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India from Indus to Gupta
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Influence of China and India China ChinaChina under the Han emperor Wudi (c. 100 bce) and (inset) at the end of the Chunqiu (Spring and Autumn) Period (c. 500 bce). Between approximately 150 bce and 150 ce, most of Southeast Asia was first influenced by the more mature cultures of its neighbours to the north and west. Thus began a process that lasted for the better part of a millennium and fundamentally changed Southeast Asia. In some ways the circumstances were very different. China, concerned about increasingly powerful chiefdoms in Vietnam disturbing its trade, encroached into the region and by the end of the 1st century bce had incorporated it as a remote province of the Han empire. For generations, the Vietnamese opposed Chinese rule, but they were unable to gain their independence until 939 ce. From India, however, there is no evidence of conquests, colonization, or even extensive migration. Indians came to Southeast Asia, but they did not come to rule, and no Indian power appears to have pursued an interest in controlling a Southeast Asian power from afar, a factor that may help to explain why only the Vietnamese accepted the Chinese model. Yet, in other ways the processes of Indianization and Sinicization were remarkably similar. Southeast Asia already was socially and culturally diverse, making accommodation easy. Furthermore, indigenous peoples shaped the adaption and adoption of outside influences and, indeed, seem to have sought out concepts and practices that enhanced rather than redirected changes already underway in their own societies. They also rejected some components: for example, some of the vocabulary and general theories related to the Indian notions of social hierarchy were borrowed but much of the specific practices were not, and neither Indian nor Chinese views of women as socially and legally inferior were accepted. In the later stages of the assimilation process—particularly in the Indianized areas—local syncretism often produced exuberant variations, which, despite familiar appearances, were expressions of local genius rather than just inspired borrowings. Get Unlimited Access Try Britannica Premium for free and discover more. Sculptures at Borobudur, central Java, Indonesia. 1 of 2 Sculptures at Borobudur, central Java, Indonesia. Pagan, Myanmar 2 of 2 Pagan, MyanmarRuins of ancient Buddhist shrines and pagodas, Pagan, Myanmar. Still, Chinese and Indian influences were anything but superficial. They provided writing systems and literature, systems of statecraft, and concepts of social hierarchy and religious belief, all of which were both of intrinsic interest and pragmatic significance to Southeast Asians of the day. For elites seeking to gain and retain control over larger and more complex populations, the applications of these ideas were obvious, but it would also seem that the sheer beauty and symbolic power of Hindu and Buddhist arts tapped a responsive vein in the Southeast Asian soul. The result was an imposing array of architectural and other cultural wonders, at first very much in the Indian image and hewing close to current styles and later in more original, indigenous interpretations. The seriousness and profundity with which all this activity was undertaken is unmistakable. By the 7th century ce, Palembang in southern Sumatra was being visited by Chinese and other Buddhist devotees from throughout Asia, who came to study doctrine and to copy manuscripts in institutions that rivaled in importance those in India itself. Later, beginning in the 8th century, temple and court complexes of surpassing grandeur and beauty were constructed in central Java, Myanmar, and Cambodia; the Borobudur of the Śailendra dynasty in Java, the myriad temples of the Burman dynastic capital of Pagan, and the monuments constructed at Angkor during the Khmer empire in Cambodia rank without question among the glories of the ancient world.India Where Is It? India is a country in Asia. Much of it is surrounded by water. To the south and west is the Arabian Sea. To the south and east is the Bay of Bengal. The capital of India is New Delhi (DEL-ee). It is part of the much larger city of Delhi. More than twenty million people live in Delhi and New Delhi. People. More than one billion people live in India. Only China has more people than India. Most Indian people live in the countryside. The cities do not have as many people. They are very crowded, though. Around half of the people in India make their living from growing food. They grow crops or raise sheep, goats, and chickens for meat. They do not raise cows for meat. Most Indians are Hindu. Hurting a cow is against the Hindu religion. Land. India has many mountains and different kinds of flat land. The mountains are in the north. They are the highest in the world. Rich land covers the north of India. It was formed long ago as rivers flooded over and over. In the west is the dry desert. In the south is raised, flat land. This land takes up more than half of India. In May or June every year, winds bring a large amount of rain. This is called the monsoon season. Most of India's rain falls during this season. Celebrations People in India celebrate many special days. Diwali (dih-WAH-lee) lasts for five days. During this festival, people light small candles. They shoot firecrackers and give sweets to family and friends. Holi (HOH-lee) is a spring Hindu festival. During Holi, people celebrate the end of winter. They throw colored water and powder on each other. Animals. Many kinds of animals live in India. It is the only country in the world with both lions and tigers. Elephants live in the flat lands and forests. The mountains are home to bears, foxes, sheep, and wild goats. India is also home to the world's largest mangrove forest. Here, tigers swim with sea turtles, sharks, and crocodiles. Conclusion. India is a country of many people. People farm its rich soil to feed the nation. Its mountains and forests are home to many animals. Which part of India would you like to see? Need for resources Find gold More land Find faster route to India & China Spread Christianity Sailors & warriors from Scandinavia 1st Europeans in North America Reached Newfoundland, Canada, 932 C.E. Found grapes, timber, furs Quit coming around 1010 Italian sent by Spain Tried to reach Asia Landed in the Caribbean islands in 1492 Made 4 total voyages Claimed land for Spain Italian sent by England Looked for route to Asia Explored the coast of New Foundland, Canada in 1497 Claimed land for England Made 3 voyages across the Atlantic Italian navigator on Spanish ship Wrote a popular book about travels North & South America were named for him Spanish explorer Crossed the Isthmus of Panama to the Pacific Ocean in 1513 1st European to reach the Pacific through the New World French explorer Sailed up St. Lawrence River looking for a NW Passage Named & claimed Canada for France Made 3 voyages to explore Canada Spanish explorer & governor of Puerto Rico Searched for a mythical “Fountain of Youth” Claimed Florida for Spain in 1513 Spanish conquistador Conquered the Aztecs in 1519-1521 Claimed Mexico for Spain Spanish explorer & conquistador Searched for the mythical “7 Cities of Gold” 1st European to see the Grand Canyon & American southwest Claimed land north of Mexico for Spain Englishman who sailed for the English and Dutch, 1609-1611 Claimed Hudson River and modern NY for Dutch Claimed Hudson Bay area for England French explorer Explored & established forts from the Great Lakes down the Mississippi River Claimed Louisiana for FranceTea Ships Arrive When the British East India Company's tea ships sailed into American ports, protesters kept them from unloading their cargoes, causing more than one ship to turn back for England still filled with tea. In Boston, however, the royal governor ordered the British navy to block the exit from Boston Harbor, insisting that the three tea ships would not leave without unloading their tea. On December 16, 1773, the Sons of Liberty decided to unload the tea, but not in the way the governor had in mind. That night, about 60 men boarded the three ships. One of them, George Hewes, described what happened: “We then were ordered by our commander to open the hatches and take out all the chests of tea and throw them overboard ... and we immediately proceeded to execute his orders, ... In about three hours from the time we went on board, we had thus broken and thrown overboard every tea chest to be found on the ship.. We were surrounded by British armed ships, but no attempt was made to resist us.” The Sons of Liberty dumped about 90,000 pounds of tea into the sea that night, leaving everything else aboard the ship untouched. News of the Boston Tea Party excited Patriots throughout the colonies. "This is the most magnificent moment of all," wrote John Adams in his journal the next day. "This destruction of the tea is So bold, so daring, so firm ... it must have. ... important consequences?" He was right.Guidance Movement in India: Introduce the historical development of guidance programs in India. Discuss milestones, such as policies and initiatives introduced by education commissions. Meaning and Definitions of Guidance: Define guidance and its significance in education. Highlight its role in helping individuals make informed choices and decisions. Need and Scope of Guidance: Explain why guidance is necessary, especially in schools, to support students' academic, personal, and career development. Discuss the broad scope of guidance, from self-understanding to achieving self-realization. Goals of Guidance: Break down the goals into: Self-understanding: Helping individuals understand their strengths and weaknesses. Self-realization: Assisting students in recognizing their potential. Self-direction: Enabling students to make informed decisions. Self-acceptance: Promoting mental well-being through self-acceptance.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.Gr''ade 3 Questions based on this chapter: English Alexander was a king of the ancient Greek kingdom of Macedonia. By the age of thirty, he had created one of the largest empires in the world, stretching from Greece to northwestern India. When Alexander was young, a trader brought a horse which was difficult to mount. Let us read about how Alexander tames the horse. One day King Philip bought a fine horse. He was a strong animal and the king paid a high price for him. But he was wild and no man could mount him, or do anything at all with him. This horse is really wild. It cannot be tamed by the royal men. Many have tried and failed. We tried everything possible, your Majesty. We tried to whip him but that only made him worse. Glossary wild rough/harsh mount a horse to climb onto the back of a horse to tame to control whip to beat using a long rope King Philip asked his men to take the horse away. It is a pity to send such a fine horse away. I think the men do not know how to tame him. I can try taming this beautiful horse. Perhaps you can do better than them. But be careful, my son. You are still very young to mount this violent animal. Alexander wanted to (mount/feed/tame/ ride) the horse. If you would give me the order, I will try. I am sure I can manage this horse better than anyone else. Antonym(s) worse x better young x old fail x succeed If I fail, I will pay you the price of the horse, Father. The courtiers told Alexander that it might be dangerous for a young boy to try taming the wild horse. They laughed at him. Alexander went near the horse and turned his head towards the sun. He had noticed that the horse was afraid of his own shadow. I will name you Bucephalus. Stay calm and I will do no harm. The horse was afraid of his own (body/courtiers/King Philip/shadow). English He then spoke gently to the horse. Bucephalus means 'ox-head'— head of an ox, in Ancient Greek. When he had quietened him a little, he made a quick spring and leapt upon the horse's back. I thought the little prince would be killed by this dangerous animal. What a miracle! The horse has recognized the young prince as his master. Alexander let the horse run. When Bucephalus had become tired of running, Alexander reined him in and rode back to the place where his father was standing. Glossary noticed (here) to see afraid scared/frightened calm quiet gently softly quietened to become calmer and less noisy a miracle a wonder/unusual event to rein to check or guide a horse Look at the young prince! He is mounted well! But the horse is still wild! Antonym(s); laughed x cried afraid x brave. English When he reached the place where his father was standing, he leapt to the ground. His father ran and kissed him. Dear Father! I shall add My son! Macedonia is a small kingdom more territories and bring for you. You must seek a larger kingdom glory to our kingdom. that will be worthy of you. Fascinating Fact(s) Alexandria Bucephalus was a city founded by Alexander in memory of his loyal horse Bucephalus. During Alexander's invasion of India, he had fought against the Indian King, Porus, near the river Hydaspes (modern day river Jhelum, Pakistan). His horse Bucephalus died there and he honoured his horse by naming the city after it. Antonym(s) worthy x unworthy proud x ashamed You have carried me across countries and stood bravely beside me as I fought to win the numerous fierce battles. You have saved my life many times. I am truly proud of you, Bucephalus. (Mesopotamia/Minneapolis/ Macedonia/Minnesota) was a small kingdom for Alexander to rule. Glossary numerous many fierce strong and violent Alexander and Bucephalus were said to be always together, for when one of them was seen, the other was sure to be not far away. Bucephalus would never allow anyone to mount him, but his master. Alexander became the most famous king and warrior, and for that reason, he is called 'Alexander the Great!. The Story of Ramayana by Maharshi Valmiki Long ago, Dasharatha, the wise king of Ayodhya of Sarayu, India had three wives. Though the King had three wives, he didn’t have any children with them. The Chief priest Vasishta advised the king to make fire sacrifice to obtain a blessing from the gods. After the gods were pleased, one of them appeared out of the flame and handed him a pot full of nectar. The god told the king to share the nectar with his three queens namely Kausalya, Kaikeye, and Sumitra. While the nectar had been shared, the three queens gave birth to sons: Kausalya had Rama; Kaikeye had Bharatha; and Sumitra had twins Lakshmana and Shatrughna. A sage took the boys out to train them in archery. In a neighboring city, the ruler's daughter was named Sita. When it was time for Sita to choose her bridegroom, at a ceremony called a Swayamvara, the princes were asked to string a giant bow. No one else could even lift the bow, but as Rama bent it, he did not only string it but also broke it into two. Sita indicated that she chose Rama as her husband by putting a garland around his neck. The disappointed suitors were watching. 6 CO_Q3_English8_Module 4 King Dasharatha, Rama's father, decided it was time to give his throne to his eldest son Rama and retired to the forest to seek moksha. Everyone seems pleased. This plan fulfilled the rules of dharma because an eldest son should rule and, if a son can take over one's responsibilities, one's last years may be spent in a search for moksha. In addition, everyone loved Rama. However, Rama's stepmother, the king's second wife, was not pleased. She wanted her son, Bharata, to rule. Because of an oath Dasharatha had made to her years before, she got the king to agree to banish Rama for fourteen years and to crown Bharata even though the king, on bended knee, begged her not to demand such things. Broken-hearted, the devastated king could not face Rama with the news that Kaikeyi must tell him. Rama, always obedient, was as content to go into banishment in the forest as to be crowned king. Sita convinced Rama that she would always be at his side and his brother Lakshmana also begged to accompany them. Rama, Sita, and Lakshmana set out to the forest. Bharata, whose mother's evil plot had won him the throne, was very upset when he found out what had happened. Not for a moment he did consider breaking the rules of dharma and becoming king in Rama's place. He went to Rama's forest retreat and begged Rama to return and rule, but Rama refused. "We must obey father," Rama says. Bharata then took Rama's sandals saying, "I will put these on the throne, and every day I shall place the fruits of my work at the feet of my Lord." Embracing Rama, he took the sandals and returned to Ayodhya. Years passed and Rama, Sita, and Lakshmana were very happy in the forest. Rama and Lakshmana destroyed the rakshasas (evil creatures) who disturbed the sages in their meditations. One day a rakshasa princess named Shurpanakha tried to seduce Rama, and Lakshmana wounded her and drove her away. She returned to her brother Ravana, the ten-headed ruler of Lanka (Sri Lanka, formerly Ceylon), and told her brother, who is always attracted to beautiful women, about lovely Sita. Ravana devised a plan to abduct Sita. He sent a magical golden deer which Sita desired Rama to hunt. A long time had passed, but Rama didn’t return. Thus, Lakshmana went off to find his brother. Before leaving Sita, Lakshmana drew a protective circle around Sita and warned her that she would be safe if she would stay within the circle. As they went off, Ravana, who could change his shape, appeared as a holy man begging alms. The moment Sita stepped outside the circle to give him food, Ravana grabbed her and carried her off to his kingdom in Lanka. Rama was broken-hearted when he returned to the empty hut and could not find Sita. A band of monkeys led by Hanuman offered to help him find Sita. Ravana carried Sita to his palace in Lanka, but he could not force her to be his wife. So, he put her in a grove and alternately sweet-talked her and threatened her in an attempt to get her to agree to marry him. Sita would not even look at him but thought only of her beloved Rama. Hanuman, the general of the monkey band could fly since his father was the wind, and he flew to Lanka and found Sita in the grove, comforted her, and told her Rama would come soon and save her. 7 CO_Q3_English8_Module 4 Ravana's men captured Hanuman, and Ravana ordered them to wrap Hanuman's tail in cloth and to set it on fire. With his tail burning, Hanuman hopped from house-top to house-top, setting Lanka a fire. He then flew back to Rama to tell him where Sita was. Rama, Lakshmana, and the monkey army built a causeway from the tip of India crossing over to Lanka. A mighty battle took place. Rama killed several of Ravana's brothers and then Rama confronted ten-headed Ravana. Rama finally killed Ravana and freed Sita. After Sita gained her freedom from Ravana, she proved her purity through the trial by fire. Then, they returned to Ayodhya and Rama became the king. As Rama became the king, he ruled Ayodhya with Ramrajya - an ideal time when everyone does his or her duties and responsibilities