Given what we know, we can confirm that due to Soviet rule, most people in Central Asia speak Russian, but there are numerous other languages and dialects in the region that descend from primarily indigenous roots.
<h3>What is meant by indigenous roots?</h3>
- By indigenous roots, we refer to the ancestors of the current-day civilization of Russia.
- These are the first inhabitants of the land to form civilized groups.
- Russia is home to many indigenous tribes, that have now adapted to modern life.
- However, some aspects of the tribes, such as the languages, remain.
Therefore we can confirm that due to Soviet rule, most people in Central Asia speak Russian, but there are numerous other languages and dialects in the region that descend from primarily indigenous roots.
To learn more about indigenous people visit:
brainly.com/question/582972?referrer=searchResults
6x^2 + 3xy - 2xy +y^2
6x^2 + xy + y^2
Answer:
13.72units
Explanation:
Given parameters:
Coordinates of the two points = (-5.2, 7) and (3,- 4)
Unknown:
Distance between the two points = ?
Solution:
To find the distance between two points, we use the mathematical expression below;
D = 
From the given coordinates;
x₁ = -5.2 x₂ = 3
y₁ = 7 y₂ = -4
Now; input the parameters and solve;
D = ![\sqrt{[3-(-5.2)]^{2} + (-4 -7)^{2} }](https://tex.z-dn.net/?f=%5Csqrt%7B%5B3-%28-5.2%29%5D%5E%7B2%7D%20%2B%20%28-4%20-7%29%5E%7B2%7D%20%20%7D)
= 
= 13.72units
The distance between the two points is 13.72units
Answer:
D. Seafloor bedrock is younger near the ridge and older farther away.
Explanation:
In a divergence boundary oceanic plates or continental plates move apart. The plates moves apart causing an uprising of molten magma to form a new crust. The divergent movement of plate is very prevalent in the oceanic plates.
The plates in the oceanic crust moves apart due to the up welling of aesthenosphere materials . These aesthenosphere materials(molten magma) are introduce to the ocean floor through the mid oceanic ridge . As this materials are introduced through cracks and fissures, the plates continue to drift apart. The molten magma later solidified to form a new crust closer to the oceanic ridge. This is why sea floor bedrock closer to the ridge is younger as new rocks are formed here. But as one move farther away from the ridge the rocks become older. This phenomenon provide ample evidence that the seafloor is spreading. The older rocks found father away from the ridge proves the seafloor has been spreading given way for new rocks closer to the ridge.
