The Pampas (from Quechua, meaning “plain”) are the fertile South American lowlands that include the Argentine provinces of Buenos Aires, La Pampa, Santa Fe, and Córdoba, most of Uruguay, and the southernmost end of Brazil, covering more than 750,000 km² (290,000 square miles). These vast plains are only interrupted by the low Ventania mountain range near Bahía Blanca (Argentina), with 1,300 m height. The climate is mild, with precipitation of 600 to 1,200 mm, more or less evenly distributed through the year, making the soils appropriate for agriculture.

Frequent fires ensure that only small plants such as grasses flourish and trees are exceptional. The dominant vegetation types are grassy prairie and grass steppe in which numerous species of the grass genus Stipa are particularly conspicuous. ‘Pampas Grass’ (Cortaderia selloana) is an iconic species of the Pampas. Vegetation typically includes perennial grasses and herbs. Different strata of grasses occur due to gradients of water availability. The Pampas are home to a wide variety of native species, although there is an almost absolute lack of native trees, except along main watercourses.

Its climate, as in the mid-latitudes, is naturally changeable. Winters are cool to mild and summers are very warm and humid. Rainfall is fairly uniform throughout the year but is a little heavier during the summer. Annual rainfall is heaviest near the coast and decreases gradually further inland. Rain during the late spring and summer usually arrives in the form of brief heavy showers and thunderstorms. More general rainfall occurs the remainder of the year as cold fronts and storm systems move through. Although cold spells during the winter often send nighttime temperatures below freezing, snow is quite rare. In most winters, a few light snowfalls occur over inland areas. Snow is extremely rare near the coast.

Central Argentina boasts a successful agricultural business, with crops grown on the Pampas south and west of the Buenos Aires. In particular, the harvested area of soybeans is on pace to set a record, according to the Food and Agricultural Service. Much of the area is also used for grazing cattle. These farming regions (i.e., modified of disturbed Pampas) are particularly susceptible to flooding during heavy rainfall. In October 2001 an estimated 3.5 million hectares (35,000 km²) of the pampas were flooded, with thousands of hectares of fields and grazing lands being submerged. Buenos Aires reported nearly 250 mm (9.84 in) of rainfall during that month, which is more than double the normal amount.

The Strait of Magellan is a navigable route immediately south of mainland South America. The strait is arguably the most important natural passage between the Pacific and the Atlantic oceans, but it is considered a difficult route to navigate because of the inhospitable climate and the narrowness of the passage.

Until the Panama Canal was finished in 1914, the Strait of Magellan was often the only safe way to move between the Atlantic and Pacific Oceans. Protected by the Tierra del Fuego to the south and the bulk of South America to the north, ships crossed with relative ease, removed from the dangers of Drake Passage. The Drake Passage is the relatively narrow stretch of ocean separating Cape Horn (the southern tip of South America) from Antarctica, the waters of which are notoriously turbulent, unpredictable, and frequented by icebergs and sea ice. Until the Panama Canal was finished, the strait was the second-most used route for ships crossing between the Atlantic and the Pacific oceans (the Drake Passage was the most used route).

Ferdinand Magellan became the first European to navigate the strait in 1520, during his global circumnavigation voyage. Because Magellan’s ships entered it on November 1, it was originally named Estreito de Todos los Santos (Strait of All Saints).

On May 23, 1843 Chile took possession of the channel, under whose sovereignty it remains as of 2005. On the coast of the Strait lies the city of Punta Arenas and the village of Porvenir.

Early explorers, including Ferdinand Magellan, Francis Drake, Charles Darwin, among others, crossed this path. Prospectors during the 1849 California gold rush used this route as well.

The Pampas (from Quechua, meaning “plain”) are the fertile South American lowlands that include the Argentine provinces of Buenos Aires, La Pampa, Santa Fe, and Córdoba, most of Uruguay, and the southernmost end of Brazil, covering more than 750,000 km² (290,000 square miles). These vast plains are only interrupted by the low Ventania mountain range near Bahía Blanca (Argentina), with 1,300 m height. The climate is mild, with precipitation of 600 to 1,200 mm, more or less evenly distributed through the year, making the soils appropriate for agriculture.

Frequent fires ensure that only small plants such as grasses flourish and trees are exceptional. The dominant vegetation types are grassy prairie and grass steppe in which numerous species of the grass genus Stipa are particularly conspicuous. ‘Pampas Grass’ (Cortaderia selloana) is an iconic species of the Pampas. Vegetation typically includes perennial grasses and herbs. Different strata of grasses occur due to gradients of water availability. The Pampas are home to a wide variety of native species, although there is an almost absolute lack of native trees, except along main watercourses.

Its climate, as in the mid-latitudes, is naturally changeable. Winters are cool to mild and summers are very warm and humid. Rainfall is fairly uniform throughout the year but is a little heavier during the summer. Annual rainfall is heaviest near the coast and decreases gradually further inland. Rain during the late spring and summer usually arrives in the form of brief heavy showers and thunderstorms. More general rainfall occurs the remainder of the year as cold fronts and storm systems move through. Although cold spells during the winter often send nighttime temperatures below freezing, snow is quite rare. In most winters, a few light snowfalls occur over inland areas. Snow is extremely rare near the coast.

Central Argentina boasts a successful agricultural business, with crops grown on the Pampas south and west of the Buenos Aires. In particular, the harvested area of soybeans is on pace to set a record, according to the Food and Agricultural Service. Much of the area is also used for grazing cattle. These farming regions (i.e., modified of disturbed Pampas) are particularly susceptible to flooding during heavy rainfall. In October 2001 an estimated 3.5 million hectares (35,000 km²) of the pampas were flooded, with thousands of hectares of fields and grazing lands being submerged. Buenos Aires reported nearly 250 mm (9.84 in) of rainfall during that month, which is more than double the normal amount.

The Strait of Magellan is a navigable route immediately south of mainland South America. The strait is arguably the most important natural passage between the Pacific and the Atlantic oceans, but it is considered a difficult route to navigate because of the inhospitable climate and the narrowness of the passage.

Until the Panama Canal was finished in 1914, the Strait of Magellan was often the only safe way to move between the Atlantic and Pacific Oceans. Protected by the Tierra del Fuego to the south and the bulk of South America to the north, ships crossed with relative ease, removed from the dangers of Drake Passage. The Drake Passage is the relatively narrow stretch of ocean separating Cape Horn (the southern tip of South America) from Antarctica, the waters of which are notoriously turbulent, unpredictable, and frequented by icebergs and sea ice. Until the Panama Canal was finished, the strait was the second-most used route for ships crossing between the Atlantic and the Pacific oceans (the Drake Passage was the most used route).

Ferdinand Magellan became the first European to navigate the strait in 1520, during his global circumnavigation voyage. Because Magellan’s ships entered it on November 1, it was originally named Estreito de Todos los Santos (Strait of All Saints).

On May 23, 1843 Chile took possession of the channel, under whose sovereignty it remains as of 2005. On the coast of the Strait lies the city of Punta Arenas and the village of Porvenir.

Early explorers, including Ferdinand Magellan, Francis Drake, Charles Darwin, among others, crossed this path. Prospectors during the 1849 California gold rush used this route as well.

Located in South America, the Andes Mountain stretches from the north to the south, going along the western coast some 4,500 miles, making this one of the longest and highest mountain ranges in the entire world. When visiting South America, this area is one that you certainly should see. Keep in mind that because some places in the Andes are closer to the equator than other places, the climate is not the same.

This particular mountain range is divided into three specific and natural regions. First, there is the south, second the central region, and third, the northern region. In the southern region, you will find that the temperatures are quite a bit colder due to the mountains being closer to the Antarctic. However, if you were to visit the northern region, you would notice temperatures being hot because the mountain range is closer to the equator.

Because of high humidity levels in the northern ranges, the Andes Mountains has beautiful rainforests. To keep everything so magnificent and green, this region also gets a lot of rain. Typically, when people visit the Andes Mountains, they will head to the northern region because it is far more beautiful, there is more to see, and the temperatures are more pleasant whereas in the southern region, you see few people.

Now, if you head to the central region of the Andes Mountains, the weather tends to be more on the mild side since it is a neutral location. This too is a beautiful part of the mountain range to visit. Interestingly, the Puya Raimondii, which is the largest herb on the planet, grows in the central region, surviving and flourishing at elevations of 13,000 feet above sea level. In fact, this particular herb has been growing in this are for the past century. With this, the leaves grow out from one stem, which means the moisture can run from the leaves to the plant’s base so during drought, the plant easily survives.

You will find that a large number of the plants growing in the Andes stay small, which is their natural process for conserving needed energy. Therefore, you will often find plants that are stiff but strong so they can handle cold weather and frost. In addition to plants, the Andes Mountains are also home to many different species of birds. For example, you will find the Condor, Flamingo, Hillstar Hummingbird, and Andean Flicker. Then, there is magnificent wildlife such as the Red Perll, Llamas, the Mountain Lion, the Speckled Bear, Andean Iguana, and the Giant Toad.

Unfortunately, with too much logging, some areas of the Andes Mountains have experienced terrible destruction. With that, the animals have lost shelter and food. Then when you add in the fact that more and more people are now mining for gold, silver, and copper, the soil in some areas has become eroded, this time damaging plants. Even with these challenges, the Andes Mountains are spectacular.

Now, while many areas of the Andes Mountains are perfectly safe for traveling, some areas of South America are considered dangerous due to drug problems and guerilla activity. However, if you work with a reputable and skilled guide, and follow information provided by your travel agent, you will do find. Once there, you will be amazed at how beautiful this area of the world is, simply a slice of heaven waiting to be explored.

Weaving is an ancient textile art and craft that involves placing two sets of threads or yarn made of fiber called the warp and weft of the loom and turning them into cloth. This cloth can be plain (in one color or a simple pattern), or it can be woven in decorative or artistic designs, including tapestries.

The majority of commercial fabrics are woven on computer-controlled Jacquard looms. In the past, simpler fabrics were woven on other dobby looms and the Jacquard harness adaptation was reserved for more complex patterns. The efficiency of the Jacquard loom makes it more economical for mills to use them to weave all of their fabrics, regardless of the complexity of the design.

Hand weaving, along with hand spinning, is a popular craft. Weavers use wooden looms to create rugs, fabrics, and tapestries. Fabric in which the warp and/or weft is tie-dyed before weaving is called ikat. Fabric decorated using a wax resist method is called batik.

Process

In general, weaving involves the interlacing of two sets of threads at right angles to each other: the warp and the weft. The warp’s many threads are held taut and in parallel order by means of a loom. The loom is dressed, or set up, with the warp threads. The weft threads can be wound onto shuttles. The weft thread crosses the warp in some over/under sequence. The nature of that sequence gives rise to many possible patterns and structures from the simplest plain weave, through twills and satins to complex computer-generated interlacing.

Both warp and weft can be visible in the final product. By spacing the warp more closely, it can completely cover the weft that binds it, giving a warp-faced textile. Conversely, if the warp is spread out, the weft can slide down and completely cover the warp, giving a weft faced textile, such as a tapestry or a Kilim rug. There are a variety of loom styles for hand weaving and tapestry. In tapestry, the image is created by only placing weft in certain areas, rather than in the weave structure itself.

Pronounced yerba mahtay, this South American drink is very popular in Argentina and similar to tea. However, what makes Yerba Mate so unique is not only its flavor but is beneficial ingredients as well. In fact, this particular drink is so popular that in Buenos Aires and other cities in Argentina, people carry it around with them all day long, sipping as they go through their normal day, much as Americans would sip on soda.

This “tea” is a natural stimulant that produces zero side effects and toxicity levels. As a natural source of nutrition, Yerba Mate also promotes good health. This drink was first introduced from colonists where it was used by the ancient Guarani Indians of Paraguay and Argentina. Today, Yerba Mate is popular around the world and for good reason, as you will soon discover.

Said to boost immunity, heal the nervous system, detoxify the blood, slow down aging, restore healthy hair, fight fatigue, decrease the appetite, reduce stress, combat insomnia, and a number of other benefits, you can see why it is such a popular drink. The “mate” part of the drink is actually a member of evergreen that falls within the holly family.

Grown wild in South America, it is very aromatic with a slight bitter taste. Interesting, when grown in the wild, it takes about 25 years for the plant to develop to maturity. In the late fall and early winter months, the plant will actually produce beautiful flowers. Just as with any other type of tea, Yerba Mate is typically brewed as a cold or hot drink, using tea bags or loose, dried tea.

The traditional cup used to drink Yerba Mate is called Mate, which when originally made was a dried and decorated gourde. To prepare Yerba Mate, dried minced leaves are placed into the Mate or cup, adding hot water. Then, the fusion is sucked up through a metal or wood pipe called a Bombilla, which is designed with a strainer on the end to prevent the small pieces of tea from going into the mouth.

Some people prefer to add milk and/or sugar, or other herbs such as mint to enhance the flavor. In this case, you would use hot milk in place of the hot water. Although at first the taste is foreign, there is something about it that makes you want to go back for more. Then when you realize your body is energized, your mind is stimulated, you begin to lose weight, sickness starts to fade, and you feel better overall, you really become hooked on Yerba Mate. With its powerful stimulant effects and loaded with minerals and vitamins, people in Argentina and other parts of South America love it, and so will you.

The tagua nut has a strong resemblance to animal ivory, making it a wonderful resource for creating all types of beautiful things. For many years, the tagua nut was used primarily for making buttons but with new technology and more affordable materials such as plastics, a decline began. Even so, the tagua nut still has value in the making of other things to include chess set pieces, jewelry, handles for canes, dice, figurines, etc. In fact, many of the Victorian jewelry pieces made from the tagua nut are quite expensive.

The positive aspect of the tagua nut is that just one tree produces enough ivory to equal that of a female elephant trunk, meaning by choosing tagua, innocent animals are spared. Because of this, today we see the tagua nut again becoming very popular as more and more people are fighting to protect endangered species used for ivory. The only downfall is that these nuts, which grow in the rainforests of Panama, Ecuador, and a few other places around the world, are all harvested by hand to ensure the trees are not harmed. As you can imagine, the process is labor intensive. However, it does create needed jobs in these areas of the world!

The other benefit of using the tagua nut from Panama is that the rainforest is being protected as a sustainable income for the people. By growing these trees and keeping them harvested, forests are not degrading into poor quality land. That means the rainforest can remain a beautiful part of our world while the local tribesmen have income that helps when caring for their families.

The tagua tree is more like a palm tree that will grow upwards of 30 feet tall. Thriving on the damp areas of the rainforest, you will actually find different species of the tagua palm. As the tagua nut grows, it develops into protected clusters, each consisting of several egg-sized nuts. When the nuts are young, they are very tender, almost jelly like. Inside the young nuts is a special type of liquid that the people living in the rainforest love to drink. Additionally, many of the animals eat the tagua nut as a part of their regular diet. Then, as the tagua nut matures, it becomes extremely hard and durable, thus becoming a perfect choice for magnificent creations.

Tagua nut carvings from Panama have been such a great source of income for the forest people, giving them back self-sufficiency and pride. Many of these people are no longer able to live a full tribal life simply because of the demise of the rainforest so this type of harvesting allows them to retain their sense of self and history. Today, we sadly see many highways and modern buildings being built right through rainforests, causing this natural resource to erode. The good news is that many organizations have been formed to protect this type of land, with great success.

Once the tagua nuts are picked from the ground, the artisans carve them into amazing pieces. Interestingly, these carvings are so detailed and perfect, that many have become prized collections throughout the world. You will find that many of the tagua nut carvings from Panama depict the nature of the rainforest to include monkeys, birds, and various other animals. In fact, the carvings are typically considered an artistic expression for these tribal men, giving them the opportunity to incorporate their feelings, dreams, and aspirations into the designs.

In addition to figurines, the tagua nut is also commonly used for making everyday eating and cooking utensils. Some of the spirit sticks were used for ceremonies by the rainforest shamans (witch doctors) as well. Today, you can visit the Bernheim Gallery, Smithsonian Tropical Research Institute, and Panama Audubon Society all displaying many of these beautiful pieces. For this reason, collectors around the globe try to get their hands on any type of carving, viewing them as incredible pieces of art.

Located in the northwest portion of Ecuador, a unique venture began called the Tagua Initiative was formed. This began in 1990 by Conservation International as a means of creating economic incentives associated with the tagua palm nut, trying to find a way for the harvests to be sustained. Because of this initiative, today we see almost 2,000 people belonging to the Comuna Rio Santiago-Cayapas, holding down jobs. However, these jobs depend on the rainforest being left unharmed, allowing the tagua nut to continue growing.

The tagua plant is somewhat like a palm tree that produces a nut. When this nut is young it tender, being filled with a liquid that the people living in the rainforest drink. However, as the tagua nut matures, it becomes very hard at which time it falls from the tree. Once on the ground, the people harvest it to create amazing things. Interesting, the nuts that are not used for carving are created into “bricks” used as a fuel source because of the high heat production.

The tagua plant must grow for about 20 years before it starts to produce fruit. Even so, the nuts are not good for harvesting for five to eight years after fruit is produced. Therefore, it is not a plant that could be profitable but its nuts are. The root system of this plant has a 98% survival rate if burned. Therefore, even if there were to be a horrendous fire, the tree would be rained on and continue to grow. Because the tree produces such a versatile nut, by purchasing things made from the tagua, the rainforest is being protected.

Although the tagua plant can be found in other places, Ecuador is just one of a few countries where you can find it. Because the tagua nut is hard and resistant, while still being beautiful, it is considered a prized possession, often used in the making of precious jewelry. Other things the tagua nut is used for include chess set pieces, figurines, key chains, buttons, and much more.

Prior to plastic buttons being introduced in the United States, approximately 20% were actually made from the tagua nut. In fact, during the 1920’s, $5 million annually was brought into Ecuador for the exportation of the tagua buttons. These buttons, along with the other type of tagua carvings are often called vegetable ivory because of the color and texture. Since animal ivory is on the decline, the tagua nuts have been considered a great substitute without anything being harmed.

Sadly, much of the rainforest area in this part of the world has been destroyed. However, this Comuna sits by the Cotacachi-Cayapas Ecological Reserve, which is a very diverse area and one that is protected. This is an important hotspot since today, less than 1% of the earth is covered by rainforest hotspots yet it contains as much as 40% of biodiversity. Therefore, the Ecological Reserve protects this area so that workers can continue making their tagua nut carvings.

The Shipibo people live near the Ucayali River in areas of eastern Peru around in the Amazon Basin. These natives are extremely talented, making distinctive pottery that is traditional for their lifestyles. For example, Shipibo vases are handmade and then decorated using natural pigments from the earth. The geometric designs are representation of the visions of the Shipibo people, which is why this type of pottery is so unique and prized.

After the creation of a Shipibo vase or other piece of pottery, they are decorated and then fired in low heated, open fires. When done, the pieces of pottery are finished with a vegetable-based compound that makes it waterproof while creating a gorgeous sheen. These people live deep in the Amazon rainforest. Although they live a primitive life with limited contact with outside civilizations, the pottery made is unbelievable beautiful.

The men of the tribe are hunters and gatherers that still practice head hunting. However, the women are the pottery makers. Typically, clay is found, which takes several days in a dugout canoe to reach. The clay is then mixed with ashes coming from the bark of trees growing in the area. This mixture is then ground up into small fragments of broken pottery. From this, each piece is hand crafted, without using a potter’s wheel.

The sides of the pottery are made thin, which is what makes each pottery piece so amazingly lightweight. Once the pieces have dried in the warm sun for several days, the clay goes through the firing process. The white base color is created from a clay slip whereas the red and black geometric designs come from the process of boiling bark. Then, resin is obtained from tree sap, which gives the Shipibo pottery its unique glaze.

Most often, you would see the design of a cross and serpent. However, the geometric patterns are all easily recognized and characteristic of things seen in everyday life. For example, for special occasions, the decorations on the Shipibo pottery will depict a face and a body, which is believed to be a magical and religious expression. However, outsiders are not quite sure of the true meaning.

Keep in mind that Shipibo pottery actually started for utilitarian purposes. Pieces would be used for eating, preserving food, carrying water, and so on. However, as the Shipibo people discovered money and the things it could buy, they began selling the pottery, thus getting word out to the rest of the world about their amazing talent. Unfortunately, the trip to reach the market for the Shipibo people is a long, dangerous one.

Patagonia is that portion of South America which, to the east of the Andes, lies mainly south of the Rio Negro (41°S), and, to the west of the Andes, south of (42°S). The Chilean portion embraces the southern part of the region of Los Lagos, and the regions of Aysen and Magallanes (excluding the portion of Antarctica claimed by Chile). East of the Andes the Argentine portion of Patagonia is divided into four provinces:

A lake in Neuquén, Argentine portion of PatagoniaNeuquén, covering 36,324 sq. miles, including the triangle between the rivers Limay and Neuquen, and extending southward to the northern shore of Lake Nahuel-Huapi (41°S) and northward to the Rio Colorado;

Río Negro, covering 78,383 sq. miles, extending from the Atlantic to the Cordillera of the Andes, to the north of 42°S; Chubut, covering 86,751 sq. miles, embracing the region between 42° and 46°S; and Santa Cruz, which stretches from the last-named parallel as far south as the dividing line with Chile, and between Point Dungeness and the watershed of the Cordillera: an area of 94,186 sq. miles.

The general character of the Argentine portion of Patagonia is for the most part a region of vast steppe-like plains, rising in a succession of abrupt terraces about 100 meters (330 feet) at a time, and covered with an enormous bed of shingle almost bare of vegetation. In the hollows of the plains are ponds or lakes of brackish and fresh water. Towards the Andes the shingle gives place to porphyry, granite, and basalt lavas, animal life becomes more abundant and vegetation more luxuriant, acquiring the characteristics of the flora of the western coast, and consisting principally of southern beech and conifers.

Among the depressions by which the plateau is intersected transversely, the principal are the Gualichu, south of the Rio Negro, the Maquinchao and Valcheta (through which previously flowed the waters of lake Nahuel Huapi, which now feed the river Limay); the Senguerr, the Deseado. Besides these transverse depressions (some of them marking lines of ancient inter-oceanic communication), there are others which were occupied by more or less extensive lakes, such as the Yagagtoo, Musters, and Colhue Huapi, and others situated to the south of Puerto Deseado, in the centre of the country. In the central region volcanic eruptions, which have taken part in the formation of the plateau from the Tertiary period down to the present era, cover a large part with basaltic lava-caps; and in the western third more recent glacial deposits appear above the lava. There, in contact with folded Cretaceous rocks, uplifted by the Tertiary granite, erosion, caused principally by the sudden melting and retreat of the ice, aided by tectonic changes, has scooped out a deep longitudinal depression, which generally separates the plateau from the first lofty hills, the ridges generally called the pre-Cordillera, while on the west of these there is a similar longitudinal depression all along the foot of the snowy Andean Cordillera. This latter depression contains the richest and most fertile land of Patagonia.

The geological constitution is in accordance with the orographic physiognomy. The Tertiary plateau, flat on the east, gradually rising on the west, shows Upper Cretaceous caps at its base. First come Lower Cretaceous hills, raised by granite and dioritic rocks, undoubtedly of Tertiary origin, as in some cases these rocks have broken across the Tertiary beds, so rich in mammal remains; then follow, on the west, metamorphic schists of uncertain age; then quartzites appear, resting directly on the primitive granite and gneiss which form the axis of the Cordillela. Porphyritic rocks occur between the schists and the quartzites. The Tertiary deposits are greatly varied in character, and there is considerable difference of opinion concerning the succession and correlation of the beds.

Glaciers occupy the valleys of the main chain and some of the lateral ridges of the Cordillera, and descend to lakes San Martín, Viedma, Argentino and others in the same locality, strewing them with icebergs. In Patagonia an immense ice-sheet extended to the east of the present Atlantic coast during the first ice age, at the close of the Tertiary epoch, while, during the second glacial age in modern times, the terminal moraines have generally stopped, 30 miles (50 km) in the north and 50 miles (80 km) in the south, east of the summit of the Cordillera. These ice-sheets, which scooped out the greater part of the longitudinal depressions, and appear to have rapidly retreated to the point where the glaciers now exist, did not, however, in their retirement fill up with their detritus the fjords of the Cordillera, for these are now occupied by deep lakes on the east, and on the west by the Pacific channels, some of which are as much as 250 fathoms (460 m) in depth, and soundings taken in them show that the fjords are as usual deeper in the vicinity of the mountains than to the west of the islands. Several of the high peaks are still active volcanoes.

In so far as its main characteristics are concerned, Patagonia seems to be a portion of the Antarctic continent, the permanence of which dates from very recent times, as is evidenced by the apparent recent emergence of the islets around Chiloé, and by the general character of the pampean formation. Some of the promontories of Chiloé are still called huapi, the Araucanian equivalent for “islands”; and this may perhaps be accepted as perpetuating the recollection of the time when they actually were islands. They are composed of caps of shingle, with great, more or less rounded boulders, sand and volcanic ashes, precisely of the same form as occurs on the Patagonian plateau. From an examination of the pampean formation it is evident that in recent times the land of the province of Buenos Aires extended farther to the east, and that the advance of the sea, and the salt-water deposits left by it when it retired, forming some of the lowlands which occur on the littoral and in the interior of the pampas, are much more recent phenomena; and certain caps of shingle, derived from rocks of a different class from those of the neighbouring hills, which are observed on the Atlantic coasts of the same province, and increase in quantity and size towards the south, seem to indicate that the caps of shingle which now cover such a great part of the Patagonian territory recently extended farther to the east, over land which has now disappeared beneath the sea, while other marine deposits along the same coasts became converted into bays during the subsequent advance of the sea. There are besides, in the neighbourhood of the present coast, deposits of volcanic ashes, and the ocean throws up on its shores blocks of basaltic lava, which in all probability proceed from eruptions of submerged volcanoes now extinct. One fact, however, which apparently demonstrates with greater certainty the existence in recent times of land that is now lost, is the presence of remains of pampean mammals in Pleistocene deposits in the bay of San Julian and in Santa Cruz. The animals undoubtedly reached these localities from the east; it is not at all probable that they advanced from the north southwards across the plateau intersected at that cime by great rivers and covered by the ice-sheet. With the exception of the discoveries at the inlet of Ultima Esperanza, which is in close communication with the Atlantic valley of Río Gallegos, none of these remains have been discovered in the Andean regions.

On the upper plains of Neuquen territory thousands of cattle can be fed, and the forests around Lakes Tiaful and Nahuel-Huapi yield large quantities of valuable timber. The Neuquen river is not navigable, but as its waters are capable of being easily dammed in places, large stretches of land in its valley are utilized; but the lands on each side of its lower part are of little commercial value. As the Cordillera is approached the soil becomes more fertile, and suitable districts for the rearing of cattle and other agricultural purposes exist between the regions that surround the Tromen volcano and the first ridges of the Andes. Chos Malal, the capital of the territory, is situated in one of these valleys. More to the west is the mining region, in great part unexplored, but containing deposits of gold, silver, copper and lignite. In the centre of the territory, also in the neighbourhood of the mining districts, are the valleys of Norquin and Las Lajas, the general camp of the Argentine army in Patagonia, with excellent timber in the forest on the Andean slope. The wide valleys occur near Rio Malleo, Lake Huechulafquen, the river Chimehuin, and Vega de Chapelco, near Lake Lacar, where are situated villages of some importance, such as Junin de los Andes and San Martin de los Andes. Close to these are the famous apple orchards supposed to have been planted by the Jesuits in the 17th and 18th centuries. The river Collon Cura, the principal affluent of the river Limay, drains these regions. Lake Lacar is now a contributary of the Pacific, its outlet having been changed to the west, owing to a passage having been opened through the Cordillera.

The Rio Negro runs along a wide transverse depression. the middle part of which is followed by the railway which runs to the settlement of Neuquen at the confluence of the rivers Limay and Neuquen. In this depression are several settlements, among them Viedma, the capital of the Rio Negro territory, Pringles, General Conesa, Choele Choel and General Roca. To the south of the Rio Negro the Patagonian plateau is intersected by the depressions of the Gualicho and Maquinchao, which in former times directed the waters of two great rivers (now disappeared) to the gulf of San Matias, the first-named depression draining the network of the Collon Cura and the second the Nahuel Huapi lake system. In 42°S there is a third broad transverse depression, apparently the bed of another great river, now perished, which carried to the Atlantic the waters of a portion of the eastern slope of the Andes, between 41° and 42°30;S.

Chubut territory presents the same characteristics as the Rio Negro territory. Rawson, the capital, is situated at the mouth of the river Chubut on the Atlantic (42°30′S). The town was founded in 1865 by a group of colonists from Wales, assisted by the Argentine government; and its prosperity has led to the foundation of other important centres in the valley, such as Trelew and Gaiman, which is connected by railway with Puerto Madryn on Bahia Nueva. Here is the seat of the governor of the territory, and by 1895 the inhabitants of this part of the territory, composed principally of Argentines, Welsh and Italians, numbered 2585. The valley has been irrigated and cultivated, and produces the best wheat of the Argentine Republic. Between the Chubut and the Senguerr there are vast stretches of fertile land, spreading over the Andean region to the foot of the Cordillera and the lateral ridges of the Pre-Cordillera, and filling the basins of some desiccated lakes, which have been occupied since 1885, and farms and colonies founded upon them. The chief of these colonies is that of 16 de Octubre, formed in 1886, mainly by the inhabitants of Chubut colony, in the longitudinal valley which extends to the eastern foot of the Cordillera. Other rivers in this territory flow into the Pacific through breaches in the Cordillera, e.g. the upper affluents of the Futaleufu, Palena and Rio Cisnes. The principal affluent of the Palena, the Carrenleufu, carries off the waters of Lake General Paz, situated on the eastern slope of the Cordillera. Rio Pico, an affluent of the same river, receives nearly the whole of the waters of the extensive undulating plain which lies between the Rio Tecka and the Rio Senguerr to the east of the Cordillera, while the remainder are carried away by the affluents of Rio Jehua: the Cherque, Omkel, and Appeleg. This region contains auriferous drifts, but these, like the auriferous deposits, veins of galena and lignite in the mountains farther west which flank the Cordillera, have not been properly investigated. At Lake Fontana there are auriferous drifts and lignite deposits which abound in fossil plants of the Cretaceous age. The streams which form the rivers Mayo and Chalia join the tributaries of the Rio Aisen, which flows into the Pacific, watering in its course extensive and valuable districts where colonization has been initiated by Argentine settlers. Colonies have also been formed in the basin of Lakes Musters and Colhué Huapi; and on the coasts near the Atlantic, along Bahia Camarones and the Gulf of San Jorge, there are extensive farms.

The territory of Santa Cruz is arid along the Atlantic coast and in the central portion between 46° and 50°S. With the exception of certain valleys at Puerto Deseado (Port Desired) and in the transverse basins which occur as far south as Puerto San Julian, and which contain several cattle farms, few spots are capable of cultivation, the pastures being poor, water insufficient and salt lagunas fairly numerous. Puerto Deseado is the outlet for the produce of the Andean region situated between Lakes Buenos Aires and Pueyrredon.

Into this inlet there flowed at the time of the conquest a voluminous river, which subsequently disappeared, but returned again to its ancient bed, owing to the river Fenix, one of its affluents, which had deviated to the west, regaining its original direction. Lake Buenos Aires, the largest lake in Patagonia, measuring 120 kilometers (75 miles) in length, poured its waters into the Atlantic even in post-Glacial times by means of the river Deseado; and it is so depicted on the maps of the 17th and 18th centuries; and so too did Lake Pueyrredon, which, through the action of erosion, now empties itself westward, through the river Las Heras, into the Calen inlet of the Pacific, in 48°S.

San Julian on Puerto San Julian, where Ferdinand Magellan wintered, was the centre of a cattle farming colony, and colonists have pushed into the interior up the valley of a now extinct river which in comparatively recent times carried down to Puerto San Julian the waters of Lakes Volcan, Beigrano, Azara, Nansen, and some other lakes which now drain into the river Mayer and so into Lake San Martin. The valleys of the Rio Chico throughout their whole extent, as well as those of Lake Shehuen, afford excellent grazing, and around Lakes Belgrano, Burmeister and Rio Mayer and San Martin there are spots suitable for cultivation. In the Cretaceous hills which flank the Cordillera important lignite beds and deposits of mineral oils have been discovered. The Rio Santa Cruz, originally explored by Captain Fitzroy and Charles Darwin, is an important artery of communication between the regions bordering upon the Cordillera and the Atlantic. In Santa Cruz bay an important trade centre has been established. But the present cattle region par excellence of Patagonia is the department of Rio Gallegos, the farms extending from the Atlantic to the Cordillera. Puerto Gallegos itself is an important business center, which bids fair to rival the Chilean colony of Punta Arenas, on the Straits of Magellan. Owing to the produce of the cattle farms established there, the working of coal in the neighborhood, and the export of timber from the surrounding forests, the town of Punta Arenas is in a flourishing condition. Its population in 1911 numbered about 4000. But the colonization of the western (Chilean) coast has generally failed, principally owing to the adverse climatic conditions of the Cordillera in those latitudes.

Climate

The climate is less severe than was supposed by early travelers. The east slope is warmer than the west, especially in summer, as a branch of the southern equatorial current reaches its shores, whereas a cold current washes the west coast. At Puerto Montt, on the inlet behind Chiloé Island. the mean annual temperature is 11 °C (52°F) and the average extremes 25.5 °C (78°F) and -1.5 °C (29.5°F), whereas at Bahia Blanca near the Atlantic coast and just outside the northern confines of Patagooia the annual temperature is 15C (59°F) and the range much greater. At Punta Arenas, in the extreme south, the mean temperature is 6 °C (43°F) and the average extremes 24.5 °C (76°F) and -2 °C (28°F). The prevailing winds are westerly, and the westward slope has a much heavier precipitation than the eastern; thus at Puerto Montt the mean annual precipitation is 2.46 m (97 inches), but at Bahia Blanca it is 480 mm (19 inches). At Punta Arenas it is 560 mm (22 inches).

Fauna

The guanaco, the puma, the zorro or Brazilian fox (Canis azarae), the zorrino or Mephitis patagonica (a kind of skunk), and the tuco-tuco or Ctenomys niagellanicus (a rodent) are the most characteristic mammals of the Patagonian plains. The guanaco roam in herds over the country and form with the rhea (Rhea americana, and more rarely Rhea darwinii) the chief means of subsistence for the natives, who hunt them on horseback with dogs and bolas. Bird-life is often wonderfully abundant. The carancho or carrion-hawk (Polyborus tharus) is one of the characteristic objects of a Patagonian landscape; the presence of long-tailed green parakeets (Conurus cyanolysius) as far south as the shores of the strait attracted the attention of the earlier navigators; and hummingbirds may be seen flying amidst the falling snow. Of the many kinds of water-fowl it is enough to mention the flamingo, the upland goose, and in the strait the remarkable steamer duck.

History

Patagonia was discovered in 1520 by Ferdinand Magellan, who on his passage along the coast named many of the more striking features — Gulf of San Matias, Cape of 11,000 Virgins (now simply Cape Virgenes). Patagonia means ‘land of the big feet’. Legends say that Magellan and his crew saw a tribe of nine-foot tall giants with big feet. He named the tribe the Patagons or big feet. Later explorers confirmed the existence of and made drawings of the Patagons. Cortés also claimed to see a tribe of giants of the same height in the Andes.

By 1611 the Patagonian god Setebos (Settaboth in Pigafetta) was familiar to the hearers of the Tempest. Rodrigo de Isla, despatched inland in 1535 from San Matias by Alcazava Sotomayor (on whom western Patagonia had been conferred by the king of Spain), was the first to traverse the great Patagonian plain, and, but for the mutiny of his men, he would have struck across the Andes to the Chilean side. Pedro de Mendoza, on whom the country was next bestowed, lived to found Buenos Aires, but not to carry his explorations to the south. Alonzo de Camargo (1539), Juan Ladrilleros (1557) and Hurtado de Mendoza (1558) helped to make known the western coasts, and Sir Francis Drake’s voyage in 1577 down the eastern coast through the strait and northward by Chile and Peru was memorable for several reasons; but the geography of Patagonia owes more to Pedro Sarmiento de Gamboa (1579-1580), who, devoting himself especially to the south-west region, made careful and accurate surveys. The Spanish government neglected the settlement that he founded at Nombre de Dios and San Felipe, and the latter was in such a miserable state when Thomas Cavendish visited it in 1587 that he called it Port Famine. The district in the neighborhood of Puerto Deseado, explored by John Davis about the same period, was taken possession of by Sir John Narborough in the name of King Charles II of England in 1669. In the second half of the 18th century knowledge of Patagonia was augmented by Byron (1764-1765), Samuel Wallis (1766) and L.A. de Bougainville (1766); Thomas Falkner, a Jesuit who resided near forty years in those parts, published his Description of Patagonia (Hereford, 1774); Francesco Viedma founded El Carmen, and Antonio advanced inland to the Andes (1782); and Basilio Villarino ascended the Rio Negro (1782). The Adventure and Beagle expeditions under Philip King (1826-1830) and Robert Fitzroy (1832-1836) were of first-rate importance, the latter especially from the participation of Charles Darwin; but of the interior of the country nothing was observed except 200 miles (320 km) of the course of the Santa Cruz. Captain George Chaworth Musters in 1869 wandered in company with a band of Tehuelches through the whole length of the country from the strait to the Manzaneros in the north-west, and collected a great deal of information about the people and their mode of life.

The history of Latin America is a rich one. This country has long been known for their festive dancing, colorful clothes, delicious food, and warm-hearted people. However, one interesting question has surfaced time and time again - “Did Latin Americans actually speak Latin?”

Interestingly, Latin was one of the many different Italic languages spoken in central Italy during the 5th century. The area known as Latium or Lazio and then again in Rome were specifically fluent in Latin. Historians tell us that there were early inscriptions discovered in Latin that date back to the 6th century. These inscriptions were written in a various forms of the Greek alphabet and then brought over to Italy by the colonist from Greece.

Then, Rome expanded its influence and power over some parts of Italy and then into various areas of Europe. Over time, the Roman Empire became massive, stretching across a large region of North Africa, Europe, and even the Middle East. Throughout the Roman Empire, Latin was a common language used on an every day basis. In fact, the Roman people were very literate, which is why we see many great Latin authors from Rome.

In addition, the Greeks remained the lingua franca in eastern Mediterranean and the Romans, who were highly educated, became very fluent in both languages. The earliest surviving examples of Latin literature were in fact the translations from Greek plays, along with a farming manual that is estimated back to around 150 BC.

From there, we know that Latin was commonly used in early Latin literature, classical Latin, and various means from colloquial Latin, which was called Vulgar Latin. However, there were some writers that included Petronius and Cicero that often spoke Vulgar Latin during work. What we have seen is the Latin language changing over the centuries with it moving away from the standards of literacy into modern Romance/Italic languages, which would include French, Italian, Portuguese, Romanian, Catalan, Spanish, and so on.

When the Roman Empire collapsed in AD 476, the Latin language continued being used for literacy throughout central and Western Europe. Then, Medieval Latin literature became popular in many different styles that included scholarly work of Anglo-Saxon and Irish writers to people giving sermons. Then in the 15th century, Latin started to lose its position as the standard language spoken and written throughout most of Europe, being replaced by versions of vernacular languages, which were actually descendants of Latin or with its influence.

The Latin language of modern society was used significantly in the Roman Catholic Church. However, by the 20th century, we see a decline in the use of Latin, although there are some areas that still use it extensively to include Vatican City. Another area where we commonly see Latin used is by biologists and various scientists. Interesting, for the Romans to write Latin there were 23 letters used, similar to the English alphabet but minus the letters J, U, and W.

When it comes to rich legacies left behind by pre-Hispanic cultures, Peru lands at the top of the list. At the hub of Peru is a city called Cuzco, which is the ancient capital of the Inca Empire. Cuzco, Peru is known as the archaeological capital of all South America, which is a complex culture that comes from the Inca and Spanish. In Cuzco, you can see this amazing blend by the Spanish colonial architecture and the famous Inca ruins.

Starting in the 14th century, Cuzco was the capital of the Incan Empire. However, in 1533, Francisco Pizarro, a Spanish leader came and conquered Peru, following a very difficult voyage that took him and his entourage through Panama and then over the Andes mountains. Once the Spanish arrived, they found massive riches to include gold. This incredible find pushed Peru into a new era that would make history.

One of the most fascinating aspects of the Incan capital is the architecture. There, you will discover massive cut-stone blocks that fit perfectly but without modern day mortar. One of the buildings is the temple of the sun called Coricancha, along with a fortress known as Sacsahuaman, both built with boulders weighing more than 190 tons. Now, consider that during this era, the people had no backhoes, no cranes, and no modern equipment to lift such enormous weight; we can only imagine the amazing challenge to complete the structures, and then the celebration once completed.

Keep in mind that the city of Cuzco was established in the form of a puma, using the fortress as the head and the Tullumayo and Huatanay Rivers as the tail. In addition, ancient Cuzco was located in the exact place as the modern city square, although twice as large. Then all around the palaces of the past kings was gravel, which was the site of important ceremonies. There are four roads going to the four corners, which were eventually paved. With so much attention to detail and the unbelievable engineering that went into building this city, it was breathtakingly beautiful.

You will discover that the city of Cuzco is also spelled in a number of ways to include Cusco, Qozqo, and Qosqo. However, no matter the name or the spelling, this ancient, Incan Empire capital today stands as a blend of modern buildings and amenities with colonial additions. Interestingly, the spelling “Qosqo” translates to “bellybutton” or “navel” in Quechua, which is a beautiful valley that supported civilization prior to the Incas. As visitors came to the city, they would hear chants of “Ama Sua, Ama Quella, Amam Lulla, which means, “Don’t lie, don’t steal, and don’t be lazy”.

When visiting Cuzco, Peru, you will be amazed and impressed at the artistry and techniques used to create this empire. Most of the structures have outlived earthquakes, living on for future generations to enjoy. The plaza was the core of the Suvos, or Four Regions of the Inca Empire, which stretches from Quito, Ecuador all the way to northern Chile. There in the plaza stood ceremonial and official buildings along with residences of the rulers. From this vantage point, fast runners could take messages from the center of the city out in all directions to form a network of communication.

All around Cuzco are varied populations to include artisan, agricultural, and industrial. Sadly, the Spanish destroyed a good number of the structures and what couldn’t be demolished was used to build churches and other buildings, many that still exist today. Getting to Cuzco, Peru is actually easy. Once there, you will find the climate to be very comfortable but keep in mind the rainy season is from November to March.

In addition to the ruins, the streets of the city are quaint, dotted with colonial red roofs, blue doors, and whitewashed walls. The people are hard working and warm, and very interested in outside visitors. In the city, there are great places to visit such as the San Blas church, the Cathedral, and the Art School. Other attractions worth seeing while in Cuzco, Peru include Qorikancha, the Sun Temple, which is best viewed at night when it is fully illuminated and the La Compania Church, a true masterpiece.

You might also plan a trip to Q’engo, a temple dedicated to Mother Earth, Puca Pukara, a fortress watchtower that has an amazing view, Lago, Lanlakuyoq, and Kusilluchayoq, believe to be sites used for ceremonies or observations, and the incredible Machu Picchu, one of the most magical places on earth. You can also visit the Sunday market called Chinceros located in the center of town, the Urubamba River Valley, which winds from Pisac to Ollantaytamob, the salt flats called Maras, or you might simply enjoy hiking or rafting down the Vilcamayu River.

Patagonia is that portion of South America which, to the east of the Andes, lies mainly south of the Rio Negro (41°S), and, to the west of the Andes, south of (42°S). The Chilean portion embraces the southern part of the region of Los Lagos, and the regions of Aysen and Magallanes (excluding the portion of Antarctica claimed by Chile). East of the Andes the Argentine portion of Patagonia is divided into four provinces:

A lake in Neuquén, Argentine portion of PatagoniaNeuquén, covering 36,324 sq. miles, including the triangle between the rivers Limay and Neuquen, and extending southward to the northern shore of Lake Nahuel-Huapi (41°S) and northward to the Rio Colorado;

Río Negro, covering 78,383 sq. miles, extending from the Atlantic to the Cordillera of the Andes, to the north of 42°S; Chubut, covering 86,751 sq. miles, embracing the region between 42° and 46°S; and Santa Cruz, which stretches from the last-named parallel as far south as the dividing line with Chile, and between Point Dungeness and the watershed of the Cordillera: an area of 94,186 sq. miles.

The general character of the Argentine portion of Patagonia is for the most part a region of vast steppe-like plains, rising in a succession of abrupt terraces about 100 meters (330 feet) at a time, and covered with an enormous bed of shingle almost bare of vegetation. In the hollows of the plains are ponds or lakes of brackish and fresh water. Towards the Andes the shingle gives place to porphyry, granite, and basalt lavas, animal life becomes more abundant and vegetation more luxuriant, acquiring the characteristics of the flora of the western coast, and consisting principally of southern beech and conifers.

Among the depressions by which the plateau is intersected transversely, the principal are the Gualichu, south of the Rio Negro, the Maquinchao and Valcheta (through which previously flowed the waters of lake Nahuel Huapi, which now feed the river Limay); the Senguerr, the Deseado. Besides these transverse depressions (some of them marking lines of ancient inter-oceanic communication), there are others which were occupied by more or less extensive lakes, such as the Yagagtoo, Musters, and Colhue Huapi, and others situated to the south of Puerto Deseado, in the centre of the country. In the central region volcanic eruptions, which have taken part in the formation of the plateau from the Tertiary period down to the present era, cover a large part with basaltic lava-caps; and in the western third more recent glacial deposits appear above the lava. There, in contact with folded Cretaceous rocks, uplifted by the Tertiary granite, erosion, caused principally by the sudden melting and retreat of the ice, aided by tectonic changes, has scooped out a deep longitudinal depression, which generally separates the plateau from the first lofty hills, the ridges generally called the pre-Cordillera, while on the west of these there is a similar longitudinal depression all along the foot of the snowy Andean Cordillera. This latter depression contains the richest and most fertile land of Patagonia.

The geological constitution is in accordance with the orographic physiognomy. The Tertiary plateau, flat on the east, gradually rising on the west, shows Upper Cretaceous caps at its base. First come Lower Cretaceous hills, raised by granite and dioritic rocks, undoubtedly of Tertiary origin, as in some cases these rocks have broken across the Tertiary beds, so rich in mammal remains; then follow, on the west, metamorphic schists of uncertain age; then quartzites appear, resting directly on the primitive granite and gneiss which form the axis of the Cordillela. Porphyritic rocks occur between the schists and the quartzites. The Tertiary deposits are greatly varied in character, and there is considerable difference of opinion concerning the succession and correlation of the beds.

Glaciers occupy the valleys of the main chain and some of the lateral ridges of the Cordillera, and descend to lakes San Martín, Viedma, Argentino and others in the same locality, strewing them with icebergs. In Patagonia an immense ice-sheet extended to the east of the present Atlantic coast during the first ice age, at the close of the Tertiary epoch, while, during the second glacial age in modern times, the terminal moraines have generally stopped, 30 miles (50 km) in the north and 50 miles (80 km) in the south, east of the summit of the Cordillera. These ice-sheets, which scooped out the greater part of the longitudinal depressions, and appear to have rapidly retreated to the point where the glaciers now exist, did not, however, in their retirement fill up with their detritus the fjords of the Cordillera, for these are now occupied by deep lakes on the east, and on the west by the Pacific channels, some of which are as much as 250 fathoms (460 m) in depth, and soundings taken in them show that the fjords are as usual deeper in the vicinity of the mountains than to the west of the islands. Several of the high peaks are still active volcanoes.

In so far as its main characteristics are concerned, Patagonia seems to be a portion of the Antarctic continent, the permanence of which dates from very recent times, as is evidenced by the apparent recent emergence of the islets around Chiloé, and by the general character of the pampean formation. Some of the promontories of Chiloé are still called huapi, the Araucanian equivalent for “islands”; and this may perhaps be accepted as perpetuating the recollection of the time when they actually were islands. They are composed of caps of shingle, with great, more or less rounded boulders, sand and volcanic ashes, precisely of the same form as occurs on the Patagonian plateau. From an examination of the pampean formation it is evident that in recent times the land of the province of Buenos Aires extended farther to the east, and that the advance of the sea, and the salt-water deposits left by it when it retired, forming some of the lowlands which occur on the littoral and in the interior of the pampas, are much more recent phenomena; and certain caps of shingle, derived from rocks of a different class from those of the neighbouring hills, which are observed on the Atlantic coasts of the same province, and increase in quantity and size towards the south, seem to indicate that the caps of shingle which now cover such a great part of the Patagonian territory recently extended farther to the east, over land which has now disappeared beneath the sea, while other marine deposits along the same coasts became converted into bays during the subsequent advance of the sea. There are besides, in the neighbourhood of the present coast, deposits of volcanic ashes, and the ocean throws up on its shores blocks of basaltic lava, which in all probability proceed from eruptions of submerged volcanoes now extinct. One fact, however, which apparently demonstrates with greater certainty the existence in recent times of land that is now lost, is the presence of remains of pampean mammals in Pleistocene deposits in the bay of San Julian and in Santa Cruz. The animals undoubtedly reached these localities from the east; it is not at all probable that they advanced from the north southwards across the plateau intersected at that cime by great rivers and covered by the ice-sheet. With the exception of the discoveries at the inlet of Ultima Esperanza, which is in close communication with the Atlantic valley of Río Gallegos, none of these remains have been discovered in the Andean regions.

On the upper plains of Neuquen territory thousands of cattle can be fed, and the forests around Lakes Tiaful and Nahuel-Huapi yield large quantities of valuable timber. The Neuquen river is not navigable, but as its waters are capable of being easily dammed in places, large stretches of land in its valley are utilized; but the lands on each side of its lower part are of little commercial value. As the Cordillera is approached the soil becomes more fertile, and suitable districts for the rearing of cattle and other agricultural purposes exist between the regions that surround the Tromen volcano and the first ridges of the Andes. Chos Malal, the capital of the territory, is situated in one of these valleys. More to the west is the mining region, in great part unexplored, but containing deposits of gold, silver, copper and lignite. In the centre of the territory, also in the neighbourhood of the mining districts, are the valleys of Norquin and Las Lajas, the general camp of the Argentine army in Patagonia, with excellent timber in the forest on the Andean slope. The wide valleys occur near Rio Malleo, Lake Huechulafquen, the river Chimehuin, and Vega de Chapelco, near Lake Lacar, where are situated villages of some importance, such as Junin de los Andes and San Martin de los Andes. Close to these are the famous apple orchards supposed to have been planted by the Jesuits in the 17th and 18th centuries. The river Collon Cura, the principal affluent of the river Limay, drains these regions. Lake Lacar is now a contributary of the Pacific, its outlet having been changed to the west, owing to a passage having been opened through the Cordillera.

The Rio Negro runs along a wide transverse depression. the middle part of which is followed by the railway which runs to the settlement of Neuquen at the confluence of the rivers Limay and Neuquen. In this depression are several settlements, among them Viedma, the capital of the Rio Negro territory, Pringles, General Conesa, Choele Choel and General Roca. To the south of the Rio Negro the Patagonian plateau is intersected by the depressions of the Gualicho and Maquinchao, which in former times directed the waters of two great rivers (now disappeared) to the gulf of San Matias, the first-named depression draining the network of the Collon Cura and the second the Nahuel Huapi lake system. In 42°S there is a third broad transverse depression, apparently the bed of another great river, now perished, which carried to the Atlantic the waters of a portion of the eastern slope of the Andes, between 41° and 42°30;S.

Chubut territory presents the same characteristics as the Rio Negro territory. Rawson, the capital, is situated at the mouth of the river Chubut on the Atlantic (42°30′S). The town was founded in 1865 by a group of colonists from Wales, assisted by the Argentine government; and its prosperity has led to the foundation of other important centres in the valley, such as Trelew and Gaiman, which is connected by railway with Puerto Madryn on Bahia Nueva. Here is the seat of the governor of the territory, and by 1895 the inhabitants of this part of the territory, composed principally of Argentines, Welsh and Italians, numbered 2585. The valley has been irrigated and cultivated, and produces the best wheat of the Argentine Republic. Between the Chubut and the Senguerr there are vast stretches of fertile land, spreading over the Andean region to the foot of the Cordillera and the lateral ridges of the Pre-Cordillera, and filling the basins of some desiccated lakes, which have been occupied since 1885, and farms and colonies founded upon them. The chief of these colonies is that of 16 de Octubre, formed in 1886, mainly by the inhabitants of Chubut colony, in the longitudinal valley which extends to the eastern foot of the Cordillera. Other rivers in this territory flow into the Pacific through breaches in the Cordillera, e.g. the upper affluents of the Futaleufu, Palena and Rio Cisnes. The principal affluent of the Palena, the Carrenleufu, carries off the waters of Lake General Paz, situated on the eastern slope of the Cordillera. Rio Pico, an affluent of the same river, receives nearly the whole of the waters of the extensive undulating plain which lies between the Rio Tecka and the Rio Senguerr to the east of the Cordillera, while the remainder are carried away by the affluents of Rio Jehua: the Cherque, Omkel, and Appeleg. This region contains auriferous drifts, but these, like the auriferous deposits, veins of galena and lignite in the mountains farther west which flank the Cordillera, have not been properly investigated. At Lake Fontana there are auriferous drifts and lignite deposits which abound in fossil plants of the Cretaceous age. The streams which form the rivers Mayo and Chalia join the tributaries of the Rio Aisen, which flows into the Pacific, watering in its course extensive and valuable districts where colonization has been initiated by Argentine settlers. Colonies have also been formed in the basin of Lakes Musters and Colhué Huapi; and on the coasts near the Atlantic, along Bahia Camarones and the Gulf of San Jorge, there are extensive farms.

The territory of Santa Cruz is arid along the Atlantic coast and in the central portion between 46° and 50°S. With the exception of certain valleys at Puerto Deseado (Port Desired) and in the transverse basins which occur as far south as Puerto San Julian, and which contain several cattle farms, few spots are capable of cultivation, the pastures being poor, water insufficient and salt lagunas fairly numerous. Puerto Deseado is the outlet for the produce of the Andean region situated between Lakes Buenos Aires and Pueyrredon.

Into this inlet there flowed at the time of the conquest a voluminous river, which subsequently disappeared, but returned again to its ancient bed, owing to the river Fenix, one of its affluents, which had deviated to the west, regaining its original direction. Lake Buenos Aires, the largest lake in Patagonia, measuring 120 kilometers (75 miles) in length, poured its waters into the Atlantic even in post-Glacial times by means of the river Deseado; and it is so depicted on the maps of the 17th and 18th centuries; and so too did Lake Pueyrredon, which, through the action of erosion, now empties itself westward, through the river Las Heras, into the Calen inlet of the Pacific, in 48°S.

San Julian on Puerto San Julian, where Ferdinand Magellan wintered, was the centre of a cattle farming colony, and colonists have pushed into the interior up the valley of a now extinct river which in comparatively recent times carried down to Puerto San Julian the waters of Lakes Volcan, Beigrano, Azara, Nansen, and some other lakes which now drain into the river Mayer and so into Lake San Martin. The valleys of the Rio Chico throughout their whole extent, as well as those of Lake Shehuen, afford excellent grazing, and around Lakes Belgrano, Burmeister and Rio Mayer and San Martin there are spots suitable for cultivation. In the Cretaceous hills which flank the Cordillera important lignite beds and deposits of mineral oils have been discovered. The Rio Santa Cruz, originally explored by Captain Fitzroy and Charles Darwin, is an important artery of communication between the regions bordering upon the Cordillera and the Atlantic. In Santa Cruz bay an important trade centre has been established. But the present cattle region par excellence of Patagonia is the department of Rio Gallegos, the farms extending from the Atlantic to the Cordillera. Puerto Gallegos itself is an important business center, which bids fair to rival the Chilean colony of Punta Arenas, on the Straits of Magellan. Owing to the produce of the cattle farms established there, the working of coal in the neighborhood, and the export of timber from the surrounding forests, the town of Punta Arenas is in a flourishing condition. Its population in 1911 numbered about 4000. But the colonization of the western (Chilean) coast has generally failed, principally owing to the adverse climatic conditions of the Cordillera in those latitudes.

Climate

The climate is less severe than was supposed by early travelers. The east slope is warmer than the west, especially in summer, as a branch of the southern equatorial current reaches its shores, whereas a cold current washes the west coast. At Puerto Montt, on the inlet behind Chiloé Island. the mean annual temperature is 11 °C (52°F) and the average extremes 25.5 °C (78°F) and -1.5 °C (29.5°F), whereas at Bahia Blanca near the Atlantic coast and just outside the northern confines of Patagooia the annual temperature is 15C (59°F) and the range much greater. At Punta Arenas, in the extreme south, the mean temperature is 6 °C (43°F) and the average extremes 24.5 °C (76°F) and -2 °C (28°F). The prevailing winds are westerly, and the westward slope has a much heavier precipitation than the eastern; thus at Puerto Montt the mean annual precipitation is 2.46 m (97 inches), but at Bahia Blanca it is 480 mm (19 inches). At Punta Arenas it is 560 mm (22 inches).

Fauna

The guanaco, the puma, the zorro or Brazilian fox (Canis azarae), the zorrino or Mephitis patagonica (a kind of skunk), and the tuco-tuco or Ctenomys niagellanicus (a rodent) are the most characteristic mammals of the Patagonian plains. The guanaco roam in herds over the country and form with the rhea (Rhea americana, and more rarely Rhea darwinii) the chief means of subsistence for the natives, who hunt them on horseback with dogs and bolas. Bird-life is often wonderfully abundant. The carancho or carrion-hawk (Polyborus tharus) is one of the characteristic objects of a Patagonian landscape; the presence of long-tailed green parakeets (Conurus cyanolysius) as far south as the shores of the strait attracted the attention of the earlier navigators; and hummingbirds may be seen flying amidst the falling snow. Of the many kinds of water-fowl it is enough to mention the flamingo, the upland goose, and in the strait the remarkable steamer duck.

History

Patagonia was discovered in 1520 by Ferdinand Magellan, who on his passage along the coast named many of the more striking features — Gulf of San Matias, Cape of 11,000 Virgins (now simply Cape Virgenes). Patagonia means ‘land of the big feet’. Legends say that Magellan and his crew saw a tribe of nine-foot tall giants with big feet. He named the tribe the Patagons or big feet. Later explorers confirmed the existence of and made drawings of the Patagons. Cortés also claimed to see a tribe of giants of the same height in the Andes.

By 1611 the Patagonian god Setebos (Settaboth in Pigafetta) was familiar to the hearers of the Tempest. Rodrigo de Isla, despatched inland in 1535 from San Matias by Alcazava Sotomayor (on whom western Patagonia had been conferred by the king of Spain), was the first to traverse the great Patagonian plain, and, but for the mutiny of his men, he would have struck across the Andes to the Chilean side. Pedro de Mendoza, on whom the country was next bestowed, lived to found Buenos Aires, but not to carry his explorations to the south. Alonzo de Camargo (1539), Juan Ladrilleros (1557) and Hurtado de Mendoza (1558) helped to make known the western coasts, and Sir Francis Drake’s voyage in 1577 down the eastern coast through the strait and northward by Chile and Peru was memorable for several reasons; but the geography of Patagonia owes more to Pedro Sarmiento de Gamboa (1579-1580), who, devoting himself especially to the south-west region, made careful and accurate surveys. The Spanish government neglected the settlement that he founded at Nombre de Dios and San Felipe, and the latter was in such a miserable state when Thomas Cavendish visited it in 1587 that he called it Port Famine. The district in the neighborhood of Puerto Deseado, explored by John Davis about the same period, was taken possession of by Sir John Narborough in the name of King Charles II of England in 1669. In the second half of the 18th century knowledge of Patagonia was augmented by Byron (1764-1765), Samuel Wallis (1766) and L.A. de Bougainville (1766); Thomas Falkner, a Jesuit who resided near forty years in those parts, published his Description of Patagonia (Hereford, 1774); Francesco Viedma founded El Carmen, and Antonio advanced inland to the Andes (1782); and Basilio Villarino ascended the Rio Negro (1782). The Adventure and Beagle expeditions under Philip King (1826-1830) and Robert Fitzroy (1832-1836) were of first-rate importance, the latter especially from the participation of Charles Darwin; but of the interior of the country nothing was observed except 200 miles (320 km) of the course of the Santa Cruz. Captain George Chaworth Musters in 1869 wandered in company with a band of Tehuelches through the whole length of the country from the strait to the Manzaneros in the north-west, and collected a great deal of information about the people and their mode of life.

The history of Latin America is a rich one. This country has long been known for their festive dancing, colorful clothes, delicious food, and warm-hearted people. However, one interesting question has surfaced time and time again - “Did Latin Americans actually speak Latin?”

Interestingly, Latin was one of the many different Italic languages spoken in central Italy during the 5th century. The area known as Latium or Lazio and then again in Rome were specifically fluent in Latin. Historians tell us that there were early inscriptions discovered in Latin that date back to the 6th century. These inscriptions were written in a various forms of the Greek alphabet and then brought over to Italy by the colonist from Greece.

Then, Rome expanded its influence and power over some parts of Italy and then into various areas of Europe. Over time, the Roman Empire became massive, stretching across a large region of North Africa, Europe, and even the Middle East. Throughout the Roman Empire, Latin was a common language used on an every day basis. In fact, the Roman people were very literate, which is why we see many great Latin authors from Rome.

In addition, the Greeks remained the lingua franca in eastern Mediterranean and the Romans, who were highly educated, became very fluent in both languages. The earliest surviving examples of Latin literature were in fact the translations from Greek plays, along with a farming manual that is estimated back to around 150 BC.

From there, we know that Latin was commonly used in early Latin literature, classical Latin, and various means from colloquial Latin, which was called Vulgar Latin. However, there were some writers that included Petronius and Cicero that often spoke Vulgar Latin during work. What we have seen is the Latin language changing over the centuries with it moving away from the standards of literacy into modern Romance/Italic languages, which would include French, Italian, Portuguese, Romanian, Catalan, Spanish, and so on.

When the Roman Empire collapsed in AD 476, the Latin language continued being used for literacy throughout central and Western Europe. Then, Medieval Latin literature became popular in many different styles that included scholarly work of Anglo-Saxon and Irish writers to people giving sermons. Then in the 15th century, Latin started to lose its position as the standard language spoken and written throughout most of Europe, being replaced by versions of vernacular languages, which were actually descendants of Latin or with its influence.

The Latin language of modern society was used significantly in the Roman Catholic Church. However, by the 20th century, we see a decline in the use of Latin, although there are some areas that still use it extensively to include Vatican City. Another area where we commonly see Latin used is by biologists and various scientists. Interesting, for the Romans to write Latin there were 23 letters used, similar to the English alphabet but minus the letters J, U, and W.

When it comes to rich legacies left behind by pre-Hispanic cultures, Peru lands at the top of the list. At the hub of Peru is a city called Cuzco, which is the ancient capital of the Inca Empire. Cuzco, Peru is known as the archaeological capital of all South America, which is a complex culture that comes from the Inca and Spanish. In Cuzco, you can see this amazing blend by the Spanish colonial architecture and the famous Inca ruins.

Starting in the 14th century, Cuzco was the capital of the Incan Empire. However, in 1533, Francisco Pizarro, a Spanish leader came and conquered Peru, following a very difficult voyage that took him and his entourage through Panama and then over the Andes mountains. Once the Spanish arrived, they found massive riches to include gold. This incredible find pushed Peru into a new era that would make history.

One of the most fascinating aspects of the Incan capital is the architecture. There, you will discover massive cut-stone blocks that fit perfectly but without modern day mortar. One of the buildings is the temple of the sun called Coricancha, along with a fortress known as Sacsahuaman, both built with boulders weighing more than 190 tons. Now, consider that during this era, the people had no backhoes, no cranes, and no modern equipment to lift such enormous weight; we can only imagine the amazing challenge to complete the structures, and then the celebration once completed.

Keep in mind that the city of Cuzco was established in the form of a puma, using the fortress as the head and the Tullumayo and Huatanay Rivers as the tail. In addition, ancient Cuzco was located in the exact place as the modern city square, although twice as large. Then all around the palaces of the past kings was gravel, which was the site of important ceremonies. There are four roads going to the four corners, which were eventually paved. With so much attention to detail and the unbelievable engineering that went into building this city, it was breathtakingly beautiful.

You will discover that the city of Cuzco is also spelled in a number of ways to include Cusco, Qozqo, and Qosqo. However, no matter the name or the spelling, this ancient, Incan Empire capital today stands as a blend of modern buildings and amenities with colonial additions. Interestingly, the spelling “Qosqo” translates to “bellybutton” or “navel” in Quechua, which is a beautiful valley that supported civilization prior to the Incas. As visitors came to the city, they would hear chants of “Ama Sua, Ama Quella, Amam Lulla, which means, “Don’t lie, don’t steal, and don’t be lazy”.

When visiting Cuzco, Peru, you will be amazed and impressed at the artistry and techniques used to create this empire. Most of the structures have outlived earthquakes, living on for future generations to enjoy. The plaza was the core of the Suvos, or Four Regions of the Inca Empire, which stretches from Quito, Ecuador all the way to northern Chile. There in the plaza stood ceremonial and official buildings along with residences of the rulers. From this vantage point, fast runners could take messages from the center of the city out in all directions to form a network of communication.

All around Cuzco are varied populations to include artisan, agricultural, and industrial. Sadly, the Spanish destroyed a good number of the structures and what couldn’t be demolished was used to build churches and other buildings, many that still exist today. Getting to Cuzco, Peru is actually easy. Once there, you will find the climate to be very comfortable but keep in mind the rainy season is from November to March.

In addition to the ruins, the streets of the city are quaint, dotted with colonial red roofs, blue doors, and whitewashed walls. The people are hard working and warm, and very interested in outside visitors. In the city, there are great places to visit such as the San Blas church, the Cathedral, and the Art School. Other attractions worth seeing while in Cuzco, Peru include Qorikancha, the Sun Temple, which is best viewed at night when it is fully illuminated and the La Compania Church, a true masterpiece.

You might also plan a trip to Q’engo, a temple dedicated to Mother Earth, Puca Pukara, a fortress watchtower that has an amazing view, Lago, Lanlakuyoq, and Kusilluchayoq, believe to be sites used for ceremonies or observations, and the incredible Machu Picchu, one of the most magical places on earth. You can also visit the Sunday market called Chinceros located in the center of town, the Urubamba River Valley, which winds from Pisac to Ollantaytamob, the salt flats called Maras, or you might simply enjoy hiking or rafting down the Vilcamayu River.

The carnival is a celebration that is seen throughout South America, with festivities somewhat unique from country to country. For four days, starting on a Saturday and ending on Fat Tuesday (Mardi Gras), you will have the most amazing time imaginable. As an example, in Rio de Janeiro, the carnival occurs at the peak time during the summer months. Literally thousands of people come from around the globe to watch and participate in the festivities.

Although the origin of this carnival is unknown, most experts agree the event started as some type of pagan celebration somewhere in Greece or Rome. Carnival balls were introduced from Italy in the late 19th century although they were at their most popular from 1930 through the 1950s. In fact, two of the most famous of these balls include those held at the Municipal Theater and the Copacabana Palace.

In addition, during the 1930s the Samba Parade began where it eventually settled at the Sambodrome in the downtown area, in 1984. The Samba is of West African heritage that consists of rhythmic beating of the drums that get your feet moving and soon, dancing. All along the parade route will be Escola dancers displaying their talent to the beat of the Samba drums.

Although the Samba Parade is a major part of the carnival festivities, there are many other things going on. For instance, you can get involved with Banda de Ipanema, which was founded in 1964 and draws in more than 15,000 people. When celebrating the carnival in Brazil, the Portuguese tradition is called Entrudo, which involves throwing flower and mud at unsuspecting spectators. The streets are flooded with all types of colorful parades, some that compete against each other.

Remember, different countries and cities have their own unique style of the carnival. Take Salvador for example, there the music is provided by groups known as Trios Electricos. The sound and volume is so intense that it can almost be deafening. Then in Recife, the music style is called Frevo, and in Bahia, you hear music that sounds more like religious tunes called Afoxe.

If you plan to go watch the proceedings of the Carnival while in South America, we highly recommend that you dress in comfortable clothing and most importantly, blend in. Remember, if you look like a tourist, you will have flour and mud thrown on you. Therefore, the more casual you can dress the better. Additionally, because the crowds are so large, there are unfortunately some pickpockets so keep anything of value at home or at the hotel.

Colombia is a magnificent place that offers rainforests, beaches, mountain ranges, beautiful cities, and warm, inviting people. Although there are many incredible places in the world, Colombia deserves to rank near or at the top. Unfortunately, ongoing cocaine cartels and guerilla war has put a damper on travel and even given Colombia the nickname “Locombia”, which translates to “mad country.”

Sadly, still today an average of 3,000 people are abducted, most being officials. However, this violence has even extended to innocent backpackers out for an adventure to discover the backcountry. Even so, by staying within the safe zones in the major cities and tourist areas, and avoiding the parts of Colombia known for danger, you can travel there to enjoy the country’s beauty and rich culture. We recommend you pay attention to any travel news and/or alerts, and work with a reputable travel agent who will steer you in the right direction.

To ensure your safety, remember that travel to the urban areas by any means of transportation is considered highly dangerous. Additionally, when visiting Colombia, do not take or wear any expensive jewelry or clothing, leave high priced cameras, shoes, and purses at home, stay away from any type of public gatherings or crowds, and use the local police only if absolutely necessary in that many have reputations for being two-sided. Finally, regarding safety, if you were approached by a stranger offering to sell you a drink or cigarettes, never accept them as they could be laced with a soporific drug called Borrachero.

In the early years, you would see scattered pockets of various cultures to include the Muisca, Quimbaya, San Agustin, Sinu, Tayrona, and Tierradentro. Many of these tribes were highly skilled in making pottery and gold work. In fact, through years of excavations, some of these treasures have been uncovered in burial chambers, along with magnificent rock paintings, giving us a better glimpse of life in the early, pre-Colombia times.

In 1499, a companion of Christopher Columbus named Alonso de Ojeda came to the Guajira Peninsula, which was the beginning of some of the largest number of expeditions. When the Spaniards arrived, they were merely tolerated by the Indians but when slavery began and land was confiscated, the Indians rebelled. Interestingly, much of modern day Colombia was conquered by the Spanish and in 1544, Colombia was incorporated into Peru. However, in 1739, Colombia split from Peru, becoming a part of the New Granada.

The Spanish took more than land and the Indian’s freedom, they also took over the commerce and taxes, which during the 18th century, led to a huge protest. During this time, autonomy occurred but not until 1819 was independence won. Even with this incredible victory, unrest continued over the years between the Liberals and Conservatives. Violence in Colombia had rose to an all-time high by 1990 due to the establishment of paramilitary death squads and the powerful drug cartels. However, the head of the Medellin cocaine cartel was captured in 1991 and a year later escaped but when found, he was assassinated.

One of the greatest challenges of Colombia today is the continuing unrest associated with drug trafficking. This internal conflict has placed this country among the 10 bloodiest places in the entire world. Keep in mind that while this country has struggled from the beginning, there are still wonderful people who want desperately to take back control. In fact, in an effort to help, the United States approved $1.3 billion in aid to support the government in winning the war against the drug cartels and guerrillas.

Again, if you stay within the safe zones, Colombia has much to offer, which includes a number of different ethnic groups that bring with them fabulous cultures, arts, and folklore. As the fourth largest country in all of South America yet the only one that has coastlines on both the Pacific and Caribbean oceans, this is a remarkable country with extreme diversity. Colombia borders with Panama to the northwest, Brazil to the southeast, Venezuela to the east, Peru to the south, and then Ecuador to the southwest.

You will notice that the western regions of Colombia are mountainous, with the Cordillera de los Andes running the entire length of South America, some 5,000 miles. In addition to the beautiful mountains, there are two valleys called Valle del Magdalena and Valle del Cauca. Then when you reach the territory to the east of the Andes, you will find that more than 50% is lowland covered with dense rainforest where rivers meander through.

Another interesting fact about Colombia is that this country has the highest number of animals and plants per unit area of any other country on the planet. For ex