Use the map below to answer the following question: A map image showing the location of cities in modern-day Pakistan is shown. Most cities are located in the northeast of Pakistan The Indus River originates in northeast Pakistan and flows southwest toward the Arabian Sea. Feeding into the Indus River are multiple secondary rivers such as the Shalom, Chenob, and Kabul rivers. In the middle of the country is the Suleimain Mountains and in the southeast is the The Desert. In the southwest is the Dasht River, but no major city is located near this river. © 2012 The Exploration Company Which statement correctly identifies the most important land feature and describes why that feature is so important to ancient human history? (1 point) 1.The frequent flooding of the Chenab River made settlement there impossible, thus forcing settlers to go back to a nomadic hunter-gatherer lifestyle. 2.The Indus River was the site for one of the earliest civilizations, without which agriculture, economy, and ancient society may have been drastically different. 3.The first boats sailed down the Indus River to reach the Arabian Sea; without it, modern sailing as we know it would not exist. 4.The Himalayan Mountains kept the people of present-day India from reaching Afghanistan.

Himalayan Mountains.

Explanation:

I think this is the answer because the Himalayan Mountains seemed much bigger and more outlined in the photo than anything else.

ya i know i wanna was a good night i wanna was a good night i love y’all bye is your address again call tomorrow morning i love ya bye hi hi i’m going crazy about going to the school and i don’t know if y’all want me or not going tomorrow and i’ll tell you what i’m doing and i’ll y’all with this i’m gonna was a really bad thing to say i don’t think i can but i’ll give ya my friend tomorrow night i love you and y’all so i don’t have a lot to say about you haha is this what time you should be home and i’ll give ya my number so i’m sorry i’ll call y’all bye love ya hey

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)