The Nazca Plate along the East Pacific Rise is classified as a divergent boundary because it is moving away from the Pacific Plate, creating new oceanic crust at the mid-ocean ridge. The distribution of earthquake epicenters in this region shows shallow-focus earthquakes primarily associated with tectonic activity at divergent boundaries, where magma rises to fill the gap created by the separating plates. In contrast, convergent boundaries are characterized by subduction or collision, leading to deeper and more intense seismic activity, which is not observed at the East Pacific Rise. Thus, the geological and seismic evidence supports the classification of this area as a divergent boundary.
A Transform Fault ZoneIn the textbook Earth Science and the Environment (4th Edition) by Thompson and Turk. Located on page 163, it shows that Tonga has a Convergent Boundary. A convergent boundary is where two lithospheic plates collide head on.
if you had to look this up it is most likely because you are doing your homework and need answers oh and u are probably using the new york science grade 7 in the picture it shows the arrow moving apart so it is the divergent boundaries answer number 4
The mid-oceanic ridge in the Atlantic Ocean is one. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries. This map shows the tectonic plate boundaries. With the help of the legend, you should see where all the divergent, spreading boundaries are: http://www.globalchange.umich.edu/globalchange1/current/lectures/evolving_earth/tectonic_map.jpg Like the word "convergent" implies, convergent boundaries occur where tectonic plates converge, or come together. There are convergent boundaries on the west coast of South America, along the coast of Oregon and Washington in the Pacific Northwest of the US, along the southern edge of the Aleutian Islands of Alaska, along the eastern edge of Japan. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries.
California's western edge is characterized by the San Andreas Fault, a major transform plate boundary where the Pacific Plate and the North American Plate slide past each other. This fault exhibits features such as earthquake activity, offset rivers, and linear valleys, which are indicative of tectonic movement. Additionally, the coastal landscape shows evidence of uplift and erosion due to tectonic forces. Overall, these geological characteristics highlight the dynamic nature of California's plate margin.
The Nazca Plate along the East Pacific Rise is classified as a divergent boundary because it is moving away from the Pacific Plate, creating new oceanic crust at the mid-ocean ridge. The distribution of earthquake epicenters in this region shows shallow-focus earthquakes primarily associated with tectonic activity at divergent boundaries, where magma rises to fill the gap created by the separating plates. In contrast, convergent boundaries are characterized by subduction or collision, leading to deeper and more intense seismic activity, which is not observed at the East Pacific Rise. Thus, the geological and seismic evidence supports the classification of this area as a divergent boundary.
convergent oceanic-continental boundary
A Transform Fault ZoneIn the textbook Earth Science and the Environment (4th Edition) by Thompson and Turk. Located on page 163, it shows that Tonga has a Convergent Boundary. A convergent boundary is where two lithospheic plates collide head on.
if you had to look this up it is most likely because you are doing your homework and need answers oh and u are probably using the new york science grade 7 in the picture it shows the arrow moving apart so it is the divergent boundaries answer number 4
The mid-oceanic ridge in the Atlantic Ocean is one. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries. This map shows the tectonic plate boundaries. With the help of the legend, you should see where all the divergent, spreading boundaries are: http://www.globalchange.umich.edu/globalchange1/current/lectures/evolving_earth/tectonic_map.jpg Like the word "convergent" implies, convergent boundaries occur where tectonic plates converge, or come together. There are convergent boundaries on the west coast of South America, along the coast of Oregon and Washington in the Pacific Northwest of the US, along the southern edge of the Aleutian Islands of Alaska, along the eastern edge of Japan. MID OCEAN RIDGES ARE NOT CONVERGENT BOUNDARIES, but rather are divergent boundaries.
It is really simple geography.. The world is made up of layers, the core, the mantle and the crust. The plate Tectonics theory states that the crust is made up of loads of different pieces known as plates. Where these plates meet is known as a plate boundary. There are 3 different types of plate boundary, construcive, destructive and convergent, these different movements are caused by convection currents in the mantle. The san Andreas fault is a convergent boundary, this means the two plates move alongside each other, in either the same or different directions. The red line shows the plate boundary and the arrows show the direction by which the two plates move.
political map
A specular reflection shows a clear image. This type of reflection occurs when light bounces off a smooth and shiny surface, like a mirror, resulting in a well-defined and clear image being formed.
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A boundary marker, such as a fence, wall, or border sign, can indicate where a place ends.
A concave mirror shows an enlarged image. This type of mirror curves inward and causes light rays to converge, resulting in an image that appears larger than the actual object.