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Abruzzo (UK: /æˈbrʊtsoʊ/,[5] US: /ɑːˈbruːtsoʊ, əˈ-/; Italian: [aˈbruttso]; Abbrùzze [abˈbruttsə], Abbrìzze [abˈbrittsə] or Abbrèzze [abˈbrɛttsə] in Neapolitan Abruzzese; Aquilano: Abbrùzzu) or Abruzzi is a region of Southern Italy with an area of 10,763 square km (4,156 sq mi) and a population of 1.3 million. It is divided into four provinces: L'Aquila, Teramo, Pescara, and Chieti. Its western border lies 80 km (50 mi) east of Rome. Abruzzo borders the region of Marche to the north, Lazio to the west and south-west, Molise to the south-east, and the Adriatic Sea to the east. Geographically, Abruzzo is divided into a mountainous area in the west, which includes the Gran Sasso d'Italia, and a coastal area in the east with beaches on the Adriatic Sea.
Abruzzo is considered a region of Southern Italy in terms of its culture, language, history and economy, although geographically it may also be considered central.[8] The Italian Statistical Authority (ISTAT) also deems it to be part of Southern Italy, partly because of Abruzzo's historic association with the Kingdom of the Two Sicilies.
Abruzzo is known as "the greenest region in Europe" as almost half of its territory, the largest in Europe,[9] is set aside as national parks and protected nature reserves. There are three national parks, one regional park, and 38 protected nature reserves. These ensure the survival of 75% of Europe's living species, including rare species such as the golden eagle, the Abruzzo (or Abruzzese) chamois, the Apennine wolf and the Marsican brown bear.[10] Abruzzo is also home to Calderone, Europe's southernmost glacier.
The visiting nineteenth-century Italian diplomat and journalist Primo Levi (1853–1917) said that the adjectives "forte e gentile" (strong and kind) best describe the beauty of the region and the character of its people. "Forte e gentile" has since become the motto of the region and its inhabitants.
Provinces and politics
Abruzzo provinces
Provinces
Abruzzo is divided into four administrative provinces:
Province Area (km2) Population Density (inh./km2)
Chieti 2,588 396,190 153.1
L'Aquila 5,034 308,876 61.3
Pescara 1,225 318,701 260.1
Teramo 1,948 308,769 158.5
Politics
History
Human settlements in Abruzzo have existed since at least the Neolithic times. A skeleton from Lama dei Peligni in the province of Chieti dates back to 6,540 BC under radiometric dating.[13] The name Abruzzo appears to be derivative of the Latin word "Aprutium". In Roman times, the region was known as Picenum, Sabina et Samnium, Flaminia et Picenum, and Campania et Samnium.[14] The region was known as Aprutium in the Middle Ages, arising from four possible sources: it is a combination of Praetutium, or rather of the name of the people Praetutii, applied to their chief city, Interamnia, the old Teramo.
Many cities in Abruzzo date back to ancient times. Corfinio was known as Corfinium when it was the chief city of the Paeligni, and later was renamed Pentima by the Romans. Chieti is built on the site of the ancient city of Teate, Atri was known as Adria. Teramo, known variously in ancient times as Interamnia and Teramne, has Roman ruins which attract tourists.
After the fall of the Roman Empire, a string of invasions and rulers dominated the region, including the Lombards, Byzantines, and Hungarians. Between the 9th and 12th centuries, the region was dominated by the popes. Subsequently, the Normans took over, and Abruzzo became part of the Kingdom of Sicily, later the Kingdom of Naples. Spain ruled the kingdom from the sixteenth to the eighteenth centuries. The French Bourbon dynasty took over in 1815, establishing the Kingdom of the Two Sicilies, and ruled until Italian unification (also known as the Risorgimento) in 1860.
Until 1963, Abruzzo was part of the combined Abruzzi e Molise region. The term Abruzzi (plural of Abruzzo) derives from the time when the region was part of the Kingdom of the Two Sicilies. The territory was administered as Abruzzo Citeriore (nearer Abruzzo) and Abruzzo Ulteriore I and II (farther Abruzzo I and II) from Naples, the capital of the kingdom.[14] Abruzzo Citeriore is now Chieti province. Teramo and Pescara provinces now comprise what was Abruzzo Ulteriore I. Abruzzo Ulteriore II is now the province of L'Aquila.
In the twentieth century, war had a great impact on the region. During the Second World War, Abruzzo was on the Gustav Line, part of the German's Winter Line. One of the most brutal battles was the Battle of Ortona. Abruzzo was the location of two prisoner of war camps, Campo 21 in Chieti,[18] and Campo 78 in Sulmona. The Sulmona camp also served as a POW camp in World War 1; much of the facility is still intact and attracts tourists interested in military history.
Geography
Geographically, Abruzzo is located in central Italy and southern Italy, stretching from the heart of the Apennines to the Adriatic Sea, and includes mainly mountainous and wild land. The mountainous land is occupied by a vast plateau, including Gran Sasso, at 2,912 metres (9,554 ft) the highest peak of the Apennines, and Mount Majella at 2,793 metres (9,163 ft). The Adriatic coastline is characterized by long sandy beaches to the North and pebbly beaches to the South. Abruzzo is well known for its landscapes and natural environment, parks and nature reserves, characteristic hillside areas rich in vineyards and olive groves, and one of the highest densities of Blue Flag beaches.
Climate
The Abruzzo region has two types of climate that are strongly influenced by the Apennine Mountains, dividing the climate of the coastal and sub-Apennine hills from the interior's high mountain ranges. Coastal areas have a Mediterranean climate with hot dry summers and mild winters and rainy hills with a sublittoral climate where temperatures decrease progressively with increasing altitude and precipitation with altitude. Precipitation is also strongly affected by the presence of the Apennines mountain ridges of the region; it increases with the proportion being more abundant in the field and on the slopes exposed to the west, instead of decreasing towards the east and east-facing slopes. Often the Adriatic coast are sidelined rainfall from the west to the barrier effect of the Apennines undergoing the action of gentle winds descending from it (or Libeccio).[21] The minimum annual rainfall, however, is found in some inland valleys, sheltered from much disturbance to the blocking action of mountain ridges, such as the Peligna Valley, or the valley of the river Tirino, which in some places (Ofena, Capestrano) showed barely 500 millimetres (19.7 inches), and not along the coast where it never falls below 600 millimetres (23.6 inches); for if Teramo is relatively little watered by rain (Teramo less than 800 millimetres (31.5 inches)), the metre is exceeded in Chieti, reaching maximum levels in the Adriatic, while between Ortona and Vasto in Costa dei Trabocchi decrease again.[21] The highest rainfall occurs in upland areas on the border with Lazio; they are especially vulnerable to Atlantic disturbances. Around 1,500 to 2,000 millimetres (59 to 79 inches) of precipitation is typical (Pescara in 2010 showed a value close to 2,800 millimetres (110.2 inches)).
Flora and fauna
As with many Mediterranean regions, Abruzzo's vegetation is characterized by different Mediterranean ecosystems. The coast and the surrounding areas are characterized by the presence of typical plants of Mediterranean shrubland, such as myrtle, heather and mastic, while in the hilly areas other species grow, including olive, pine, willow, oak, poplar, alder, arbutus, broom, acacia, capers, rosemary, hawthorn, licorice and almond trees, interspersed with oak trees. At elevations between 600 and 1,000 metres (2,000 and 3,300 ft) there is sub-montane vegetation, mainly characterized by mixed forests of oak and turkey oak, maple and hornbeam; shrubs include dog rose and red juniper. Elevations between 1,000 and 1,900 metres (3,300 and 6,200 ft) are dominated by beech trees. In the Apennine Mountains at elevations above 2,000 metres (6,600 ft) species include alpine orchid, mountain juniper, silver fir, black cranberry and the Abruzzo edelweiss.
The fauna of Abruzzo is highly varied, including the region's symbol, the Abruzzo chamois (Rupicapra pyrenaica ornata), which has recovered from near-extinction. Animals typical of this region include: marsican brown bear, along with Italian wolf, deer, lynx, roe deer, snow vole, fox, porcupine, wild cat, wild boar, badger, otter, and viper.
The natural parks of the region include the Abruzzo National Park, the Gran Sasso and Monti della Laga National Park,[24] the Maiella National Park and the Sirente-Velino Regional Park, as well as many other natural reserves and protected areas.
Economy
Until a few decades ago, Abruzzo was a region of poverty in Southern Italy; over the past decades, however, it has developed to such an extent that it has escaped from the spiral of underdevelopment to become the 'first' region of the 'Italian Mezzogiorno'. This confirms its pivotal role in the national economic system. Since the 1950s, Abruzzo has had steady economic growth. In 1951, Abruzzo per capita income or GDP was 53% of that of Northern Italy, the nation's richest region. By 1971, Abruzzo was at 65% and, by 1994, per capita income was at 76% of Northern Italy's per capita income, giving Abruzzo the highest per capita GDP of Southern Italy and surpassing the growth of every other region of Italy. The construction of autostrade (motorways) from Rome to Teramo (A24) and Rome to Pescara (A25) opened Abruzzo to easy access. State and private investment in the region increased, and Abruzzo attained higher per capita education levels and greater productivity growth than the rest of the South. As of 2003, Abruzzo's per capita GDP was €19,506 or 84% of the national average of €23,181 and well outpacing that of the South (€15,808). The region's average GDP per capita was approximately 20,100 EUR.
The 2009 L'Aquila earthquake led to a sharp economic slowdown. However, according to statistics at the end of 2010, it seems that the economy of Abruzzo is recovering, despite the negative on regarding employment.[28] In fact, at the end of 2010, Abruzzo's growth was 1.47%, which placed it fourth among the Italian regions with the highest annual growth rates after Lazio, Lombardy and Calabria.[30] In 2011 Abruzzo's economic growth was +2.3%, the highest percentage among the regions of Southern Italy.[31] The region is also the richest region of Southern Italy, with a GDP per capita of €25,700.[21]
Travel poster from the 1920s.
Abruzzo's industrial sector expanded rapidly, especially in mechanical engineering, transportation equipment and telecommunications. The structure of production in the region reflects the transformation of the economy from agriculture to industry and services. Although industry has developed strongly, it retains weak points due to the existence of only a few large businesses alongside a huge fabric of small and medium-sized businesses. Both pure and applied research are carried out in the region, where there are major institutes and factories involved in research in the fields of pharmaceutics, biomedicine, electronics, aerospace and nuclear physics. The industrial infrastructure is spread throughout the region in industrial zones. The most important of these are: Val Pescara, Val Sangro, Val Trigno, Val Vibrata and Conca del Fucino. A further activity worthy of note is seaside and mountain tourism, which is of considerable importance to the economy of the region.[33] Agriculture, involving small holdings, has succeeded in modernising and offering high-quality products. The mostly small, agricultural holdings produce: wine, cereals, sugar beet, potatoes, olives, vegetables, fruit and dairy products. Traditional products are saffron and liquorice. Most famous in the world is Abruzzo's wine Montepulciano d'Abruzzo; in the late 20th and early 21st century, Montepulciano d'Abruzzo earned a reputation as being one of the most widely exported DOC classed wine in Italy.[34]
In the past decade, tourism has increased, in particular by internal and European arrivals. Abruzzo is world-famous for its wildlife parks (Abruzzo National Park, Gran Sasso and Monti della Laga National Park, Maiella National Park) and regional park (Sirente Velino), and 38 protected areas between oasis, regional reserves, and state reserves. The inland mountainous region contains several ski resorts, and coastal tourism is also well-developed, in particular, the Trabocchi Coast. Abruzzo's castles and medieval towns, especially around the town of L'Aquila, have earned it in some quarters the nickname of "Abruzzoshire", by analogy with the "Chiantishire", nickname sometimes used to refer to the Chianti area of Tuscany, but Abruzzo is still off the beaten path for most visitors to Italy.[35]
Chieti
Although the population density of Abruzzo has increased over recent decades, it is still well below the Italian national average: in 2008, 123.4 inhabitants per km2, compared to 198.8. In the provinces, the density varies: as of 2008 Pescara is the most densely populated with 260.1 inhabitants per km2, whereas L'Aquila is the least densely populated with 61.3 inhabitants per km2, although it has the largest area. After decades of emigration from the region, the main feature of the 1980s is immigration from third world countries. The population increase is due to the positive net migration. Since 1991 more deaths than births were registered in Abruzzo (except for 1999, when their numbers were equal).[36] In 2008, the Italian national institute of statistics ISTAT estimated that 59,749 foreign-born immigrants live in Abruzzo, equal to 4.5% of the total regional population.
The most serious demographic imbalance is between the mountainous areas of the interior and the coastal strip. The largest province, L'Aquila, is situated entirely in the interior and has the lowest population density. The movement of the population of Abruzzo from the mountains to the sea has led to the almost complete urbanization of the entire coastal strip especially in the province of Teramo and Chieti. The effects on the interior have been impoverishment and demographic aging, reflected by an activity rate in the province of L'Aquila which is the lowest among the provinces in Abruzzo – accompanied by geological degradation as a result of the absence of conservation measures. In the coastal strip, however, there is such a jumble of accommodations and activities that the environment has been negatively affected. The policy of providing incentives for development has resulted in the setting-up of industrial zones, some of which (Vasto, Avezzano, Carsoli, Gissi, Val Vibrata, Val di Sangro) have made genuine progress, while others (Val Pescara, L'Aquila) have run into trouble after their initial success. The zones of Sulmona and Guardiagrele have turned out to be more or less failures. Outside these zones, the main activities are agriculture and tourism.
Main settlements
L'Aquila is both the capital city of the Abruzzo region and of the Province of L'Aquila and second largest city (pop. 73,000). L'Aquila was hit by an earthquake on 6 April 2009, which destroyed much of the city centre. The other provincial capitals are Pescara, which is Abruzzo's largest city and major port (pop. 123,000); Teramo (pop. 55,000) and Chieti (pop. 55,000). Other large municipalities in Abruzzo include the industrial and high tech center Avezzano (pop. 41,000), as well as three important industrial and touristic centers such as Vasto (pop. 40,636), Lanciano (pop. 36,000), and Sulmona (pop. 25,000).
Transport
Airports
Abruzzo International Airport is the only international airport in the region. Open to civilian traffic since 1996, the number of passengers has increased over the years because of low-cost air carriers' use of the facility. Today, the airport has a catchment area of over 500,000 passengers annually and connects the city of Pescara and the entire region with many Italian and Europe destinations.
L'Aquila-Preturo Airport is located in the nearby village of Courts and was recently renovated and modernized to accommodate presidential flights for G8 activities.
Ports
There are four main ports in Abruzzo: Pescara, Ortona, Vasto and Giulianova.
Over the years the Port of Pescara became one of the most important tourist ports of Italy and the Adriatic Sea. Heavily damaged in World War II, it underwent some sixty years of major restoration and was reborn as a modern marina with advanced moorings and shipbuilding facilities. It has been honored with the European Union's blue flag for the quality of services offered. The port of Pescara has lost passenger traffic because of its shallowness and silting, but its fishery and aquaculture activities are thriving.[38]
Railways
There is a significant disparity between the railways of the Abruzzo coast and the inland areas, which badly need modernization to improve the service, in particular, the Rome-Pescara line.
Existing railway lines:
Adriatic railway runs through the whole of Italy from north to south, along the Adriatic Sea.
Train Rome – Sulmona – Pescara
Sulmona – Carpinone
Sulmona–Terni railway
Avezzano railroad – Roccasecca
Giulianova – Teramo
Sangritana (Lanciano – Castel di Sangro)
Highways
There are three highways that serve the region:
Highway A24 Rome – L'Aquila – Teramo, was built in the 1970s and connects Rome with Lazio and more specifically to the Abruzzo Teramo via L'Aquila. It performs an important liaison function of the region, both Tyrrhenian to the Adriatic, due to the presence of several interchanges of connecting roads and highways. The Gran Sasso tunnel, the longest road tunnel entirely on Italian territory, was opened in 1984. It connects L'Aquila and Teramo on the A24 making the northern Abruzzo coast reachable within two hours from Rome.
Highway A25 Turin – Avezzano – Pescara makes the connection between Rome and Pescara. The road running out of Turin begins its journey where it branches off the A24, runs into the Conca del Fucino, crosses the Abruzzo Apennines, comes to the valley of Peligna, and ends at the exit for Pescara-Villanova to join the A14.
Motorway A14 Bologna – Taranto known as the A14 "Adriatica", includes 743 km (461.68 mi) of road, including lengths in the cities of Bologna and Taranto. Opened to traffic in 1965, it is now a major tourist road, running through the coastal towns of Emilia Romagna, Marche, Abruzzo, Molise, and Apulia.
Culture
Castel del Monte, one of Abruzzo's little-known hill towns
Gabriele d'Annunzio from Pescara
Abbazia di San Liberatore a Majella (Serramonacesca)
Ovid from Sulmona
Cathedral of San Giustino (Chieti)
Fishing trabucco of San Vito Chietino
The museum Museo Archeologico Nazionale d'Abruzzo in Chieti houses the famed warrior statue Warrior of Capestrano which was found in a necropolis from 6th century B.C. Of cultural importance are: Teramo Cathedral, its archeological museum and Roman theater, the Castello della Monica, the Collurania-Teramo Observatory, the famous L'Aquila Basilica of Santa Maria di Collemaggio (which holds the remains of Pope Celestine V), the Museo Nazionale d'Abruzzo, Santa Maria del Suffragio, the Forte Spagnolo, the Fountain of 99 Spouts, Gabriele D'Annunzio's house in Pescara, Campli's Scala Sancta and its church, the church of Santissima Annunziata in Sulmona, the cathedrals of Chieti, Lanciano, Guardiagrele, Atri and Pescara along with the castles of Ortona, Celano and Ortucchio.
Every 28–29 August, L'Aquila's Santa Maria di Collemaggio commemorates the Perdonanza Celestiniana, the indulgence issued by Pope Celestine V to any who, "truly repentant and confessed" would visit that Church from the Vespers of the vigil to the vespers of 29 August.[39] Sulmona's Holy Week is commemorated with traditional celebrations and rituals, such as 'La Madonna che Scappa in Piazza', where a large statue of the Madonna, carried by a group of Sulmonesi part of Confraternities, is taken through the square towards her resurrected Son.[40] Cocullo, in the province of L'Aquila, holds the annual 'Festa dei serpari' (festival of snake handlers) in which a statue of St. Dominic, covered with live snakes, is carried in a procession through the town; it attracts thousands of Italian and foreign visitors. In many Abruzzo villages, Anthony the Great's feast is celebrated in January with massive and scenic bonfires.[41] In the past, the region of Abruzzo was well known for the transumanza, the migratory movement of sheep principally south to the region of Puglia during the cold winter months.[42] The Feast of St. Biagio, protector of wool dealers, is the most widespread in Abruzzo. On the third of February in Taranta Peligna every year since the sixteenth century an evocative ritual is carried out, entailing the distribution of panicelle, which are small loaves made of flour and water, in the shape of a blessing hand, which are distributed to the faithful.
Historical figures include: the Roman orator Asinius Pollio; Latin poets Sallust and Ovid, who were born in L'Aquila and Sulmona respectively, Gaius Cassius Longinus, Roman senator and leading instigator of the plot to kill Julius Caesar; and Pontius Pilate, who was born in the province of Teramo and is best known for authorizing the crucifixion of Jesus. Abruzzo's religious personalities include Saint Berardo; John of Capistrano, who led a crusade against the Ottoman Empire; Thomas of Celano, author of three hagiographies about Saint Francis of Assisi; and Alessandro Valignano, who introduced Catholicism to the Far East and Japan. The Polish Pope John Paul II loved the mountains of Abruzzo, where he would retire often and pray in the church of San Pietro della Ienca. When he died, Cardinal Stanislaw Dziwisz, gave the local Abruzzo community some of the late pontiff's blood as a token of the love he had felt for the mountainous area.[43] The greatest Italian poet of the 20th century Gabriele D'Annunzio was from Pescara; other notable Abruzzo personalities in the field of humanities include: poet Ignazio Silone, director Ennio Flaiano who co-wrote La dolce vita, philosopher Benedetto Croce, composer Sir Paolo Tosti and the sculptor Venanzo Crocetti.
American artists and celebrities such as: Madonna, Dean Martin, Bradley Cooper, Perry Como, Henry Mancini, Nancy Pelosi, Rocky Marciano, Rocky Mattioli, Bruno Sammartino, Mario Batali, John and Dan Fante, Tommy Lasorda, Dan Marino, Mario Lanza, Garry Marshall, Penny Marshall, Al Martino, Ariana Grande and Canadian Michael Bublé have Abruzzo origins.
Some international movies shot in Abruzzo include The American, Jean-Jacques Annaud's The Name of the Rose, Fellini's La Strada and I Vitelloni, Schwarzenegger's Red Sonja, Ladyhawke, King David, Francesco, Keoma, The Barbarians, The Fox and the Child and Krull.
Medieval and Renaissance hill towns
The fortress of Civitella is the most visited monument in Abruzzo
For most of its history, a large number of the Abruzzese people have been hill people, often working as shepherds in mountainous areas, or establishing hill towns, especially in the parts of Abruzzo further from the Adriatic coast.[citation needed] Before the 2009 earthquake, Abruzzo was the region with the highest number of castles and hill towns in Italy, but it still holds many of Italy's best-preserved medieval and Renaissance hill towns, twenty-three of which are among The Most Beautiful Villages in Italy.[44] These awards are not only for aesthetic beauty but also for art and culture, historical importance and livability.
The abrupt decline of Abruzzo's agricultural economy in the early to mid-20th-century saved some of the region's historic hill towns from modern development. Many lie entirely within regional and national parks. Among the most well preserved are Castel del Monte and Santo Stefano di Sessanio, which lie in the Gran Sasso National Park on the edge of the high plain of Campo Imperatore and nestled beneath the Apennines' highest peaks. Both hill towns, which were ruled by the Medicis for over a century-and-a-half, have relatively little tourism. Between the two towns sits Rocca Calascio, the ruin of an ancient fortress popular with filmmakers. Both Monteferrante and Roccascalegna are two of the most representative Abruzzo villages in the province of Chieti. Within the Gran Sasso National Park is also found Castelli, an ancient pottery center whose artisans produced ceramics for most of the royal houses of Europe.
Civitella del Tronto played a crucial role in the history of the unification of Italy. The fortress of Civitella is the most visited monument in the Abruzzo region today.[45] Other medieval hill towns located fully within Abruzzo's park system are Pacentro in the Maiella National Park and Pescasseroli in the Abruzzo National Park. Pacentro, which features a 14th-century castle with two intact towers, has been little touched by modernisation. The Shrine of Gabriel of Our Lady of Sorrows, in the province of Teramo, which attracts some two million visitors per year, is one of the 15 most-visited sanctuaries in the world.[46] Capestrano, a small town in the province of L'Aquila, is the hometown of Saint John of Capistrano, Franciscan friar and Catholic priest, as well as the namesake of the Franciscan missions San Juan Capistrano in Southern California, the mission Mission San Juan Capistrano (Texas) and the city of San Juan Capistrano in Orange County. Giulianova is a notable example of a Renaissance "ideal city."
The proximity to Rome, the protected natural reserves and landscapes which make the region one of the greenest in Europe, the presence of some of the most beautiful Italian villages, its rich and heterogeneous gastronomy, along with a long history of deep-rooted local tradition and authentic Italian culture, make Abruzzo fifth among Italian regions for tourist visits after Calabria, Marche, Sardinia and Trentino. In 2010, visitors included 6,381,067 Italians and 925,884 foreign tourists.
In 2015, the American organization Live and Invest Overseas included Abruzzo on its list of World's Top 21 Overseas Retirement Havens. The study was based on such factors as climate, infrastructure, health care, safety, taxes, cost of living and more. In 2017 the Chamber of Commerce of Pescara presented Abruzzo region to the Annual conference of Live and Invest Overseas in Orlando (USA). One year later, in October 2018, Live and Invest Overseas held its first conference in Abruzzo.
Universities
There are three universities in the Abruzzo region:
University of L'Aquila
D'Annunzio University of Chieti–Pescara
University of Teramo
Harvard University bases an intensive summer Italian language and culture program in Vasto, a resort town on Abruzzo's southern coast.
Science
Between the province of Teramo and L'Aquila, under the Gran Sasso Tunnel, is the Laboratori Nazionali del Gran Sasso (LNGS) of the INFN, one of the three underground astroparticle laboratories in Europe.
The Istituto Zooprofilattico Sperimentale dell'Abruzzo e del Molise "Giuseppe Caporale", which conducts research in veterinary and environmental public health, is located in Teramo.
The Gran Sasso Science Institute, located in L'Aquila, is an advanced research institute which offers doctorates in astroparticle physics, computer science, and mathematics as well as urban studies and regional science, and which also conducts scientific research.
Sports
Interamnia World Cup, the largest international youth handball competition worldwide, takes place yearly in Teramo.[51]
There are several football clubs in Abruzzo. Delfino Pescara 1936 is a Serie B club; based in Pescara, its home stadium is Stadio Adriatico – Giovanni Cornacchia.
Dialects
The regional dialects of Abruzzo include Teramano, Abruzzese Orientale Adriatico and Abruzzese Occidentale. The first two form part of the dialect of southern Italy also known simply as "Neapolitan" since the region has been part of the Kingdom of Naples and the Kingdom of the Two Sicilies, while Aquilano is related to the Central Italian dialects including Romanesco. The dialects spoken in the Abruzzo region can be divided into three main groups:
Sabine dialect, in the province of L'Aquila (central Italian dialects)
Abruzzo Adriatic dialect, in the province of Teramo, Pescara and Chieti, that is virtually abandoned in the province of Ascoli Piceno (southern Italian dialects)
Abruzzo western dialect, in the province of L'Aquila (southern Italian dialects)
Cuisine
Renowned for its variety and richness due to the heterogeneity of its territory, Abruzzo's cuisine is among the best in Italy. In 2013 an Italian organization Confesercenti survey of foreign tourists showed that Abruzzo is the best Italian region to eat in. Both the agricultural and coastal aspects of Abruzzo have contributed to its cuisine. Due to the mountains, much of Abruzzo was isolated from international influence until the 20th century. As a result, the region's cuisine remained unique.
Popular dishes
One of the most popular regional dishes is spaghetti alla chitarra which is made by pressing or cutting pasta through a chitarra, an implement to form long thin noodles similar to spaghetti. The pasta is served with a tomato-based sauce, often flavored with peppers, pork, goose, or lamb. This dish is complemented by regional side dishes, such as the bean and noodle soup, sagne e fagioli. This soup is traditionally flavored with tomatoes, garlic, oil, and peperoncini. In terms of common ingredients, cuisine in Abruzzo often includes:
Lamb and mutton, primarily in the mountains.[54] Sheep's milk (or ricotta) is an important source of Abruzzese cheese, and lamb intestines are used as sausage casing or for stuffed meat rolls.[54][55] Mountain goat meat is also common in Abruzzo.
Truffles and mushrooms, particularly wild mushrooms from the forests and hills
Garlic, especially red garlic
Rosemary
Hot chili pepper or peperoncini, regionally known as diavolilli or diavoletti, is common in Abruzzese cuisine and often used to add spice to dishes. Abruzzo residents are well known for frequently adding peperoncini, or hot peppers, to their meals.
Vegetables such as lentils, grasspeas and other legumes, artichoke, eggplant, and cauliflower[54][55][56][57]
Other popular dishes include:
Gnocchi carrati, flavored with bacon, eggs and pecorino cheese
Scrippelle, a rustic French-style crêpe served either mbusse (a type of soup) or used to form a sort of soufflé with some ragù and stuffed with chicken liver, meatballs, hard-boiled eggs, and cheese
Pastuccia, a polenta stew with sausage, eggs, and cheese
Across the region, roast lamb is enjoyed in several variations. Some of these variations include:
Arrosticini, a skewered lamb dish
Pecora al cotturo, lamb stuffed with a variety of mountain herbs and cooked in a copper pot
Lamb cooked whole in a bread oven
Agnello cacio e ovo, a lamb-based fricassee
Mazzerella: lamb intestines stuffed with lamb, garlic, marjoram, lettuce, and spices
Le virtù: a soup from Teramo filled with legumes, vegetables and pork, usually eaten in the spring at celebrations
Timballo abruzzese: lasagna-like dish with pasta sheets (scrippelle) layered with meat, vegetables and rice; often served for Christmas and Easter[58]
Porchetta abruzzese: moist boneless-pork roast, slow-roasted with rosemary, garlic, and pepper[58]
Seafood is also popular, especially in coastal areas. The variety of fish available to the area has resulted in several fish-based Brodetti (broths), coming from such places as Vasto, Giulianova, and Pescara. These broths are often made by cooking fish, flavored with tomatoes, herbs, and peperoncino, in an earthenware pot. Rustic pizzas are also very common. Some of these are:
Easter Pizza, a rustic cake with cheese and pepper from the Teramo area
Fiadoni from Chieti, a dough of eggs and cheese well risen, cooked in the oven in a thin casing of pastry
A rustic tart pastry filled with everything imaginable: eggs, fresh cheeses, ricotta, vegetables, and all sorts of flavorings and spices.
Also from Teramo are the spreadable sausages flavored with nutmeg, and liver sausages tasting of garlic and spices. The ventricina from the Vasto area is made with large pieces of fat and lean pork, pressed and seasoned with powdered sweet peppers and fennel all encased in the dehydrated stomach of the pig itself. Atri and Rivisondoli are famous for cheeses. Mozzarella, either fresh or seasoned, is made from ewe's milk, although a great number of lesser known varieties of these cheeses can be found all over Abruzzo and Molise.
Sweets
The Abruzzo's sweets are world-famous and include:
Confetti, sugar-coated almonds, from Sulmona
Torrone Nurzia, a chocolate nougat from L'Aquila
Parrozzo , a cake-like treat made from a mixture of crushed almonds, and coated in chocolate.
Ferratelle (also known as Pizzelle). A wafer cookie, often flavored with anise
Croccante, a type of nougat made from almonds and caramelized suger, often flavored with lemon[59]
A Montepulciano d'Abruzzo wine labelled as being made from old vines.
Olive oil
The extra-virgin olive oil produced in Colline Teramane (Teramo hills) is marked by the DOP.[60]
The region has several cultivars that includes Carboncella, Dritta (Dritta Francavillese and Dritta di Moscufo), Gentile del Chieti, Nostrana (Nostrana di Brisighella), and Sargano olive cultivars.[61]
Wines and liquors
Renowned wines like Montepulciano DOCG and Trebbiano d'Abruzzo DOC are judged to be amongst the world's finest.[62] In 2012, a bottle of Trebbiano d'Abruzzo ranked No. 1 in the top 50 Italian wine awards.[63] In recent decades these wines have been joined, particularly, by wines from lesser known (heritage) white grapes, such as, Pecorino, Cococciola, Passerina, Montonico Bianco and Fiano.[64]
The region is also well known for the production of liquors such as Centerbe, Limoncello, Ratafia and Genziana.
Combine near McBaine in rural Boone County Missouri by Notley Hawkins Photography. Taken with a Canon EOS 5D Mark IV camera with a Canon EF16-35mm f/4L IS USM lens at ƒ/5.0 with a 76 second exposure at ISO 100. Processed with Adobe Lightroom CC.
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Cloudy night but the moon popped up for a bit! Composite one shot of the pier wide angle and one of the moon telephoto combined in photoshop.
I combined two prompts today. From LOAD216, my landmark is the Mickey Ear Tunnel you enter as you board the cruise ship. Entering the tunnel means check in is over and it's time for the fun to begin! I was inspired by Whimsical Musings Prompt #181 to use banners. This paper from Simple Stories had banners on it and then I created a big banner from the paper I matted the journaling on. Thanks for all the inspiration today and happy #200 to you , @LisaInRe
Visited Washington during the arctic blast... Freezing weather, but had to go see the meeting place of the Federal Reserve Board of Governors. Combining two interests (pun intended) of mine: photography and economics!
Combine near McBaine in rural Boone County Missouri by Notley Hawkins Photography. Taken with a Canon EOS 5D Mark IV camera with a Canon EF16-35mm f/4L IS USM lens at ƒ/5.0 with a 47 second exposure at ISO 100. Processed with Adobe Lightroom CC.
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©Notley Hawkins
I think there may have been a mechanical issue. One man looking into the innards. And shortly another man drove up to have a look see.
Stargazy pie (sometimes called starrey gazey pie or other variants) is a Cornish dish made of baked pilchards, along with eggs and potatoes, covered with a pastry crust. Although there are a few variations with different fish being used, the unique feature of stargazy pie is fish heads (and sometimes tails) protruding through the crust, so that they appear to be gazing skyward. This allows the oils released during cooking to flow back into the pie.
The dish is traditionally held to have originated from the village of Mousehole in Cornwall and is traditionally eaten during the festival of Tom Bawcock's Eve to celebrate his heroic catch during a very stormy winter. According to the modern festival, which is combined with the Mousehole village illuminations, the entire catch was baked into a huge stargazy pie, encompassing seven types of fish and saving the village from starvation. The story of Bawcock was popularised by Antonia Barber's children's book The Mousehole Cat, which featured the star-gazy pie.
Arches National Park is a national park in eastern Utah, United States. The park is adjacent to the Colorado River, 4 miles (6 km) north of Moab, Utah. More than 2,000 natural sandstone arches are located in the park, including the well-known Delicate Arch, as well as a variety of unique geological resources and formations. The park contains the highest density of natural arches in the world.
The park consists of 310.31 square kilometres (76,680 acres; 119.81 sq mi; 31,031 ha) of high desert located on the Colorado Plateau. The highest elevation in the park is 5,653 feet (1,723 m) at Elephant Butte, and the lowest elevation is 4,085 feet (1,245 m) at the visitor center. The park receives an average of less than 10 inches (250 mm) of rain annually.
Administered by the National Park Service, the area was originally named a national monument on April 12, 1929, and was re designated as a national park on November 12, 1971. The park received more than 1.6 million visitors in 2018.
As stated in the foundation document in U.S. National Park Service website:
The purpose of Arches National Park is to protect extraordinary examples of geologic features including arches, natural bridges, windows, spires, and balanced rocks, as well as other features of geologic, historic, and scientific interest, and to provide opportunities to experience these resources and their associated values in their majestic natural settings.
The national park lies above an underground evaporite layer or salt bed, which is the main cause of the formation of the arches, spires, balanced rocks, sandstone fins, and eroded monoliths in the area. This salt bed is thousands of feet thick in places and was deposited in the Paradox Basin of the Colorado Plateau some 300 million years ago (Mya) when a sea flowed into the region and eventually evaporated. Over millions of years, the salt bed was covered with debris eroded from the Uncompahgre Uplift to the northeast. During the Early Jurassic (about 200 Mya), desert conditions prevailed in the region and the vast Navajo Sandstone was deposited. An additional sequence of stream laid and windblown sediments, the Entrada Sandstone (about 140 Mya), was deposited on top of the Navajo. Over 5,000 feet (1,500 m) of younger sediments were deposited and have been mostly eroded. Remnants of the cover exist in the area including exposures of the Cretaceous Mancos Shale. The arches of the area are developed mostly within the Entrada formation.
The weight of this cover caused the salt bed below it to liquefy and thrust up layers of rock into salt domes. The evaporites of the area formed more unusual "salt anticlines" or linear regions of uplift. Faulting occurred and whole sections of rock subsided into the areas between the domes. In some places, they turned almost on edge. The result of one such 2,500-foot (760 m) displacement, the Moab Fault, is seen from the visitor center.
As this subsurface movement of salt shaped the landscape, erosion removed the younger rock layers from the surface. Except for isolated remnants, the major formations visible in the park today are the salmon-colored Entrada Sandstone, in which most of the arches form, and the buff-colored Navajo Sandstone. These are visible in layer-cake fashion throughout most of the park. Over time, water seeped into the surface cracks, joints, and folds of these layers. Ice formed in the fissures, expanding and putting pressure on surrounding rock, breaking off bits and pieces. Winds later cleaned out the loose particles. A series of free-standing fins remained. Wind and water attacked these fins until, in some, the cementing material gave way and chunks of rock tumbled out. Many damaged fins collapsed. Others, with the right degree of hardness and balance, survived despite their missing sections. These became the famous arches.
Although the park's terrain may appear rugged and durable, it is extremely fragile. More than 1 million visitors each year threaten the fragile high-desert ecosystem. The problem lies within the soil's crust, which is composed of cyanobacteria, algae, fungi, and lichens that grow in the dusty parts of the park. Factors that make Arches National Park sensitive to visitor damage include being a semiarid region, the scarce, unpredictable rainfall, lack of deep freezing, and lack of plant litter, which results in soils that have both a low resistance to and slow recovery from, compressional forces such as foot traffic. Methods of indicating effects on the soil are cytophobic soil crust index, measuring of water infiltration, and t-tests that are used to compare the values from the undisturbed and disturbed areas.
Geological processes that occurred over 300 million years ago caused a salt bed to be deposited, which today lies beneath the landscape of Arches National Park.[ Over time, the salt bed was covered with sediments that eventually compressed into rock layers that have since been named Entrada Standstone. Rock layers surrounding the edge of the salt bed continued to erode and shift into vertical sandstone walls called fins. Sand collected between vertical walls of the fins, then slightly acidic rain combined with carbon dioxide in the air allowed for the chemical formation of carbonic acid within the trapped sand. Over time, the carbonic acid dissolved the calcium carbonate that held the sandstone together. Many of the rock formations have weaker layers of rock on bottom that are holding stronger layers on top. The weaker layers would dissolve first, creating openings in the rock. Gravity caused pieces of the stronger rock layer to fall piece by piece into an arch shape. Arches form within rock fins at points of intense fracturing localization, or weak points in the rock's formation, caused by horizontal and vertical discontinuities. Lastly, water, wind, and time continued this erosion process and ultimately created the arches of Arches National Park. All of the arches in the park are made of Entrada Sandstone, however, there are slight differences in how each arch was developed. This allows the Entrada Sandstone to be categories into 3 groups including Slick rock members, Dewey rock members, and Moab members. Vertical arches can be developed from Slick rock members, a combination of Slick rock members and Moab members, or Slick rock members resting above Dewey rock members. Horizontal arches (also called potholes) are formed when a vertical pothole formation meets a horizontal cave, causing a union into a long arch structure. The erosion process within Arches National Park will continue as time continues to pass. Continued erosion combined with vertical and horizontal stress will eventually cause arches to collapse, but still, new arches will continue to form for thousands of years.
Humans have occupied the region since the last ice age 10,000 years ago. Fremont people and Ancestral Puebloans lived in the area until about 700 years ago. Spanish missionaries encountered Ute and Paiute tribes in the area when they first came through in 1775, but the first European-Americans to attempt settlement in the area were the Mormon Elk Mountain Mission in 1855, who soon abandoned the area. Ranchers, farmers, and prospectors later settled Moab in the neighboring Riverine Valley in the late 1870s. Word of the beauty of the surrounding rock formations spread beyond the settlement as a possible tourist destination.
The Arches area was first brought to the attention of the National Park Service by Frank A. Wadleigh, passenger traffic manager of the Denver and Rio Grande Western Railroad. Wadleigh, accompanied by railroad photographer George L. Beam, visited the area in September 1923 at the invitation of Alexander Ringhoffer, a Hungarian-born prospector living in Salt Valley. Ringhoffer had written to the railroad to interest them in the tourist potential of a scenic area he had discovered the previous year with his two sons and a son-in-law, which he called the Devils Garden (known today as the Klondike Bluffs). Wadleigh was impressed by what Ringhoffer showed him, and suggested to Park Service director Stephen T. Mather that the area be made a national monument.
The following year, additional support for the monument idea came from Laurence Gould, a University of Michigan graduate student (and future polar explorer) studying the geology of the nearby La Sal Mountains, who was shown the scenic area by local physician Dr. J. W. "Doc" Williams.
A succession of government investigators examined the area, in part due to confusion as to the precise location. In the process, the name Devils Garden was transposed to an area on the opposite side of Salt Valley that includes Landscape Arch, the longest arch in the park. Ringhoffer's original discovery was omitted, while another area nearby, known locally as the Windows, was included. Designation of the area as a national monument was supported by the Park Service in 1926 but was resisted by President Calvin Coolidge's Interior Secretary, Hubert Work. Finally, in April 1929, shortly after his inauguration, President Herbert Hoover signed a presidential proclamation creating the Arches National Monument, consisting of two comparatively small, disconnected sections. The purpose of the reservation under the 1906 Antiquities Act was to protect the arches, spires, balanced rocks, and other sandstone formations for their scientific and educational value. The name Arches was suggested by Frank Pinkely, superintendent of the Park Service's southwestern national monuments, following a visit to the Windows section in 1925.
In late 1938, President Franklin D. Roosevelt signed a proclamation that enlarged the Arches to protect additional scenic features and permit the development of facilities to promote tourism. A small adjustment was made by President Dwight Eisenhower in 1960 to accommodate a new road alignment.
In early 1969, just before leaving office, President Lyndon B. Johnson signed a proclamation substantially enlarging the Arches. Two years later, President Richard Nixon signed legislation enacted by Congress, which significantly reduced the total area enclosed, but changed its status. Arches National Park was formally dedicated in May 1972.
In 1980, vandals attempted to use an abrasive kitchen cleanser to deface ancient petroglyphs in the park, prompting park officials to recruit physicist John F. Asmus, who specialized in using lasers to restore works of art, to use his technology to repair the damage. Asmus "zapped the panel with intense light pulses and succeeded in removing most of the cleanser".
Climbing Balanced Rock or any named or unnamed arch in Arches National Park with an opening larger than 3 ft (0.9 m) is banned by park regulations. Climbing on other features in the park is allowed but regulated; in addition, slacklining and BASE jumping are banned parkwide.
Climbing on named arches within the park had long been banned by park regulations, but following Dean Potter's successful free climb on Delicate Arch in May 2006, the wording of the regulations was deemed unenforceable by the park attorney. In response, the park revised its regulations later that month, eventually imposing the current ban on arch climbing in 2014.
Approved recreational activities include auto touring, hiking, bicycling, camping at the Devils Garden campground, backpacking, canyoneering, and rock climbing, with permits required for the last three activities. Guided commercial tours and ranger programs are also available.
Astronomy is also popular in the park due to its dark skies, despite the increasing light pollution from towns such as Moab.
Delicate Arch is the subject of the third 2014 quarter of the U.S. Mint's America the Beautiful Quarters program commemorating national parks and historic sites. The Arches quarter had the highest production of the five 2014 national park quarters, with more than 465 million minted.
American writer Edward Abbey was a park ranger at Arches National Monument in 1956 and 1957, where he kept journals that became his book Desert Solitaire. The success of Abbey's book, as well as interest in adventure travel, has drawn many hikers, mountain bikers, and off-pavement driving enthusiasts to the area. Permitted activities within the park include camping, hiking along designated trails, backpacking, canyoneering, rock climbing, bicycling, and driving along existing roads, both paved and unpaved. The Hayduke Trail, an 812 mi (1,307 km) backpacking route named after one of Edward Abbey's characters, begins in the park.
An abundance of wildlife occurs in Arches National Park, including spadefoot toads, antelope squirrels, scrub jays, peregrine falcons, many kinds of sparrows, red foxes, desert bighorn sheep, kangaroo rats, mule deers, cougars, midget faded rattlesnakes, yucca moths, western rattlesnakes, and collared lizards.
A number of plant species are common in the park, including prickly pear cactus, Indian ricegrass, bunch grasses, cheatgrass, moss, liverworts, Utah juniper, Mormon tea, blackbrush, cliffrose, four-winged saltbrush, pinyon pine, evening primrose, sand verbena, yucca, and sacred datura.
Biological soil crust consisting of cyanobacteria, lichen, mosses, green algae, and microfungi is found throughout southeastern Utah. The fibrous growths help keep soil particles together, creating a layer that is more resistant to erosion. The living soil layer readily absorbs and stores water, allowing more complex forms of plant life to grow in places with low precipitation levels.
Among the notable features of the park are the following:
Balanced Rock – a large balancing rock, the size of three school buses
Courthouse Towers – a collection of tall stone columns
Dark Angel – a free-standing 150 ft-tall (46 m) sandstone pillar at the end of the Devils Garden Trail
Delicate Arch – a lone-standing arch that has become a symbol of Utah and the most recognized arch in the park
Devils Garden – many arches and columns scattered along a ridge
Double Arch – two arches that share a common end
Fiery Furnace – an area of maze-like narrow passages and tall rock columns (see biblical reference, Book of Daniel, chapter 3)
Landscape Arch – a very thin and long arch in the Devils Garden with a span of 290 ft (88 m) (the longest arch in the park)
Petrified Dunes – petrified remnants of dunes blown from the ancient lakes that covered the area
The Phallus – a rock spire that resembles a phallus
Wall Arch – located along the popular Devils Garden Trail; collapsed sometime on August 4/5, 2008
The Three Gossips –a mid-sized sandstone tower located in the Courthouse Towers area.
Utah is a landlocked state in the Mountain West subregion of the Western United States. It borders Colorado to its east, Wyoming to its northeast, Idaho to its north, Arizona to its south, and Nevada to its west. Utah also touches a corner of New Mexico in the southeast. Of the fifty U.S. states, Utah is the 13th-largest by area; with a population over three million, it is the 30th-most-populous and 11th-least-densely populated. Urban development is mostly concentrated in two areas: the Wasatch Front in the north-central part of the state, which is home to roughly two-thirds of the population and includes the capital city, Salt Lake City; and Washington County in the southwest, with more than 180,000 residents. Most of the western half of Utah lies in the Great Basin.
Utah has been inhabited for thousands of years by various indigenous groups such as the ancient Puebloans, Navajo, and Ute. The Spanish were the first Europeans to arrive in the mid-16th century, though the region's difficult geography and harsh climate made it a peripheral part of New Spain and later Mexico. Even while it was Mexican territory, many of Utah's earliest settlers were American, particularly Mormons fleeing marginalization and persecution from the United States via the Mormon Trail. Following the Mexican–American War in 1848, the region was annexed by the U.S., becoming part of the Utah Territory, which included what is now Colorado and Nevada. Disputes between the dominant Mormon community and the federal government delayed Utah's admission as a state; only after the outlawing of polygamy was it admitted in 1896 as the 45th.
People from Utah are known as Utahns. Slightly over half of all Utahns are Mormons, the vast majority of whom are members of the Church of Jesus Christ of Latter-day Saints (LDS Church), which has its world headquarters in Salt Lake City; Utah is the only state where a majority of the population belongs to a single church. A 2023 paper challenged this perception (claiming only 42% of Utahns are Mormons) however most statistics still show a majority of Utah residents belong to the LDS church; estimates from the LDS church suggests 60.68% of Utah's population belongs to the church whilst some sources put the number as high as 68%. The paper replied that membership count done by the LDS Church is too high for several reasons. The LDS Church greatly influences Utahn culture, politics, and daily life, though since the 1990s the state has become more religiously diverse as well as secular.
Utah has a highly diversified economy, with major sectors including transportation, education, information technology and research, government services, mining, multi-level marketing, and tourism. Utah has been one of the fastest growing states since 2000, with the 2020 U.S. census confirming the fastest population growth in the nation since 2010. St. George was the fastest-growing metropolitan area in the United States from 2000 to 2005. Utah ranks among the overall best states in metrics such as healthcare, governance, education, and infrastructure. It has the 12th-highest median average income and the least income inequality of any U.S. state. Over time and influenced by climate change, droughts in Utah have been increasing in frequency and severity, putting a further strain on Utah's water security and impacting the state's economy.
The History of Utah is an examination of the human history and social activity within the state of Utah located in the western United States.
Archaeological evidence dates the earliest habitation of humans in Utah to about 10,000 to 12,000 years ago. Paleolithic people lived near the Great Basin's swamps and marshes, which had an abundance of fish, birds, and small game animals. Big game, including bison, mammoths and ground sloths, also were attracted to these water sources. Over the centuries, the mega-fauna died, this population was replaced by the Desert Archaic people, who sheltered in caves near the Great Salt Lake. Relying more on gathering than the previous Utah residents, their diet was mainly composed of cattails and other salt tolerant plants such as pickleweed, burro weed and sedge. Red meat appears to have been more of a luxury, although these people used nets and the atlatl to hunt water fowl, ducks, small animals and antelope. Artifacts include nets woven with plant fibers and rabbit skin, woven sandals, gaming sticks, and animal figures made from split-twigs. About 3,500 years ago, lake levels rose and the population of Desert Archaic people appears to have dramatically decreased. The Great Basin may have been almost unoccupied for 1,000 years.
The Fremont culture, named from sites near the Fremont River in Utah, lived in what is now north and western Utah and parts of Nevada, Idaho and Colorado from approximately 600 to 1300 AD. These people lived in areas close to water sources that had been previously occupied by the Desert Archaic people, and may have had some relationship with them. However, their use of new technologies define them as a distinct people. Fremont technologies include:
use of the bow and arrow while hunting,
building pithouse shelters,
growing maize and probably beans and squash,
building above ground granaries of adobe or stone,
creating and decorating low-fired pottery ware,
producing art, including jewelry and rock art such as petroglyphs and pictographs.
The ancient Puebloan culture, also known as the Anasazi, occupied territory adjacent to the Fremont. The ancestral Puebloan culture centered on the present-day Four Corners area of the Southwest United States, including the San Juan River region of Utah. Archaeologists debate when this distinct culture emerged, but cultural development seems to date from about the common era, about 500 years before the Fremont appeared. It is generally accepted that the cultural peak of these people was around the 1200 CE. Ancient Puebloan culture is known for well constructed pithouses and more elaborate adobe and masonry dwellings. They were excellent craftsmen, producing turquoise jewelry and fine pottery. The Puebloan culture was based on agriculture, and the people created and cultivated fields of maize, beans, and squash and domesticated turkeys. They designed and produced elaborate field terracing and irrigation systems. They also built structures, some known as kivas, apparently designed solely for cultural and religious rituals.
These two later cultures were roughly contemporaneous, and appear to have established trading relationships. They also shared enough cultural traits that archaeologists believe the cultures may have common roots in the early American Southwest. However, each remained culturally distinct throughout most of their existence. These two well established cultures appear to have been severely impacted by climatic change and perhaps by the incursion of new people in about 1200 CE. Over the next two centuries, the Fremont and ancient Pueblo people may have moved into the American southwest, finding new homes and farmlands in the river drainages of Arizona, New Mexico and northern Mexico.
In about 1200, Shoshonean speaking peoples entered Utah territory from the west. They may have originated in southern California and moved into the desert environment due to population pressure along the coast. They were an upland people with a hunting and gathering lifestyle utilizing roots and seeds, including the pinyon nut. They were also skillful fishermen, created pottery and raised some crops. When they first arrived in Utah, they lived as small family groups with little tribal organization. Four main Shoshonean peoples inhabited Utah country. The Shoshone in the north and northeast, the Gosiutes in the northwest, the Utes in the central and eastern parts of the region and the Southern Paiutes in the southwest. Initially, there seems to have been very little conflict between these groups.
In the early 16th century, the San Juan River basin in Utah's southeast also saw a new people, the Díne or Navajo, part of a greater group of plains Athabaskan speakers moved into the Southwest from the Great Plains. In addition to the Navajo, this language group contained people that were later known as Apaches, including the Lipan, Jicarilla, and Mescalero Apaches.
Athabaskans were a hunting people who initially followed the bison, and were identified in 16th-century Spanish accounts as "dog nomads". The Athabaskans expanded their range throughout the 17th century, occupying areas the Pueblo peoples had abandoned during prior centuries. The Spanish first specifically mention the "Apachu de Nabajo" (Navaho) in the 1620s, referring to the people in the Chama valley region east of the San Juan River, and north west of Santa Fe. By the 1640s, the term Navaho was applied to these same people. Although the Navajo newcomers established a generally peaceful trading and cultural exchange with the some modern Pueblo peoples to the south, they experienced intermittent warfare with the Shoshonean peoples, particularly the Utes in eastern Utah and western Colorado.
At the time of European expansion, beginning with Spanish explorers traveling from Mexico, five distinct native peoples occupied territory within the Utah area: the Northern Shoshone, the Goshute, the Ute, the Paiute and the Navajo.
The Spanish explorer Francisco Vázquez de Coronado may have crossed into what is now southern Utah in 1540, when he was seeking the legendary Cíbola.
A group led by two Spanish Catholic priests—sometimes called the Domínguez–Escalante expedition—left Santa Fe in 1776, hoping to find a route to the California coast. The expedition traveled as far north as Utah Lake and encountered the native residents. All of what is now Utah was claimed by the Spanish Empire from the 1500s to 1821 as part of New Spain (later as the province Alta California); and subsequently claimed by Mexico from 1821 to 1848. However, Spain and Mexico had little permanent presence in, or control of, the region.
Fur trappers (also known as mountain men) including Jim Bridger, explored some regions of Utah in the early 19th century. The city of Provo was named for one such man, Étienne Provost, who visited the area in 1825. The city of Ogden, Utah is named for a brigade leader of the Hudson's Bay Company, Peter Skene Ogden who trapped in the Weber Valley. In 1846, a year before the arrival of members from the Church of Jesus Christ of latter-day Saints, the ill-fated Donner Party crossed through the Salt Lake valley late in the season, deciding not to stay the winter there but to continue forward to California, and beyond.
Members of the Church of Jesus Christ of Latter-day Saints, commonly known as Mormon pioneers, first came to the Salt Lake Valley on July 24, 1847. At the time, the U.S. had already captured the Mexican territories of Alta California and New Mexico in the Mexican–American War and planned to keep them, but those territories, including the future state of Utah, officially became United States territory upon the signing of the Treaty of Guadalupe Hidalgo, February 2, 1848. The treaty was ratified by the United States Senate on March 10, 1848.
Upon arrival in the Salt Lake Valley, the Mormon pioneers found no permanent settlement of Indians. Other areas along the Wasatch Range were occupied at the time of settlement by the Northwestern Shoshone and adjacent areas by other bands of Shoshone such as the Gosiute. The Northwestern Shoshone lived in the valleys on the eastern shore of Great Salt Lake and in adjacent mountain valleys. Some years after arriving in the Salt Lake Valley Mormons, who went on to colonize many other areas of what is now Utah, were petitioned by Indians for recompense for land taken. The response of Heber C. Kimball, first counselor to Brigham Young, was that the land belonged to "our Father in Heaven and we expect to plow and plant it." A 1945 Supreme Court decision found that the land had been treated by the United States as public domain; no aboriginal title by the Northwestern Shoshone had been recognized by the United States or extinguished by treaty with the United States.
Upon arriving in the Salt Lake Valley, the Mormons had to make a place to live. They created irrigation systems, laid out farms, built houses, churches, and schools. Access to water was crucially important. Almost immediately, Brigham Young set out to identify and claim additional community sites. While it was difficult to find large areas in the Great Basin where water sources were dependable and growing seasons long enough to raise vitally important subsistence crops, satellite communities began to be formed.
Shortly after the first company arrived in the Salt Lake Valley in 1847, the community of Bountiful was settled to the north. In 1848, settlers moved into lands purchased from trapper Miles Goodyear in present-day Ogden. In 1849, Tooele and Provo were founded. Also that year, at the invitation of Ute chief Wakara, settlers moved into the Sanpete Valley in central Utah to establish the community of Manti. Fillmore, Utah, intended to be the capital of the new territory, was established in 1851. In 1855, missionary efforts aimed at western native cultures led to outposts in Fort Lemhi, Idaho, Las Vegas, Nevada and Elk Mountain in east-central Utah.
The experiences of returning members of the Mormon Battalion were also important in establishing new communities. On their journey west, the Mormon soldiers had identified dependable rivers and fertile river valleys in Colorado, Arizona and southern California. In addition, as the men traveled to rejoin their families in the Salt Lake Valley, they moved through southern Nevada and the eastern segments of southern Utah. Jefferson Hunt, a senior Mormon officer of the Battalion, actively searched for settlement sites, minerals, and other resources. His report encouraged 1851 settlement efforts in Iron County, near present-day Cedar City. These southern explorations eventually led to Mormon settlements in St. George, Utah, Las Vegas and San Bernardino, California, as well as communities in southern Arizona.
Prior to establishment of the Oregon and California trails and Mormon settlement, Indians native to the Salt Lake Valley and adjacent areas lived by hunting buffalo and other game, but also gathered grass seed from the bountiful grass of the area as well as roots such as those of the Indian Camas. By the time of settlement, indeed before 1840, the buffalo were gone from the valley, but hunting by settlers and grazing of cattle severely impacted the Indians in the area, and as settlement expanded into nearby river valleys and oases, indigenous tribes experienced increasing difficulty in gathering sufficient food. Brigham Young's counsel was to feed the hungry tribes, and that was done, but it was often not enough. These tensions formed the background to the Bear River massacre committed by California Militia stationed in Salt Lake City during the Civil War. The site of the massacre is just inside Preston, Idaho, but was generally thought to be within Utah at the time.
Statehood was petitioned for in 1849-50 using the name Deseret. The proposed State of Deseret would have been quite large, encompassing all of what is now Utah, and portions of Colorado, Idaho, Nevada, Wyoming, Arizona, Oregon, New Mexico and California. The name of Deseret was favored by the LDS leader Brigham Young as a symbol of industry and was derived from a reference in the Book of Mormon. The petition was rejected by Congress and Utah did not become a state until 1896, following the Utah Constitutional Convention of 1895.
In 1850, the Utah Territory was created with the Compromise of 1850, and Fillmore (named after President Fillmore) was designated the capital. In 1856, Salt Lake City replaced Fillmore as the territorial capital.
The first group of pioneers brought African slaves with them, making Utah the only place in the western United States to have African slavery. Three slaves, Green Flake, Hark Lay, and Oscar Crosby, came west with this first group in 1847. The settlers also began to purchase Indian slaves in the well-established Indian slave trade, as well as enslaving Indian prisoners of war. In 1850, 26 slaves were counted in Salt Lake County. Slavery didn't become officially recognized until 1852, when the Act in Relation to Service and the Act for the relief of Indian Slaves and Prisoners were passed. Slavery was repealed on June 19, 1862, when Congress prohibited slavery in all US territories.
Disputes between the Mormon inhabitants and the federal government intensified after the Church of Jesus Christ of Latter-day Saints' practice of polygamy became known. The polygamous practices of the Mormons, which were made public in 1854, would be one of the major reasons Utah was denied statehood until almost 50 years after the Mormons had entered the area.
After news of their polygamous practices spread, the members of the LDS Church were quickly viewed by some as un-American and rebellious. In 1857, after news of a possible rebellion spread, President James Buchanan sent troops on the Utah expedition to quell the growing unrest and to replace Brigham Young as territorial governor with Alfred Cumming. The expedition was also known as the Utah War.
As fear of invasion grew, Mormon settlers had convinced some Paiute Indians to aid in a Mormon-led attack on 120 immigrants from Arkansas under the guise of Indian aggression. The murder of these settlers became known as the Mountain Meadows massacre. The Mormon leadership had adopted a defensive posture that led to a ban on the selling of grain to outsiders in preparation for an impending war. This chafed pioneers traveling through the region, who were unable to purchase badly needed supplies. A disagreement between some of the Arkansas pioneers and the Mormons in Cedar City led to the secret planning of the massacre by a few Mormon leaders in the area. Some scholars debate the involvement of Brigham Young. Only one man, John D. Lee, was ever convicted of the murders, and he was executed at the massacre site.
Express riders had brought the news 1,000 miles from the Missouri River settlements to Salt Lake City within about two weeks of the army's beginning to march west. Fearing the worst as 2,500 troops (roughly 1/3rd of the army then) led by General Albert Sidney Johnston started west, Brigham Young ordered all residents of Salt Lake City and neighboring communities to prepare their homes for burning and evacuate southward to Utah Valley and southern Utah. Young also sent out a few units of the Nauvoo Legion (numbering roughly 8,000–10,000), to delay the army's advance. The majority he sent into the mountains to prepare defenses or south to prepare for a scorched earth retreat. Although some army wagon supply trains were captured and burned and herds of army horses and cattle run off no serious fighting occurred. Starting late and short on supplies, the United States Army camped during the bitter winter of 1857–58 near a burned out Fort Bridger in Wyoming. Through the negotiations between emissary Thomas L. Kane, Young, Cumming and Johnston, control of Utah territory was peacefully transferred to Cumming, who entered an eerily vacant Salt Lake City in the spring of 1858. By agreement with Young, Johnston established the army at Fort Floyd 40 miles away from Salt Lake City, to the southwest.
Salt Lake City was the last link of the First Transcontinental Telegraph, between Carson City, Nevada and Omaha, Nebraska completed in October 1861. Brigham Young, who had helped expedite construction, was among the first to send a message, along with Abraham Lincoln and other officials. Soon after the telegraph line was completed, the Deseret Telegraph Company built the Deseret line connecting the settlements in the territory with Salt Lake City and, by extension, the rest of the United States.
Because of the American Civil War, federal troops were pulled out of Utah Territory (and their fort auctioned off), leaving the territorial government in federal hands without army backing until General Patrick E. Connor arrived with the 3rd Regiment of California Volunteers in 1862. While in Utah, Connor and his troops soon became discontent with this assignment wanting to head to Virginia where the "real" fighting and glory was occurring. Connor established Fort Douglas just three miles (5 km) east of Salt Lake City and encouraged his bored and often idle soldiers to go out and explore for mineral deposits to bring more non-Mormons into the state. Minerals were discovered in Tooele County, and some miners began to come to the territory. Conner also solved the Shoshone Indian problem in Cache Valley Utah by luring the Shoshone into a midwinter confrontation on January 29, 1863. The armed conflict quickly turned into a rout, discipline among the soldiers broke down, and the Battle of Bear River is today usually referred to by historians as the Bear River Massacre. Between 200 and 400 Shoshone men, women and children were killed, as were 27 soldiers, with over 50 more soldiers wounded or suffering from frostbite.
Beginning in 1865, Utah's Black Hawk War developed into the deadliest conflict in the territory's history. Chief Antonga Black Hawk died in 1870, but fights continued to break out until additional federal troops were sent in to suppress the Ghost Dance of 1872. The war is unique among Indian Wars because it was a three-way conflict, with mounted Timpanogos Utes led by Antonga Black Hawk fighting federal and Utah local militia.
On May 10, 1869, the First transcontinental railroad was completed at Promontory Summit, north of the Great Salt Lake. The railroad brought increasing numbers of people into the state, and several influential businessmen made fortunes in the territory.
Main article: Latter Day Saint polygamy in the late-19th century
During the 1870s and 1880s, federal laws were passed and federal marshals assigned to enforce the laws against polygamy. In the 1890 Manifesto, the LDS Church leadership dropped its approval of polygamy citing divine revelation. When Utah applied for statehood again in 1895, it was accepted. Statehood was officially granted on January 4, 1896.
The Mormon issue made the situation for women the topic of nationwide controversy. In 1870 the Utah Territory, controlled by Mormons, gave women the right to vote. However, in 1887, Congress disenfranchised Utah women with the Edmunds–Tucker Act. In 1867–96, eastern activists promoted women's suffrage in Utah as an experiment, and as a way to eliminate polygamy. They were Presbyterians and other Protestants convinced that Mormonism was a non-Christian cult that grossly mistreated women. The Mormons promoted woman suffrage to counter the negative image of downtrodden Mormon women. With the 1890 Manifesto clearing the way for statehood, in 1895 Utah adopted a constitution restoring the right of women's suffrage. Congress admitted Utah as a state with that constitution in 1896.
Though less numerous than other intermountain states at the time, several lynching murders for alleged misdeeds occurred in Utah territory at the hand of vigilantes. Those documented include the following, with their ethnicity or national origin noted in parentheses if it was provided in the source:
William Torrington in Carson City (then a part of Utah territory), 1859
Thomas Coleman (Black man) in Salt Lake City, 1866
3 unidentified men at Wahsatch, winter of 1868
A Black man in Uintah, 1869
Charles A. Benson in Logan, 1873
Ah Sing (Chinese man) in Corinne, 1874
Thomas Forrest in St. George, 1880
William Harvey (Black man) in Salt Lake City, 1883
John Murphy in Park City, 1883
George Segal (Japanese man) in Ogden, 1884
Joseph Fisher in Eureka, 1886
Robert Marshall (Black man) in Castle Gate, 1925
Other lynchings in Utah territory include multiple instances of mass murder of Native American children, women, and men by White settlers including the Battle Creek massacre (1849), Provo River Massacre (1850), Nephi massacre (1853), and Circleville Massacre (1866).
Beginning in the early 20th century, with the establishment of such national parks as Bryce Canyon National Park and Zion National Park, Utah began to become known for its natural beauty. Southern Utah became a popular filming spot for arid, rugged scenes, and such natural landmarks as Delicate Arch and "the Mittens" of Monument Valley are instantly recognizable to most national residents. During the 1950s, 1960s, and 1970s, with the construction of the Interstate highway system, accessibility to the southern scenic areas was made easier.
Beginning in 1939, with the establishment of Alta Ski Area, Utah has become world-renowned for its skiing. The dry, powdery snow of the Wasatch Range is considered some of the best skiing in the world. Salt Lake City won the bid for the 2002 Winter Olympics in 1995, and this has served as a great boost to the economy. The ski resorts have increased in popularity, and many of the Olympic venues scattered across the Wasatch Front continue to be used for sporting events. This also spurred the development of the light-rail system in the Salt Lake Valley, known as TRAX, and the re-construction of the freeway system around the city.
During the late 20th century, the state grew quickly. In the 1970s, growth was phenomenal in the suburbs. Sandy was one of the fastest-growing cities in the country at that time, and West Valley City is the state's 2nd most populous city. Today, many areas of Utah are seeing phenomenal growth. Northern Davis, southern and western Salt Lake, Summit, eastern Tooele, Utah, Wasatch, and Washington counties are all growing very quickly. Transportation and urbanization are major issues in politics as development consumes agricultural land and wilderness areas.
In 2012, the State of Utah passed the Utah Transfer of Public Lands Act in an attempt to gain control over a substantial portion of federal land in the state from the federal government, based on language in the Utah Enabling Act of 1894. The State does not intend to use force or assert control by limiting access in an attempt to control the disputed lands, but does intend to use a multi-step process of education, negotiation, legislation, and if necessary, litigation as part of its multi-year effort to gain state or private control over the lands after 2014.
Utah families, like most Americans everywhere, did their utmost to assist in the war effort. Tires, meat, butter, sugar, fats, oils, coffee, shoes, boots, gasoline, canned fruits, vegetables, and soups were rationed on a national basis. The school day was shortened and bus routes were reduced to limit the number of resources used stateside and increase what could be sent to soldiers.
Geneva Steel was built to increase the steel production for America during World War II. President Franklin D. Roosevelt had proposed opening a steel mill in Utah in 1936, but the idea was shelved after a couple of months. After the attack on Pearl Harbor, the United States entered the war and the steel plant was put into progress. In April 1944, Geneva shipped its first order, which consisted of over 600 tons of steel plate. Geneva Steel also brought thousands of job opportunities to Utah. The positions were hard to fill as many of Utah's men were overseas fighting. Women began working, filling 25 percent of the jobs.
As a result of Utah's and Geneva Steels contribution during the war, several Liberty Ships were named in honor of Utah including the USS Joseph Smith, USS Brigham Young, USS Provo, and the USS Peter Skene Ogden.
One of the sectors of the beachhead of Normandy Landings was codenamed Utah Beach, and the amphibious landings at the beach were undertaken by United States Army troops.
It is estimated that 1,450 soldiers from Utah were killed in the war.
Gjirokastra - Central place.
Gjirokastra, the "Stone City", situated in the southern part of Albania, on the the easter slope of mountain Mali i Gjere. It is a commercial center in South Albania, it produces foodstuffs, leather, and textiles. There are several 18th-century mosques and churches and an old citadel (rebuilt in the 19th cent.) in the town. Dating probably from the 4th cent., Gjirokastër passed to the Turks in the 15th cent. It was captured (1811) by Ali Pasha and was the center (late 1800s) of anti-Turkish resistance. In World War II it was occupied by Italy, Greece, and Germany in succession. Enver Hoxha, the Albanian Communist party leader, was born there . Gjirokastra is museum city with charasterist houses made from stone.
What strikes the visitors most in Gjirokastra are its typical and characteristic houses which resemble little fortresses, clustered one above the other. Their exterior combines roughness with the beauty of windows, small rooms and light pillars supporting the roofs prtotruding from the walls.
Gjirokastra´s population is around 40,000 and one of the biggest cities of southern Albania. The name Gjirokastra comes from Illyrian Argyres Tribe which inhabited these parts of Europe.
Gjirokastra is a home of traditional Albanian folk festival.
Trying to recreate the feeling of a 1940s Hollywood portrait.
Key light studio strobe with small reflector feathered in front of subject.
Combined background light and fill bounced back from side wall camera left. Hair light behind subject camera right.
A mid-scale combine to harvest grains on the Thirdwigg Farm. This combine matches the Atmos Tractor in scale and design. Instructions are at rebrickable.com/mocs/MOC-98202/thirdwigg/synthe-combine/#..., and the grain header instructions can be found at rebrickable.com/mocs/MOC-99038/thirdwigg/grain-head-for-s...
The Combine features the following:
Steering
Front wheel driven two stage thresher
Straw spreader
Adjustable grain extractor
Opening hopper
Opening right side
Header lift
Removeable header
Working cutbar
Cutting edge auger
Opening cabin door
Find the video at www.youtube.com/watch?v=syEdF3BfznY&t=6s
The Jovian System!
The Planet Jupiter & Galilean Moons last night.
Seeing was boiling...so I went down to lower power to get Jupiter & the Nicely placed Galilean Moons. I ran the Chip ROI at 1280 x 400 @30fps to fit them all in.
Jupiter with Ganymede, Io, Callisto, & Europa. Turned out okay..C8 at Prime focus with the QHY5IIL CCD camera, (1800 frames) 600 frames each RGB, Stacked in Registax, then RGB combined in Maxim DL.
Best Regards,
John Chumack
Cabin Creek & Hellam Combine No.7
The Cabin Creek & Hellam Railroad ( CC&H RR ) is a freelanced (fictional) railroad set in 1912.
Chartered in 1850, with construction finished in 1854, the Cabin Creek & Hellam’s route begins by following the Cabin Creek as it meanders its way up from its mouth at the Susquehanna river at Long Level in the eastern part York County, Pennsylvania. The route brings the railroad to the small town of East Prospect, one of three station stops along the line. From there it continues to follow the creek valley until reaching the Margaretta Mill (which it services), and former site of the Margaretta Iron Furnace. The iron furnace was the primary reason for the railroad being built, allowing the railroad to bring in raw materials, and then ship out finished iron products. Once leaving the Margaretta Mill and the banks of the Cabin Creek, the railroad turns toward the town of Yorkana where it makes another station stop. Finally, the route continues on to the railroad’s namesake town of Hellam, Pennsylvania where the railroad terminates as it interchanges with the York-Wrightsville branch of the Northern Central Railroad.
Combine no.7 had an interesting history on the railroad. Originally a much longer car built by the Billmeyer & Small of York, Pa, combine 7 suffered heavy damage from a derailment on the line in 1905. The car was rebuilt by the railroad by removing the damaged end of the car, salvaging parts, and shortening it to its current length. The idea for the shortened car came from the railroad’s chief mechanical officer who a few years earlier had seen a similar short combine car while traveling out west on the Gorre & Depheted Railroad. The CC&H still had need for the combine, but not the capacity of the full car. Shortening the wrecked car was deemed an economical way of repairing the car and getting it back into service quickly.
Combine no. 7 was almost always seen accompanying the market and milk cars on the early morning market train. The car doubled as caboose for these runs while also carrying merchants accompanying their produce to market. Combine no. 7 also found use on the weekend trains when extra capacity was needed during the summer. These trains ferried people to and from Valley Veiw Park, and swimmers down to the Susquehanna river.
This model was originally a design by my friend Glenn Holland. He sent out the instruction for this car as a Christmas gift in 2020 to his close friends from the LEGO train community. Glenn’s inspiration for this car came from the late John Allen, who is remembered for revolutionizing the art and hobby of model railroading, introducing countless new techniques to the scene, and creating what is regarded as one of the greatest model railroads of all time. This “shorty” combine (combination coach baggage car) was a model built by John Allen for his model railroad, the Gorre & Dapheted. In addition to being a great modeler, Mr. Allen had a wonderful sense of humor and a gift for whimsy. The shorty combine certainly shows that.
Glenn’s recreation of this car in LEGO captures both the attention to detail, and humor of John Allen’s model perfectly. It was an honor to have received the instructions for his model as a gift.
While I could have built this car in its Gorre & Dapheted dark red paint scheme as modeled by Glenn, I decided to take a different route. I had the idea for a freelanced railroad, set in the area of York, Pa where I grew up, brewing for some time. After some thought I came to the conclusion that the combine would be a great first model for my little fictional railroad. I have been dying to use bright yellow in a model for ages, and so that is what I started with. Adding dark green trim, and a reddish brown roof completed the paint scheme. The CC&H logo for the decals was designed by me and printed by OKBrickworks. I am very happy with how this car turned out and it will be treasured part of my model collection.
G540, X50, 48121 & 8101 pass through Rookwood with a combined 5938 Manildra Flour & 5136 Weston Millings Grain, on Sunday 5th August 2012.
Combined a visit to the Gallery and photos by Vanda Raleska and Eddie Hyde as well as wander among the vines. This tractor driver was not keen to be photographed or maybe he was concerned about running me over
20210729-DSC09050 1400x1050
Combine near Glasgow in rural Saline County Missouri by Notley Hawkins Photography. Taken with a Canon EOS 5D Mark IV camera with a Canon EF16-35mm f/4L IS USM lens at ƒ/4.0 with a 39 second exposure at ISO 200. Processed with Adobe Lightroom CC.
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©Notley Hawkins
Hi!
Today I present you my 5th combine alt model after 5765, 5761, 31024, 31027! Hope you like it!
You can find the previous four models on my MOCpage !
The Chesapeake Bay Bridge–Tunnel
The Chesapeake Bay Bridge–Tunnel (CBBT) is a 23-mile (37 km) bridge–tunnel crossing at the mouth of the Chesapeake Bay, the Hampton Roads harbor, and nearby mouths of the James and Elizabeth Rivers in the American state of Virginia. It connects Northampton County on the Delmarva Peninsula and Eastern Shore with Virginia Beach, Norfolk, Chesapeake, and Portsmouth on the Western Shore and South side / Tidewater which are part of the Hampton Roads metropolitan area of eight close cities around the harbor's shores and peninsula. The Bridge-Tunnel originally combined 12 miles (19 km) of trestle, two 1-mile-long (1.6 km) tunnels, four artificial islands, four high-level bridges, approximately 2 miles (3.2 km) of causeway, and 5.5 miles (8.9 km) of northeast and southwest approach roads—crossing the Chesapeake Bay and preserving traffic on the Thimble Shoals and Chesapeake dredged shipping channels leading to the Atlantic. It replaced vehicle ferry services that operated from South Hampton Roads and from the Virginia Peninsula since the 1930s. Financed by toll revenue bonds, the Bridge–Tunnel was opened on April 15, 1964,[1] and remains one of only ten bridge–tunnel systems in the world, three of which are located in the water dominated Hampton Roads area of Tidewater Virginia.
As of May 2018 the Chesapeake Bay Bridge–Tunnel has been crossed by more than 130 million vehicles.[2] The CBBT complex carries U.S. Route 13, the main north–south highway on Virginia's Eastern Shore on the Delmarva peninsula, and, as part of the East Coast's longstanding Ocean Highway, provides the only straight direct link along the East Coast and Atlantic Ocean, between the Eastern Shore and South Hampton Roads regions, as well as an alternate route to link the Northeast U.S.A. and points in between with Norfolk and further south to the Carolinas and Florida. The Bridge–Tunnel saves motorists 95 miles (153 km) and 1 1⁄2 hours on a trip between Virginia Beach/Norfolk and points north and east of the Chesapeake and Delaware Valley, River and Bay without going through the traffic congestion in the Baltimore–Washington Metropolitan Area further west in Maryland and Northern Virginia. The $15 toll is partially offset by some savings of highway tolls in Maryland and Delaware and avoiding often heavy traffic on north-south Interstate 95 (I-95) built in the 1960s and completed in the late 1970s and parallel older United States Route 1 (US-1) from the 1920s. From 1995 to 1999, at an additional cost of almost $200 million, the capacity of the above-water portion of bridges on the facility was increased and widened to four lanes. An upgrade of the two-lane tunnels is currently underway. [3] The crossing was officially named the Lucius J. Kellam Jr. Bridge–Tunnel in August 1987, 23 years after opening, honoring one of the civic leaders who had long worked for its development, construction and operation; it continues however to be best known as the Chesapeake Bay Bridge–Tunnel. The complex was built by and is operated by the Chesapeake Bay Bridge and Tunnel District, a political subdivision of the Commonwealth of Virginia governed by the Chesapeake Bay Bridge and Tunnel Commission and in cooperation with the state Department of Transportation. Costs are recovered through toll collections. In 2002, a Joint Legislative Audit and Review Commission (JLARC) study commissioned by the Virginia General Assembly concluded that "given the inability of the state to fund future capital requirements of the CBBT, the District and Commission should be retained to operate and maintain the Bridge–Tunnel as a toll facility in perpetuity."
Occasionally because of similar names, the Bridge-Tunnel is often confused with the Chesapeake Bay Bridge (also known as the Governor William Preston Lane, Jr. Memorial Bridge) further north in Maryland crossing the middle portion of the Bay from Annapolis to Kent Island on the Maryland Eastern Shore of Delmarva. It was built with two lanes and a higher suspension segment in the middle from 1949 - 1952, with a second parallel wider span of three lanes in 1973. It is one of the longest and highest bridges in the world.
Source: en.wikipedia.org/wiki/Chesapeake_Bay_Bridge%E2%80%93Tunnel
Chesapeake Bay
-was formed nearly 12,000 years ago when glaciers melted and flooded the Susquehanna River valley;
-is—most historians believe—named after the Algonquin word chesepiooc, meaning "great shellfish bay;"
-is approximately 200 miles long, stretching from Havre de Grace, Maryland, to Norfolk, Virginia;
-has an average depth of 21 feet (the deepest part of the Bay, a.k.a. "The Hole," is 174 feet deep and located off of Bloody Point, southeast of
Annapolis, Maryland;
-ranges from 3.4 to 35 miles wide;
-holds more than 15 trillion gallons of water;
-supports 348 species of finfish and 173 species of shellfish;
-supports more than 3,600 species of plant and animal life, including 2,700 types of plants and more than 16 species of underwater grasses;
-is fed by 50 major tributaries (or streams and rivers) every day—the largest of these are the Susquehanna, Potomac, Rappahannock, York, and James;
-produces more than 500 millions pounds of seafood harvest each year.
Source: www.cbf.org/about-the-bay/chesapeake-bay-watershed-geogra...
Fisherman Island National Wildlife Refuge
Fisherman Island is the southernmost island on the Delmarva Peninsula chain of barrier islands. Located at the entrance to the Chesapeake Bay, the island is subject to great changes in its landscape from waves and runoff. It first formed about 200 to 250 years ago.
Fisherman Island National Wildlife Refuge is located within the United States Fish and Wildlife Service's Eastern Shore of Virginia National Wildlife Refuge, and is cut in half by the presence of U.S. Highway 13 and the Chesapeake Bay Bridge Tunnel. The refuge is closed to the public.
The island is the habitat to migratory waterfowl, shorebirds, and nesting waterbirds. In September 2003, the island was almost entirely flooded by Hurricane Isabel.
Source: en.wikipedia.org/wiki/Fisherman_Island_(Virginia)
+++ DISCLAIMER +++
Nothing you see here is real, even though the model, the conversion or the presented background story might be based on historical facts. BEWARE!
Some background:
The AH-1 Cobra was developed in the mid-1960s as an interim gunship for the U.S. Army for use during the Vietnam War. The Cobra shared the proven transmission, rotor system, and the T53 turboshaft engine of the UH-1 "Huey". By June 1967, the first AH-1G HueyCobras had been delivered. Bell built 1,116 AH-1Gs for the U.S. Army between 1967 and 1973, and the Cobras chalked up over a million operational hours in Vietnam.
The U.S. Marine Corps was very interested in the AH-1G Cobra, too, but it preferred a twin-engine version for improved safety in over-water operations, and also wanted a more potent turret-mounted weapon. At first, the Department of Defense had balked at providing the Marines with a twin-engine version of the Cobra, in the belief that commonality with Army AH-1Gs outweighed the advantages of a different engine fit. However, the Marines won out and awarded Bell a contract for 49 twin-engine AH-1J SeaCobras in May 1968. As an interim measure the U.S. Army passed on thirty-eight AH-1Gs to the Marines in 1969. The AH-1J also received a more powerful gun turret with a three-barrel 20 mm XM197 cannon based on the six-barrel M61 Vulcan cannon.
During the 1990s, the US forces gradually phased out its Cobra fleet. The withdrawn AH-1s were typically offered to other potential operators, usually NATO allies. Some were also given to the USDA's Forest Service for fire surveillance, and a handful AH-1s went into private hands, including the NASA. Among these airframes were some USMC AH-1Js, which had in part been mothballed in the Mojave Desert since their replacement through more powerful and modern AH-1 variants and the AH-64.
About twenty airframes were, after having been de-militarized, bought by the Kaman Corporation in 2003, in a bold move to quickly respond to more than 20 inquiries for the company’s K-1200 ‘K-Max’ crane synchropter since the type’s end of production in 2001 from firefighting, logging and industry transport requirements. While not such a dedicated medium lift helicopter as the K-1200, which had from the outset been optimized for external cargo load operations, the twin-engine AH-1J promised to be a very effective alternative and a powerful basis for a conversion into a crane helicopter.
The result of this conversion program was the Kaman K-1300, also known as the “K-Cobra” or “Crane Cobra”. While the basic airframe of the AH-1J was retained, extensive detail modifications were made. To reduce weight and compensate for the extensive hardware changes, the SeaCobra lost its armor, the chin turret, and the stub wings. Beyond that, many invisible changes were made; the internal structure between the engine mounts was beefed up with an additional cage structure and a cargo hook was installed under the fuselage in the helicopter’s center of lift.
To further optimize the K-Cobra’s performance, the dynamic components were modified and improved, too. While the engine remained the same, its oil cooler was enlarged and the original output limit to 1.500 shp was removed and the gearbox was strengthened to fully exploit the twin-engine’s available power of 1,800 shp (1,342 kW). The rotor system was also modified and optimized for the transport of underslung loads: the original UH-1 dual-blade rotors were replaced with new four-blade rotors. The new main rotor with rugged heavy-duty blades offered more lift at less rotor speed, and the blades’ lift sections were moved away from the hub so that downwash and turbulences directly under the helicopter’s CoG and man hook were reduced to keep the cargo load more stable. Due to the main rotor’s slightly bigger diameter the tail rotor was changed into a slightly smaller four-blade rotor, too. This new arrangement made the K-1300 more stable while hovering or during slow speed maneuvers and more responsive to steering input.
The Cobra’s crew of two was retained, but the cockpit was re-arranged and split into two compartments: the pilot retained the original rear position in the tandem cockpit under the original glazing, but the gunner’s station in front of him, together with the secondary dashboard, was omitted and replaced by a new, fully glazed cabin under the former gunner position. This cabin occupied the former gun station and its ammunition supply and contained a rearward-facing workstation for a second pilot with full controls. It was accessible via a separate door or a ladder from above, through a trap door in the former gunner’s station floor, where a simple foldable bench was available for a third person. This arrangement was chosen due to almost complete lack of oversight of the slung load from the normal cockpit position, despite a CCTV (closed circuit television) system with two cameras intended for observation of slung loads. The second pilot would control the helicopter during delicate load-handling maneuvers, while the primary pilot “above” would fly the helicopter during transfer flights, both sharing the workload.
To accommodate the cabin under the fuselage and improve ground handling, the AH-1J’s skids were replaced by a stalky, fixed four-wheel landing gear that considerably increased ground clearance (almost 7 feet), making the attachment of loads on the ground to the main ventral hook easier, as the K-1300 could be “rolled over” the cargo on the ground and did not have to hover above it to connect. However, an external ladder had to be added so that the pilot could reach his/her workstation almost 10 feet above the ground.
The bulky ventral cabin, the draggy landing gear and the new lift-optimized rotor system reduced the CraneCobra’s top speed by a third to just 124 mph (200 km/h), but the helicopter’s load-carrying capacity became 35% higher and the Cobra’s performance under “hot & high” conditions was markedly improved, too.
For transfer flights, a pair of external auxiliary tanks could be mounted to the lower fuselage flanks, which could also be replaced with cargo boxes of similar size and shape.
K-1300 buyers primarily came from the United States and Canada, but there were foreign operators, too. A major operator in Europe became Heliswiss, the oldest helicopter company in Switzerland. The company was founded as „Heliswiss Schweizerische Helikopter AG“, with headquarters in Berne-Belp on April 17, 1953, what also marked the beginning of commercial helicopter flying in Switzerland. During the following years Heliswiss expanded in Switzerland and formed a network with bases in Belp BE, Samedan GR, Domat Ems GR, Locarno TI, Erstfeld UR, Gampel VS, Gstaad BE and Gruyères FR. During the build-up of the rescue-company Schweizerische Rettungsflugwacht (REGA) as an independent network, Heliswiss carried out rescue missions on their behalf.
Heliswiss carried out operations all over the world, e. g. in Greenland, Suriname, North Africa and South America. The first helicopter was a Bell 47 G-1, registered as HB-XAG on September 23, 1953. From 1963 Heliswiss started to expand and began to operate with medium helicopters like the Agusta Bell 204B with a turbine power of 1050 HP and an external load of up to 1500 kg. From 1979 Heliswiss operated a Bell 214 (external load up to 2.8 t).
Since 1991 Heliswiss operated a Russian Kamov 32A12 (a civil crane version of the Ka-27 “Helix”), which was joined by two K-1300s in 2004. They were frequently used for construction of transmission towers for overhead power lines and pylons for railway catenary lines, for selective logging and also as fire bombers with underslung water bags, the latter managed by the German Helog company, operating out of Ainring and Küssnacht in Germany and Switzerland until 2008, when Helog changed its business focus into a helicopter flight training academy in Liberia with the support of Germany's Federal Ministry of Education and Research.
A second Kamov 32A12 joined the fleet in 2015, which replaced one of the K-1300s, and Heliswiss’ last K-1300 was retired in early 2022.
General characteristics:
Crew: 2, plus space for a passenger
Length: 54 ft 3 in (16,56 m) including rotors
44 ft 5 in (13.5 m) fuselage only
Main rotor diameter: 46 ft 2¾ in (14,11 m)
Main rotor area: 1,677.64 sq ft (156,37 m2)
Width (over landing gear): 12 ft 6 in (3.85 m)
Height: 17 ft 8¼ in (5,40 m)
Empty weight: 5,810 lb (2,635 kg)
Max. takeoff weight: 9,500 lb (4,309 kg) without slung load
13,515 lb (6,145 kg) with slung load
Powerplant:
1× P&W Canada T400-CP-400 (PT6T-3 Twin-Pac) turboshaft engine, 1,800 shp (1,342 kW)
Performance:
Maximum speed: 124 mph (200 km/h, 110 kn)
Cruise speed: 105 mph (169 km/h, 91 kn)
Range: 270 mi (430 km, 230 nmi) with internal fuel only,
360 mi (570 km 310 nmi) with external auxiliary tanks
Service ceiling: 15,000 ft (4,600 m)
Hovering ceiling out of ground effect: 3,000 m (9,840 ft)
Rate of climb: 2,500 ft/min (13 m/s) at Sea Level with flat-rated torque
External load capacity (at ISA +15 °C (59.0 °F):
6,000 lb (2,722 kg) at sea level
5,663 lb (2,569 kg) at 5,000 ft (1,524 m)
5,163 lb (2,342 kg) at 10,000 ft (3,048 m)
5,013 lb (2,274 kg) at 12,100 ft (3,688 m)
4,313 lb (1,956 kg) at 15,000 ft (4,600 m)
The kit and its assembly:
This is/was the second contribution to the late 2022 “Logistics” Group Build at whatifmodellers.com, a welcome occasion and motivation to tackle a what-if project that had been on my list for a long while. This crane helicopter conversion of a HueyCobra was inspired by the Mil Mi-10K helicopter – I had built a 1:100 VEB Plasticart kit MANY years ago and still remembered the helicopter’s unique ventral cabin under the nose with a rearward-facing second pilot. I always thought that the AH-1 might be a good crane helicopter, too, esp. the USMC’s twin-engine variant. And why not combine everything in a fictional model?
With this plan the basis became a Fujimi 1:72 AH-1J and lots of donor parts to modify the basic hull into “something else”. Things started with the removal of the chin turret and part of the lower front hull to make space for the ventral glass cabin. The openings for the stub wings were faired over and a different stabilizer (taken from a Revell EC 135, including the end plates) was implanted. The attachment points for the skids were filled and a styrene tube was inserted into the rotor mast opening to later hold the new four-blade rotor. Another styrene tube with bigger diameter was inserted into the lower fuselage as a display holder adapter for later flight scene pictures. Lead beads filled the nose section to make sure the CraneCobra would stand well on its new legs, with the nose down. The cockpit was basically taken OOB, just the front seat and the respective gunner dashboard was omitted.
One of the big challenges of this build followed next: the ventral cabin. Over the course of several months, I was not able to find a suitable donor, so I was forced to scratch the cabin from acrylic and styrene sheet. Size benchmark became the gunner’s seat from the Cobra kit, with one of the OOB pilots seated. Cabin width was less dictated through the fuselage, the rest of the cabin’s design became a rather simple, boxy thing – not pretty, but I think a real-life retrofitted cabin would not look much different? Some PSR was done to hide the edges of the rather thick all-clear walls and create a 3D frame - a delicate task. Attaching the completed thing with the second pilot and a dashboard under the roof to the Cobra’s lower hull and making it look more or less natural without major accidents was also a tricky and lengthy affair, because I ignored the Cobra’s narrowing nose above the former chin turret.
With the cabin defining the ground helicopter’s clearance, it was time for the next donors: the landing gear from an Airfix 1:72 Kamow Ka-25, which had to be modified further to achieve a proper stance. The long main struts were fixed to the hull, their supporting struts had to be scratched, in this case from steel wire. The front wheels were directly attached to the ventral cabin (which might contain in real life a rigid steel cage that not only protects the second crew member but could also take the front wheels’ loads?). Looks pretty stalky!
Under the hull, a massive hook and a fairing for the oil cooler were added. A PE brass ladder was mounted on the right side of the hull under the pilot’s cockpit, while a rear-view mirror was mounted for the ventral pilot on the left side.
The rotor system was created in parallel, I wanted “something different” from the UH-1 dual-blade rotors. The main rotor hub was taken from a Mistercraft 1:72 Westland Lynx (AFAIK a re-boxed ZTS Plastyk kit), which included the arms up to the blades. The hub was put onto a metal axis, with a spacer to make it sit well in the new styrene tube adapter inside of the hull, and some donor parts from the Revell EC 135. Deeper, tailored blades were glued to the Lynx hub, actually leftover parts from the aforementioned wrecked VEB Plasticart 1:100 Mi-10, even though their length had to be halved (what makes you aware how large a Mi-6/10 is compared with an AH-1!). The tail rotor was taken wholesale from the Lynx and stuck to the Cobra’s tail with a steel pin.
Painting and markings:
Another pushing factor for this build was the fact that I had a 1:72 Begemot aftermarket decal sheet for the Kamow Ka-27/32 in The Stash™, which features, among many military helicopters, (the) two civil Heliswiss machines – a perfect match!
Using the Swiss Helix’ as design benchmark I adapted their red-over-white paint scheme to the slender AH-1 and eventually ended up with a simple livery with a white belly (acrylic white from the rattle can, after extensive masking of the clear parts with Maskol/latex milk) and a red (Humbrol 19) upper section, with decorative counter-colored cheatlines along the medium waterline. A black anti-glare panel was added in front of the windscreen. The auxiliary tanks were painted white, too, but they were processed separately and mounted just before the final coat of varnish was applied. The PE ladder as well as the rotors were handled similarly.
The cockpit and rotor opening interior were painted in a very dark grey (tar black, Revell 06), while the interior of the air intakes was painted bright white (Revell 301). The rotor blades became light grey (Revell 75) with darker leading edges (Humbrol 140), dark grey (Humbrol 164) hubs and yellow tips.
For the “HELOG/Heliswiss” tagline the lower white section had to be raised to a medium position on the fuselage, so that they could be placed on the lower flanks under the cockpit. The white civil registration code could not be placed on the tail and ended up on the engine cowling, on red, but this does not look bad or wrong at all.
The cheatlines are also decals from the Ka-32 Begemot sheet, even though they had to be trimmed considerably to fit onto the Cobra’s fuselage – and unfortunately the turned out to be poorly printed and rather brittle, so that I had to improvise and correct the flaws with generic red and white decal lines from TL Modellbau. The white cross on the tail and most stencils came from the Begemot sheet, too. Black, engine soot-hiding areas on the Cobra’s tail were created with generic decal sheet material, too.
The rotor blades and the wheels received a black ink treatment to emphasize their details, but this was not done on the hull to avoid a dirty or worn look. After some final details like position lights the model was sealed with semi-matt acrylic varnish, while the rotors became matt.
A weird-looking what-if model, but somehow a crane-copter variant of the AH-1 looks quite natural – even more so in its attractive red-and-white civil livery. The stalky landing gear is odd, though, necessitated by the ventral cabin for the second pilot. I was skeptical, but scratching the latter was more successful than expected, and the cabin blend quite well into the AH-1 hull, despite its boxy shape.