic crust forms through seafloor spreading. Magma rises to the surface and solidifies, creating mid-ocean ridges. As the plates move apart, they create new oceanic crust, which can lead to the formation of rift valleys.

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Fault Lines. A transform boundary connects two diverging boundaries, creating a fault line. ...

Trenches. Trenches are geological features formed by convergent boundaries. ...

Volcanoes. ...

Mountain Ranges. ...

Ridges. ...

Rift Valleys.

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Hot-spot volcanoes form at intraplate boundaries, where a plume of hot magma rises from deep within the mantle, creating volcanic activity away from tectonic plate boundaries.

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"Binadangan" is a Filipino term that refers to the act of separating or dividing. It can also pertain to setting boundaries or creating distinctions between things or individuals.

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tectonic plates, where magma from the mantle rises to the surface. At convergent boundaries, one plate sinks beneath the other, creating intense heat and pressure that can lead to volcanic activity. At divergent boundaries, plates move apart, allowing magma to well up and form new crust.

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New Earth's crust is added at divergent plate boundaries, where tectonic plates move away from each other. At these boundaries, molten rock rises from the mantle and solidifies, creating new crust. A prime example of this is the Mid-Atlantic Ridge.

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Africa is a good example of geometric boundaries. When Europe had control over Africa around 1884, boundaries were drawn according to Europe's egotistical desires. Tribes, cultures, and historical ways of life were not taken into account when the borders were created, creating much conflict between native peoples. Conflict and instability are common with geometric boundaries because usually outside forces with selfish desires determine these.

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Convergent boundaries are where tectonic plates move towards each other. This movement can result in the plates colliding, causing subduction (one plate moving under the other), or in the plates crumpling and creating mountain ranges. These boundaries are associated with seismic activity and volcanic eruptions.

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Yes, ocean ridges are divergent plate boundaries where tectonic plates move away from each other. As the plates separate, molten rock rises from the mantle and solidifies to form new oceanic crust, creating the underwater mountain range characteristic of ocean ridges.

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Volcanoes at divergent plate boundaries often occur along mid-ocean ridges, where tectonic plates are moving apart. As the plates separate, magma rises to the surface, creating underwater volcanic activity. These volcanic eruptions contribute to the formation of new oceanic crust.

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Volcanoes are most likely to form along tectonic plate boundaries, such as convergent and divergent plate boundaries. Convergent boundaries occur when two plates collide, causing one plate to subduct beneath the other, creating volcanic activity. Divergent boundaries occur when two plates move apart, creating gaps where magma rises to the surface and forms volcanoes. Additionally, volcanoes can also form within hotspots, where a plume of hot magma rises through the Earth's mantle.

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Volcanic mountain ranges are formed from oceanic-continental convergent-subduction boundaries, much like with volcanic islands. When a plate is subducted, the crust forming this plate is heated and melted creating magma which erupts from the crust and creates volcanic mountain ranges.

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A mid-ocean ridge forms along divergent plate boundaries, where tectonic plates are moving apart. These boundaries occur where magma rises to the surface, creating new oceanic crust and extending the ocean floor.

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The types of plate boundaries found in or along the continental US are primarily transform boundaries, where the Pacific Plate and the North American Plate slide past each other, creating faults like the San Andreas Fault in California. Additionally, subduction zones are found along the west coast, where the Juan de Fuca Plate is being subducted beneath the North American Plate.

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convergent boundaries, divergent boundaries, transform boundaries and plate boundaries

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convergent boundaries, divergent boundaries, transform boundaries and plate boundaries

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After World War I, the Treaty of Versailles in 1919 redrew many European boundaries, particularly in Central and Eastern Europe, creating new countries such as Poland, Czechoslovakia, and Yugoslavia. The treaty aimed to weaken Germany and Austria-Hungary by transferring territories to neighboring countries or creating new nations altogether. These boundary changes had significant political and ethnic implications that shaped the region's history throughout the 20th century.

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convergent boundaries, divergent boundaries, transform boundaries and plate boundaries

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convergent boundaries, divergent boundaries, transform boundaries and plate boundaries

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Mountains are commonly found near convergent plate boundaries where tectonic plates collide, causing crustal uplift and the formation of mountain ranges. Additionally, mountains can also be found at divergent plate boundaries where plates move away from each other, creating rift valleys and volcanic mountains.

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The process of measuring property to determine the boundaries of a person's land is called land surveying. It involves determining the size and shape of a piece of land and identifying its boundaries using specialized equipment and techniques. Land surveying is crucial for establishing property lines, resolving boundary disputes, and creating accurate maps.

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Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries.

um actually they are divergent, convergent, and transform

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Divergent boundaries can form along mid-ocean ridges, where tectonic plates move away from each other, creating new ocean crust. They can also form on continents, where rift valleys develop as plates pull apart, leading to the formation of new ocean basins.

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A hot spot is a volcanically active place that is far from any plate boundaries. It occurs when a plume of hot mantle material rises through the Earth's crust, creating volcanic activity on the overlying plate. An example of this is the Hawaiian Islands.

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Hot springs and fracture zones are typically found at tectonic plate boundaries, where the Earth's crust is fractured and allows for hot water to rise to the surface. One common example is at divergent plate boundaries, where plates are moving apart and creating cracks in the crust for water to circulate and become heated.

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The three types of plate movements that cause earthquakes are: 1) Transform boundaries, where plates slide past each other horizontally; 2) Convergent boundaries, where plates collide and one is forced beneath the other; 3) Divergent boundaries, where plates move apart from each other, creating tension and potential for earthquakes.

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Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries.

um actually they are divergent, convergent, and transform

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Tectonic plates interact with each other at plate boundaries. They can move apart at divergent boundaries, collide at convergent boundaries, or slide past each other at transform boundaries. These interactions can result in the formation of mountains, earthquakes, and volcanic activity.

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No, a stratovolcano is not a divergent volcano. Stratovolcanoes are typically found at convergent plate boundaries where one tectonic plate is being subducted beneath another, leading to the formation of explosive volcanoes. Divergent volcanoes, on the other hand, are associated with divergent plate boundaries where plates move away from each other, creating rift zones and shield volcanoes.

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