Nafis N

27 Januari 2022 03:34

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Nafis N

27 Januari 2022 03:34

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The most common causes of tsunamis are underwater earthquakes. To understand underwater earthquakes, you must first understand plate tectonics. The theory of plate tectonics suggests that the lithosphere, or top layer of the Earth, is made up of a series of huge plates. These plates make up the continents and seafloor. They rest on an underlying viscous called the asthenosphere. Think of a pie cut into eight slices. The pie crust would be the lithosphere and the hot, sticky pie filling underneath would be the asthenosphere. On the Earth, these plates are constantly in motion, moving along each other at a speed of 1 to 2 inches (2.5-5 em) per year. The movement occurs most dramatically along fault lines (where the pie is cut). These motions are capable of producing earthquakes and volcanism, which, when they occur at the bottom of the ocean, are two possible sources of tsunamis. When two plates come into contact at a region known as a plate boundary, a heavier plate can slip under a lighter one. This is called subduction. Underwater subduction often leaves enormous "hand prints" in the form of deep ocean trenches a long the seafloor. In some cases of subduction, part of the seafloor connected to the lighter plate may "snap up" suddenly due to pressure from the sinking plate. This result in an earthquake. The focus of the earthquake is the point within the Earth where the rupture first occurs, rocks break and the first seismic waves a re generated. The epicenter is the point on the seafloor directly above the focus. When this piece of the plate snaps up and sends tons of rock shooting upward with tremendous force, the energy of that force is transferred to the water. The energy pushes the water upward above normal sea level. Th is is the birth of a tsunami. The earthquake that generated the December 26, 2004 tsunami in the Indian Ocean was a 9.0 on the Richter scale - one of the biggest in recorded history. The main idea of this text is that … a. A deep ocean trench is a result of an earthquake b. The energy of subduction can lead to earthquakes c. Plate tectonics lead to an earthquake and volcanism d. Tsunamis in Indian Ocean are biggest in the history e. Strong movements of undersea fault lines cause tsunami

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T. Azzahra

Master Teacher

Mahasiswa/Alumni Universitas Bengkulu

31 Januari 2022 03:12

Jawaban terverifikasi

Halo Nafis N, kakak bantu jawab ya. Jawaban untuk soal di atas adalah e. Strong movements of undersea fault lines cause tsunami. Soal ini menanyakan ide pokok dari teks. Pada paragraf pertama terdapat kalimat "The most common causes of tsunami are underwater earthquakes" yang artinya "Penyebab tsunami yang paling umum adalah gempa bumi bawah laut." Selain itu pada paragraf kedua terdapat pernyataan pendukung paragraf sebelumnya, yaitu "The movement occurs most dramatically along fault lines" yang artinya "Pergerakan terjadi paling dramatis di sepanjang garis patahan." Kemudian pada paragraf selanjutnya adalah pendukung tentang terjadinya tsunami akibat pergeseran kuat di laut. Berdasarkan kalimat tersebut, dapat disimpulkan bahwa teks ini berbicara tentang "Strong movements of undersea fault lines cause tsunami" yang artinya "Terjadinya tsunami akibat pergeseran kuat patahan bawah laut." Jadi, jawaban yang tepat adalah e. Strong movements of undersea fault lines cause tsunami. Semoga membantu ya.


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The word gambut (peat) is taken from the name of a village, Desa Gambut (now Garnbut sub-district), which is located about 10 km east of Banjarmasin, South Kalimantan. It is at this place that for the first time, rice has been successfully cultivated in peat soiled rice fields. In the soil taxonomy system, peat soils are grouped into a separate soil order called hisiosols, which means that the land is predominantly composed of organic soil materials in the form of remains of plant tissues. The nature and the characteristics of peat soils can be determined based on their physical and chemical properties. Gambut has dark brown to blackish colors. Although its basic materials are gray, brown or reddish, after decomposition, the dark humid compounds will appear. Furthermore, based on the weight of the contents, peat soil or gambut, which has undergone further decomposition, has a content weight ranging from 0.2 to 0 3 g cm2. Due to the low content weight, peat has a large capacity-as water storage about 2-4 times its dry weight. In fact, moss peat that has not decomposed can store up to 12 or 15 even 20 times more water than its own weight. In addition, peat soil has a large absorption area, which is up to 4 times greater than montmorillonite clay. Next, peat soil has acidic reaction properties. Decomposition of organic matters will produce organic acids that accumulate in the bodv of the soil hence increasing the acidity of the peat soil. Generally, peat soil shows real resistance to changes in pH when compared to mineral soils. As a result, peat soil requires more limestone to increase the pH at the same level of the value of mineral soil. Thus, peat soil requires a higher dose of fertilizers than mineral soil. Furthermore, based on the nutrients contained in it, peal soil is a type of nutrient-poor soil. High levels of N and organic matters in peat soils are also accompanied by a high N nitrification process so that the activity of heterotrophic organisms is not well stimulated and the organisms active in the nitrification process can carry out (heir activities. Therefore, the levels of P (phosphorus) and K (potassium) of peat soils are generally lower than that of the mineral soils. Also, the plants cultivated on the peat soil are very responsive to the fertilization using P and K. (adapted fiom hilps://freelearningji.wordpress.com} The phrase * large capacity as water storage* in paragraph 2 can be replaced by ... A. Power to withstand heavy water currents B. Capacity to keep water flowing stable C. High quality and quantity of water D. Potential to make large water storage E. Ability to deposit a large amount of water

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