Slope!!! Period 4 | Quizalize

Continental Drift Theory. From the discussion of the rock cycle, it has been pointed out that through Earth's external and internal processes. Earth's surface is constantly changing. However, this idea of a changing environment did not conform with the belief of earlier scientists. Rather, they thought that the geographic positions of ocean basins and continents have been static since the beginning of time. It was around the 1500s when Leonardo da Vinci, upon his discovery of fossil seashells found at the high mountains of Italy, first thought of the idea that the areas where mountains are located may have been oceans in the past. Through time, other fossils of marine organisms found far above the current sea level further supported the idea that mountains were uplifted and weathering wore them down. At around the 1800s, most scientists have accepted the idea that Earth's crust is undergoing large vertical movements or uplifting. There was also evidence of possible horizontal movements, but the scientists then were not convinced about it. Alfred Wegener showed evidence of horizontal or lateral movement of the continents in his continental drift theory. According to him, the continents have drifted around the world and have once formed a giant landmass or supercontinent called Pangaea. To support his theory, Alfred Wegener presented a set of geographical, biological, and climatic evidence.Wegener's geographical evidence included the jigsaw puzzle fit of the current continents. He pointed out that the coastlines of South America and Africa seem to fit together. He also pointed the presence of mountain ranges having similar rock types and age but separated by vast oceans, like that of the folded rocks of the Caledonian mountains. The same folded rocks run through West Africa, North America, Newfoundland, Ireland, Wales, Scotland, Greenland, and Norway, all of which are now separated by the Atlantic Ocean. A geographical evidence on the similar rock types in West Africa, North America, Greenland, and Europe is found. The biological evidence came in the discovery of similar plant and animal fossils in different continents separated by oceans. The animal fossils of Mesosaurus and Lystrosaurus indicate that they were not capable of crossing the oceans to reach the other continents. If they were, the fossils should have been more widely distributed Africa, Australia, India, and South America were too large to be carried by wind. This indicates that the areas where the fossils were found were closely linked. It has also been found out that the plant only grew in areas with subpolar climate, which would indicate that the landmasses were located near the South Pole.Lastly, for his climatic evidence, Wegener discovered that a glacial period occurred during the late Paleozoic era in Southern Africa, South America, Australia, and India. The initial explanation for this event was global cooling, but it was rejected because large tropical swamps with so much vegetation were found at the same time in the Northern Hemisphere. This further supported the idea that the supercontinent was indeed near the South Pole, and the continents in Northern Hemisphere were once near the equator. The glacial period also left glacial striations, or the scratches glaciers make as they move across on the underlying bedrock, on the aforementioned continents. For such an event to happen, the continents would have to be connected. SCIENCE PIONEER. Alfred Wegener (1880-1930). Alfred Wegener was a German polar researcher, geophysicist, and meteorologist. He was known for his work on the continental drift theory. In his effort to defend his work, he went to the Greenland ice sheet where he died.Even with all the compelling evidence, the continental drift theory hardly convinced the scientific community at that time because Wegener was unable to identify a credible mechanism that drives the continental drift. He was unable to clearly explain how the continents moved and how the larger continents broke through the ocean floor. Eventually, critics of the continental drift began to accept the theory when new evidence supporting the theory was discovered. The new evidence led to a more encompassing theory the theory of plate tectonics. This theory provided a more convincing explanation as to how the continents moved. The evidence that paved the way for the theory of plate tectonics was the idea of wandering poles. Scientists began studying volcanic rocks to determine the location of the magnetic poles. When volcanic rocks crystallize, the minerals with magnetic properties align themselves parallel to Earth's magnetic field at the time the minerals were formed. This finding allowed scientists to determine the polarity of Earth's magnetic field and the magnetic inclination that showed the location of the poles. Upon studying the paleomagnetism of the rocks, geophysicists found out that rocks from various locations point to different magnetic north poles, suggesting that the poles have wandered. Since movement of magnetic poles is very unlikely, scientists have accepted the idea that the continents are indeed moving. And if the continents are moving, scientists thought that maybe the ocean basins are moving too. They also discovered that some rocks showed magnetic reversals, which led them to believe that the magnetic north pole now was not always the magnetic north pole. Seafloor Spreading. After World War II, exploration on the ocean floor became the focus of many geologic studies. It was only then that the ocean ridge system was discovered. A geologist in Princeton University named Harry Hess, along with other scientists, studied this ocean ridge system and hypothesized that the oceanic crust was moving away from the ridge. His hypothesis, known as seafloor spreading, showed that the ocean floor is split along the ridge where the magma rises to form the new ocean floor.Because of this, rocks located near the ridge are younger than those that are located magnetic polarity of Earth is also preserved in those rocks. Withe ridge scientists were able to see the magnetic reversals in the ocean floor, and they were able to make use of information to determine that the ocean floor is moving at a rate of about 10 cm per year. Plate Tectonics. Confirmation of the seafloor spreading hypothesis proved that continents are not moving above the ocean floor. Rather, it is the fragments of the lithosphere. The lithosphere is the rigid layer that is composed of the uppermost mantle and the crust that carry the continents and the ocean basins along. These fragments of the lithosphere are called plates. Underneath the lithosphere is a weaker region in the mantle known as asthenosphere that behaves like a fluid. Thus, the lithosphere floats above the asthenosphere, making it detached and free to move. This became the basis of the theory of plate tectonics. Now that it has been made clear that it is the plates which are moving, the question as to how they move remained. Sir Arthur Holmes proposed the driving force for this plate movement in 1919. He suggested that the movement in the mantle carries the plates along. It was previously discussed that Earth's interior is very hot due to the heat produced by radioactive decay. Convection takes place in the mantle, keeping the asthenosphere hot and weak. The convection currents produced in the asthenosphere are the ones carrying the lithospheric plates and making them move. However, convection currents are not enough. Mechanisms such as ridge push and slab pull aid the convection currents to slowly move the lithospheric plates. Ridge push occurs at mid ocean ridges which are higher in elevation than the surrounding trenches and abyssal plains. The new ocean floor from the ridge is hot and relatively thin. As it moves away from the ridge, it cools down and gets denser, heavier, and thicker. Below this cooling ocean floor is the asthenosphere, which is less dense. This area becomes a massive shear zone and the new ocean floor will effectively slide down the slope of the asthenosphere. When the plate collides with another plate with lesser density, the denser plate sinks and a subduction zone is formed. When the subducting plate sinks, it pulls on the rest of the plate behind it. These mechanisms explain the movement of the plates.Earth has seven major lithospheric plates that account for 94% of Earth's surface. These are the North American Plate, South American Plate, Pacific Plate, African Plate, Eurasian Plate, Indo-Australian Plate, and Antarctic Plate. These plates are constantly moving relative to the other plates. Thus, the interaction of plates occurs mostly along the boundaries. These movements are plotted using information from earthquakes and volcanic activities. There are three main types of plate boundaries: convergent, divergent, and transform boundaries Convergent boundaries are boundaries where two plates move towards each other A convergent boundary is also known as destructive margin since this is where the collision between two plates occhins. There are three types of convergence-oceanic oceanic, oceanic-continental, and continental-continental. Trenches are features of the ocean floor that are present in both oceanic-oceanic boundary and oceanic-continental boundary. Subduction occurs at the trenches, therefore, these are characterized as the deepest parts of Earth. A divergent boundary is the opposite of convergent boundary: two plates move away from each other. Divergent boundaries create new crust; thus, they are also known as constructive margins. The ocean ridge system is a divergent boundary where new ocean floor is produced as magma rises, pushing the older rocks aside.Transform boundary is also known as conservative plate margin since two plates just move past one another, neither creating nor destroying land. Earthquake epicenters are usually detected at transform boundaries because the rocks tend to break and not fold or sink, like in convergent boundaries. Evolution of the Ocean Basins. Both the movement of the plates and seafloor are responsible for the evolution of ocean basins. Along the divergent boundary where ocean ridge systems are found, magma is released and new ocean floor is created. Along convergent boundaries, the ocean floor is being destroyed. The evolution of the ocean basins started during the time when Pangaea was still present and was surrounded by the vast ocean or superocean known as Panthalassa, also called Paleo-Pacific or "old Pacific." Upon the initial break up of Pangaea into Laurasia and Gondwanaland, the Tethys Sea began to form. Then, the Eurasian and North about, forming the North Atlantic. The South Atlantic only started to form when the African Plate and South American Plate separated. The continued movement of the plates created the Himalayas at one side and separated the Pacific Ocean and Atlantic Ocean at the other side, which consequently formed the current ocean basins. Both the movement of the plates and seafloor are responsible for the evolution of ocean basins. Along the divergent boundary where ocean ridge systems are found, magma is released and new ocean floor is created. Along convergent boundaries, the ocean floor is being destroyed. The evolution of the ocean basins started during the time when Pangaea was still present and was surrounded by the vast ocean or superocean known as Panthalassa, also called Paleo-Pacific or "old Pacific." Upon the initial break up of Pangaea into Laurasia and Gondwanaland, the Tethys Sea began to form. Then, the Eurasian and North about, forming the North Atlantic. The South Atlantic only started to form when the African Plate and South American Plate separated. The continued movement of the plates created the Himalayas at one side and separated the Pacific Ocean and Atlantic Ocean at the other side, which consequently formed the current ocean basins.Continents do not immediately end at the point where the ocean meets the land. They may extend slightly into the oceans. The portion of the continent that is submerged is called continental margin. There are two types of continental margin: passive margin and active margin. A passive continental margin consists of a continental shelf, continental slope, and continental rise. It is not associated with plate boundaries; thus, there are very little tectonic activities. An active continental margin only has a continental shelf and a continental slope. It is associated with plate boundaries; thus, a main feature of this boundary is a trench. The different features of a continental margin are the following: 1. The continental shelf is the gently-sloping submerged portion of the continent. 2. The continental slope is the steep slope after the continental shelf. It is still part of the continent. 3. The continental rise is the gently-sloping area after the continental slope and before the ocean floor. 4. The trenches are the deepest parts of the ocean. These are narrow depressions caused by the subduction of the ocean floor along the convergent boundaries. 5. The mid-oceanic ridge is the mountain range system in the ocean. It is responsible for the production of new ocean floor. This is the region where new magma constantly emerges from. SCIENCE CAREER. A scientific illustrator uses art to inform and communicate complex details and concepts of science. He/She makes use of scientifically informed observations and research along with his/her technical art and aesthetic skills to make accurate representations. In Natural History, the scientific illustrators recreate how the extinct species look like by working with scientists and fossil records. Moreover, with the advances in technology, illustrators are now into 3D modelling, animation, and video making. Earth's History. All the processes that have been discussed require long periods of time to create a noticeable change on Earth's surface. You can just imagine how long it would take to create an oceanas vast as the Pacific Ocean if the ocean floor moves only at about 10 cm/year. It is then important to know the history of Earth to learn the complexities of its past and be able to use it to understand the present. Just like learning the history of a country that requires one to read a lot of books, learning the history of Earth involves studying a lot of rocks. Rocks, especially sedimentary rocks, contain a lot of information about Earth's past. It holds the key to most of the geologic processes that happened on Earth and the key to uncovering how life on Earth evolved. But these discoveries are worthless if there is no time perspective. Thus, one of the most important contributions of geologists to mankind is the geologic time scale, which holds a history that is exceedingly long.

hysical features of Southeast Asia The physiography of Southeast Asia has been formed to a large extent by the convergence of three of the Earth’s major crustal units: the Eurasian, Indian-Australian, and Pacific plates. The land has been subjected to a considerable amount of faulting, folding, uplifting, and volcanic activity over geologic time, and much of the region is mountainous. There are marked structural differences between the mainland and insular portions of the region. Mainland Southeast Asia The mainland is characterized by a series of generally north–south-trending mountain ranges separated by a number of major river valleys and their associated deltas. In many ways these ranges resemble ribs in a fan, where the interstices are deep trenches carved by the rivers. Although the mainland as a whole is similar in a structural sense, its various geologic components and the time periods of their orogenic (mountain-building) episodes differ. Much of the region has been affected by the gradual, continuing collision of the Indian subcontinent with the Eurasian Plate over roughly the past 50 million years, an event that—with diminishing intensity from west to east—has been responsible for deforming the land. Nonetheless, mainland Southeast Asia is relatively stable geologically, with no active or recently active volcanoes and, except in the northwest and north, little seismic activity. The ranges fan out southward from the southeastern corner of the Plateau of Tibet, where they are tightly spaced. A major rib of this system extends through the entire western margin of Myanmar (Burma); describing an elongated letter S, it consists of (from north to south) the Pātkai Range, Nāga Hills, Chin Hills, and Arakan Mountains. Farther to the south the same rib emerges from beneath the sea to become the Andaman and Nicobar Islands of India. Another major system extends along a straight north-south axis from eastern Myanmar east of the Salween River through northwestern Thailand to south of the Isthmus of Kra on the Malay Peninsula. It consists of a series of elongated blocks rather than one continuous ridge. The core of these blocks is granite, which has intruded into previously folded and faulted limestone and sandstone. The altitudes of the ranges diminish from above 8,000 feet (2,440 meters) on the Chinese border in the north to below 4,000 feet on the Isthmus of Kra, and the ranges are spread farther apart toward the south. The easternmost major mountain feature on the mainland is the Annamese Cordillera (Chaîne Annamitique) in Laos and Vietnam. In the portion between Laos and Vietnam, the chain forms a nearly straight spine of ranges from northwest to southeast, with a steep face rising from the South China Sea to the east and a more gradual slope to the west. The mountains thin out considerably south of Laos and become asymmetrical in form. The upland zone is characterized by a number of plateau remnants. The rather neat fanlike pattern of the mountain ranges is interrupted occasionally by several old blocks of strata that have been folded, faulted, and deeply dissected. These ancient massifs now form either low platforms or high plateaus. The westernmost of these, the Shan Plateau of eastern Myanmar, measures some 250 miles (400 km) from north to south and 75 miles from east to west and has an average elevation of about 3,000 feet. The largest of these features is the Korat Plateau in eastern Thailand and west-central Laos. This area actually is more of a low platform, which on average is only a few hundred feet above the floodplains of the surrounding rivers. It consists of a string of hills that direct surface drainage eastward to the Mekong River. The hills range in elevation from 500 to 2,000 feet, with the highest altitudes occurring near the southwestern rim. The broad river valleys between the uplands and the even wider deltas at the southernmost points contain most of the mainland’s lowland areas. These regions generally are covered with alluvial sediments that support much of the mainland’s cultivation and, in turn, most of its population centers. The most extensive coastal lowland is the lower Mekong basin, which encompasses most of Cambodia and southern Vietnam. The Cambodian portion is a broad, bowl-shaped area lying just above sea level, with numerous hill outcrops jutting above the landscape; at its center is a large freshwater lake, the Tonle Sap. To the south the river’s vast, flat delta occupies the entire southern tip of Vietnam. Outside the river deltas, the coastal lowlands are little more than narrow strips between the mountains and the sea, except around the southern half of the Malay Peninsula. The Malay Peninsula stretches south for some 900 miles from the head of the Gulf of Thailand (Siam) to Singapore and thus extends the mainland into insular Southeast Asia. The narrowest point, the Isthmus of Kra (about 40 miles wide), also roughly divides the peninsula into two parts: the long linear mountain ranges of the northern part described above give way just south of the isthmus to blocks of short, parallel ranges aligned north-south, so that the southern portion trends to the southeast and becomes much wider. In areas such as the west coast between southern Thailand and northwestern Malaysia, distinctive karst-limestone landscapes have developed. Peaks on the peninsula range from 5,000 to 7,000 feet in elevation.

ASEAN, international organization established by the governments of Indonesia, Malaysia, the Philippines, Singapore, and Thailand in 1967 to accelerate economic growth and promote peace and security in Southeast Asia. Brunei joined in 1984, followed by Vietnam in 1995, Laos and Myanmar in 1997, and Cambodia in 1999. East Timor has been granted observer status and is expected to become a full member in 2025. The ASEAN region has a population of more than 700 million, covers a total area of 1.7 million square miles (4.5 million square km), and had a combined gross domestic product of $3.62 trillion as of 2022. Since its establishment, ASEAN has substantially enhanced security and stability throughout Southeast Asia, while also promoting economic growth and cooperation on international issues. Yet certain regional issues remain divisive within ASEAN, such as Myanmar’s civil war, which has proved challenging for the bloc to address uniformly, and relations with China, particularly with regards to economic ties and territorial disputes in the South China Sea. ASEAN’s history ASEAN's 50th Summit ASEAN's 50th SummitDelegates from Southeast Asian nations gather at the 50th ASEAN Summit in Melbourne, March 2024. ASEAN’s origins can be traced back to earlier regional organizations such as the Southeast Asia Treaty Organization (SEATO), founded in 1954, and the Association of Southeast Asia (ASA), established in 1961. These early efforts, however, were limited in scope and membership. In 1967 ASEAN was established by Thailand, Indonesia, Malaysia, the Philippines, and Singapore with the signing of the ASEAN Declaration in Bangkok. The initial aim was to encourage regional cooperation and create a collective front against the spread of communism in Asia, reflecting the geopolitical concerns of the era. Lee Kuan Yew Lee Kuan YewPrime Minister Lee Kuan Yew of Singapore at the Third ASEAN Summit, 1987, in Manila. The organization gained a new level of cohesion in the mid-1970s following the Vietnam War. ASEAN’s first summit meeting, held in Bali, Indonesia, in 1976, resulted in several significant agreements, including the signing of the Treaty of Amity and Cooperation. The end of the Cold War and increased regional development and stability saw ASEAN expand its membership, incorporating Brunei, Vietnam, Laos, Myanmar, and Cambodia by the end of the 1990s. This period also marked a shift toward deeper economic integration, exemplified by the establishment of the ASEAN Free Trade Area (AFTA) in 1992 and the response to the 1997 Asian financial crisis with the Chiang Mai Agreement. The adoption of the ASEAN Charter in 2007 provided a legal and institutional framework defined by three core pillars: the ASEAN Economic Community, the ASEAN Political-Security Community, and the ASEAN Socio-Cultural Community. This structure has helped promote increased cooperation and mutual understanding, despite enormous differences in the political structures, cultural backgrounds, and development levels of member states.

ENGLISH GROUP PROJECT: THE GLOBAL VENTURE (Thailand) Comprehensive Presentation Script & Role Outline (5-Person Distribution) 1. Strategic Role & Workload Distribution Matrix Role / Name Core Domain / Responsibility Presentation Delivery Scope Member 1Member 1 Tan Finance & Housing (Rent, cost of living, deposits, urban/rural margins)Finance & Housing (Rent, cost of living, deposits, urban/rural margins) Slide 3: Finance Lead, Slide 8: Data VisualizerSlide 3: Finance Lead, Slide 8: Data Visualizer Member 2Member 2 Huy Work Culture & Professional Etiquette (Hierarchy, industry growth, networking)Work Culture & Professional Etiquette (Hierarchy, industry growth, networking) Slide 3: Culture Lead, Slide 9: Adaptation ExpertSlide 3: Culture Lead, Slide 9: Adaptation Expert Member 3Member 3 Minh Legal, Immigration & Visa Pathways (Non-Immigrant B visas, extensions, 90-day rules)Legal, Immigration & Visa Pathways (Non-Immigrant B visas, extensions, 90-day rules) Slide 3: Legal Anchor, Slide 4: Legal FrameworkSlide 3: Legal Anchor, Slide 4: Legal Framework Member 4Member 4 THanh Healthcare Ecosystem & Public Safety (Insurance, emergency networks, local hazards)Healthcare Ecosystem & Public Safety (Insurance, emergency networks, local hazards) Slide 3: Safety Anchor, Slide 10: Matrix PresenterSlide 3: Safety Anchor, Slide 10: Matrix Presenter Member 5Member 5 Sơn(project manager),Kiên Logistics, Climate & Project Manager (Transit, weather, group synthesis)Logistics, Climate & Project Manager (Transit, weather, group synthesis) Slide 1-2: Opener, Slide 6: Email Lead, Slide 11-12: CloserSlide 1-2: Opener, Slide 6: Email Lead, Slide 11-12: Closer 3. Complete Presentation Script (Slide-by-Slide) Execution Note: During delivery, presenters should display the corresponding slide from the HTML presentation tool. Speak clearly, maintaining eye contact with the grading panel. 12-Slide Presentation Guide: Secondments in Thailand Slide 1: Title Slide Purpose: Introduce the topic clearly. Content guide: Include the presentation title, group members’ names, course/module name, and date. Speaker guide: Briefly say that the presentation explains what employees and companies should consider before sending someone on secondment to Thailand. Slide 2: Agenda / Overview Welcome everyone. Our presentation is about secondments in Thailand. We will cover the main areas that a company and employee should prepare for before relocation. These include finance and housing, work culture, legal and visa requirements, healthcare and safety, and daily logistics such as transport and climate. By the end of the presentation, we hope to show that a successful secondment depends not only on the job itself, but also on good planning before and after arrival in Thailand. Slide 3: What Is a Secondment? A secondment is a temporary work assignment where an employee is transferred to another country, branch, client site, or partner organization while usually remaining connected to the original employer. Secondments require coordination between the employee, home employer, host organization, and local authorities. Slide 4: Finance & Housing — Cost of Living Finance and housing are one of the first things a secondee should plan before moving to Thailand. The cost of living can vary a lot depending on whether the employee is based in Bangkok, another major city, or a regional area. Urban areas usually have higher rent, but they also offer better access to transport, hospitals, offices, and international services. In smaller cities or rural areas, rent may be lower, but transport and convenience can become bigger concerns. So, the key point is that secondees should not only compare prices, but also consider location, commute, and what support the employer provides. Slide 6: Work Culture — Hierarchy & Etiquette Purpose: Help secondees understand workplace expectations. Content guide: Cover respect for seniority, polite communication, indirect feedback, saving face, punctuality, proper greetings, and professional dress. Speaker guide: Explain that foreign employees should avoid being too blunt in meetings and should observe how local colleagues communicate with managers or senior staff. Suggested visual: “Do and Don’t” etiquette list. Slide 7: Work Culture — Industry Growth & Networking Purpose: Connect secondments to career and business opportunities. Content guide: Mention sectors where Thailand often attracts foreign professionals, such as manufacturing, tourism, logistics, finance, technology, and regional business operations. Discuss relationship-building and networking. Speaker guide: Emphasize that trust and long-term relationships are important in Thai professional settings. Networking can happen through industry events, chambers of commerce, company introductions, and informal business meals. Suggested visual: Thailand industry opportunity map or sector icons. Slide 8: Legal & Immigration — Visa Pathways Purpose: Explain the main legal entry pathway for work-related secondments. Content guide: Introduce the Non-Immigrant B visa as a common work/business visa category. Mention that supporting documents may include passport, application forms, employment or company letters, and other evidence requested by Thai authorities. Speaker guide: Make clear that a visa alone may not be enough to legally work; seconded employees normally need the correct visa and work authorization. The exact process depends on the employer, role, nationality, and assignment structure. Suggested visual: Simple flowchart: Home employer → Host company → Visa application → Arrival → Work permit/compliance. Slide 9: Legal & Immigration — Compliance Rules Purpose: Explain ongoing responsibilities after arrival. Content guide: Cover visa extensions, work permit validity, re-entry permits, address reporting, and 90-day reporting for eligible long-stay foreigners. Speaker guide: Stress that compliance is not a one-time task. Employees and HR teams should track deadlines carefully because missing reporting or renewal dates can cause fines, delays, or legal issues. Suggested visual: Compliance checklist or timeline. Slide 10: Healthcare & Public Safety Purpose: Explain how secondees should prepare for health and safety risks. Content guide: Cover international health insurance, access to private hospitals, emergency numbers, vaccinations or health checks if required, and common local hazards such as road safety, flooding, heat, food hygiene, and mosquito-borne illnesses. Speaker guide: Explain that Thailand has strong healthcare options in major cities, but employees should confirm insurance coverage before arrival. They should also know what to do in an emergency and save important contact numbers. Suggested visual: Emergency preparation checklist. Slide 11: Logistics & Climate Purpose: Explain practical relocation and daily-life planning. Content guide: Cover public transit, taxis, ride-hailing, domestic travel, airport access, SIM cards, banking, weather, rainy season, heat, and packing needs. Speaker guide: Mention that weather affects commuting, clothing, housing choice, and travel planning. Employees should plan around heat, rain, and possible flooding, especially during the rainy season. Suggested visual: Seasonal calendar showing hot, rainy, and cool periods. Slide 12: Project Manager / Group Synthesis Purpose: Bring the presentation together and end with key recommendations. Content guide: Summarize the main risks and preparation steps: budget early, secure compliant visa/work permit arrangements, understand workplace culture, arrange insurance, and prepare for climate/logistics. Speaker guide: Conclude by saying that a successful secondment in Thailand depends on both professional readiness and personal relocation planning. End with 3–5 recommendations for companies and employees. Suggested visual: Final checklist: “Before departure,” “Upon arrival,” and “During secondment.” A simple way to divide the work is: Member 1: Slides 1–3 introduction. Member 2: Slides 4–5 finance and housing. Member 3: Slides 6–7 work culture. Member 4: Slides 8–9 legal and immigration. Member 5: Slides 10–12 healthcare, logistics, and conclusion.

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