Soal Dan Pembahasan Simak Ui 2017/2018 Matematika Ipa By Soal Terbaru Last updated 27 Dec 2018 104 0 Seleksi Masuk Universitas Indonesia sering dikenal dengan istilah SIMAK UI. Buku ini berisi informasi mengenai seluk beluk kampus UI, informasi SIMAK UI, tips dan trik lolos SIMAK UI, soal dan pembahasan SIMAK UI 2014 sampai 2016.
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The Cerebrum: Also known as the cerebral cortex, the cerebrum is the largest part of the human brain, and it is associated with higher brain function such as thought and action. Nerve cells make up the gray surface, which is a little thicker than our thumb. White nerve fibers beneath the surface carry signals between nerve cells in other parts of the brain and body.
Its wrinkled surface increases the surface area, and is a six-lay ered structure found in mammals, called the neocortex. It is divided into four sections, called “lobes”. They are; the frontal lobe, the parietal lobe, the occipital lobe and the temporal lobe. Parietal Lobe – The parietal lobe is located at the upper rear of our brain, and controls our complex behaviors, including senses such as vision, touch, body awareness and spatial orientation. It play s important roles in integrating sensory information from various parts of our body, knowledge of numbers and their relations, and in the manipulation of objects.
Portions are involved with our visuospatial processing, language comprehension, the ability to construct, body positioning and movement, neglect/inattention, left-right differentiation and self-awareness/insight. 1What is the main idea of the passage?. (A) The description of surface carry signals between nerve cells in other parts of the brain and body.
(B) The explanation about A bundle of axons, called the corpus callosum, connects the two hemispheres. (C) The overview about the structure and function of the human brain.
(D) The findings of the important roles of parietal lobe in integrating sensory information from various parts of our body. (E) The argument of the perception and recognition of auditory stimuli in human brain.Lihat/Tutup Pembahasan. Pembahasan:Soal ini menanyakan tentang ide pokok yang merupakan inti utama dari seluruh isi tulisan. Ide pokok wacana ini adalah mengenai gambaran mengenai struktur dan fungsi otak manusia.
Informasi ini dapat ditemukan di paragraf awal ‘Human brain structure is composed of three main parts: the forebrain, midbrain and hindbrain, each with multiple parts’ dan kemudian setiap poin struktur dan fungsi dijelaskan di setiap paragraf. Wacana ini bersifat deduktif karena ide pokok terdapat di paragraf pertama.TIPS:Topic/Main Idea: Baca paragraf pertama dan kalimat awal tiap paragraf. Temukan objek/istilah y ang sering berulang.Jawaban: C. Pembahasan:Pernyataan ulang dari kalimat: ‘Lobus parietal terletak di bagian belakang atas otak kita, dan mengendalikan perilaku kompleks kita, termasuk indera seperti penglihatan, sentuhan, kesadaran tubuh, dan orientasi spasial’ adalah ‘Lokasi lobus parietal berada di bagian belakang atas otak kita, dan mengendalikan perilaku kompleks kita, yaitu indera seperti penglihatan, sentuhan, kesadaran tubuh, dan orientasi spasial’.
Kalimat ini dapat menggantikan kalimat soal karena memiliki makna yang sama.Jawaban: D. Pembahasan:Kesimpulan merupakan sebuah gagasan yang tercapai pada akhir pembicaraan.
Dengan kata lain, kesimpulan adalah hasil dari suatu pembicaraan dalam hal ini wacana. Maka dapat disimpulkan dari wacana ada tiga bagian utama otak manusia, otak depan, otak tengah, dan otak belakang, masing-masing dengan beberapa bagian, memiliki peran signifikan dalam mengendalikan aktivitas manusia. Hal ini sejalan dengan topik wacana yang berbicara tentang bagian-bagian otak di mana tiap bagian memiliki peran yang penting bagi tubuh manusia.Jawaban: A. Questions number 6 to 9 are based on the following text.Hawaii's Kilauea volcano keeps erupting with syrupy lava flows, serving as a fiery reminder of nature's destructive power. There are two contents flow out as molten rock and they both have to do with volcanoes.
But as the ongoing eruption captures headlines, a question might occur to the readers: What's the difference between magma and lava?The distinction between magma and lava is all about location. When geologists refer to magma, they're talking about molten rock that's still trapped underground. If this molten rock makes it to the surface and keeps flowing like a liquid, it's called lava. Lava is molten rock generated by geothermal energy and expelled through fractures in planetary crust or in an eruption, usually at temperatures from 700 to 1,200 °C (1,292 to 2,192 °F).
The structures resulting from subsequent solidification and cooling are also sometimes described as lava. The molten rock is formed in the interior of some planets, including Earth, and some of their satellites, though such material located below the crust is referred to by other terms.Magmas vary in their chemical composition, which gives them—and the volcanoes that contain them—different properties. Mafic magmas like those in Hawaii tend to form when the heavier crust that forms the ocean floor melts. They contain between 47 to 63 percent silica, the mineral that makes up glass and quartz. Silicic magmas, on the other hand, tend to form when the lighter continental crust melts. These magmas are more than 63 percent silica, which makes them more viscous: At their runniest, silicic magmas flow about as well as lard orcaulk—which is to say not well at all. They're also cooler than mafic magmas.
Rhyolite, an especially silica-rich type of lava, hits temperatures between only 1,200 degrees to 1,500 degrees Fahrenheit.When silicic magmas are no longer confined under sufficiently high pressure, the gases dissolved within them come out of solution and form bubbles. And just like opening a shaken-up can of soda, the resulting rush of vapor triggers an explosive eruption. Iconic cone-shaped volcanoes called stratovolcanoes, such as Mount Pinatubo, are loaded with silicic magmas. Hawaii's volcanoes, on the other hand, contain especially low-silica magmas made of basalt, which means they have much less explosive oomph. Instead, they ooze and spatter, creating shield volcanoes—gently sloped formations that have become the islands' signature geologic silhouette.Adapted from:https://news.nationalgeographic.com/2018/05/volcano-magma-lava-difference-science/. Pembahasan:Paragraf yang membahas tentang hal yang menyebabkan tinggi rendahnya sebuah letusan merapi adalah paragraf 4.
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Informasi tersebut terdapat pada kalimat ‘And just like opening a shaken-up can of soda, the resulting rush of vapor triggers an explosive eruption’. Gagasan ini kemudian dijelaskan oleh kalimat-kalimat berikutnya yang menjelaskan bahwa yang menyebabkan gunung merapi di Hawai memiliki daya letus yang rendah karena kandungan magmanya.Jawaban: CBaca juga:.