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Natural Wonders

Zion National Park

Zion National Park is located in the Southwestern United States, near Springdale, Utah. A prominent feature of the 229-square-mile park is Zion Canyon, which is 15 miles long and up to half a mile deep, cut through the reddish and tan-colored Navajo Sandstone by the North Fork of the Virgin River. The lowest elevation is 3,666 ft at Coalpits Wash and the highest elevation is 8,726 ft at Horse Ranch Mountain. Located at the junction of the Colorado Plateau, Great Basin, and Mojave Desert regions, the parks unique geography and variety of life zones allow for unusual plant and animal diversity. Numerous plant species as well as 289 species of birds, 75 mammals, and 32 reptiles inhabit the parks four life zones: desert, riparian, woodland, and coniferous forest. Zion National Park includes mountains, canyons, buttes, mesas, monoliths, rivers, slot canyons, and natural arches. Human habitation of the area started about 8,000 years ago with small family groups of Native Americans; the semi-nomadic Basketmaker Anasazi stem from one of these groups. In turn, the Virgin Anasazi culture developed as the Basketmakers settled in permanent communities. A different group, the Parowan Fremont, lived in the area as well. Both groups moved away by 1300 and were replaced by the Parrusits and several other Southern Paiute subtribes. Mormons came into the area in 1858 and settled there in the early 1860s. In 1909 the President of the United States, William Howard Taft, named the area a National Monument to protect the canyon, under the name of Mukuntuweap National Monument. In 1918, however, the acting director of the newly created National Park Service changed the parks name to Zion, the name used by the Mormons. According to historian Hal Rothman: "The name change played to a prevalent bias of the time. Many believed that Spanish and Indian names would deter visitors who, if they could not pronounce the name of a place, might not bother to visit it. The new name, Zion, had greater appeal to an ethnocentric audience." The United States Congress established the monument as a National Park on November 19, 1919. The Kolob section was proclaimed a separate Zion National Monument in 1937, but was incorporated into the park in 1956. The geology of the Zion and Kolob canyons area includes 9 formations that together represent 150 million years of mostly Mesozoic-aged sedimentation. At various periods in that time warm, shallow seas, streams, ponds and lakes, vast deserts, and dry near-shore environments covered the area. Uplift associated with the creation of the Colorado Plateaus lifted the region 10,000 feet starting 13 million years ago.

Glacier National Park

Glacier National Park is a national park located in the U.S. state of Montana, on the Canada–United States border with the Canadian provinces of Alberta and British Columbia. The park encompasses over 1 million acres and includes parts of two mountain ranges, over 130 named lakes, more than 1,000 different species of plants, and hundreds of species of animals. This vast pristine ecosystem is the centerpiece of what has been referred to as the "Crown of the Continent Ecosystem", a region of protected land encompassing 16,000 square miles . The region that became Glacier National Park was first inhabited by Native Americans. Upon the arrival of European explorers, it was dominated by the Blackfeet in the east and the Flathead in the western regions. Soon after the establishment of the park on May 11, 1910, a number of hotels and chalets were constructed by the Great Northern Railway. These historic hotels and chalets are listed as National Historic Landmarks and a total of 350 locations are on the National Register of Historic Places. By 1932 work was completed on the Going-to-the-Sun Road, later designated a National Historic Civil Engineering Landmark, which provided greater accessibility for automobiles into the heart of the park. The mountains of Glacier National Park began forming 170 million years ago when ancient rocks were forced eastward up and over much younger rock strata. Known as the Lewis Overthrust, these sedimentary rocks are considered to have some of the finest fossilized examples of extremely early life found anywhere on Earth. The current shapes of the Lewis and Livingston mountain ranges and positioning and size of the lakes show the telltale evidence of massive glacial action, which carved U-shaped valleys and left behind moraines which impounded water, creating lakes. Of the estimated 150 glaciers which existed in the park in the mid-19th century, only 25 active glaciers remained by 2010. Scientists studying the glaciers in the park have estimated that all the glaciers may disappear by 2030 if the current climate patterns persist. Glacier National Park has almost all its original native plant and animal species. Large mammals such as the grizzly, moose, and mountain goat, as well as rare or endangered species like the wolverine and Canadian lynx, inhabit the park. Hundreds of species of birds, more than a dozen fish species, and a few reptile and amphibian species have been documented. The park has numerous ecosystems ranging from prairie to tundra. Notably, the easternmost forests of western redcedar and hemlock grow in the southwest portion of the park. Large forest fires are uncommon in the park. However, in 2003 over 13% of the park burned. Glacier National Park borders Waterton Lakes National Park in Canada—the two parks are known as the Waterton-Glacier International Peace Park and were designated as the worlds first International Peace Park in 1932. Both parks were designated by the United Nations as Biosphere Reserves in 1976, and in 1995 as World Heritage sites.

Great Barrier Reef

The Great Barrier Reef is the world's largest coral reef system composed of over 2,900 individual reefs and 900 islands stretching for over 2,300 kilometres over an area of approximately 344,400 square kilometres . The reef is located in the Coral Sea, off the coast of Queensland, Australia. The Great Barrier Reef can be seen from outer space and is the world's biggest single structure made by living organisms. This reef structure is composed of and built by billions of tiny organisms, known as coral polyps. It supports a wide diversity of life and was selected as a World Heritage Site in 1981. CNN labelled it one of the seven natural wonders of the world. The Queensland National Trust named it a state icon of Queensland. A large part of the reef is protected by the Great Barrier Reef Marine Park, which helps to limit the impact of human use, such as fishing and tourism. Other environmental pressures on the reef and its ecosystem include runoff, climate change accompanied by mass coral bleaching, and cyclic population outbreaks of the crown-of-thorns starfish. According to a study published in October 2012 by the Proceedings of the National Academy of Sciences, the reef has lost more than half its coral cover since 1985. The Great Barrier Reef has long been known to and used by the Aboriginal Australian and Torres Strait Islander peoples, and is an important part of local groups' cultures and spirituality. The reef is a very popular destination for tourists, especially in the Whitsunday Islands and Cairns regions. Tourism is an important economic activity for the region, generating over $3 billion per year. In November 2014, Google launched Google Underwater Street View in 3D of the Great Barrier Reef.

Namib Desert

The Namib is a coastal desert in southern Africa. The name Namib is of Nama origin and means "vast place". According to the broadest definition, the Namib stretches for more than 2,000 kilometres along the Atlantic coasts of Angola, Namibia, and South Africa, extending southward from the Carunjamba River in Angola, through Namibia and to the Olifants River in Western Cape, South Africa. The Namib's northernmost portion, which extends 450 kilometres from the Angola-Namibia border, is known as Moçâmedes Desert, while its southern portion approaches the neighboring Kalahari Desert. From the Atlantic coast eastward, the Namib gradually ascends in elevation, reaching up to 200 kilometres inland to the foot of the Great Escarpment. Annual precipitation ranges from 2 millimetres in the most arid regions to 200 millimetres at the escarpment, making the Namib the only true desert in southern Africa. Having endured arid or semi-arid conditions for roughly 55–80 million years, the Namib may be the oldest desert in the world. The desert geology consists of sand seas near the coast, while gravel plains and scattered mountain outcrops occur further inland. The sand dunes, some of which are 300 metres high and span 32 kilometres long, are the second largest in the world after the Badain Jaran Desert dunes in China. Temperatures along the coast are stable and generally range between 9–20 °C annually, while temperatures further inland are variable—summer daytime temperatures can exceed 45 °C while nights can be freezing. Fogs that originate offshore from the collision of the cold Benguela Current and warm air from the Hadley Cell create a fog belt that frequently envelops parts of the desert. Coastal regions can experience more than 180 days of thick fog a year. While this has proved a major hazard to ships—more than a thousand wrecks litter the Skeleton Coast—it is a vital source of moisture for desert life. The Namib is almost completely uninhabited by humans except for several small settlements and indigenous pastoral groups, including the Ovahimba and Obatjimba Herero in the north, and the Topnaar Nama in the central region. Owing to its antiquity, the Namib may be home to more endemic species than any other desert in the world. Most of the desert wildlife is arthropods and other small animals that live on little water, although larger animals inhabit the northern regions. Near the coast, the cold ocean water is rich in fishery resources and supports populations of brown fur seals and shorebirds, which serve as prey for the Skeleton Coast's lions. Further inland, the Namib-Naukluft National Park, the largest game park in Africa, supports populations of African Bush Elephants, Mountain Zebras, and other large mammals. Although the outer Namib is largely barren of vegetation, lichens and succulents are found in coastal areas, while grasses, shrubs, and ephemeral plants thrive near the escarpment. A few types of trees are also able to survive the extremely arid climate.

Canaima National Park

Canaima National Park is a 30,000 km2 park in south-eastern Venezuela that borders Brazil and Guyana. It is located in Bolívar State, and roughly occupies the same area as the Gran Sabana region. The park was established on 12 June 1962. It is the second largest park in the country, after Parima-Tapirapecó, and sixth biggest national park in the world. It is the size of Belgium or Maryland. About 65% of the park is occupied by plateaus of rock called tepuis, which are a kind of plateau of millions of years old, with vertical walls and almost flat tops. These constitute a unique biological environment and are also of great geological interest. Their sheer cliffs and waterfalls create spectacular landscapes. The most famous tepuis in the park are Mount Roraima, the tallest and easiest to climb, and Auyantepui, the site of Angel Falls. The tepuis are sandstone and date back to a time when South America and Africa were part of a super-continent. The park is home to indigenous Pemon Indians, part of the Carib linguistic group. The Pemon have an intimate relationship with the tepuis, and believe they are the home of the Mawari spirits. The park is relatively remote, with only a few roads connecting towns. Most transport within the park is done by light plane from the airstrips built by various Capuchin missions, or by foot and canoe. Pemons have developed some basic and luxurious camps, which are mainly visited by tourists from across the world. In 1994, the Canaima National Park was named a World Heritage Site by UNESCO, as a natural reserve that has abrupt relief special and unique around the world, the tepuis.

Crater Lake National Park

Crater Lake National Park is a United States National Park located in southern Oregon. Established in 1902, Crater Lake National Park is the fifth oldest national park in the United States and the only one in the state of Oregon. The park encompasses the caldera of Crater Lake, a remnant of a destroyed volcano, Mount Mazama, and the surrounding hills and forests. The lake is 1,943 feet deep at its deepest point, which makes it the deepest lake in the United States, the second deepest in North America and the ninth deepest in the world. Crater Lake is often referred to as the seventh deepest lake in the world, but this former listing excludes the approximately 3,000-foot depth of subglacial Lake Vostok in Antarctica, which resides under nearly 13,000 feet of ice, and the recent report of a 2,740-foot maximum depth for Lake O'Higgins/San Martin, located on the border of Chile and Argentina. However, when comparing its average depth of 1,148 feet to the average depth of other deep lakes, Crater Lake becomes the deepest in the Western Hemisphere and the third deepest in the world. The impressive average depth of this volcanic lake is due to the nearly symmetrical 4,000-foot deep caldera formed 7,700 years ago during the violent climactic eruptions and subsequent collapse of Mount Mazama and the relatively moist climate that is typical of the crest of the Cascade Range. The caldera rim ranges in elevation from 7,000 to 8,000 feet . The United States Geological Survey benchmarked elevation of the lake surface itself is 6,178 feet . This National Park encompasses 183,224 acres . Crater Lake has no streams flowing into or out of it. All water that enters the lake is eventually lost from evaporation or subsurface seepage. The lake's water commonly has a striking blue hue, and the lake is re-filled entirely from direct precipitation in the form of snow and rain.

Niagara Falls

Niagara Falls is the collective name for three waterfalls that straddle the international border between Canada and the United States; more specifically, between the province of Ontario and the state of New York. They form the southern end of the Niagara Gorge. From largest to smallest, the three waterfalls are the Horseshoe Falls, the American Falls and the Bridal Veil Falls. The Horseshoe Falls lie mostly on the Canadian side and the American Falls entirely on the American side, separated by Goat Island. The smaller Bridal Veil Falls are also on the American side, separated from the other waterfalls by Luna Island. The international boundary line was originally drawn through Horseshoe Falls in 1819, but the boundary has long been in dispute due to natural erosion and construction. Located on the Niagara River, which drains Lake Erie into Lake Ontario, the combined falls form the highest flow rate of any waterfall in the world, with a vertical drop of more than 165 feet . Horseshoe Falls is the most powerful waterfall in North America, as measured by vertical height and flow rate. The falls are 17 miles north-northwest of Buffalo, New York, and 75 miles south-southeast of Toronto, between the twin cities of Niagara Falls, Ontario, and Niagara Falls, New York. Niagara Falls were formed when glaciers receded at the end of the Wisconsin glaciation , and water from the newly formed Great Lakes carved a path through the Niagara Escarpment en route to the Atlantic Ocean. While not exceptionally high, the Niagara Falls are very wide. More than six million cubic feet of water falls over the crest line every minute in high flow, and almost four million cubic feet on average. The Niagara Falls are renowned both for their beauty and as a valuable source of hydroelectric power. Balancing recreational, commercial, and industrial uses has been a challenge for the stewards of the falls since the 19th century.

Ha Long Bay

Hạ Long Bay is a UNESCO World Heritage Site, and a popular travel destination, in Quảng Ninh Province, Vietnam. Administratively, the bay belongs to Hạ Long City, Cẩm Phả town, and the part of Vân Đồn District. The bay features thousands of limestone karsts and isles in various sizes and shapes. Hạ Long Bay is a center of a larger zone which includes Bái Tử Long bay to the northeast, and Cát Bà islands to the southwest. These larger zones share similar geological, geographical, geomorphological, climate, and cultural characters. Hạ Long Bay has an area of around 1,553 km2, including 1,960-2,000 islets, most of which are limestone. The core of the bay has an area of 334 km2 with a high density of 775 islets. The limestone in this bay has gone through 500 million years of formation in different conditions and environments. The evolution of the karst in this bay has taken 20 million years under the impact of the tropical wet climate. The geo-diversity of the environment in the area has created biodiversity, including a tropical evergreen biosystem, oceanic and sea shore biosystem. Hạ Long Bay is home to 14 endemic floral species and 60 endemic faunal species. Historical research surveys have shown the presence of prehistorical human beings in this area tens of thousands years ago. The successive ancient cultures are the Soi Nhụ culture around 18,000-7000 BC, the Cái Bèo culture 7000-5000 BC and the Hạ Long culture 5,000-3,500 years ago. Hạ Long Bay also marked important events in the history of Vietnam with many artifacts found in Bài Thơ Mount, Đầu Gỗ Cave, Bãi Cháy. 500 years ago, Nguyễn Trãi praised the beauty of Hạ Long Bay in his verse Lộ nhập Vân Đồn, in which he called it "rock wonder in the sky". In 1962, the Ministry of Culture, Sports and Tourism of North Vietnam listed Hạ Long Bay in the National Relics and Landscapes publication. In 1994, the core zone of Hạ Long Bay was listed by UNESCO as a World Heritage Site according to criterion vii, and listed for a second time according to criterion viii.

Point Reyes National Seashore

Point Reyes is a prominent cape and popular Northern California tourist destination on the Pacific coast of northern California. It is located in Marin County approximately 30 miles west-northwest of San Francisco. The term is often applied to the Point Reyes Peninsula, the region bounded by Tomales Bay on the northeast and Bolinas Lagoon on the southeast. The headland is protected as part of Point Reyes National Seashore. The cape protects Drakes Bay on its southern side. The headland is largely drained by Drakes Estero. Drakes Bay and Drakes Estero are named after English seafarer Sir Francis Drake who possibly hauled his ship, the Golden Hinde, up onto the beach for repairs in June 1579. Inverness Ridge runs along the peninsulas northwest-southeast spine, with forested peaks around 430 meters . West of the ridge, the land flattens out and the vegetation turns to scrub. The Mount Vision fire in 1995 burned part of Inverness Ridge. Point Reyes lends its name to the town of Point Reyes Station, California. The point may once have been known as Lobes Lighthouse by the sailors of clipper ships on the meat trade. (Lobes are ridges of slide material commonly referred in the literature from erosion events and the point is of that shape out to sea). The Spanish explorer Sebastián Vizcaíno named the land Punto de los Reyes ("Kings Point") when his ship, the Capitana anchored in Drakes Bay on the Day of the Three Kings (Epiphany, or the end of the 12 Days of Christmas) on January 6, 1603. Point Reyes first inhabitants, the Coast Miwok, lived on the land for thousands of years. They left evidence of well over a hundred encampments on the peninsula, with a population estimated to have been nearly 3,000. Seasonal hunters and gatherers, rather than cultivators, they were nourished by fish, clams, mussels, and crab, in addition to the deer, elk, bear, mud hen, geese, and small game they hunted with spears and bows. Although they did not cultivate the land, they used the plentiful acorns as a staple part of their diet by removing the tannic acid and making a pulp that was stored in dry granaries. Although the exact location of Sir Francis Drakes 1579 anchorage at Point Reyes is still being debated, evidence has confirmed that he landed near a Coast Miwok settlement. Observations, presumably written by his chaplain, describe the genial welcome Drake and his men received, complete with ceremony and gifts. The Coast Miwok continued their peaceful existence until late in the 18th century when the Spanish built Mission San Rafael and padres began journeying to Point Reyes to recruit them to move to the mission. While attempting to convert them, these padres disrupted their traditional way of life in addition to inadvertently introducing diseases that brought untimely deaths, fewer births, and significantly increasing infant mortality rates. In 1992, Coast Miwok descendants established the Federated Indians of Graton Rancheria and, by 2001, had 400 members who could prove their descent from local tribes. Today, they enjoy a rebirth of traditional customs and ceremonies, often held in Kule Loklo, "Valley of the Bear", a replica Miwok village in Point Reyes National Seashore. Although early explorers and Spanish trading galleons journeying between the Philippines and Acapulco passed by Point Reyes, some even anchoring briefly, it is the landing by Sir Francis Drake that dominates discussion of this era of Point Reyes early history. The exact location of his landing, significant as the first European landing in Northern California, has sparked countless hours of spirited debate spanning four centuries. Experts agree, however, that he landed somewhere near the area on June 17, 1579 and proclaimed it Nova Albion (New England). Most likely, as validated by a National Historic Landmark designation, the precise place of Drakes landing is Drakes Cove at Point Reyes National Seashore. Rumors of Drakes discovery of a safe harbor on the California coast intrigued the Spanish. Their trade between the Philippines and Mexico was booming, and they were constantly seeking safe harbors along their route. Many believe that Drakes discovery of such a harbor inspired the Spanish to order Sebastian Rodriguez Cermeno, a Portuguese captain trading for Spain, to survey the California coast on his journey to Mexico from the Philippines in 1595. Commanding the San Augustin, a Manilla galleon laden with a luxury cargo of Chinese silks, spices, and Ming porcelain bound for Acapulco, Cermeno endured both the first of hundreds of documented shipwrecks at Point Reyes, as well as one of the most amazing journeys to safety. Struggling with a decrepit, heavily-laden ship and a tired, rebellious crew that wanted to go home, Cermeno explored the California coast, eventually anchoring near the Point Reyes inlet now called Drakes Estero. Within a few days, a November storm beached the ship where it listed and was relentlessly pounded by the furious surf. It soon broke apart, killing several men and dumping the precious cargo, some of which was eventually collected, and used, by local Coast Miwok tribesmen. Cermeno salvaged a small, open launch, likened to a large canoe, and loaded it with the 70 surviving crew members to begin the long journey home. After a grueling two-month voyage, remembered as a remarkable feat of seamanship, Cermeno and all crew arrived safely in Acapulco in January 1596. Despite his amazing journey, Cermeno received no celebratory welcome, for he had not only lost his ship and cargo, but had also failed to locate the safe harbor he was ordered to find. Despite reports of a lovely land populated by friendly tribes, Spain neglected California until the second half of the 18th century. By that time, trade had become an important source of income, and it was becoming clear that the nation controlling Californias harbors would reap incredible profits. When England, France, and Russia began to covet Californias coast, the King of Spain knew it was time to fortify the coast. To identify sites for presidios and missions, an overland expedition of 67 men and 100 pack mules left San Diego in 1769. Led by Gaspar de Portolà, the governor of Baja California, they began walking to the largest known harbor, Monterey Bay. Portola expected more of a harbor than what they found at Monterey, and decided they must not have reached it yet. Pushing on north along the coast, they instead discovered San Francisco Bay. Prior to that, from a high point on the coast south of Pacifica, they saw and recognized (from the description of Manila Galleon pilot Cabrera Bueno) Point Reyes and the Farallon Islands. The expedition was blocked from going farther north toward Point Reyes by the Golden Gate and San Francisco Bay, since they had no boats. Beginning with Portolas expedition, Spain began establishing presidios and missions. By 1817, Mission San Rafael was established and padres began journeying to Point Reyes, intent on enticing the Coast Miwok to the mission. Although they were successful in convincing many to settle at the mission to begin a life of backbreaking labor, it was soon clear that the Coast Miwoks were not thriving. Serious outbreaks of smallpox and pneumonia killed many. Those who survived sickened from a wide variety of other illnesses, such as colds and measles. Birth rates dropped, and mortality rates increased at an alarming rate. Since the missions depended upon healthy workers for their prosperity, these illnesses foretold their demise. Mexico gained independence from Spain and possession of California in 1821. The deterioration of Mission San Rafael accelerated when secularization of the missions by Mexico in 1834 ended the era of mission domination that had destroyed the self-sufficient, centuries-old Coast Miwok way of life. Most mission land was subdivided and into large land grants used mainly for cattle ranching. Being mostly unsuitable for cattle, Point Reyes itself and Drakes Bay became part of Rancho Punta de los Reyes Sobrante (Sobrante means "leftover") in 1843. This was only a few years before cession of California to the United States, which led to decades of confusion and boundary battles. When the Spanish missions in California were dismantled, virtually all of Point Reyes was given to Rafael Garcia, a corporal in the Mexican Army, who was awarded two leagues (8911 acres) in March 1836. Named Rancho Tomales y Baulines, it is believed to have included the entire Olema Valley from Tomales Bay to Bolinas Lagoon, although its borders were never clearly defined. Garcias failure to survey and confirm boundaries, as required by Mexican law, set the stage for confusion and lengthy court battles when the rancho was dissolved. Unlike many rancheros, Garcia obeyed the law by actually living there. He built a wood and thatch home near todays National Seashore Bear Valley Headquarters and soon had a comfortable home for his family as well as headquarters for his extensive ranching operation consisting of approximately 3,000 cattle, 400 horses, and large herds of sheep and hogs. Thriving quickly, the rancho was soon largely self-sufficient. Grains and produce were grown, and a wild steer was slaughtered each day to provide the staple diet of tortillas and beefsteak. Additionally, wool was processed and woven for clothing, and hides were crafted into a wide variety of leather products, including shoes and saddles. To acquire luxury items he could not produce, Garcia, like most coastal rancheros, traded hides, tallow, and produce to smugglers. As a result, his rancho was adorned with bronze candlesticks, fine candles, artificial flowers, framed engravings, and elegant furniture. He also enjoyed seemingly unlimited supplies of wine and champagne. Although it is likely Garcia got most of his luxury items from smugglers, he may have obtained some of them from another source - Point Reyes many shipwrecks. When Mexico lost California to the United States, Garcia continued to prosper for a while. Soon after the American takeover, the 1849 Gold Rush brought floods of prospectors. Where his wild cattle had been valued only for hides and tallow, he could now sell them to feed hungry gold-seekers, netting as much as $35 each. Unfortunately for Garcia, these gold-rich years ended quickly: in 1851, the United States passed a law requiring rancheros to prove legal ownership of their land grants. While the Garcias continued ranching, their land began to disappear until, after 15 years of litigation, multiple court appearances, and high legal fees, Garcia had sold all but 3085 acres of his grant at bargain basement prices. Although Garcia believed he owned virtually all of Point Reyes, another Point Reyes land grant was awarded the same year, 1836. It was given to an Irishman James Berry who had become a Mexican citizen and colonel in the army. This land grant was also in the Olema Valley, and, to add to the boundary confusion, he soon left the area and hired Garcia to oversee it. A mere two years later Berry sold nearly 9,000 acres of it to a sea captain, Joseph Snook, an act clearly prohibited by Mexican law and grounds for forfeiture of the entire grant. Although Berry understandably wanted to keep the sale secret, Snook wanted legal title. He discovered that the only way he could obtain legal title of the land he had illegally purchased was to formally denounce Berrys ownership on the grounds that he had never occupied it. He was successful and gained legal title to the land he had illegally purchased, stocked it with 56 head of cattle, and, like Berry, hired Garcia to oversee it. Three months after he won legal title, he illegally sold it. And began a confusing series of sales and transfers that no one seemed to be able to untangle. Finally, in 1844, the rancheros themselves asked the Mexican government to investigate titles and clarify ownership. Little was clarified, and it was not until the United States took possession of California and required rancheros to conduct surveys and make court appearances to retain their land that the confusing pattern of sales and trades were untangled. Most ranchero were eventually able to prove ownership. Unfortunately, by this time, they had run out of cash and were forced to sell to pay the survey and daunting legal fees. Entrepreneurial Americans were delighted to capitalize on the opportunity. With cash in hand, they purchased these huge Mexican land grants, often paying less than $2 per acre, thus beginning Point Reyes next chapter as a dairying empire. Settlement patterns at Point Reyes were forever changed when the Shafters acquired it. Lords of Point Reyes for decades, the Shafter Brothers, Oscar and James, and son-in-law Charles Webb Howard, established large-scale, high-quality dairies that became prime examples of cleanliness, organization, and success. 13 of the 31 dairies they established still thrive today. Oscar was the first to arrive. A Vermont lawyer intent upon making his fortune and returning home as soon as possible, he left his family to journey to booming San Francisco. His separation from them became intolerable when his two youngest children died while he was away. Still not willing to give up the promise of wealth, he convinced his wife to come, bringing their surviving daughter. They thrived, and Oscar fathered four more California-born daughters. Oscar soon convinced his younger brother, James, also a lawyer, to join him. They became known as San Franciscos foremost authorities on title litigation. Using their title expertise, they began acquiring Point Reyes land. When Oscars oldest daughter married Charles Webb Howard, also a lawyer, the trio partnered to transform windswept Point Reyes into prosperous dairies. Determined to supply booming San Francisco with its butter, by 1857, the partners began fencing huge expenses of land (eventually resulting in 40 miles of fencing), building homes and barns, and stocking the dairies with the finest pure-bred bulls and rams, some costing over $1,400. By 1868, they had 3,500 cows on 17 dairies and were producing over 700,000 pounds of butter a year. All their dairies were operated by renters. When the most industrious of these renters tried to buy the dairy they worked, they failed. Many eventually left, establishing some of Californias major dairies. Despite their boundless optimism about the promise of Point Reyes, they did not get rich from it. Although they lived the opulent lifestyles of the wealthy of San Francisco, they were plagued by financial worries. Their children tried to hold on to the dairies, trying unsuccessfully to stop their decline despite aging ranches, sickening herds, and often unhappy tenants. Finally, in 1937, an era ended when the last of the Shafter Empire was sold, ushering in a new parade of owners. Four towns comprise the communities of Point Reyes: Bolinas, Olema, Inverness, and Point Reyes Station. For centuries, Bolinas remote lagoon made it the perfect secret harbor. Although not documented, it is likely that the 1808 Russian expedition to Bodega Bay that nearly decimated the local otters and fur seals hunted in Bolinas Lagoon. During Spanish and Mexican rule, this remote lagoon was used by American, British, and Russian smugglers intent on avoiding tariffs and regulations. Later, when the Gold Rush of 1849 generated a huge market for lumber, Bolinas became the port for nearby timber operations and, briefly, quarrying limestone. By the late 1960s, Bolinas had become home to a large community of idealistic hippies, many of whom had left San Franciscos Haight-Ashbury for a less populated paradise. In 1971, they succeeded in scrapping a master plan calling for a population of 28,000 by imposing a moratorium on new homes and defeating efforts to widen its access highway. Instead, a plan was approved that made agriculture, fishing, and small business the towns economic base. Bolinas soon gained renown for its unusual structures and recreational drug use, illustrating disregard for building codes and drug laws. Although those days are gone, Bolinas remains a unique corner of this magnificent peninsula with some residents who continue to tear down road signs in hope tourists will not find it. As soon as the Shafter dairies began to thrive, it became evident that Point Reyes needed a centrally-located town for supplies, services, and entertainment. In 1857, a hotel and saloon were built and the young town was named "Olema", meaning "coyote" in the Coast Miwok dialect. Within three years, it had emerged as the regions commercial center with a post office, grocery store, saloon, butcher, livery stable, and two hotels. By 1867, a wagon road from San Rafael was built and a stage coach arrived twice a week. It soon gained the reputation as a great place to drink. To combat this reputation, Druids Hall was completed in 1885. While this Olema chapter of the United Ancient Order of Druids adhered to principles of mutual support, intellectual growth, and social consciousness, it also served as a temperance society. Virtually deserted when the railroad stopped at Point Reyes Station instead of Olema, it languished until the 1960s when millions of visitors began coming to the adjacent Point Reyes National Seashore. Inverness remains a small community of charming cottages, lovely gardens, and uncontested streets amid a stunning setting. It exudes an aura of a village of yesteryear, populated with modern residents who are clearly aware of their good fortune to live there. The Shafters lobbied hard for a railroad to serve Point Reyes. When it was finally built, it bypassed Olema, terminating, instead, two miles away. When the first train arrived early in 1875, Point Reyes Station was a cow pasture. Passengers were not happy to be dropped there with no services to accommodate them, and it was soon clear that a town must be built. By 1880, it had a hotel, saloon, blacksmith shop, livery stable, butcher shop, and school. Its post office was completed in 1882, and its first store opened in 1883. When the railroad era ended, growth was slow. It was not until after World War II that a medical center and an impressive shopping center, including a drugstore, dentist, coffee shop, and library, had been completed. The train station became the local post office, while the former engine house was converted into a community center. In the 1970s, hippies established cottage industries in abandoned houses and shops. At the same time, the Coast Guard bought 30 acres of land formerly used as cattle pens, and built military housing. Unlikely comrades, locals watched in amusement as their new military and peace-loving residents learned to co-exist. Continuing as the regions supply and service center, it is a popular destination rich with charming shops, fine restaurants, extraordinary butter-filled pastures at the Bovine Bakery, and an annual music festival As developers and loggers submitted plans that would change Point Reyes forever, a 1956 National Park Service (NPS) study of possible seashore parks recommended acquisition of the peninsula. By 1958, a report was published recommending immediate NPS acquisition of 35,000 acres. Controversy raged, with environmentalists applauding the proposal and the ranchers who owned and worked the land fervently opposing it. Finally, a compromise was crafted which allowed the ranchers to lease their land and continue dairying while coexisting with tourists and park activities. On September 13, 1962, President John F. Kennedy signed the bill authorizing the acquisition of 53,000 acres and allocating $13 million. Eventually 18,000 acres purchased by the NPS were leased back to ranchers. In cooperation with the NPS, volunteers have restored and maintain a historic coastal radiotelegraph marine station, KSM (ex-KPH), at Point Reyes. It remains one of the few commercial Morse code stations operating in the world, and is the only one in the U.S. During the Cold War, submarines repaired at Mare Island Naval Shipyard were tested in the shallow waters off Point Reyes following shipyard repairs. Navy safety personnel used a small monitoring and communications hut on the peninsula for monitoring submarines during these sea trials. In April and May 1979, part of John Carpenters The Fog was shot at the Point Reyes Lighthouse and the small town of Inverness. Two large mammalian species, nearly extirpated in the nineteenth century, have made a remarkable recovery at Point Reyes: the Northern elephant seal and the Tule elk. Beginning in the 18th century Northern elephant seals (Mirounga angustirostris) were hunted extensively almost to extinction by the end of the 19th century, being prized for oil that could be made from their blubber, and the population may have fallen as low as 20. In 1874 American whaleman Charles Melville Scammon recorded in Marine Mammals of the Northwestern Coast of America, that "the elephant seal...known to the Old Californians as Elefante marino had a geographical distribution from Cape Lazaro (about 1/4 of the way up the Baja peninsula) in the south to Point Reyes in the north". They were thought to be extinct in 1884 until a remnant population of eight individuals was discovered on Guadalupe Island in 1892 by a Smithsonian expedition, who promptly killed seven of the eight for their collections. The elephant seals managed to survive, and were finally protected by the Mexican government in 1922. Subsequently the U.S. protection was strengthened after passage of the Marine Mammal Protection Act in 1972, and numbers have now recovered to over 100,000. The first breeding pair was discovered on a sheltered beach below Point Reyes Chimney Rock in 1981 and has multiplied at a remarkable 16% per year to the present population of 1,500 to 2,000 individuals each winter. In 1978, ten Tule Elk (Cervus canadensis ssp. nannodes) were re-introduced to Point Reyes from the San Luis National Wildlife Refuge near Los Banos. By 2009, over 440 elk were counted at Tomales Points 2,600 acres of coastal scrub and grasslands. In 1999, one hundred of the Tomales Point elk were moved to roam free in the Limantour wilderness area of the Seashore and above Drakes Beach. The tule elk and the native black-tailed deer had been hunted, and the population of the black-tailed deer had also been suppressed by two introduced competitors, axis deer and fallow deer. Vegetation native to Point Reyes includes Bishop pine, Douglas-fir, coyote brush, monkeyflower, poison oak, California blackberry, salal and coast redwood, among others. Nearly 490 species of birds have been observed in the park and on adjacent waters. The entire Point Reyes Peninsula is a piece of the Salinian Block transported northward by the San Andreas Fault. Its core is granite, unlike the terrain east of Tomales Bay. The granite rocks that form the peninsula were once continuous with the Tehachapi Mountains 350 miles south. In the 1906 earthquake, Point Reyes moved north 21 feet. Point Reyes is bounded to the east by the San Andreas Fault, which runs directly under Tomales Bay, and is structurally dominated by the Point Reyes Syncline. The Point Reyes Peninsula is on the Pacific Plate, while the rest of Marin County land is on the North American Plate. The peninsula is a member of the Salinian Terrane, a segment of the southernmost Sierra Nevada range transported north from Southern California by movement along the San Andreas fault. Simply speaking the peninsula consists of three major members: the Salinian Cretaceous crystalline basement, the overlying Pliocene sedimentary rocks, and the late Pleistocene marine terrace deposits of the southern peninsula. It can get very foggy and windy during certain parts of the year at the lighthouse, and to be effective, the lighthouse had to be situated below the characteristic high fog. When foggy, visibility is so slim that one cannot even view the lighthouse from the top of the approximately 300 steps necessary to walk down to reach it. The lighthouse serves a great purpose in such a foggy area, as there is no beach to wash up on; it is on a rocky cliff. Day or night, the light may be the only thing visible to ships. The peninsula is a popular recreational destination for the nearby San Francisco Bay Area, especially for hiking on its many trails and sea kayaking the shores of Tomales Bay and the coast. Point Reyes National Seashore offers some of the finest birdwatching in the United States, It is also one of the best places to watch Northern Elephant Seals in the winter months. More than 70,000 acres (300 km2) of habitat harbor an incredible variety of bird life. There are also popular oyster farms in and near the peninsula.

Tikal

Tikal is the ruins of an ancient city found in a rainforest in Guatemala. Ambrosio Tut, a gum-sapper, reported the ruins to a La Gaceta, a Guatemalan newspaper, which named the site Tikal. The Berlin Academy of Sciences’ Magazine then republished the report in 1853. Archeologists and treasure hunters then began visiting the forest. Today tourism to the site may help protect the rainforest. It is one of the largest archaeological sites and urban centers of the pre-Columbian Maya civilization. It is located in the archaeological region of the Petén Basin in what is now northern Guatemala. Situated in the department of El Petén, the site is part of Guatemalas Tikal National Park and in 1979 it was declared a UNESCO World Heritage Site. Tikal was the capital of a conquest state that became one of the most powerful kingdoms of the ancient Maya. Though monumental architecture at the site dates back as far as the 4th century BC, Tikal reached its apogee during the Classic Period, ca. 200 to 900 AD. During this time, the city dominated much of the Maya region politically, economically, and militarily, while interacting with areas throughout Mesoamerica such as the great metropolis of Teotihuacan in the distant Valley of Mexico. There is evidence that Tikal was conquered by Teotihuacan in the 4th century AD. Following the end of the Late Classic Period, no new major monuments were built at Tikal and there is evidence that elite palaces were burned. These events were coupled with a gradual population decline, culminating with the site’s abandonment by the end of the 10th century. Tikal is the best understood of any of the large lowland Maya cities, with a long dynastic ruler list, the discovery of the tombs of many of the rulers on this list and the investigation of their monuments, temples and palaces.

Sierra Nevada National Park

The Parque Nacional Sierra Nevada is located in Granada and Almería provinces in south-eastern Spain. It was declared a national park on 14 January 1999. It stretches from the Alpujarra to El Marquesado and the Lecrin Valley, covering a total area of 85,883 hectares, making it the largest national park in Spain. It incorporates the municipalities of Abla, Abrucena, Alboloduy, Alsodux, Bayárcal, Beires, Canjáyar, Fiñana, Fondón, Laujar de Andarax, Nacimiento, Ohanes, Paterna del Río, Rágol, Las Tres Villas, Aldeire, Alpujarra de La Sierra, Bérchules, Bubión, Busquístar, Cáñar, Capileira, Dílar, Dólar, Dúrcal, Ferreira, Güéjar Sierra, Huéneja, Jerez del Marquesado, Juviles, Lanjarón, Lanteira, Lecrín, Lugros, Monachil, Nevada, Nigüelas, Pampaneira, Pórtugos, Soportújar, La Taha, Trevélez, Valor and La Zubia. There are more than 20 peaks over 3,000 meters, with the highest being Mulhacén , Veleta and Alcazaba . The rivers that rise on the north face of the range feed the Guadalquivir basin, the most important ones being the Fardes and Genil. Meanwhile, the rivers that rise on the west and south faces run down into the Mediterranean. These include the Dúrcal, Ízbor, Trevélez and Poqueira, which are all tributaries of the Guadalfeo, which itself rises in the Sierra Nevada, and the Adra and Andarax, with their tributaries. The south and west faces are where you will find the majority of the almost 50 high-mountain lakes that exist in the Sierra Nevada, many of which are also the sources of streams and rivers. Much of the landscape, particularly above 2,400 metres (which was the perpetual snow line prior to the Holocene period) was shaped by the action of glaciers, resulting in characteristic U-shaped valleys.

Brooks Camp

Brooks Camp is a visitor attraction and archeological site in Katmai National Park and Preserve, noted for its opportunities for visitors to observe Alaskan brown bears catching fish in the falls of the Brooks River during salmon spawning season. The Brooks River connects Lake Brooks and Naknek Lake over about 2 kilometres . This natural choke point for salmon runs made it an attractive location for prehistoric Alaskans, who occupied the area from 4500 BP. The Aglegmut Eskimo people lived along the Brooks River in historical times. The Brooks River Archeological District, which includes Brooks Camp, was designated a National Historic Landmark in 1993. Five thousand years before present the level of Naknek Lake was significantly higher, and Lake Brooks was part of Naknek. As the Naknek River cut through glacial moraines, the level of Naknek Lake fell, creating Lake Brooks and the Brooks River. Permanent habitation was established along the river about 4000 years ago. The area was inhabited when the first Russian explorers reached what is now Brooks Camp in the 18th century. The National Park Service operates a seasonal visitor center at Brooks Camp, with an exhibit of a reconstructed native house built in 1967-68 in the footprint of a documented house site. Visitors arrive at the Lake Brooks Seaplane Base via floatplane. The camp was developed in 1950 by Northern Consolidated Airlines, a National Park Service concessioner who operated a chain of camps in Katmai, served by float planes. Brooks Lodge continues to operate as a concession within the park. Bear viewing season peaks in July, when the salmon are migrating, and in September, when the salmon are dying after spawning and are washing downstream. Peak visitor season is in July.

Mariposa Grove

Mariposa Grove is a sequoia grove located near Wawona, California, United States, in the southernmost part of Yosemite National Park. It is the largest grove of Giant Sequoias in the park, with several hundred mature examples of the tree. Two of its trees are among the 30 largest Giant Sequoias in the world. The Mariposa Grove was first visited by non-natives in 1857 when Galen Clark and Milton Mann found it. They named the grove after Mariposa County, California, where the grove is located. The Giant Sequoia named Grizzly Giant is between probably 1900–2400 years old: the oldest tree in the grove. In 1932, park officials claimed it as the fifth largest tree in the world, but other trees were subsequently found to be larger. It has a volume of 34,010 cubic feet, and is counted as the 25th largest tree in the world. It is 210 feet tall, and has a heavily buttressed base with a basal circumference of 28 m or a diameter of 30 feet; above the buttresses at 2.4 m above ground, the circumference is only 23 m. Grizzly Giants first branch from the base is 2 m in diameter. Another tree, the Wawona Tree, had a tunnel cut through it in the nineteenth century that was wide enough for horse-drawn carriages and early automobiles to drive through. Weakened by the large opening at its base, the tree fell down in a storm in 1969. Abraham Lincoln signed an Act of Congress on June 30, 1864 ceding Mariposa Grove and Yosemite Valley to the state of California. Criticism of stewardship over the land led to the states returning the grove to federal control with the establishment of Yosemite National Park. The Mariposa Grove Museum is listed on the National Register of Historic Places.

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