Activity 2: Fill in the missing word to complete the steps.

Activity 2: Direction: Fill in the missing word.

Activity 2: Fill in the Blank. Complete the sentences using the correct form of the verb in passive or active voice.

Got it ✅ I’ll create 4 simple sections of assignments based on these two pages (1.1 What is a network? and 1.2 Network connections). Total marks = 25. Suitable for Oxford International Primary Computing Grade 5. --- Assignment – Computer Networks Grade 5 – Total Marks: 25 --- Section A: Choose the Correct Answer (6 marks) Circle the correct option. Each question = 2 marks. 1. A group of computers connected together is called a: a) Website b) Network c) Software 2. Which type of network connects computers inside a school? a) LAN b) WAN c) Wi-Fi 3. To use a network safely, you need: a) A strong password b) A printer c) A hotspot --- Section B: Fill in the Blanks (6 marks) Each correct answer = 2 marks. 1. We can use a network to share files and ________. 2. A wireless connection is also called ________. 3. Network ________ help devices work together. --- Section C: Short Answer Questions (7 marks) 1. Write two advantages of using a network. (2 marks) 2. What is the difference between a wired connection and a wireless connection? (2 marks) 3. Write one rule to keep your password safe. (1 mark) 4. Create a strong password example using numbers and symbols. (2 marks) --- Section D: Activity / Problem Solving (6 marks) 1. Web Valley School has 60 network connections. Each cable is 50 meters long. How many meters of cable are used in total? (2 marks) 2. Convert your answer into kilometers. (2 marks) 3. Why is it important to hide or lock network equipment? (2 marks) --- ✅ Total = 25 marks --- Would you like me to also make a teacher’s marking guide with answers and mark distribution?

Here are 12 questions based on the Word Wall Spin the Wheel Activity focusing on Robber Barons and Labor Unions: Multiple Choice: What is a "Trust"? A) A labor organization formed by skilled workers. B) A large business combination that aims to control markets and reduce competition. C) A worker strike that demands higher wages. D) A type of factory producing steel. Answer: B Which labor union sought to include all workers, regardless of skill, gender, or race? A) American Federation of Labor (AFL) B) Industrial Workers of the World (IWW) C) Knights of Labor D) Pullman Company Answer: C Who was the founder of Standard Oil, known for his monopolistic practices? A) Andrew Carnegie B) Eugene V. Debs C) John D. Rockefeller D) Samuel Gompers Answer: C Which event involved a nationwide railroad strike that led to federal intervention and the arrest of Eugene V. Debs? A) Haymarket Square Riot B) Pullman Strike C) Homestead Strike D) Coal Strike of 1902 Answer: B What is "Vertical Integration"? A) A system where one company controls all phases of production from raw materials to finished product. B) A labor union negotiation process for better working conditions. C) The consolidation of competing businesses under a single company. D) A strike where workers occupy a factory to prevent its operation. Answer: A Which of the following was a key goal of the American Federation of Labor (AFL)? A) Overthrow the capitalist system. B) Establish worker-run factories. C) Secure higher wages, shorter hours, and better working conditions. D) Eliminate all forms of skilled labor. Answer: C Fill in the Blank: John D. Rockefeller used ___________ to gain control over the oil industry and eliminate his competition. Answer: Trusts The labor organization founded by Samuel Gompers that focused on craft unionism and collective bargaining was the ___________. Answer: American Federation of Labor (AFL) The ___________ advocated for direct action and sought to organize all workers into one large union, regardless of skill or background. Answer: Industrial Workers of the World (IWW) The ___________ was an 1894 labor strike against the Pullman Company that resulted in federal troops being sent to restore order. Answer: Pullman Strike Andrew Carnegie’s belief that the wealthy had a moral obligation to use their wealth for the betterment of society was known as the ___________. Answer: Gospel of Wealth The ___________ began as a peaceful rally for an eight-hour workday but turned violent after a bomb was thrown, leading to a nationwide backlash against labor unions. Answer: Haymarket Square Riot These questions combine multiple choice and fill-in-the-blank formats, reinforcing key concepts related to labor unions and robber barons.

Soils Southeast Asia, on balance, has a higher proportion of relatively fertile soils than most tropical regions, and soil erosion is less severe than elsewhere. Much of the region, however, is covered by tropical soils that generally are quite poor in nutrients. Often the profusion of plant life is more related to heat and moisture than to soil quality, even though these climatic conditions intensify both chemical weathering and the rate of bacterial action that usually improve soil fertility. Once the vegetation cover is removed, the supply of humus quickly disappears. In addition, the often heavy rainfall leaches the soils of their soluble nutrients, hastens erosion, and damages the soil texture. The leaching process in part results in laterites of reddish clay that contain hydroxides of iron and alumina. Laterite soils are common in parts of Myanmar, Thailand, and Vietnam and also occur in the islands of the Sunda Shelf, notably Borneo. The most fertile soils occur in regions of volcanic activity, where the ejecta is chemically alkaline or neutral. Such soils are found in parts of Sumatra and much of Java in Indonesia. The alluvial soils of the river valleys also are highly fertile and are intensively cultivated. Climate All of Southeast Asia falls within the warm, humid tropics, and its climate generally can be characterized as monsoonal (i.e., marked by wet and dry periods). Changing seasons are more associated with rainfall than with temperature variations. There is, however, a high degree of climatic complexity within the region. Temperatures Regional temperatures at or near sea level remain fairly constant throughout the year, although monthly averages tend to vary more with increasing latitude. Thus, with the exception of northern Vietnam, annual average temperatures are close to 80 °F (27 °C). Increasing elevation acts to decrease average temperatures, and such locations as the Cameron Highlands in peninsular Malaysia and Baguio in the Philippines have become popular tourist destinations in part because of their relatively cooler climates. Proximity to the sea also tends to moderate temperatures. Precipitation Much of Southeast Asia receives more than 60 inches (1,500 millimeters) of rainfall annually, and many areas commonly receive double and even triple that amount. The rainfall pattern is distinctly affected by two prevailing air currents: the northeast (or dry) monsoon and the southwest (or wet) monsoon. The northeast monsoon occurs roughly from November to March and brings relatively dry, cool air and little precipitation to the mainland. As the southwestward-flowing air passes over the warmer sea, it gradually warms and gathers moisture. Precipitation is especially heavy where the airstream is forced to rise over mountains or encounters a landmass. The east coast of peninsular Malaysia, the Philippines, and parts of eastern Indonesia receive the heaviest rains during this period. The southwest monsoon prevails from May to September, when the air current reverses and the dominant flow is to the northeast. The mainland receives the bulk of its rainfall during this period. Over much of the southern Malay Peninsula and insular Southeast Asia there is little or no prolonged dry season. This is especially marked in much of the equatorial region and along the east coast of the Philippines. While the dry and wet monsoons are important in explaining rainfall patterns, so too are such factors as relief, land and sea breezes, convectional overturning and cyclonic disturbances. These factors often are combined with monsoonal effects to produce highly variable rainfall patterns over relatively short distances. While many of the cyclonic disturbances produce only moderate rainfall, others mature into tropical storms—called cyclones in the Indian Ocean and typhoons in the Pacific—that bring heavy rains and destruction to the areas over which they pass. The Philippines are particularly affected by these storms. Plant life Tropical forests in Southeast Asia Tropical forests in Southeast Asia The seasonal nature and pattern of Southeast Asia’s rainfall, as well as the region’s physiography, have strongly affected the development of natural vegetation. The hot, humid climate and enormous variety of habitats have given rise to an abundance and diversity of vegetative forms unlike that in any other area of the world. Much of the natural vegetation has been modified by human action, although large areas of relatively untouched land still can be found. The vegetation can be grouped into two broad categories: the tropical-evergreen forests of the equatorial lowlands and the open type of tropical-deciduous, or “monsoon,” forests in areas of seasonal drought. The evergreen forests are characterized by multiple stories of vegetation, consisting of a variety of trees and plants. Although a large diversity of tree species is found in these forests, members of the Dipterocarpaceae family account for roughly half of the varieties. Deciduous forests are found in eastern Indonesia and those parts of the mainland where annual rainfall does not exceed 80 inches. Just as in the equatorial forest, a wide variety of species is normally the rule. Certain species, such as teak, have become highly valued commercially. Teak is found in parts of Indonesia, Myanmar, Thailand, and Laos. In addition to these two basic types of vegetation, other regional patterns reflect topography. Especially noteworthy are coastal and highland plant communities. Mangrove belts, of which there are more than 30 varieties, occur where silt is deposited in coastal areas. Upland forests dominated by maples, oaks, and magnolias are found especially on mainland mountain slopes. Human activity has been rapidly altering the stands of virgin forest in Southeast Asia. Most deforestation results from removal for fuelwood and clearing for agriculture and grazing. Although only a relatively small portion of the total land area has been permanently cleared for cultivation—e.g., in Java (Indonesia) and western Luzon (the Philippines)—in some areas shifting cultivation has brought about the replacement of virgin forest with secondary growth. In addition, nearly all countries have commercial logging industries; notable are those in Indonesia, Malaysia, Thailand, and Myanmar. A growing problem has been illegal logging. Thus, timber harvesting has come to contribute significantly to deforestation. Programs in social forestry and reforestation have yet to halt the rapid denuding of the landscape. Animal life Southeast Asia is situated where two major divisions of the world’s fauna meet. The region itself constitutes the eastern half of what is called the Oriental, or Indian, zoogeographic region (part of the much larger realm of Megagaea). Bordering along the south and east is the Australian zoogeographic region, and the eastern portion of insular Southeast Asia—Celebes (Sulawesi), the Moluccas, and the Lesser Sunda Islands—constitutes a transition zone between these two faunal regions. a classroom in Brazil More From Britannica education: Southeast Asia Southeast Asia is notable, therefore, for a considerable diversity of wildlife throughout the region. These differences are especially striking between the species of the eastern and western fringes as well as between those of the archipelagic south and the mainland north. The differences stem largely from the isolation, over varying lengths of geologic time, of species following their migration from the Asian continent. In addition, the tropical rain forests in many parts of the region, with their great diversity of vegetation, have made possible the development of complex communities of animals that fill specialized ecological niches. Especially numerous are arboreal and flying creatures. orangutans orangutansOrangutans (Pongo pygmaeus) in Sumatra, Indonesia. The distinction between the two faunal regions is best depicted by their mammal populations. In general, Australia is inhabited largely by marsupials (pouched mammals) and monotremes (egg-laying mammals), while Southeast Asia contains placental mammals and such hybrid species as the bandicoot of eastern Indonesia. Small mammals such as monkeys and shrews are the most numerous, while in many areas the larger mammals have been pushed into more remote areas and national preserves. Bears, gibbons, elephants, deer, civets, and pigs are found in both mainland and insular Southeast Asia, as are diminishing numbers of tigers. The Malayan tapir, a relative of the rhinoceros, is native to the Malay Peninsula and Sumatra, while the tarsier is found in the Philippines and parts of Indonesia. A number of rare endemic species are found in Indonesia and East (insular) Malaysia, including the Sumatran and Javan rhinoceros, the orangutan, the anoa (a dwarf buffalo), the babirusa (a wild swine), and the palm civet. As the pace of development accelerates and populations continue to expand in Southeast Asia, concern has increased regarding the impact of human activity on the region’s environment. A significant portion of Southeast Asia, however, has not changed greatly and remains an unaltered home to wildlife. The nations of the region, with only few exceptions, have become aware of the need to maintain forest cover not only to prevent soil erosion but to preserve the diversity of flora and fauna. Indonesia, for example, has created an extensive system of national parks and preserves for this purpose. Even so, such species as the Javan rhinoceros face extinction, with only a handful of the animals remaining in western Java

Pressure, or decompression, enables the mantle rock to melt and form magma. Decompression melting often occurs at divergent boundaries, where tectonic plates separate. The rifting movement causes the buoyant magma below to rise and fill the space of lower pressure. The rock then cools into new crust. Decompression melting also occurs at mantle plumes, columns of hot rock that rise from Earth's high-pressure core to its lower-pressure crust. When located beneath the ocean, these plumes, also known as hot spots, push magma onto the seafloor. These volcanic mounds can grow into volcanic islands over millions of years of activity. Transfer of Heat Magma can also be created when hot, liquid rock intrudes into Earth's cold crust. As the liquid rock solidifies, it loses its heat to the surrounding crust. Much like hot fudge being poured over cold ice cream, this transfer of heat is able to melt the surrounding rock (the "ice cream") into magma. Transfer of heat often happens at convergent boundaries, where tectonic plates are crashing together. As the denser tectonic plate subducts, or sinks below, or the less-dense tectonic plate, hot rock from below can intrude into the cooler plate above. This process transfers heat and creates magma. Over millions of years, the magma in this subduction zone can create a series of active volcanoes known as a volcanic arc. Flux Melting Flux melting occurs when water or carbon dioxide are added to rock. These compounds cause the rock to melt at lower temperatures. This creates magma in places where it originally maintained a solid structure. Much like heat transfer, flux melting also occurs around subduction zones. In this case, water overlying the

Create a sentence fill the gaps activity to practice the verb to be in english

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