What are the four main reasons as to why, despite having an abundance of minerals and natural resources, Pakistan has been unable to realise its potential and has not been able to succeed like other countries having similar resources? if same answer from someone else i will report

Heavy Debt Burden

High population growth

Terrorism

Unemployment

Explanation:

The country of Pakistan has faced many issues since the inception. The illiteracy, unemployment, over population growth are the issues that have contributed to the nations decline. The country Pakistan is blessed with numerous natural resources but the heavy debt burden has limited the access to those natural resources. The early marriage system give rise to high population growth in the country which ultimately gave rise to child labor and child abuse. The terrorism in the areas where there are abundance of natural resources pulls back the country from development.

the earth’s crust is broken into separate pieces called tectonic plates (fig. 7.14). recall that the crust is the solid, rocky, outer shell of the planet. it is composed of two distinctly different types of material: the less-dense continental crust and the more-dense oceanic crust. both types of crust rest atop solid, upper mantle material. the upper mantle, in turn, floats on a denser layer of lower mantle that is much like thick molten tar.

each tectonic plate is free-floating and can move independently. earthquakes and volcanoes are the direct result of the movement of tectonic plates at fault lines. the term fault is used to describe the boundary between tectonic plates. most of the earthquakes and volcanoes around the pacific ocean basin—a pattern known as the “ring of fire”—are due to the movement of tectonic plates in this region. other observable results of short-term plate movement include the gradual widening of the great rift lakes in eastern africa and the rising of the himalayan mountain range. the motion of plates can be described in four general patterns:

collision: when two continental plates are shoved together

subduction: when one plate plunges beneath another (fig. 7.15)

spreading: when two plates are pushed apart (fig. 7.15)

transform faulting: when two plates slide past each other (fig. 7.15)