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One Hundred Years of Solitude - Chapters 1-3 Review
Quiz by Barbara Franks
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Let's Play Ball! Baseball is an exciting game that is played all around the world. Players hit a ball with a bat. When you learn the rules, you can play the game. What Is Baseball? Baseball is a game with two teams. A team has nine players. Baseball teams play in an open field. Players use a bat, a ball, gloves, and four bases. A pitcher on one team throws the ball to a catcher on the same team. A batter on the other team hits the ball with the bat. The batter runs to first base, second base, and third base. The runner scores one point if he or she reaches the fourth base– home plate. The Story of Baseball. People have played baseball for hundreds of years. Long ago, people from England brought ball games to America. The games were like baseball in many ways. Over time, people made new rules and the games became one game-baseball. Famous Fields. Baseball fans love the fields where their teams play. In Boston, the team plays at Fenway Park. It is the oldest ballpark in America. Wrigley Field is an old ballpark in Chicago. Teams played there over one hundred years ago. They still play there today. Famous Players. Many people think Babe Ruth was the best baseball player ever. He hit 659 home runs with one team. He played for twenty-one years. Jackie Robinson is a hero. He was the first black baseball player to play on teams with white players. People look up to him for being a great athlete. Roberto Clemente played baseball with his team for eighteen years. He was really good at hitting the baseball. He scored 240 home runs for his team. Derek Jeter played baseball for twenty years. He scored 260 home runs for his team. People will always remember him as a great player. Everybody's Sport. Baseball time begins in the spring and goes until fall. Boys, girls, and grown-ups like to play and watch baseball. Many people think it is the best game in the world. Model Rockets Liftoff! Three... two... one... liftoff! A model rocket shoots into the sky. The rocket can fly up to 1,500 feet (457 m) high! Watching these small rockets fly can be fun and exciting. Model rockets aren't just for fun, though. They also teach us about science and space. The History of Rockets. People in China invented rockets about eight hundred years ago. They filled tubes with gunpowder and shot them at their enemies. Later, scientists built rockets that could go into space. Starting in the 1950s, people began building model rockets for fun. Parts of a Model Rocket. A model rocket kit comes with all the parts a rocket needs. A model rocket's body is a long tube made of cardboard or plastic. The nose cone fits into the top of the tube. The size and shape of a rocket's body and nose cone can change how it flies. Fins help the rocket fly straight. The engine burns fuel to push the rocket into the air. A parachute helps the rocket fall safely back to Earth. People like to make their rockets look great. Many people paint their rockets with different colors and designs. Every rocket is one of a kind! At the Launchpad. The only place to launch a rocket is in an open space. The launch area needs to be far away from people and buildings. A large field or a playground is a good spot. First, set up the launchpad. Place the rocket over the guide wire on the pad. The guide wire keeps the rocket pointing straight up. A girl connects the wire that will allow the controller to start the rocket engine. when it lifts off. Connect the launch controller to the rocket engine. Then step back and press the button on the controller to start the engine. Whoosh! The rocket flies up and away. Clubs and Competitions. People who fly model rockets often join model rocket clubs. Schools or hobby groups can have information about model rocket clubs. A science center or museum might have a model rocket club, too. Many people enter model rocket competitions. They set off rockets and see which one flies the highest and the fastest. Model rocket competitions are held all over the world. In the United States, students between twelve and eighteen can enter the Team America Rocketry Challenge. Every spring, one hundred teams compete to become the best in the country. The winners go on to compete against other teams from around the world. Model rockets are a fun way to learn about science. Who knows how high a model rocket can take your imagination?Translator: Joseph Geni Reviewer: Morton Bast Before March, 2011, I was a photographic retoucher based in New York City. We're pale, gray creatures. We hide in dark, windowless rooms, and generally avoid sunlight. We make skinny models skinnier, perfect skin more perfect, and the impossible possible, and we get criticized in the press all the time, but some of us are actually talented artists with years of experience and a real appreciation for images and photography. On March 11, 2011, I watched from home, as the rest of the world did, as the tragic events unfolded in Japan. Soon after, an organization I volunteer with, All Hands Volunteers, were on the ground, within days, working as part of the response efforts. I, along with hundreds of other volunteers, knew we couldn't just sit at home, so I decided to join them for three weeks. On May the 13th, I made my way to the town of Ōfunato. It's a small fishing town in Iwate Prefecture, about 50,000 people, one of the first that was hit by the wave. The waters here have been recorded at reaching over 24 meters in height, and traveled over two miles inland. As you can imagine, the town had been devastated. We pulled debris from canals and ditches. We cleaned schools. We de-mudded and gutted homes ready for renovation and rehabilitation. We cleared tons and tons of stinking, rotting fish carcasses from the local fish processing plant. We got dirty, and we loved it. For weeks, all the volunteers and locals alike had been finding similar things. They'd been finding photos and photo albums and cameras and SD cards. And everyone was doing the same. They were collecting them up, and handing them in to various places around the different towns for safekeeping. Now, it wasn't until this point that I realized that these photos were such a huge part of the personal loss these people had felt. As they had run from the wave, and for their lives, absolutely everything they had, everything had to be left behind. At the end of my first week there, I found myself helping out in an evacuation center in the town. I was helping clean the onsen, the communal onsen, the huge giant bathtubs. This happened to also be a place in the town where the evacuation center was collecting the photos. This is where people were handing them in, and I was honored that day that they actually trusted me to help them start hand-cleaning them. Now, it was emotional and it was inspiring, and I've always heard about thinking outside the box, but it wasn't until I had actually gotten outside of my box that something happened. As I looked through the photos, there were some were over a hundred years old, some still in the envelope from the processing lab, I couldn't help but think as a retoucher that I could fix that tear and mend that scratch, and I knew hundreds of people who could do the same. So that evening, I just reached out on Facebook and asked a few of them, and by morning the response had been so overwhelming and so positive, I knew we had to give it a go. So we started retouching photos. This was the very first. Not terribly damaged, but where the water had caused that discoloration on the girl's face had to be repaired with such accuracy and delicacy. Otherwise, that little girl isn't going to look like that little girl anymore, and surely that's as tragic as having the photo damaged. (Applause) Over time, more photos came in, thankfully, and more retouchers were needed, and so I reached out again on Facebook and LinkedIn, and within five days, 80 people wanted to help from 12 different countries. Within two weeks, I had 150 people wanting to join in. Within Japan, by July, we'd branched out to the neighboring town of Rikuzentakata, further north to a town called Yamada. Once a week, we would set up our scanning equipment in the temporary photo libraries that had been set up, where people were reclaiming their photos. The older ladies sometimes hadn't seen a scanner before, but within 10 minutes of them finding their lost photo, they could give it to us, have it scanned, uploaded to a cloud server, it would be downloaded by a gaijin, a stranger, somewhere on the other side of the globe, and it'd start being fixed. The time it took, however, to get it back is a completely different story, and it depended obviously on the damage involved. It could take an hour. It could take weeks. It could take months. The kimono in this shot pretty much had to be hand-drawn, or pieced together, picking out the remaining parts of color and detail that the water hadn't damaged. It was very time-consuming. Now, all these photos had been damaged by water, submerged in salt water, covered in bacteria, in sewage, sometimes even in oil, all of which over time is going to continue to damage them, so hand-cleaning them was a huge part of the project. We couldn't retouch the photo unless it was cleaned, dry and reclaimed. Now, we were lucky with our hand-cleaning. We had an amazing local woman who guided us. It's very easy to do more damage to those damaged photos. As my team leader Wynne once said, it's like doing a tattoo on someone. You don't get a chance to mess it up. The lady who brought us these photos was lucky, as far as the photos go. She had started hand-cleaning them herself and stopped when she realized she was doing more damage. She also had duplicates. Areas like her husband and her face, which otherwise would have been completely impossible to fix, we could just put them together in one good photo, and remake the whole photo. When she collected the photos from us, she shared a bit of her story with us. Her photos were found by her husband's colleagues at a local fire department in the debris a long way from where the home had once stood, and they'd recognized him. The day of the tsunami, he'd actually been in charge of making sure the tsunami gates were closed. He had to go towards the water as the sirens sounded. Her two little boys, not so little anymore, but her two boys were both at school, separate schools. One of them got caught up in the water. It took her a week to find them all again and find out that they had all survived. The day I gave her the photos also happened to be her youngest son's 14th birthday. For her, despite all of this, those photos were the perfect gift back to him, something he could look at again, something he remembered from before that wasn't still scarred from that day in March when absolutely everything else in his life had changed or been destroyed. After six months in Japan, 1,100 volunteers had passed through All Hands, hundreds of whom had helped us hand-clean over 135,000 photographs, the large majority — (Applause) — a large majority of which did actually find their home again, importantly. Over five hundred volunteers around the globe helped us get 90 families hundreds of photographs back, fully restored and retouched. During this time, we hadn't really spent more than about a thousand dollars in equipment and materials, most of which was printer inks. We take photos constantly. A photo is a reminder of someone or something, a place, a relationship, a loved one. They're our memory-keepers and our histories, the last thing we would grab and the first thing you'd go back to look for. That's all this project was about, about restoring those little bits of humanity, giving someone that connection back. When a photo like this can be returned to someone like this, it makes a huge difference in the lives of the person receiving it. The project's also made a big difference in the lives of the retouchers. For some of them, it's given them a connection to something bigger, giving something back, using their talents on something other than skinny models and perfect skin. I would like to conclude by reading an email I got from one of them, Cindy, the day I finally got back from Japan after six months. "As I worked, I couldn't help but think about the individuals and the stories represented in the images. One in particular, a photo of women of all ages, from grandmother to little girl, gathered around a baby, struck a chord, because a similar photo from my family, my grandmother and mother, myself, and newborn daughter, hangs on our wall. Across the globe, throughout the ages, our basic needs are just the same, aren't they?" Thank you. (Applause) (Applause)Name: Marco Ramirez - “I Am Not Batman” TW: language It’s the middle of the night. And the sky is glowing like mad radioactive red. And if you squint, you could maybe see the moon through a thick layer of cigarette smoke and airplane exhaust that covers the entire city like mosquito net that won’t let the angels in. And if you look up high enough you could see me-standing on the edge of a eighty seven story building. And up there-a place for gargoyles and broken clock towers that have stayed still and dead for maybe like a hundred years-up there is me. And I’m freakin Batman. And I gots Bat-mobiles and Bat-a-rangs and freakin Bat-caves like for real, and all it takes is a broom closet or a back room or a fire escape and Danny’s hand-me-down jeans are gone. And my navy blue polo shirt? – The one that looks kinda good on me but has a hole on it near the butt from when it got snagged on the chain linked fence behind Arturo’s but it isn’t even a big deal cause I tuck that part in and its like all good? –that blue polo shirt? – It’s gone too. And I get like, like transformational. And nobody pulls out a belt and whips Batman for talking back –-Or for not talking back –And nobody calls Batman simple –- Or stupid –- Or skinny –- And nobody fires Batman’s brother from the Eastern Taxi Company ‘cause they was making cutbacks, neither, ‘cause they got nothing but respect, and not like afraid-respect. Just like respect-respect. ‘Cause nobody’s afraid of you. Cause Batman doesn’t mean nobody harm. Ever. Cause all Batman really wants to do is save people and maybe pay Abuela’s bills one day and die happy and maybe get like mad famous. For real.…And kill the Joker. Tonight, like most nights, I’m all alone. And I’m watching…And I’m waiting… Like a eagle. Or like a –no, yea, like a eagle. And my cape is flappin’ in the wind (‘cause it’s freakin’ long), and my pointy ears are on, and that mask that covers like half my face is on too, and I got like bulletproof stuff all in my chest so no one could hurt me and nobody – nobody – is gonna come between Batman, And Justice. From where I am I could hear everything. Somewhere in the city there’s a old lady picking Styrofoam leftovers up outta a trash can and she’s putting a piece of sesame chicken someone spit out into her own mouth. And somewhere there’s a doctor with a whack haircut in a black lab coat trying to find a cure for the diseases that are gonna make us all extinct for real one day. And somewhere there’s a man, a man in a janitor’s uniform, stumbling home drunk and dizzy after spending half his paycheck on forty-ounce bottles of twist-off beer and the other half on a four hour visit to some lady’s house on a street where the lights have all been shot out by people who’d rather do what they do, in this city, in the dark. And half a block away from JanitorMan there’s a group of good-for-nothings who don’t know no better waiting to beat JanitorMan with rusted bicycle chains and imitation Lousiville Sluggers, and if they don’t find a cent on him – which they won’t – they’ll just pound at him till the muscles in their arms start burning, till there’s no more teeth to crack out. But they don’t count on me. They don’t count on no dark night (with a stomach full of grocery store brand macaroni-and-cheese and cut up Vienna sausages), Cause they’d rather believe I don’t exist, And from eighty-seven stories up I could hear one of the good-for-nothings say “Gimmethecash” real fast (like that) just “Gimmethefuckingcash” and I see JAnitorMan mumble something in drunk language and turn pale and from eighty-seven stories up I could hear his stomach trying to hurl its way out of his Dickies. So I swoop down like and fast and I’m like darkness. I’m like SWOOSH –- And I throw a Bat-a-rang at the one naked lightbulb –- And they’re all like “whoa-motherfucker-who-just-turned-out-the-lights?” –“What’s that over there?” –-“What?” –- “Gimme whatchou got old man” –- “Did anybody hear that?!” –- “No, really” –- “There ain’t. No. Bat.” – But then –- One out of three good-for-nothings gets it to the head! And number Two swings blindly into the dark cape before him but before his fist hits anything I grab a trash can lid and –-- Right into the gut, and number One comes back with a jump-kick but I know judo-karate too so I’m like –-- Twice –-- but before I can do any more damage suddenly we all hear a CLIC – CLIC –And suddenly everything gets quiet And the one good-for-nothing left standing grips a handgun and aims straight up, like he’s holding Jesus hostage, like he’s threatening maybe to blow a hole in the moon. And the good-for-nothing who got it to the head who tried to jump-kick me and the other good-for-nothing who got it in the gut is both scrambling back away from the dark figure before him. And the drunk man the JanitorMan is huddled in a corner, praying to Saint Anthony ‘cause that’s the only one he could remember. And there’s me, Eyes glowing white, cape blowing softly in the wind. Bulletporoof chest heaving. My heart beating right through it in a Morse code for “fuck with me, just once, come on, just try.” And the one good-for-nothing left standing, the one with the handgun, he laughs he lowers his arm, and he points it at me and gives the moon a break, and he aims it right between my pointy ears, like goalposts and he’s special teams. And JanitorMan is still calling Saint Anthony but he ain’t pickin’ up, And for a second it seems like…maybe I’m gonna lose. Naw. SHOO – SHOO! FUACATA! --“Don’t kill me man!” –“SNAP! – Wrist CRACK – Neck – SLASH! – Skin – meets – acid – “AHH!!” –And he’s on the floor. And I’m standing over him. And I got the gun in MY hands now. And I hate guns, I hate holding ‘em cause I’m Batman, and –Batman don’t like guns ‘cause his parents got iced by guns a long time ago – but for just a second, my eyes glow white, and I hold this thing, for I could speak to the good-for-nothing in a language he maybe understands…CLIC – CLIC…And the good-for-nothings become good-for-disappearing into whatever toxic-waste-chemical-sludge-shit-hole they crawled out of. And it’s just me and JanitorMan. And I pick him up. And I wipe sweat and cheap perfume off his forehead. And he begs me not to hurt him and I grab him tight by his JanitorMan shirt collar and I pull him to my face, and he’s taller than me, but the cape helps so he listens when I look him straight in the eyes and I say two words to him: “Go home.” And he does, checking behind his shoulder every ten feet. And I SWOOSH from building to building on his way there, ‘cause I know where he lives. And I watch his hands where he lives. And I watch his hands tremble as he pulls out his keychain and opens the door to his building. And I’m back in bed before he even walks in through the front door. And I hear him turn on the faucet and pour himself a glass of warm tap water And he puts the glass back in the sink. And I hear his footsteps, And they get slower as they get to my room. And he creaks my door open like mad slow. And he takes a step in, which he never does. And he’s staring off into nowhere, his face the color of sidewalks in summer, and I act like I’m just waking up, and I say, “What’s up, Pop?” And JanitorMan says nothing to me. But I see, in the dark, I see his arms go limp and his head turns back, like towards me, and he lifts it for I could see his face, For I could see his eyes, And his cheeks is dripping but not with sweat. And he just stands there, breathing, like he remembers my eyes glowing white. Like he remembers my bulletproof chest. Like he remembers he’s my pop. And for a long time I don’t say nothing. And he turns around, hand on the doorknob, and he ain’t looking up my way but I hear him mumble two words to me. “I’m sorry.” And I lean over and open my window just a crack.… If you look up high enough you could see me. And from where I am? I could hear everything.Can you make me a 40 question quiz from the following information? he story of coffee has all the elements of a bestselling novel, such as chance happenings, luck, political intrigue, the high seas and great wealth. With research, you will find many stories and dates when this happened and dates when that happened. Often these stories and dates will conflict with each other. Whatever the history, coffee has become one of the most important trading commodities in the world. Being second only to oil and being one of the most popular beverages, behind tea, beer and of course, water. Coffee growing is a very labour-intensive operation and it provides important trading income for many nations and people throughout the world. The most famous story about the origin of coffee is the story of Kaldi a goat herder from Ethiopia. It is said he noticed that his goats became very active after eating the red berries of a certain plant. He tried a few himself and noticed the stimulating effect of the berries. It is then said that monks started drinking a beverage made from the berries to help stay awake for the prayers; this would have been around 1000 AD. Over the next few hundred years the Arab world started to use the berries as a beverage and coffee was born. In those early years, coffee was mostly confined to the Muslim world with the export of coffee plants and seeds banned. But coffee could not be hidden forever so eventually coffee was introduced to Constantinople and coffee houses were opened in 1475. European traders then brought coffee back to Europe by approximately 1600. At first, coffee was met with a hostile reaction, with some Christians calling it the ‘Devil’s Drink’ and asking Pope Vincent III to ban the beverage. He tried coffee and liked it so much that he is claimed to have said “This beverage is so delicious that it would be a sin to let only misbelievers drink it! Let’s defeat Satan by blessing this beverage, which contains nothing objectionable to a Christian!” Coffee shops sprung up in every city and became an important social and networking place to meet. This tradition continues today with the French word for coffee being ‘Café’. Coffee is said to have changed the social fabric of society by providing a popular non-alcoholic alternative to beer and wine. For the first time in recorded history people were not drunk all the time. Coffee today is grown and enjoyed worldwide and is one of the few crops that small farmers in third-world countries can profitably export. The coffee plant is a tree that is pruned to grow to a height of approximately three metres. This makes cultivating the beans easier as most of the beans are handpicked. The plant has white flowers similar to jasmine that grow in clusters and set to become red cherry-like fruit; beneath the red skin are two pips which are the coffee beans. Because the berries ripen at varying times the fruit must be handpicked to select only those beans ripe for harvest. This requires the picker to pick from the same plant many times and is very labour intensive. This is why coffee is grown in developing countries where labour is cheaper and foreign income is needed. Coffee plants grow best in a mountain tropical climate between the Tropic of Capricorn and the Tropic of Cancer. This mountainous land is another reason why machine picking is very difficult and hand picking is preferred. There are two main species of coffee grown today: Coffee Arabica. Coffee Robusta. Robusta grows at lower altitudes and produces a larger crop than Arabica; therefore, it is cheaper to produce Arabica is the most popular and generally considered to give superior flavour. Most Robusta is grown in Asia and Africa. About 75% of coffee grown is Arabica and 25% Robusta. Robusta is more often used as a blend with Arabica rather than a standalone coffee; used as a filler coffee in the production of instant or to add extra caffeine to an Arabica coffee for the European markets. Robusta is higher in caffeine than Arabica, but the flavour is not as palatable as the more popular Arabica bean. Coffee is produced in about 60 countries throughout the world but production is dominated by three countries producing approximately half the crop: Brazil, Vietnam and Colombia.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 oceanS as 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.The geologic time scale divides the history of Earth into different blocks of time by using relative dating. Since geologists use rocks to understand Earth's history, dating does not give accurate numerical dates, it only tells that an event preceded the relative dating places these rocks in their proper sequence of formation. But relative other. This method is still widely used today, alongside a more accurate method called absolute dating, which uses radioactive elements. With relative and absolute dating. geologists can trace the history of Earth. Relative Dating. Relative dating requires one to know the basic principles such as law of super-position, principle of original horizontality, principle of cross-cutting relationships, and unconformities.Law of Superposition The law of superposition is the most basic principle in relative dating. It states that in an undeformed sequence of sedimentary rock, the layers found at the top are the youngest rocks and the layers at the bottom are the oldest. It may seem too obvious, but this principle has only been clearly stated in 1669 by the Danish anatomist, geologist, and priest, Nicolaus Steno. Principle of Original Horizontality Along with the law of superposition, Steno stated that an undeformed sequence is the one where the layers are still in a horizontal position. This follows the principle of original horizontality, which states that sediments are deposited horizontally. Principle of Cross-Cutting Relationships The principle of cross-cutting relationships determines which events occurred first depending on which rocks are affected. The geologic layer that cuts another is younger than the layer it cuts across.Unconformities Rock layers that have not been interrupted are considered conformable. These sites represent spans of geologic time. But there is no place on Earth that has a complete conformable stratum since external and internal processes have always interrupted the deposition of the sediments. These breaks in the record of the rock strata are called unconformities. Using unconformities, geologic events are determined. There are three basic types of unconformities angular unconformity, disconformity, and nonconformity. Angular unconformity is characterized by having tilted or folded sedimentary rocks below younger, horizontal layers of rock. Disconformity is determined where there are missing parallel rock layers. Erosion takes place and removes the younger top layers and then deposition would once again happen. Nonconformity is characterized by an igneous or metamorphic rock found below a sedimentary rock. Figure 3-13. Three basic types of unconformities Using these principles for relative dating, one can determine the order of events However, relative dating does not give a time element as to when they happened. Absolute Dating For a much more accurate method of determining the history of Earth, geologists make use of absolute dating. This method uses unstable elements to determine the exact age of rocks. Isotopes are elements that have the same number of protons but different number of neutrons. Most isotopes are stable but some may be unstable. This is because the forces that bind the protons and neutrons in the nucleus of the isotope are not strong enough to hold them together, resulting in a radioactive decay, The unstable isotopes are called radioactive isotopes or parent isotopes. When these parent isotopes undergo radioactive decay, new isotopes, known as daughter products, are formed. The time it takes for one-half of the nuclei in the sample to decay is called half-life. This amount of time is fixed for each kind of radioactive isotope no matter what physical conditions it is subjected to. The ratio of parent daughter isotope determines how many half-lives have passed. If it is 1:1, then one half-life has passed; if it is 1:3, then two half-lives have passed; and if 1:7, then three half-lives have passed, and so on. Therefore, using the concept of half-life and parent-daughter ratio, geologists can determine the exact age of the sample. This method is called radiometric dating. It uses five radioactive isotopes to determine the age of rocks. For dating rocks that are about a million years old, rubidium-87, thorium-232, and the two isotopes of uranium (U-238 and U-235) are used. The fifth radioactive isotope is potassium-40, which has a half-life of 1.3 billion years. With these radioactive elements, determining the accurate age of rocks becomes easier. For dating events that are more recent, radiocarbon dating is used. This method uses carbon-14. Carbon-14 has a half-life of 5730 years and can be used to date back events up to 75000 years. All organisms contain a small amount of carbon-14, which is proportional with the amount of carbon-12. When an organism dies, the carbon-14 decays and is no longer replaced. The amount of carbon-14 left in the sample is then compared to the amounts of carbon-12 present, and radiocarbon dates can then be determined. This method has been particularly useful for anthropologists, archeologists, historians, and geologists for events that are much more recent.Fossils Aside from rocks, geologists also use the remains of living organisms in understanding Earth's history. Some fossils are formed from parts of an organism (body fossil), while some provide signs or clues as to which life-forms were present at that time (Frace fossils). Fossils contain a lot of information about the past the kind of organisms that have lived, the environment where organisms lived, and the evolution organisms underwent as their environment changed. However, not all organisms turned into fossils, therefore, scientists cannot learn everything about the past using fossils alone. There are also fossils that are used to determine the age of a rock. These are index fossils and these are only found in rocks of a particular age. The organisms that turned into index fossils have a relatively short life-spanning from a few million years to a few hundred million years. Index fossils are also found in most of the common rocks around the world, which makes them easier to identify.The methods used for dating the age of rocks are also used for fossils. Absolute dating is more commonly used since it can give exact numerical dates for the age, but relative dating can also be used to determine which fossils are older.By the late 1800s, the Spanish were losing control of Cuba. Concerned about insurrection in the countryside, they moved rural Cubans to “reconcentration” camps where the Spanish claimed they would be better able to protect them. U.S. Consul-General Fitzhugh Lee forwarded the following account of the conditions of the camps to the U.S. Assistant Secretary of State on November 27, 1897. Lee said the author of the note was “a man of integrity and character.” “[W]e will relate to you what we saw with our own eyes: “Four hundred and sixty women and children thrown on the ground, heaped pellet-mell as animals, some in a dying condition, others sick and others dead. . . . “There is still alive the only living witness, a young girl of 18 years, whom we found seemingly lifeless on the ground; on her right-hand side was the body of a young mother, cold and rigid, but with her young child still alive clinging to her dead body; on her left-hand side was also the corpse of a dead woman holding her son in a dead embrace. . . . “The circumstances are the following: complete accumulation of bodies dead and alive, so that it was impossible to take one step without walking over them; the greatest want of cleanliness, want of light, air, and water; the food lacking in quality and quantity what was necessary to sustain life. . . . From all this we deduct that the number of deaths among the reconcentrados has amounted to 77 per cent.” Source: Unsigned note that was included in a telegram sent by Fitzhugh Lee, U.S. Consul-General in Cuba, to the U.S. Assistant Secretary of State November 27, 1897. consul-general: a government official living in a foreign country charged with overseeing the protection of U.S. citizens and promoting trade pell-mell: state of disorder accumulation: pile want: lack reconcentrados: the reconcentration camp prisoners; The following is an excerpt from Albert J. Beveridge’s speech, delivered September 16, 1898. Beveridge gave this speech while he was campaigning to become a senator for Indiana. The speech helped him win the election and made him one of the leading advocates of American expansion. “Fellow citizens, it is a noble land that God has given us; a land that can feed and clothe the world;. . . . It is a mighty people that he has planted on this soil . . . It is a glorious history our God has bestowed upon his chosen people; . . .a history of soldiers who carried the flag across the blazing deserts and through the ranks of hostile mountains, even to the gates of sunset. . . . “The Opposition tells us that we ought not to govern a people without their consent. I answer: The rule of liberty that all just government derives its authority from the consent of the governed, applies only to those who are capable of self-government. I answer, We govern the Indians without their consent, we govern our territories without their consent, we govern our children without their consent. “They ask us how we will govern these new possessions. I answer: If England can govern foreign lands, so can America. If Germany can govern foreign lands, so can America. . . . “What does all this mean for every one of us? It means opportunity for all the glorious young manhood of the republic, the most virile, ambitious, impatient, militant manhood the world has ever seen. It means that the resources and the commerce of these immensely rich dominions will be increased. . . . “In Cuba, alone, there are 15,000,000 acres of forest unacquainted with the axe. There are exhaustless mines of iron. . . . There are millions of acres yet unexplored. . . . It means new employment and better wages for every laboring man in the Union. . . . 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.