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ช่วยตอบหน่อยค่ะ เรางงไม่ค่อยเข้าใจ

4G - 14:15 น. ← Screenshot_20230... Reading-Comprehen... Q Volcanoes Read the passage below and answer the questions on the next page. 4G 54 Volcanoes are geological formations that are created due to the movement of magma and gas from the Earth's mantle and core to its surface. The Earth's crust is made up of several large tectonic plates that are in constant motion, and when these plates collide, magma is forced to the surface, resulting in volcanic eruptions. Games4esl Volcanoes can be found all over the world and are often located in areas where tectonic plates converge, such as the Pacific Ring of Fire. Volcanoes can be classified into three main types: shield volcanoes, stratovolcanoes, and cinder cone volcanoes. Shield volcanoes are formed by repeated eruptions of fluid lava flows, which are thin and runny due to low viscosity. As the lava spreads out, it forms a wide, gently sloping mountain. Stratovolcanoes are steep, cone-shaped mountains that are formed by layers of ash, lava, and other volcanic debris. They are typically the result of explosive eruptions. Cinder cone volcanoes are small, steep-sided cones that are formed from a single vent and have a circular crater at the top. They are usually created by explosive eruptions that produce a lot of ash and cinders. |||| Volcanic eruptions can be very destructive and can cause damage to both the natural environment and human infrastructure. They can cause ash clouds that can travel for miles and disrupt air travel, as well as pyroclastic flows, which are fast-moving clouds of hot gas, ash, and rock that can be deadly. In addition to causing destruction, volcanic eruptions can also be beneficial, as they can create new land, enrich soil with minerals and nutrients, and provide sources of geothermal energy. 3 Scientists study volcanoes in order to better understand their behavior and predict when eruptions might occur. They use instruments such as seismometers, gas sensors, and satellite imagery to monitor the activity of volcanoes and track changes in their behavior. This information can be used to create early warning systems that can help protect people and communities from the effects of volcanic eruptions. www.Games4esl.com

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ช่วยอธิบายให้หน่อยค่ะ 1. มอริส ละครเอกในเรื่องทำอะไร แล้วผลเป็นอย่างไร 2. หนังสือสามารถตีความได้ว่าอย่างไรหรือเป็นสัญลักษณ์ของสิ่งใด อธิบ... อ่านต่อ

17:58 น. 4G 80% Material The FANTASTIC FINING Books of MARLORRIS ESSMORE คำอธิบาย WILLIAM JOYCE the story hot inspired the ACADEMY AWARD winning short 1,595,903 ยอดดู The Fantastic Flying Books of Mr. Morris Lessmore 2 หมื่น ชอบ 2012 21 มี.ค. x The Fantastic Flying Books of Mr. Morris Lessmore is a 2011 animated short film directed by William Joyce and Brandon Oldenburg, and produced by Moonbot Studios in Shreveport, Louisiana. Described as an "allegory about the curative powers of story," the film centers on bibliophile Lessmore and his custodianship of a magical library of flying books. It was created using computer animation, miniatures and traditional hand-drawn techniques. Versão integral do curta de animação ganhador do Oscar 2012, na mesma categoria. O curta demonstra a importância da leitura realizando uma belíssima homenagem aos livros físicos. Inspirado igualmente pelo furacão Katrina, Buster Keaton, O Mágico de Oz e pelo amor aos livros, "Morris Lessmore" trata-se de uma história bem humorada, sobre pessoas que dedicam suas vidas aos livros e livros que devolvem este favor. Filme: The Fantastic Flying Books of Mr. Morris Lessmore Autor/Ilustrador: William Joyce Co-Diretor: Brandon Oldenburg www.morrislessmore.com

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Skills 2c L Check these words • powerful mysterious cool bridge of rocks wonder of nature giant fit together enemy • eruption surface size boiling lava Reading 1 Read the summary and fill in the gaps with the words from the Check+ Check these words box. Finn MacCool and check. Finn MacCool 2 terrified huge Irish legend cross fight result place of myth and legend between Ireland and Scotland. The The Giant's Causeway is a 1) rocks have six sides that 2) to form the Giant's Causeway. People can walk on it but they can't walk to Scotland because it is under the 3) of the sea. An Irish legend says that a 4) MacCool, lived in Ireland while his 5) they couldn't 6) giant, Finn Benandonner, lived in Scotland, so the sea to fight. One day Finn threw rocks into the sea and made a bridge. After this he was tired and went to sleep. Benandonner ran across the bridge. Finn's wife saw him and tried to wake up her husband but she couldn't, so she dressed him in babies' clothes. Benandonner saw it and imagined that it was Finn's baby. He was 7) by the size of the baby and ran back home. As he ran, he pushed down the rocks to stop Finn following him. Scientists believe that the Giant's Causeway is the 8) 9) Then listen to someone telling a story of Speaking a) Listen again and take notes. b) Imagine you are a tour guide at the Giant's of a volcanic Finn MacCool and the Giant's Causeway ● main characters: Finn MacCool... where he/they lived: ... how the story began: ... what happened next: ... what was the main event: ... what happened in the end: ... Causeway. Use the verbs below in the past simple and your notes in Ex. 2a to tell the story of Finn MacCool. Use these words: once, one day, after this, then, and then, when, before, in the end. • build live cross • throw • make • go to sleep • start running try/wake up dress... in imagine ● • run back push down 20 Once, there was a giant called Finn MacCool ... . He lived with his wife in .... One day, he .... Then, he... In the end, Writing SM

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หาค่า critical micelle concentration อย่างไรบ้างคะ

ของเหลว ผลการทดลอง การทดลองที่ 14-1 – การหาค่า CMC โดยใช้ Du Nouy Tensiometer แรงตึงผิว รายงานผลปฏิบัติการเภสัชกรรมสำหรับเภสัชศาสตร์ 2 การทดลองที่ 1 A Surface and Interfacial Tension (SLS 0.00%) SLS 0.005% 0.01% 0.05% 0.10% 0.15% แรงตึงระหว่างผิว Mineral oil + un Mineral oil + SLS 0.005% 0.01% 0.05% 0.10% 0.15% ความหนาแน่นของอากาศ = ความหนาแน่นของน้ำที่ 1A-8 ค่าที่อ่านได้จากหน้าปัด ความหนาแน่น P (P) (ไดน์/ชม.) D-d (กรัม/มล.) m N/m 2 เฉลี่ย 1 73.7 738 73.75 62.3 66.9 64.8 42.8 43.8 43.3 38 39 38.5 36.4 36.4 36.4 33.4 34 33,7 0.9949 To 0.9951 0,9952 0.99 50 0.9954 0.9989 74.128 1.000.0 0.83 65.12 43.51 38.69 36.57 33,74 Correction แรงตึงผิวที่ แท้จริง factor (F) (ไตน์/ชม.) 0.93 0.93 0.93 0.93 0,93 0.93 ...................................... 68.59 60,26 40.27 35.805 33.95 31.34 กรัม/มิลลิลิตร กรัม/มิลลิลิตร ความหนาแน่นของ mineral oil - critical micelle Concentration sodium lauryl sulfate - critical micelle concentration จากกราฟระหว่างแรงตึงผิวของ mineral oil และสารละลาย sodium Lauryl sulfate กับความเข้มข้นของสารละลาย sodium lauryl sulfate = ความเข้มข้นของสารละลาย sodium lauryl sulfate ที่สามารถลดแรงตึงผิว หรือแรงตึงระหว่างผิว ได้มาก และประหยัดที่สุด จากกราฟระหว่างแรงตึงผิวและความเข้มข้นของสารละลาย ******************* ปฏิบัติการ เรื่อง Surface and Interfacial Tension E

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