At this point, i think you can allow the line to miss a plot a little bit when passes between circles
pretty much it would look like this ,
just crosscheck it with the data if you're not sure
Hope this helps
Answer:
Convergent and divergent plate boundaries
Explanation:
In a convergent plate boundary, two plates move towards each other. Due to the impact, the heavier tectonic plate subducts beneath the lighter plate. This results in the formation of a subduction zone, and there forms a trench above this zone. The rocks at greater depths, melts and mixes up with the magma and eventually rises upward, towards the surface in the over-riding plate, giving rise to the formation of volcanoes and volcanic arcs.
In a divergent plate boundary, two plates move away from one another. Due to this opposite motion of plates, there occur cracks on the seafloor and land areas, from where the magma comes out. With continuous spreading, there forms a ridge, which is commonly known as the mid-oceanic ridge. This type of plate boundary is responsible for the formation and expansion of the ocean basin. For example, the mid-Atlantic ridge.
The Parthenon had a total of 69 columns. There were 46 outer columns and 23 inner columns.
1. There are three types of tectonic plate boundaries and they includes:
- When two plates slide past each other, they form a <u>transform boundary</u>.
- The <u>divergent boundary</u> occurs when two plates pull away from each other.
- When two plates collide with each other, they formed a <u>convergent boundary</u>.
2. The newest parts of the Earth’s crust is located at mid-ocean ridges.
- The mid-ocean ridge refers to the seafloor mountain system formed by plate tectonics and are the newest parts of the Earth’s crust.
3. Not every earthquake has a foreshock, but every earthquake has aftershock that occur in places far away from the mainshock.
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