Answer:
Points A, F, and G
Explanation:
Collinear Points are points that are on the same line.
Consider these three statements from above:
1. Line k intersects diagonal line l are point A.
2. Line l intersects line m at point F.
From 1 and 2, the points of intersection of a line with another line is on both lines. Therefore point A and F are on line l.
3. Point G is also on line l.
Points A, F and G are all on line l and are therefore collinear points.
Answer:climate, and natural resources act as contributing factors to world settlement patterns. ... Explain how these physical characteristics impact settlement patterns including ... Southwest Asia. ... major population centers (large cities) in North America on the map. ... of place such as landforms, bodies of water, climate, and natural.
Explanation:
The Earth's rocky outer crust solidified billions of
years ago, soon after the Earth formed. This crust is not a solid
shell; it is broken up into huge, thick plates that drift atop the soft,
underlying mantle.
The plates are made of rock and drift all over the globe; they move both
horizontally (sideways) and vertically (up and down). Over long
periods of time, the plates also change in size as their margins are
added to, crushed together, or pushed back into the Earth's mantle. These plates are from 50 to 250 miles (80 to 400 km) thick.
Volcanoes play an important role in creating land since they are the sources of magma, which once above ground normally cools to create new land. In the ocean, this land normally forms at divergent and convergent boundaries or hot spots. At divergent boundaries (where two plates move apart), magma constantly erupts along a trench deep below the ocean's surface. This magma rarely piles upward and instead is pushed to both sides of the trench. This is how new seafloor forms. Convergent boundaries can create island arcs like Indonesia as magma erupts bit by bit. Hot spots occur in the middle of plates. They are instances where the mantle pierces through the crust and begins to erupt directly onto to seafloor. Over time, these eruptions will pile up and create underwater volcanoes until they potentially make it above sea level, thereby forming an island. This is how Hawaii was and continues to be formed.
