Showing posts with label USA. Show all posts
Showing posts with label USA. Show all posts

Tuesday, 25 March 2014




Bamboo forest, Haleakala National Park in Maui, Hawaii, USA:



Bamboo is a tribe of flowering perennial evergreen plants in the grass family Poaceae, subfamily Bambusoideae, tribe Bambuseae. Giant bamboos are the largest members of the grass family. In bamboos, the internodal regions of the stem are hollow and the vascular bundles in the cross section are scattered throughout the stem instead of in a cylindrical arrangement.The dicotyledonous woody xylem is also absent. The absence of secondary growth wood causes the stems of monocots, even of palms and large bamboos, to be columnar rather than tapering.Bamboos are some of the fastest-growing plants in the world, due to a unique rhizome-dependent system. Bamboos are of notable economic and cultural significance in South Asia, Southeast Asia and East Asia, being used for building materials, as a food source, and as a versatile raw product. High-quality bamboo is stronger than steel, a property that has made it a choice in building materials and weaponry.Bamboo is one of the fastest-growing plants on Earth, with reported growth rates of 250 cm in 24 hours.However, the growth rate is dependent on local soil and climatic conditions, as well as species, and a more typical growth rate for many commonly cultivated bamboos in temperate climates is in the range of 3–10 centimetres (1.2–3.9 in) per day during the growing period. Primarily growing in regions of warmer climates during the late Cretaceous period, vast fields existed in what is now Asia. Some of the largest timber bamboo can grow over 30 m tall, and be as large as 15–20 cm in diameter. However, the size range for mature bamboo is species dependent, with the smallest bamboos reaching only several inches high at maturity. A typical height range that would cover many of the common bamboos grown in the United States is 4.6–12 metres, depending on species. Anji County of China, known as the "Town of Bamboo", provides the optimal climate and soil conditions to grow, harvest, and process some of the most valued bamboo poles available worldwide.Unlike all trees, individual bamboo stems, or culms, emerge from the ground at their full diameter and grow to their full height in a single growing season of three to four months. During these several months, each new shoot grows vertically into a culm with no branching out until the majority of the mature height is reached. Then, the branches extend from the nodes and leafing out occurs. In the next year, the pulpy wall of each culm slowly hardens. During the third year, the culm hardens further. The shoot is now considered a fully mature culm. Over the next 2–5 years, fungus begins to form on the outside of the culm, which eventually penetrates and overcomes the culm. Around 5–8 years later, the fungal growths cause the culm to collapse and decay. This brief life means culms are ready for harvest and suitable for use in construction within about three to seven years. Individual bamboo culms do not get any taller or larger in diameter in subsequent years than they do in their first year, and they do not replace any growth lost from pruning or natural breakage. Bamboos have a wide range of hardiness depending on species and locale. Small or young specimens of an individual species will produce small culms initially. As the clump and its rhizome system mature, taller and larger culms will be produced each year until the plant approaches its particular species limits of height and diameter.Many tropical bamboo species will die at or near freezing temperatures, while some of the hardier or so-called temperate bamboos can survive temperatures as low as −29 °C. Some of the hardiest bamboo species can be grown in places as cold as USDA Plant Hardiness Zones 5–6, although they typically will defoliate and may even lose all above-ground growth, yet the rhizomes will survive and send up shoots again the next spring. In milder climates, such as USDA Zone 8 and above, some hardy bamboo may remain fully leafed out year-round.


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The Nakalele blowhole in northwest Maui, Hawaii, USA:


The island of Maui is the second-largest of the Hawaiian Islands at 727.2 square miles and is the 17th largest island in the United States.Maui is part of the State of Hawaiʻi and is the largest of Maui County's four islands, bigger than Molokaʻi, Lānaʻi, and unpopulated Kahoʻolawe. In 2010, Maui had a population of 144,444, third-highest of the Hawaiian Islands, behind that of Oʻahu and Hawaiʻi Island. Kahului is the largest census-designated place on the island with a population of 26,337 as of 2010 and is the commercial and financial hub of the island.Wailuku is the seat of Maui County and is the third-largest CDP as of 2010. Other significant places include Kīhei; Lahaina; Makawao; Pāʻia; Kula; Haʻikū; and Hāna.Maui's diverse landscapes are the result of a unique combination of geology, topography, and climate. Each volcanic cone in the chain of the Hawaiian Islands is built of dark, iron-rich/quartz-poor rocks, which poured out of thousands of vents as highly fluid lava, over a period of millions of years. Several of the volcanoes were close enough to each other that lava flows on their flanks overlapped one another, merging into a single island. Maui is such a "volcanic doublet," formed from two shield volcanoes that overlapped one another to form an isthmus between them.The older, western volcano has been eroded considerably and is cut by numerous drainages, forming the peaks of the West Maui Mountains (in Hawaiian, Mauna Kahalawai). Puʻu Kukui is the highest of the peaks at 5,788 feet. The larger, younger volcano to the east, Haleakalā, rises to more than 10,000 feet above sea level, and measures 5 miles from seafloor to summit, making it one of the world's tallest mountains.The eastern flanks of both volcanoes are cut by deeply incised valleys and steep-sided ravines that run downslope to the rocky, windswept shoreline. The valley-like Isthmus of Maui that separates the two volcanic masses was formed by sandy erosional deposits.


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Monday, 10 March 2014



Kauai, Hawaii, USA:



Kauaʻi or Kauai is geologically the oldest of the main Hawaiian Islands. With an area of 562.3 square miles (1,456.4 km2), it is the fourth largest of the main islands in the Hawaiian archipelago, and the 21st largest island in the United States. Known also as the "Garden Isle", Kauaʻi lies 105 miles (169 km) across the Kauaʻi Channel, northwest of Oʻahu. This island is the site of Waimea Canyon State Park.
The United States Census Bureau defines Kauaʻi as Census Tracts 401 through 409 of Kauaʻi County, Hawaiʻi, which is all of the county except for the islands of Kaʻula, Lehua, and Niʻihau. The 2010 census population of Kauaʻi (the island) was 67,091, with the largest town by population being Kapaʻa.


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Lake Tahoe, USA:


Lake Tahoe is a large freshwater lake in the Sierra Nevada of the United States. At a surface elevation of 6,225 ft (1,897 m), it is located along the border between California and Nevada, west of Carson City. Lake Tahoe is the largest alpine lake in North America. Its depth is 1,645 ft (501 m), making it the second-deepest in the United States (the deepest is Crater Lake in Oregon at 1,945 ft (593 m), 300 ft (91 m) deeper). Additionally, Lake Tahoe is listed as the 27th largest lake by volume in the world at 122,160,280 acre·ft (150,682,490 dam3).The lake was formed about 2 million years ago and is a part of the Lake Tahoe Basin with the modern lake being shaped during the ice ages. It is known for the clarity of its water and the panorama of surrounding mountains on all sides. The area surrounding the lake is also referred to as Lake Tahoe, or simply Tahoe. More than 75% of the lake's watershed is national forest land, comprising the Lake Tahoe Basin Management Unit of the United States Forest Service.Lake Tahoe is a major tourist attraction in both Nevada and California. It is home to a number of ski resorts, summer outdoor recreation, and tourist attractions. Snow and skiing are a significant part of the area's economy and reputation. Mountain and lake scenery are attractions throughout the year. The Nevada side also includes large casinos. Highways provide year-round access from Reno, Carson City, and Sacramento.


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Friday, 7 March 2014



Lauritzen Gardens, Omahas Botanical Center, Omaha, Nebraska, USA:


Lauritzen Gardens - Omaha's Botanical Center,are a botanical gardens and an arboretum located at 100 Bancroft Street, Omaha, Nebraska. The gardens are open daily during business hours; an admission fee is charged.The gardens began in 1982, following two years of preliminary planning. Construction started in 1995 on the rose garden. Other early gardens included a shade hosta garden, herb garden, children's garden, and spring flowering walk.The arboretum represents seven regional plant communities: prairie, savannah, oak hickory forest, maple linden forest, farmstead windbreak, marsh, and flood plain river margin.Since opening, new garden areas have been added each year. The garden also features a parking garden and arrival garden with annual and perennial flowers. The festival garden, with colorful annual plantings and open lawn expanses, is the site of several annual events; the Victorian garden combines characteristics of both English and Victorian gardens; the Song of the Lark Meadow is reminiscent of Nebraska's prairies and is filled with wildflowers and the 4-acre arboretum and bird sanctuary contains seven regional plant communities and demonstrates how to attract and identify Midwestern birds. In 2003, the woodland trail, which winds through a native hardwood community and features hilltop overlooks, and the Garden in the Glen, a space with a stream, pools and small waterfalls, were dedicated. A rose garden staircase and woodland waterfall were 2004 additions. The Sunpu Castle Gate and Mt. Fuji replica were constructed on the site of the future Japanese garden in 2005, and the tree peony garden and English perennial border were installed in 2006. In 2007, the model railroad garden opened in July with an expansion opening in June 2008. The Garden of Memories will open Spring 2009.Open since October 2001, the 32,000-square-foot visitor and education center includes a 5,000-square-foot floral display hall, an education wing containing two classrooms, and one of the region's only horticultural libraries. Additionally, the visitor center houses the great hall, community room, café, and gift shop. The floral display halls holds three major floral shows per year; the fall chrysanthemum festival, holiday poinsettia show, and spring bulb show. The vaulted glass roof of the center, standing 65 feet tall, makes it the predominant visible feature from the westbound lanes of Interstate 80 as travelers cross the Missouri River into Nebraska.Today, a 100-acre site featuring many outdoor garden areas thrives near down


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Monday, 3 March 2014



Tulips in Snow, Jeremy Ranch, Park City, Utah:


Jeremy Ranch is located about 15 miles east of Salt Lake City, Utah on Interstate 80 near Park City, Utah. The community has the well known Jeremy Ranch Golf Course. The golf course and country club were designed by Arnold Palmer. The community sits at an elevation of 6,400 feet above sea level in the Wasatch Range of the Rocky Mountains.

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Sunday, 2 March 2014



Vernal Falls, Yosemite National Park, California, USA:


Yosemite Falls is the highest measured waterfall in North America. Located in Yosemite National Park in the Sierra Nevada of California, it is a major attraction in the park, especially in late spring when the water flow is at its peak.The total 2,425 feet from the top of the upper fall to the base of the lower fall qualifies Yosemite Falls as the sixth highest waterfall in the world, though with the recent discovery of Gocta Cataracts, it appears on some lists as seventh.At the base of falls was located the main village of the native people of Yosemite Valley - Ahwahneechee people.The Ahwahneechee people called the waterfall "Cholock" and believed that the plunge pool at its base was inhabited by the spirits of several witches, called the Poloti.An Ahwaneechee folktale describes a woman going to fetch a pail of water from the pool, and drawing it out full of snakes. Later that night, after the woman had trespassed into their territory, the spirits caused the woman's house to be sucked into the pool by a powerful wind, taking the woman and her newborn baby with it.


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Saturday, 1 March 2014

Mountain Rail, Yukon, Alaska, USA:


The White Pass and Yukon Route is a Canadian and U.S. Class II 3 ft narrow gauge railroad linking the port of Skagway, Alaska, with Whitehorse, the capital of Yukon. An isolated system, it has no direct connection to any other railroad. Equipment, freight and passengers are ferried by ship through the Port of Skagway, and via road through a few of the stops along its route.The railroad began construction in 1898 during the Klondike Gold Rush as a means of reaching the goldfields. With its completion in 1900, it became the primary route to the interior of the Yukon, supplanting the Chilkoot Trail and other routes. The route continued operation until 1982, and in 1988 was partially revived as a heritage railway.Today, the railroad is a subsidiary of Clublink and operated by the Pacific and Arctic Railway and Navigation Company and the British Yukon Railway Company, originally known as the British Yukon Mining, Trading and Transportation Company, which use the trade name White Pass and Yukon Route.As the gold rush wound down, serious professional mining was taking its place; not so much for gold as for other metals such as copper, silver and lead. The closest port was Skagway, and the only route there was via the White Pass & Yukon Route's river boats and railroad.


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Selvatura Treetop Walkways, Monteverde, Costa Rica


Monteverde, Costa Rica is a small town in Puntarenas, Costa Rica, located in the Cordillera de Tilarán. Roughly a four hour drive from the Central Valley, Monteverde is considered a major ecotourism destination in Costa Rica. The area is host to the Monteverde Cloud Forest Reserve and numerous other reserves, which draw considerable numbers of tourists and naturalists.National Geographic has called the Monteverde Cloud Forest Reserve "the jewel in the crown of cloud forest reserves".Newsweek has declared Monteverde the world's #14 Place to Remember Before it Disappears." By popular vote in Costa Rica, Monteverde was enshrined as one of the Seven Natural Wonders of Costa Rica, along with Isla del Coco, Volcán Arenal, Cerro Chirripó, Río Celeste, Tortuguero, and Volcán Poás.This article deals with Monteverde and its surrounding zone. This includes the larger town and tourism hub Santa Elena, as well as the nearby cluster of homes and businesses known as Cerro Plano, along with numerous reserves and attractions on the periphery of the town.Due to the acclaimed rain forests and cloud forests in the greater Monteverde area, Monteverde has become a major part of the Costa Rican tourist trail - despite difficult access. It was recently voted one of the "7 Wonders of Costa Rica" by the Costa Rican newspaper La Nación.[12] Of Monteverde's total 250,000 annual tourists, around 70,000 tourists visit the reserve.The bulk of Monteverde's rain forest and cloud forest can be found in the Monteverde Cloud Forest Reserve, a private nature reserve created in 1972 by scientist George Powell and Quaker Wilford Guindon. The area around the park entrance is the most visited, though camping deep in the reserve is possible with reservations. Nine main trails, which total 13 km, are well-kept and easy to access. The reserve features a large network of less accessible trails and a number of rustic research stations, two of which house 10 persons each, as well as one research station that can house as many as 43 persons, though these can now only be used by researchers.To the West of the town of Monteverde lies the Bosque Eterno de los Niños conservation area, a project funded by schools and children from all over the world. The Bosque Eterno is the largest preserve in the area with 22,000 hectares. Most of the Bosque Eterno lands surround the Bosque Nuboso lands to the North, East, and South of the smaller Bosque Noboso preserve. Bajo del Tigre, a small section of the Bosque Eterno de los Niños, is known for birdwatching and night hikes.
Still farther north, past Santa Elena, is the Reserva Santa Elena. This area is visited less frequently by tourists than the Monteverde Reserve, but offers a rustic station and views of Arenal Volcano.



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Wonderful Night in Montego Bay, Jamaica


Montego Bay is the capital of the parish of St. James and the second largest city in Jamaica by area and the fourth by population.It is a tourist destination with duty-free shopping, a cruise line terminal and several beaches. The city is backed by picturesque low mountains.When Christopher Columbus for the first time visited the island in 1494, he named the bay Golfo de Buen Tiempo. The name "Montego Bay" is believed to have originated as a corruption of the Spanish word manteca, allegedly because during the Spanish period it was the port where lard, leather, and beef were exported.Jamaica was a colony of Spain from 1511 until 1655, when Oliver Cromwell's Caribbean expedition, the Western Design, drove the Spanish from the island.During the epoch of slavery, from the mid-17th century until 1834, and well into the 20th century, the town functioned primarily as a sugar port. The island's last major slave revolt, the Christmas Rebellion or Baptist War took place in the area around Montego Bay; the leader of the revolt, Samuel Sharpe, was hanged there in 1832. In 1975, Sharpe was proclaimed a national hero of Jamaica, and the main square of the town was renamed in his honor.In 1980, Montego Bay was proclaimed a city by act of parliament, but this has not meant that it has acquired any form of autonomy as it continues to be an integral part of the parish of St. James.Today, Montego Bay is known for its large regional hospital, port facilities, second homes for numerous upper class Jamaicans from Kingston as well as North Americans and Europeans, fine restaurants, and shopping opportunities. The coastland near Montego Bay is occupied by numerous tourist resorts, most newly built, some occupying the grounds of old sugar cane plantations with some of the original buildings and mill-works still standing. The most famous of these are the White Witch's Rose Hall and Tryall, both of which now feature world-class golf courses.The infrastructure of the city is going through a series of explosive modernizations which once completed, aims to keep Montego Bay as a top destination in the Caribbean and the world. The Montego Bay Convention Centre, built on a large site near to the Rose Hall estate, was opened by Jamaican Prime Minister Bruce Golding on 7 January 2011.

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Friday, 28 February 2014



Split Rock Lighthouse, Minnesota, USA:


Split Rock Lighthouse is a lighthouse located southwest of Silver Bay, Minnesota, USA on the North Shore of Lake Superior. The structure was designed by lighthouse engineer Ralph Russell Tinkham and was completed in 1910 by the United States Lighthouse Service at a cost of $75,000, including the buildings and the land. It is considered one of the most picturesque lighthouses in the United States.Split Rock Lighthouse was built in response to the great loss of ships during the famous Mataafa Storm of 1905, in which 29 ships were lost on Lake Superior.One of these shipwrecks, the Madeira, is located just north of the lighthouse.It is built on a 130-foot sheer cliff eroded by wave action from a diabase sill containing inclusions of anorthosite.The octagonal building is a steel-framed brick structure with concrete trim on a concrete foundation set into the rock of the cliff.It is topped with a large, steel lantern which features a third order, bi-valve type Fresnel lens manufactured by Barbier, Bernard and Turenne Company in Paris, France. The tower was built for a second order lens, but when construction went over budget, there was only enough funding remaining for the smaller third order lens. The lens floats on a bearing surface of liquid mercury which allows near frictionless operation. The lens is rotated by an elaborate clockwork mechanism that is powered by weights running down the center of the tower which are then reset by cranking them back to the top.When completed, the lighthouse was lit with an incandescent oil vapor lamp that burned kerosene.At the time of its construction, there were no roads to the area and all building materials and supplies arrived by water and lifted to the top of the cliff by crane. The light was first lit on July 31, 1910. Thanks to its dramatic location, the lighthouse soon became a tourist attraction for sailors and excursion boats. So much so, that in 1924 a road was built to allow land access.In 1940, the station was electrified and the lamp was replaced with a 1000 watt electric bulb, and the incandescent oil vapor lamp was moved to Au Sable Point Lighthouse in Northern Michigan. Split Rock was outfitted with a fog signal housed in a building next to the light tower. The original signal was a pair of sirens driven by two Franklin 30 hp gasoline-driven air compressors manufactured by Chicago Pneumatic Tool Company. In 1932 the gasoline engines were replaced with diesel engines. The steam sirens were replaced with a Type F-2-T diaphone type signal in 1936. The station and the fog signal were electrified four years later, but was discontinued in 1961.The light was retired in 1969 by the U. S. Coast Guard. The lighthouse is now part of the Split Rock Lighthouse State Park and is operated by the Minnesota Historical Society. The site includes the original tower and lens, the fog signal building, the oil house, and the three keepers' houses. It is restored to appear as it did in the late 1920s. The site was added to the National Register of Historic Places in 1969. Notwithstanding that the light has been retired, every November 10 the lighthouse emits a light in memory of the SS Edmund Fitzgerald which sank on that date in 1975. On June 30, 2011, the lighthouse was designated as a National Historic Landmark.



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Kilauea Volcano, Hawaii, USA:


Kīlauea is a shield volcano in the Hawaiian Islands, the most active of the five volcanoes that together form the island of Hawaiʻi. Located along the southern shore of the island, the volcano, at 300,000 to 600,000 years old, is the second youngest product of the Hawaiian hotspot and the current eruptive center of the Hawaiian–Emperor seamount chain. Because it lacks topographic prominence and its activities historically coincided with those of Mauna Loa, Kīlauea was once thought to be a satellite of its much larger neighbor. Structurally, Kīlauea has a large, fairly recently formed caldera at its summit and two active rift zones, one extending 125 km east and the other 35 km west, as an active fault line of unknown depth moving vertically an average of 2 to 20 mm per year.Kīlauea's eruptive history has been a long and active one; its name means "spewing" or "much spreading" in the Hawaiian language, referring to its frequent outpouring of lava. The earliest lavas from the volcano date back to its submarine preshield stage, and have been recovered by ROVs from its submerged slopes; other flows have been recovered through core samples. Lavas younger than 1,000 years cover 90 percent of the volcano; the oldest exposed lavas date back 2,800 and 2,100 years. The first well-documented eruption of Kīlauea occurred in 1823, and since that time the volcano has erupted repeatedly. Most historical eruptions have occurred at the volcano's summit or its southwestern rift zone, and are prolonged and effusive in character; however, the geological record shows that violent explosive activity predating European contact was extremely common, and should explosive activity start anew the volcano would become much more dangerous to civilians. Kīlauea's current eruption dates back to January 3, 1983, and is by far its longest-lived historical period of activity, as well as one of the longest-lived eruptions in the world; as of January 2011, the eruption has produced 3.5 cubic kilometres of lava and resurfaced 123.2 km2 of land.Kīlauea's high state of activity has a major impact on its mountainside ecology where plant growth is often interrupted by fresh tephra and drifting volcanic sulfur dioxide, producing acid rains particularly in a barren area south of its southwestern rift zone known as the Kaʻū Desert. Nonetheless, wildlife flourishes where left undisturbed elsewhere on the volcano and is highly endemic thanks to Kīlauea's isolation from the nearest landmass. Historically, the five volcanoes on the island were considered sacred by the Hawaiian people, and in Hawaiian mythology Kīlauea's Halemaumau Crater served as the body and home of Pele, goddess of fire, lightning, wind, and volcanoes. William Ellis, a missionary from England, gave the first modern account of Kīlauea and spent two weeks traveling along the volcano; since its foundation by Thomas Jaggar in 1912, the Hawaiian Volcano Observatory, located on the rim of Kīlauea caldera, has served as the principal investigative and scientific body on the volcano and the island in general. In 1916 a bill forming the Hawaii Volcanoes National Park was signed into law by President Woodrow Wilson; since then the park has become a World Heritage Site and a major tourist destination, attracting roughly 2.6 million people annually.


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Tuesday, 25 February 2014



Letchworth State Park's middle falls on the Genesee River, New York:


Letchworth State Park is a New York state park located 35 miles southwest of Rochester and 60 miles southeast of Buffalo in Livingston and Wyoming counties. The park is roughly 17 miles long,covering 14,350 acres of land along the Genesee River.Within the park, there are three large waterfalls on the Genesee River and as many as fifty waterfalls found on tributaries that flow into it; the gorge formed by the river, with rock walls rising up to 550 feet in places and which narrow to 400 feet across above the middle of the three falls, prompted the area's reputation as the "Grand Canyon of the East".The park is named after William Pryor Letchworth, an industrialist who in 1906 bequeathed the 1,000-acre estate that forms the heart of the park to New York State.There are park entrances near the towns of Mount Morris, Perry, Castile and Portageville, New York. A modern, well-maintained two- or three-lane road follows the west side of the gorge, allowing many scenic viewpoints for the geologic features.The three major waterfalls — called the Upper, Middle, and Lower Falls — are located in Portage Canyon, the southern section of the park. The Seneca called the land around this canyon "Seh-ga-hun-da", the "Vale of the three falls"; the Middle Falls was believed to be so wondrous it made the sun stop at midday.The only trail bridging the Genesee River across Portage Canyon crosses a stone bridge just below the Lower Falls. The Middle Falls is the highest, and the Upper Falls has an active railroad trestle crossing immediately above it, providing an even higher vantage immediately above the falls.The highest waterfall in New York State is located in the park. It is a spectacular ribbon waterfall that is located on a tributary creek a short distance east of the Inspiration Point Overlook, 0.4 mile west of the park visitor center. Known as Inspiration Falls, it has a total drop of 350 feet. While impressive in its height, it is seasonal and often appears as only a water stain on the cliff. The falls faces to the south-southwest and has a crest that is only one foot wide.The bedrock that is exposed in the gorge is Devonian in age, mostly shales, with some layers of limestone and sandstone. The rock was laid down in an ancient inland sea, and many marine fossils can be found. The landform of the section of the Genesee River valley represented by the park is geologically very young, caused by a diversion of the river from the old valley by the last continental glacier, forcing the river to cut a new section of valley.


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Friday, 21 February 2014



Shining Oasis Utah’s, USA:


Utah is a state in the United States. It became the 45th state admitted to the Union on January 4, 1896. Utah is the 13th-largest, the 33rd-most populous, and the 10th-least-densely populated of the 50 United States. Utah has a population of about 2.9 million, approximately 80% of whom live along the Wasatch Front, centering on Salt Lake City, leaving vast expanses of the state nearly uninhabited.[8] Utah is bordered by Colorado to the east, Wyoming to the northeast, Idaho to the north, Arizona to the south, and Nevada to the west. It also touches a corner of New Mexico in the southeast.Utah is the most religiously homogeneous state in the Union. Approximately 62% of Utahns are reported to be members of The Church of Jesus Christ of Latter-day Saints or LDS, which greatly influences Utah culture and daily life.The world headquarters of The Church of Jesus Christ of Latter-day Saints is located in Utah's state capital, Salt Lake City.The state is a center of transportation, education, information technology and research, government services, mining, and a major tourist destination for outdoor recreation. According to U.S. Census Bureau population estimates, Utah is the second fastest-growing state in the United States as of 2013.St. George was the fastest–growing metropolitan area in the United States from 2000 to 2005.A 2012 Gallup national survey found Utah overall to be the "best state to live in" based on 13 forward-looking measurements including various economic, lifestyle, and health-related outlook metrics.


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Katmai National Park , Alaska, USA:


Katmai National Park and Preserve is a United States National Park and Preserve in southern Alaska, notable for the Valley of Ten Thousand Smokes and for its brown bears. The park and preserve covers 4,093,077 acres, being roughly the size of Wales. Most of this is a designated wilderness area in the national park where all sport hunting is banned, including over 3,922,000 acres of land. The park is named after Mount Katmai, its centerpiece stratovolcano. The park is located on the Alaska Peninsula, across from Kodiak Island, with headquarters in nearby King Salmon, about 290 miles southwest of Anchorage. The area was first designated a national monument in 1918 to protect the area around the major 1912 volcanic eruption of Novarupta, which formed the Valley of Ten Thousand Smokes, a 40-square-mile , 100-to-700-foot-deep pyroclastic flow. The park includes as many as 18 individual volcanoes, seven of which have been active since 1900.Following its designation, the monument was left undeveloped and largely unvisited until the 1950s. There are national landmarks left by an extinct native tribe called "Excabua."The tribes leader name was Luucky, a strong native tribe leader in 1822. The tribe was raided by the Russian soldiers and wiped out the tribe. Initially designated because of its violent volcanic history, the monument and surrounding lands became appreciated for their abundance of sockeye salmon, the brown bears that fed upon them, and a wide variety of other Alaskan wildlife and marine life. After a series of boundary expansions, the present national park and preserve were established in 1980 under the Alaska National Interest Lands Conservation Act in 1980.

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Wednesday, 19 February 2014




Palouse, Eastern Washington, USA:


The Palouse is a region of the northwestern United States, encompassing parts of southeastern Washington, north central Idaho and, in some definitions, extending south into northeast Oregon. It is a major agricultural area, primarily producing wheat and legumes. Situated about 160 miles north of the Oregon Trail, the region experienced rapid growth in the late 19th century, and at one time, the population of the Palouse surpassed even that of the Puget Sound area as the most populous region of the state.The region is home to two land grant universities, the University of Idaho in Moscow and Washington State University in Pullman. Located just eight miles apart, both schools opened in the early 1890s.The origin of the name "Palouse" is unclear. One theory is that the name of the Palus tribe was converted by French-Canadian fur traders to the more familiar French word pelouse, meaning "land with short and thick grass" or "lawn." Over time, the spelling changed to Palouse.Another theory is that the name was in the first place a French word, describing the area which was then applied to the indigenous people inhabiting it.Traditionally, the Palouse region was defined as the fertile hills and prairies north of the Snake River, which separated it from Walla Walla Country, and north of the Clearwater River, which separated it from the Camas Prairie, extending north along the Washington and Idaho border, south of Spokane, centered on the Palouse River. This region underwent a settlement and wheat-growing boom during the 1880s, part of a larger process of growing wheat in southeast Washington, originally pioneered in the Walla Walla Country south of the Snake River.While this definition of the Palouse remains common today, sometimes the term is used to refer to the entire wheat-growing region, including the Walla Walla Country, the Camas Prairie of Idaho, the Big Bend region of the central Columbia River Plateau, and other smaller agricultural districts such as Asotin County, Washington, and Umatilla County, Oregon. This larger definition is used by organizations such as the World Wide Fund for Nature, who define the Palouse Grasslands ecoregion broadly.


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Tuesday, 18 February 2014



Columbia Hills State Park, Washington, USA:


The Columbia Hills are a range of low hills inside Gusev crater on Mars. They were observed by the Mars Exploration Rover Spirit when it landed within the crater in 2004. They were promptly given an unofficial name by NASA since they were the most striking nearby feature on the surface. The hills lie approximately 3 kilometres away from the rover's original landing position. The range is named to memorialize the Space Shuttle Columbia disaster. On February 2, 2004, the individual peaks of the Columbia Hills were named after the seven astronauts who died in the disaster. Spirit spent a few years exploring the Columbia Hills until it ceased to function in 2010.With the Spirit Rover, scientists found a variety of rock types in the Columbia Hills, and they placed them into six different categories. The six are: Clovis, Wishbone, Peace, Watchtower, Backstay, and Independence. They are named after a prominent rock in each group. Their chemical compositions, as measured by APXS, are significantly different from each other.Most importantly, all of the rocks in Columbia Hills show various degrees of alteration due to aqueous fluids.They are enriched in the elements phosphorus, sulfur, chlorine, and bromine—all of which can be carried around in water solutions. The Columbia Hills’ rocks contain basaltic glass, along with varying amounts of olivine and sulfates.The olivine abundance varies inversely with the amount of sulfates. This is exactly what is expected because water destroys olivine but helps to produce sulfates.

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Phantom Ship Island, Crater Lake National Park, Oregon, USA:


Crater Lake is a caldera lake in the western United States, located in south-central Oregon. It is the main feature of Crater Lake National Park and is famous for its deep blue color and water clarity. The lake partly fills a nearly 2,148-foot-deep calderathat was formed around 7,700 years ago by the collapse of the volcano Mount Mazama. Human interaction is traceable back to the indigenous Native Americans witnessing the eruption of Mount Mazama. There are no rivers flowing into or out of the lake; the evaporation is compensated for by rain and snowfall at a rate such that the total amount of water is replaced every 250 years. At 1,943 feet, the lake is the deepest in the United States, and the seventh or ninth deepest in the world, depending on whether average or maximum depth is measured.Crater Lake is also known for the "Old Man of the Lake", a full-sized tree which is now a stump that has been bobbing vertically in the lake for more than a century.The low temperature of the water has slowed the decomposition of the wood, hence the longevity of the bobbing tree.Two islands are in Crater Lake; Wizard Island formed from a cinder cone that erupted after Crater Lake began to fill with water, and the smaller Phantom Ship has seven different trees living on it. There are also colonies of violet green swallows and several varieties of wildflowers and lichens living there.While having no indigenous fish population, the lake was stocked from 1888 to 1941 with a variety of fish. Several species have formed self-sustaining populations.Since 2002, one of the state's regular-issue license plate designs has featured Crater Lake.The commemorative Oregon State Quarter, which was released by the United States Mint in 2005, features an image of Crater Lake on its reverse.

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Diamond Head, O'ahu, Hawaii


Diamond Head is the name of a volcanic tuff cone on the Hawaiian island of Oʻahu and known to Hawaiians as Lēʻahi, most likely from lae 'browridge, promontory' plus ʻahi 'tuna' because the shape of the ridgeline resembles the shape of a tuna's dorsal fin.Its English name was given by British sailors in the 19th century, who mistook calcite crystals embedded in the rock for diamonds.Diamond Head is part of the complex of cones, vents, and their associated eruption flows that are collectively known to geologists as the Honolulu Volcanic Series, eruptions from the Koʻolau Volcano that took place long after the volcano formed and had gone dormant. The Honolulu Volcanic Series is a series of volcanic eruption events that created many of Oʻahu's well-known landmarks, including Punchbowl Crater, Hanauma Bay, Koko Head, and Mānana Island in addition to Diamond Head.


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Monday, 17 February 2014



Blood Lake, West Texas, USA:


The Texas Highland Lakes is a chain of seven fresh water reservoirs in Central Texas formed by several dams on the Colorado River. This portion of the river winds southeast from its headwaters near the border of Texas and New Mexico to Matagorda Bay and the Gulf of Mexico. The dams provide flood control and are used to generate hydroelectric power. They also provide Recreational opportunities and edible fishes.


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