On the Patch - Stunning ducks , nowhere near as common as they were , rafts of 400+ in the 1970s at Pennington Flash these days if you see one its notable .

Syracuse is a historic city in Sicily, the capital of the province of Syracuse. The city is notable for its rich Greek history, culture, amphitheatres, architecture, and as the birthplace of the preeminent mathematician and engineer Archimedes. This 2,700-year-old city played a key role in ancient times, when it was one of the major powers of the Mediterranean world. Syracuse is located in the southeast corner of the island of Sicily, right by the Gulf of Syracuse next to the Ionian Sea.

 

The city was founded by Ancient Greek Corinthians and Teneans and became a very powerful city-state. Syracuse was allied with Sparta and Corinth and exerted influence over the entirety of Magna Graecia, of which it was the most important city. Described by Cicero as "the greatest Greek city and the most beautiful of them all", it equaled Athens in size during the fifth century BC. It later became part of the Roman Republic and Byzantine Empire. After this Palermo overtook it in importance, as the capital of the Kingdom of Sicily. Eventually the kingdom would be united with the Kingdom of Naples to form the Two Sicilies until the Italian unification of 1860.

 

In the modern day, the city is listed by UNESCO as a World Heritage Site along with the Necropolis of Pantalica. In the central area, the city itself has a population of around 125,000 people. The inhabitants are known as Siracusans. Syracuse is mentioned in the Bible in the Acts of the Apostles book at 28:12 as Paul stayed there.

 

A notable feature of Hanbury Hall, England, is the painting of the staircase, hall ceiling, and other rooms by the English painter Sir James Thornhill (1675-1734).

The focus of the paintings around the stairwell is the life of the Greek hero Achilles, as told by a range of classical sources. They are surmounted by a large representation of the Olympian gods on the ceiling.

The 47th notable image of Cometan sees the Founder of Astronism smiling from ear to ear on a moonlit night sky at the Birling Gap near Eastbourne, East Sussex. Featured in this image from Cometan's summer trip to the South Downs are twinkling stars, a beautiful cloud formation and the Seven Sisters cliffs stretching for as far as the eye can see in the background. This photo really does have it all; cliffs, coast, the sea, the beach, clouds, night sky and the stars.

 

© 2021 Millettarian Photographic Institute.

sometimes we feel like this

Thessaloniki (Greek: Θεσσαλονίκη, often referred to internationally as Thessalonica or Salonica, is the second-largest city in Greece and the capital of the Greek region of Macedonia, the administrative region of Central Macedonia and the Decentralized Administration of Macedonia and Thrace.[3][4] Its honorific title is Συμπρωτεύουσα (Symprotévousa), literally "co-capital",[5] and stands as a reference to its historical status as the Συμβασιλεύουσα (Symvasilévousa) or "co-reigning" city of the Eastern Roman (Byzantine) Empire, alongside Constantinople.[6]

 

According to the preliminary results of the 2011 census, the municipality of Thessaloniki today has a population of 322,240,[1] while the Thessaloniki Urban Area (the contiguous built up area forming the "City of Thessaloniki") has a population of 790,824.[1] Furthermore, the Thessaloniki Metropolitan Area extends over an area of 1,455.62 km2 (562.02 sq mi) and its population in 2011 reached a total of 1,104,460 inhabitants.[1]

 

Thessaloniki is Greece's second major economic, industrial, commercial and political centre, and a major transportation hub for the rest of southeastern Europe;[7] its commercial port is also of great importance for Greece and the southeastern European hinterland.[7] The city is renowned for its festivals, events and vibrant cultural life in general,[8] and is considered to be Greece's cultural capital.[8] Events such as the Thessaloniki International Trade Fair and the Thessaloniki International Film Festival are held annually, while the city also hosts the largest bi-annual meeting of the Greek diaspora.[9] Thessaloniki is the 2014 European Youth Capital.[10]

 

Founded in 315 BC by Cassander of Macedon, Thessaloniki's history spans some 2,300 years. An important metropolis by the Roman period, Thessaloniki was the second largest and wealthiest city of the Byzantine Empire. Thessaloniki is home to numerous notable Byzantine monuments, including the Paleochristian and Byzantine monuments of Thessaloniki, a UNESCO World Heritage Site, as well as several Roman, Ottoman and Sephardic Jewish structures. The city's main university, Aristotle University, is the largest in Greece and the Balkans.[11]

 

Thessaloniki is a popular tourist destination in Greece. In 2010, Lonely Planet ranked Thessaloniki as the world's fifth-best party city worldwide, comparable to other cities such as Dubai and Montreal.[12] For 2013 National Geographic Magazine included Thessaloniki in its top tourist destinations worldwide,[13] while in 2014 Financial Times FDI magazine (Foreign Direct Investments) declared Thessaloniki as the best mid-sized European city of the future for human capital and lifestyle.

  

Etymology

  

All variations of the city's name derive from the original (and current) appellation in Greek: Θεσσαλονίκη (from Θεσσαλός, Thessalos, and Νίκη, Nike), literally translating to "Thessalian Victory". The name of the city came from the name of a princess, Thessalonike of Macedon, half sister of Alexander the Great, so named because of her birth on the day of the Macedonian victory at the Battle of Crocus Field (353/352 BCE).[16]

 

The alternative name Salonica (or Salonika) derives from the variant form Σαλονίκη (Saloníki) in popular Greek speech, and has given rise to the form of the city's name in several languages. Names in other languages prominent in the city's history include Солѹнь (Solun) in Old Church Slavonic, סלוניקה (Salonika) in Ladino, Selanik (also Selânik) in Turkish (سلانیك in Ottoman Turkish), Solun (also written as Солун) in the local and neighboring South Slavic languages, Салоники (Saloníki) in Russian, and Sãrunã in Aromanian. In local speech, the city's name is typically pronounced with a dark and deep L characteristic of Macedonian Greek accent.[17][18]

 

The name often appears in writing in the abbreviated form Θεσ/νίκη

  

History

  

From antiquity to the Roman Empire

  

The city was founded around 315 BC by the King Cassander of Macedon, on or near the site of the ancient town of Therma and 26 other local villages.[20] He named it after his wife Thessalonike,[21] a half-sister of Alexander the Great and princess of Macedon as daughter of Philip II. Under the kingdom of Macedon the city retained its own autonomy and parliament[22] and evolved to become the most important city in Macedon.[21]

 

After the fall of the kingdom of Macedon in 168 BC, Thessalonica became a free city of the Roman Republic under Mark Antony in 41 BC.[21][23] It grew to be an important trade-hub located on the Via Egnatia,[24] the road connecting Dyrrhachium with Byzantium,[25] which facilitated trade between Thessaloniki and great centers of commerce such as Rome and Byzantium.[26] Thessaloniki also lay at the southern end of the main north-south route through the Balkans along the valleys of the Morava and Axios river valleys, thereby linking the Balkans with the rest of Greece.[27] The city later became the capital of one of the four Roman districts of Macedonia.[24] Later it became the capital of all the Greek provinces of the Roman Empire due to the city's importance in the Balkan peninsula. When the Roman Empire was divided into the tetrarchy, Thessaloniki became the administrative capital of one of the four portions of the Empire under Galerius Maximianus Caesar,[28][29] where Galerius commissioned an imperial palace, a new hippodrome, a triumphal arch and a mausoleum among others.[29][30][31]

 

In 379 when the Roman Prefecture of Illyricum was divided between the East and West Roman Empires, Thessaloniki became the capital of the new Prefecture of Illyricum.[24] In 390 Gothic troops under the Roman Emperor Theodosius I, led a massacre against the inhabitants of Thessalonica, who had risen in revolt against the Germanic soldiers. With the Fall of Rome in 476, Thessaloniki became the second-largest city of the Eastern Roman Empire.[26] Around the time of the Roman Empire Thessaloniki was also an important center for the spread of Christianity; some scholars hold that the First Epistle to the Thessalonians written by Paul the Apostle is the first written book of the New Testament.

  

Byzantine era and Middle Ages

  

From the first years of the Byzantine Empire, Thessaloniki was considered the second city in the Empire after Constantinople,[33][34][35] both in terms of wealth and size.[33] with an population of 150,000 in the mid 1100s.[36] The city held this status until it was transferred to Venice in 1423. In the 14th century the city's population exceeded 100,000 to 150,000,[37][38][39] making it larger than London at the time.[40]

 

During the 6th and 7th centuries the area around Thessaloniki was invaded by Avars and Slavs, who unsuccessfully laid siege to the city several times.[41] Traditional historiography stipulates that many Slavs settled in the hinterland of Thessaloniki,[42] however, this migration was allegedly on a much smaller scale than previously thought.[42][42][43] In the 9th century, the Byzantine Greek missionaries Cyril and Methodius, both natives of the city, created the first literary language of the Slavs, the Glagolic alphabet, most likely based on the Slavic dialect used in the hinterland of their hometown.[44][45][46][47][48]

 

An Arab naval attack in 904 resulted in the sack of the city.[49] The economic expansion of the city continued through the 12th century as the rule of the Komnenoi emperors expanded Byzantine control to the north. Thessaloniki passed out of Byzantine hands in 1204,[50] when Constantinople was captured by the forces of the Fourth Crusade and incorporated the city and its surrounding territories in the Kingdom of Thessalonica[51] — which then became the largest vassal of the Latin Empire. In 1224, the Kingdom of Thessalonica was overrun by the Despotate of Epirus, a remnant of the former Byzantine Empire, under Theodore Komnenos Doukas who crowned himself Emperor,[52] and the city became the Despotat's capital.[52][53] This era of the Despotate of Epirus is also known as the Empire of Thessalonica.[52][54][55] Following his defeat at Klokotnitsa however in 1230,[52][54] the Empire of Thessalonica became a vassal state of the Second Bulgarian Empire until it was recovered again in 1246, this time by the Nicaean Empire.[52] In 1342,[56] the city saw the rise of the Commune of the Zealots, an anti-aristocratic party formed of sailors and the poor,[57] which is nowadays described as social-revolutionary.[56] The city was practically independent of the rest of the Empire,[56][57][58] as it had its own government, a form of republic.[56] The zealot movement was overthrown in 1350 and the city was reunited with the rest of the Empire.[56]

 

In 1423, Despot Andronicus, who was in charge of the city, ceded it to the Republic of Venice with the hope that it could be protected from the Ottomans who were besieging the city (there is no evidence to support the oft-repeated story that he sold the city to them). The Venetians held Thessaloniki until it was captured by the Ottoman Sultan Murad II on 29 March 1430.

  

Ottoman period

  

When Sultan Murad II captured Thessaloniki and sacked it in 1430, contemporary reports estimated that about one-fifth of the city's population was enslaved.[60] Upon the conquest of Thessaloniki, some of its inhabitants escaped,[61] including intellectuals such as Theodorus Gaza "Thessalonicensis" and Andronicus Callistus.[62] However, the change of sovereignty from the Byzantine Empire to the Ottoman one did not affect the city's prestige as a major imperial city and trading hub.[63][64] Thessaloniki and Smyrna, although smaller in size than Constantinople, were the Ottoman Empire's most important trading hubs.[63] Thessaloniki's importance was mostly in the field of shipping,[63] but also in manufacturing,[64] while most of the city's trade was controlled by ethnic Greeks.[63]

 

During the Ottoman period, the city's population of mainly Greek Jews and Ottoman Muslims (including those of Turkish and Albanian, as well as Bulgarian Muslim and Greek Muslim convert origin) grew substantially. By 1478 Selânik (سلانیك), as the city came to be known in Ottoman Turkish, had a population of 4,320 Muslims, 6,094 Greek Orthodox and some Catholics, but no Jews. Soon after the turn of the 15th to 16th century, nearly 20,000 Sephardic Jews had immigrated to Greece from Spain following their expulsion by the 1492 Alhambra Decree.[65] By c. 1500, the numbers had grown to 7,986 Greeks, 8,575 Muslims, and 3,770 Jews. By 1519, Sephardic Jews numbered 15,715, 54% of the city's population. Some historians consider the Ottoman regime's invitation to Jewish settlement was a strategy to prevent the ethnic Greek population (Eastern Orthodox Christians) from dominating the city.[38]

 

Thessaloniki was the capital of the Sanjak of Selanik within the wider Rumeli Eyalet (Balkans)[66] until 1826, and subsequently the capital of Selanik Eyalet (after 1867, the Selanik Vilayet).[67][68] This consisted of the sanjaks of Selanik, Serres and Drama between 1826 and 1912.[69] Thessaloniki was also a Janissary stronghold where novice Janissaries were trained. In June 1826, regular Ottoman soldiers attacked and destroyed the Janissary base in Thessaloniki while also killing over 10,000 Janissaries, an event known as The Auspicious Incident in Ottoman history.[70] From 1870, driven by economic growth, the city's population expanded by 70%, reaching 135,000 in 1917.[71]

 

The last few decades of Ottoman control over the city were an era of revival, particularly in terms of the city's infrastructure. It was at that time that the Ottoman administration of the city acquired an "official" face with the creation of the Command Post[72] while a number of new public buildings were built in the eclectic style in order to project the European face both of Thessaloniki and the Ottoman Empire.[72][73] The city walls were torn down between 1869 and 1889,[74] efforts for a planned expansion of the city are evident as early as 1879,[75] the first tram service started in 1888[76] and the city streets were illuminated with electric lamp posts in 1908.[77] In 1888 Thessaloniki was connected to Central Europe via rail through Belgrade, Monastir in 1893 and Constantinople in 1896.

  

Since the 20th century

  

In the early 20th century, Thessaloniki was in the center of radical activities by various groups; the Bulgarian Internal Macedonian Revolutionary Organization, founded in 1897,[78] and the Greek Macedonian Committee, founded in 1903.[79] In 1903 an anarchist group known as the Boatmen of Thessaloniki planted bombs in several buildings in Thessaloniki, including the Ottoman Bank, with some assistance from the IMRO. The Greek consulate in Ottoman Thessaloniki (now the Museum of the Macedonian Struggle) served as the center of operations for the Greek guerillas. In 1908 the Young Turks movement broke out in the city, sparking the Young Turk Revolution.[80]

The Ottoman Feth-i Bülend being sunk in Thessaloniki in 1912 by a Greek ship during the First Balkan War.

Constantine I of Greece with George I of Greece and the Greek army enter the city.

 

As the First Balkan War broke out, Greece declared war on the Ottoman Empire and expanded its borders. When Eleftherios Venizelos, Prime Minister at the time, was asked if the Greek army should move towards Thessaloniki or Monastir (now Bitola, Republic of Macedonia), Venizelos replied "Salonique à tout prix!" (Thessaloniki, at all costs!).[81] As both Greece and Bulgaria wanted Thessaloniki, the Ottoman garrison of the city entered negotiations with both armies.[82] On 8 November 1912 (26 October Old Style), the feast day of the city's patron saint, Saint Demetrius, the Greek Army accepted the surrender of the Ottoman garrison at Thessaloniki.[83] The Bulgarian army arrived one day after the surrender of the city to Greece and Tahsin Pasha, ruler of the city, told the Bulgarian officials that "I have only one Thessaloniki, which I have surrendered".[82] After the Second Balkan War, Thessaloniki and the rest of the Greek portion of Macedonia were officially annexed to Greece by the Treaty of Bucharest in 1913.[84] On 18 March 1913 George I of Greece was assassinated in the city by Alexandros Schinas.[85]

 

In 1915, during World War I, a large Allied expeditionary force established a base at Thessaloniki for operations against pro-German Bulgaria.[86] This culminated in the establishment of the Macedonian Front, also known as the Salonika Front.[87][88] In 1916, pro-Venizelist Greek army officers and civilians, with the support of the Allies, launched an uprising,[89] creating a pro-Allied[90] temporary government by the name of the "Provisional Government of National Defence"[89][91] that controlled the "New Lands" (lands that were gained by Greece in the Balkan Wars, most of Northern Greece including Greek Macedonia, the North Aegean as well as the island of Crete);[89][91] the official government of the King in Athens, the "State of Athens",[89] controlled "Old Greece"[89][91] which were traditionally monarchist. The State of Thessaloniki was disestablished with the unification of the two opposing Greek governments under Venizelos, following the abdication of King Constantine in 1917.[86][91]

The 1st Battalion of the National Defence army marches on its way to the front.

Aerial picture of the Great Fire of 1917.

 

Most of the old center of the city was destroyed by the Great Thessaloniki Fire of 1917, which started accidentally by an unattended kitchen fire on 18 August 1917.[92] The fire swept through the centre of the city, leaving 72,000 people homeless; according to the Pallis Report, most of them were Jewish (50,000). Many businesses were destroyed, as a result, 70% of the population were unemployed.[92] Also a number of religious structures of the three major faiths were lost. Nearly one-quarter of the total population of approximately 271,157 became homeless.[92] Following the fire the government prohibited quick rebuilding, so it could implement the new redesign of the city according to the European-style urban plan[6] prepared by a group of architects, including the Briton Thomas Mawson, and headed by French architect Ernest Hébrard.[92] Property values fell from 6.5 million Greek drachmas to 750,000.[93]

 

After the defeat of Greece in the Greco-Turkish War and during the break-up of the Ottoman Empire, a population exchange took place between Greece and Turkey.[90] Over 160,000 ethnic Greeks deported from the former Ottoman Empire were resettled in the city,[90] changing its demographics. Additionally many of the city's Muslims were deported to Turkey, ranging at about 20,000 people.[94]

 

During World War II Thessaloniki was heavily bombarded by Fascist Italy (with 232 people dead, 871 wounded and over 800 buildings damaged or destroyed in November 1940 alone),[95] and, the Italians having failed to succeed in their invasion of Greece, it fell to the forces of Nazi Germany on 8 April 1941[96] and remained under German occupation until 30 October 1944 when it was liberated by the Greek People's Liberation Army.[97] The Nazis soon forced the Jewish residents into a ghetto near the railroads and on 15 March 1943 began the deportation process of the city's 56,000 Jews to its concentration camps.[98][99] They deported over 43,000 of the city's Jews in concentration camps,[98] where most were killed in the gas chambers. The Germans also deported 11,000 Jews to forced labor camps, where most perished.[100] Only 1,200 Jews live in the city today.

Part of Eleftherias Square during the Axis occupation.

 

The importance of Thessaloniki to Nazi Germany can be demonstrated by the fact that, initially, Hitler had planned to incorporate it directly in the Third Reich[101] (that is, make it part of Germany) and not have it controlled by a puppet state such as the Hellenic State or an ally of Germany (Thessaloniki had been promised to Yugoslavia as a reward for joining the Axis on 25 March 1941).[102] Having been the first major city in Greece to fall to the occupying forces just two days after the German invasion, it was in Thessaloniki that the first Greek resistance group was formed (under the name «Ελευθερία», Eleftheria, "Freedom")[103] as well as the first anti-Nazi newspaper in an occupied territory anywhere in Europe,[104] also by the name Eleftheria. Thessaloniki was also home to a military camp-converted-concentration camp, known in German as "Konzentrationslager Pavlo Mela" (Pavlos Melas Concentration Camp),[105] where members of the resistance and other non-favourable people towards the German occupation from all over Greece[105] were held either to be killed or sent to concentration camps elsewhere in Europe.[105] In the 1946 monarchy referendum, the majority of the locals voted in favour of a republic, contrary to the rest of Greece.[106]

 

After the war, Thessaloniki was rebuilt with large-scale development of new infrastructure and industry throughout the 1950s, 1960s and 1970s. Many of its architectural treasures still remain, adding value to the city as a tourist destination, while several early Christian and Byzantine monuments of Thessaloniki were added to the UNESCO World Heritage list in 1988.[107] In 1997, Thessaloniki was celebrated as the European Capital of Culture,[108] sponsoring events across the city and the region. Agency established to oversee the cultural activities of that year 1997 was still in existence by 2010.[109] In 2004 the city hosted a number of the football events as part of the 2004 Summer Olympics.[110]

 

Today Thessaloniki has become one of the most important trade and business hubs in Southeastern Europe, with its port, the Port of Thessaloniki being one of the largest in the Aegean and facilitating trade throughout the Balkan hinterland.[7] On 26 October 2012 the city celebrated its centennial since its incorporation into Greece.[111] The city also forms one of the largest student centres in Southeastern Europe, is host to the largest student population in Greece and will be the European Youth Capital in 2014

  

Geography

  

Geology

  

Thessaloniki lies on the northern fringe of the Thermaic Gulf on its eastern coast and is bound by Mount Chortiatis on its southeast. Its proximity to imposing mountain ranges, hills and fault lines, especially towards its southeast have historically made the city prone to geological changes.

 

Since medieval times, Thessaloniki was hit by strong earthquakes, notably in 1759, 1902, 1978 and 1995.[113] On 19–20 June 1978, the city suffered a series of powerful earthquakes, registering 5.5 and 6.5 on the Richter scale.[114][115] The tremors caused considerable damage to a number of buildings and ancient monuments,[114] but the city withstood the catastrophe without any major problems.[115] One apartment building in central Thessaloniki collapsed during the second earthquake, killing many, raising the final death toll to 51.[114][115]

Climate

  

Thessaloniki's climate is directly affected by the sea it is situated on.[116] The city lies in a transitional climatic zone, so its climate displays characteristics of several climates. According to the Köppen climate classification, it is a humid subtropical climate (Cfa) that borders on a semi-arid climate (BSk), with annual average precipitation of 450 millimetres (18 in) due to the Pindus rain shadow drying the westerly winds. However, the city has a summer precipitation between 20 to 30 millimetres (0.79 to 1.18 in), which borders it close to a hot-summer Mediterranean climate (Csa).

 

Winters are relatively dry, with common morning frost. Snowfalls are sporadic, but οccur more or less every winter, but the snow cover does not last for more than a few days. Fog is common, with an average of 193 foggy days in a year.[117] During the coldest winters, temperatures can drop to −10 °C (14 °F).[117] The record minimum temperature in Thessaloniki was −14 °C (7 °F).[118] On average, Thessaloniki experiences frost (sub-zero temperature) 32 days a year.[117] The coldest month of the year in the city is January, with an average 24-hour temperature of 6 °C (43 °F).[119] Wind is also usual in the winter months, with December and January having an average wind speed of 26 km/h (16 mph).[117]

 

Thessaloniki's summers are hot with rather humid nights.[117] Maximum temperatures usually rise above 30 °C (86 °F),[117] but rarely go over 40 °C (104 °F);[117] the average number of days the temperature is above 32 °C (90 °F) is 32.[117] The maximum recorded temperature in the city was 42 °C (108 °F).[117][118] Rain seldom falls in summer, mainly during thunderstorms. In the summer months Thessaloniki also experiences strong heat waves.[120] The hottest month of the year in the city is July, with an average 24-hour temperature of 26 °C (79 °F).[119] The average wind speed for June and July in Thessaloniki is 20 kilometres per hour (12 mph)

  

Government

  

According to the Kallikratis reform, as of 1 January 2011 the Thessaloniki Urban Area (Greek: Πολεοδομικό Συγκρότημα Θεσσαλονίκης) which makes up the "City of Thessaloniki", is made up of six self-governing municipalities (Greek: Δήμοι) and one municipal unit (Greek: Δημοτική ενότητα). The municipalities that are included in the Thessaloniki Urban Area are those of Thessaloniki (the city center and largest in population size), Kalamaria, Neapoli-Sykies, Pavlos Melas, Kordelio-Evosmos, Ampelokipoi-Menemeni, and the municipal unit of Pylaia, part of the municipality of Pylaia-Chortiatis. Prior to the Kallikratis reform, the Thessaloniki Urban Area was made up of twice as many municipalities, considerably smaller in size, which created bureaucratic problems.[123]

  

Thessaloniki Municipality

  

The municipality of Thessaloniki (Greek: Δήμος Θεσαλονίκης) is the second most populous in Greece, after Athens, with a population of 322,240[1] people (in 2011) and an area of 17.832 km2 (7 sq mi). The municipality forms the core of the Thessaloniki Urban Area, with its central district (the city center), referred to as the Kentro, meaning 'center' or 'downtown'.

 

The institution of mayor of Thessaloniki was inaugurated under the Ottoman Empire, in 1912. The first mayor of Thessaloniki was Osman Sait Bey, while the current mayor of the municipality of Thessaloniki is Yiannis Boutaris. In 2011, the municipality of Thessaloniki had a budget of €464.33 million[124] while the budget of 2012 stands at €409.00 million.[125]

 

According to an article in The New York Times, the way in which the present mayor of Thessaloniki is treating the city's debt and oversized administration problems could be used as an example by Greece's central government for a successful strategy in dealing with these problems.[126]

  

Other

  

Thessaloniki is the second largest city in Greece. It is an influential city for the northern parts of the country and is the capital of the region of Central Macedonia and the Thessaloniki regional unit. The Ministry of Macedonia and Thrace is also based in Thessaloniki, being that the city is the de facto capital of the Greek region of Macedonia.

 

It is customary every year for the Prime Minister of Greece to announce his administration's policies on a number of issues, such as the economy, at the opening night of the Thessaloniki International Trade Fair. In 2010, during the first months of the 2010 Greek debt crisis, the entire cabinet of Greece met in Thessaloniki to discuss the country's future.[127]

 

In the Hellenic Parliament, the Thessaloniki urban area constitutes a 16-seat constituency. As of the national elections of 17 June 2012 the largest party in Thessaloniki is New Democracy with 27.8%, followed by the Coalition of the Radical Left (27.0%) and the Panhellenic Socialist Movement (10.2%).[128] The table below summarizes the results of the latest elections.

  

Cityscape

  

Architecture

  

Architecture in Thessaloniki is the direct result of the city's position at the centre of all historical developments in the Balkans. Aside from its commercial importance, Thessaloniki was also for many centuries the military and administrative hub of the region, and beyond this the transportation link between Europe and the Levant (Syria, Lebanon, Jordan, and Israel / Palestine). Merchants, traders and refugees from all over Europe settled in the city. The need for commercial and public buildings in this new era of prosperity led to the construction of large edifices in the city center. During this time, the city saw the building of banks, large hotels, theatres, warehouses, and factories. Architects who designed some of the most notable buildings of the city, in the late 19th and early 20th century, include Vitaliano Poselli, Pietro Arrigoni, Xenophon Paionidis, Eli Modiano, Moshé Jacques, Jean Joseph Pleyber, Frederic Charnot, Ernst Ziller, Roubens Max, Levi Ernst, Angelos Siagas and others, using mainly the styles of Eclecticism and Art Nouveau.

 

The city layout changed after 1870, when the seaside fortifications gave way to extensive piers, and many of the oldest walls of the city were demolished, including those surrounding the White Tower, which today stands as the main landmark of the city. As parts of the early Byzantine walls were demolished, this allowed the city to expand east and west along the coast.[129]

 

The expansion of Eleftherias Square towards the sea completed the new commercial hub of the city and at the time was considered one of the most vibrant squares of the city. As the city grew, workers moved to the western districts, due to their proximity to factories and industrial activities; while the middle and upper classes gradually moved from the city-center to the eastern suburbs, leaving mainly businesses. In 1917, a devastating fire swept through the city and burned uncontrollably for 32 hours.[71] It destroyed the city's historic center and a large part of its architectural heritage, but paved the way for modern development and allowed Thessaloniki the development of a proper European city center, featuring wider diagonal avenues and monumental squares; which the city initially lacked – much of what was considered to be 'essential' in European architecture.

  

City Center

  

After the Great Thessaloniki Fire of 1917, a team of architects and urban planners including Thomas Mawson and Ernest Hebrard, a French architect, chose the Byzantine era as the basis of their (re)building designs for Thessaloniki's city center. The new city plan included axes, diagonal streets and monumental squares, with a street grid that would channel traffic smoothly. The plan of 1917 included provisions for future population expansions and a street and road network that would be, and still is sufficient today.[71] It contained sites for public buildings and provided for the restoration of Byzantine churches and Ottoman mosques.

The Metropolitan Church of Saint Gregory Palamas, designed by Ernst Ziller.

 

Today the city center of Thessaloniki includes the features designed as part of the plan and forms the point in the city where most of the public buildings, historical sites, entertainment venues and stores are located. The center is characterized by its many historical buildings, arcades, laneways and distinct architectural styles such as Art Nouveau and Art Deco, which can be seen on many of its buildings.

 

Also called the historic center, it is divided into several districts, of which include Ladadika (where many entertainment venues and tavernas are located), Kapani (were the city's central city market is located), Diagonios, Navarinou, Rotonta, Agia Sofia and Ippodromio (white tower), which are all located around Thessaloniki's most central point, Aristotelous Square.

 

The west point of the city center is home to Thessaloniki's law courts, its central international railway station and the port, while on its eastern side stands the city's two universities, the Thessaloniki International Exhibition Center, the city's main stadium, its archaeological and Byzantine museums, the new city hall and its central parklands and gardens, namely those of the ΧΑΝΘ/Palios Zoologikos Kipos and Pedio tou Areos. The central road arteries that pass through the city center, designed in the Ernest Hebrard plan, include those of Tsimiski, Egnatia, Nikis, Mitropoleos, Venizelou and St. Demetrius avenues.

  

Ano Poli

  

Ano Poli (also called Old Town and literally the Upper Town) is the heritage listed district north of Thessaloniki's city center that was not engulfed by the great fire of 1917 and was declared a UNESCO World Heritage Site by ministerial actions of Melina Merkouri, during the 1980s. It consists of Thessaloniki's most traditional part of the city, still featuring small stone paved streets, old squares and homes featuring old Greek and Ottoman architecture.

 

Ano Poli also, is the highest point in Thessaloniki and as such, is the location of the city's acropolis, its Byzantine fort, the Heptapyrgion, a large portion of the city's remaining walls, and with many of its additional Ottoman and Byzantine structures still standing. The area provides access to the Seich Sou Forest National Park[131] and features amphitheatric views of the whole city and the Thermaic Gulf. On clear days Mount Olympus, at about 100 km (62 mi) away across the gulf, can also be seen towering the horizon.

  

Southeastern Thessaloniki up until the 1920s was home to the city's most affluent residents and formed the outermost suburbs of the city at the time, with the area close to the Thermaic Gulf coast called Exoches, from the 19th century holiday villas which defined the area. Today southeastern Thessaloniki has in some way become a natural extension of the city center, with the avenues of Megalou Alexandrou, Georgiou Papandreou (Antheon), Vasilissis Olgas Avenue, Delfon, Konstantinou Karamanli (Nea Egnatia) and Papanastasiou passing through it, enclosing an area traditionally called Dépôt (Ντεπώ), from the name of the old tram station, owned by a French company. The area extends to Kalamaria and Pylaia, about 9 km (5.59 mi) from the White Tower in the city centre.

 

Some of the most notable mansions and villas of the old-era of the city remain along Vasilissis Olgas Avenue. Built for the most wealthy residents and designed by well known architects they are used today as museums, art galleries or remain as private properties. Some of them include Villa Bianca, Villa Ahmet Kapanci, Villa Modiano, Villa Mordoch, Villa Mehmet Kapanci, Hatzilazarou Mansion, Chateau Mon Bonheur (often called red tower) and others.

 

Most of southeastern Thessaloniki is characterized by its modern architecture and apartment buildings, home to the middle-class and more than half of the municipality of Thessaloniki population. Today this area of the city is also home to 3 of the city's main football stadiums, the Thessaloniki Concert Hall, the Posidonio aquatic and athletic complex, the Naval Command post of Northern Greece and the old royal palace (called Palataki), located on the most westerly point of Karabournaki cape. The municipality of Kalamaria is also located in southeastern Thessaloniki and has become this part of the city's most sought after areas, with many open spaces and home to high end bars, cafés and entertainment venues, most notably on Plastira street, along the coast

 

Northwestern Thessaloniki had always been associated with industry and the working class because as the city grew during the 1920s, many workers had moved there, due to its proximity near factories and industrial activities. Today many factories and industries have been moved further out west and the area is experiencing rapid growth as does the southeast. Many factories in this area have been converted to cultural centres, while past military grounds that are being surrounded by densely built neighborhoods are awaiting transformation into parklands.

 

Northwest Thessaloniki forms the main entry point into the city of Thessaloniki with the avenues of Monastiriou, Lagkada and 26is Octovriou passing through it, as well as the extension of the A1 motorway, feeding into Thessaloniki's city center. The area is home to the Macedonia InterCity Bus Terminal (KTEL), the Zeitenlik Allied memorial military cemetery and to large entertainment venues of the city, such as Milos, Fix, Vilka (which are housed in converted old factories). Northwestern Thessaloniki is also home to Moni Lazariston, located in Stavroupoli, which today forms one of the most important cultural centers for the city.

 

To read more please click :-

 

en.wikipedia.org/wiki/Thessaloniki

Leica M6 / Summarit-M 35mm f2.5 / Kodak Portra 400

 

Welbeck Street car park is an architecturally notable car park built in the Brutalist style and is found in Marylebone, just north of Oxford Street, in the City of Westminster, London.

 

The car park, designed by Michael Blampied and Partners, was completed in 1970 for the use of the nearby Debenhams store using a design of tessellated concrete polygons. It was sold in 2016 to Shiva Hotels and is due to be demolished in March 2019 after Historic England decided not to register it as a listed building

 

London, UK

Every notable town or city has its 'must see' facilities. One such is the famous Observatory Museum in Grahamstown, which houses the only Camera Obscura in the southern hemisphere, along with many other scientific and technological exhibits. www.safarinow.com/destinations/grahamstown/galleriesandmu..

Source: en.wikipedia.org/wiki/Kansas_City,_Missouri

 

Kansas City (abbreviated KC or KCMO) is the largest city in Missouri by population and area. As of the 2020 census, the city had a population of 508,090 in 2020, making it the 36th most-populous city in the United States. It is the most populated municipality and historic core city of the Kansas City metropolitan area, which straddles the Kansas–Missouri state line and has a population of 2,392,035. Most of the city lies within Jackson County, with portions spilling into Clay, Cass, and Platte counties. Kansas City was founded in the 1830s as a port on the Missouri River at its confluence with the Kansas River coming in from the west. On June 1, 1850, the town of Kansas was incorporated; shortly after came the establishment of the Kansas Territory. Confusion between the two ensued, and the name Kansas City was assigned to distinguish them soon after.

 

Sitting on Missouri's western boundary with Kansas, with Downtown near the confluence of the Kansas and Missouri Rivers, the city encompasses about 319.03 square miles (826.3 km2), making it the 23rd largest city by total area in the United States. It serves as one of the two county seats of Jackson County, along with the major suburb of Independence. Other major suburbs include the Missouri cities of Blue Springs and Lee's Summit and the Kansas cities of Overland Park, Olathe, Lenexa, and Kansas City, Kansas.

 

The city is composed of several neighborhoods, including the River Market District in the north, the 18th and Vine District in the east, and the Country Club Plaza in the south. Celebrated cultural traditions include Kansas City jazz, theater, which was the center of the Vaudevillian Orpheum circuit in the 1920s, the Chiefs and Royals sports franchises, and famous cuisine based on Kansas City-style barbecue, Kansas City strip steak, and craft breweries.

 

Source: en.wikipedia.org/wiki/Kauffman_Center_for_the_Performing_...

 

The Kauffman Center for the Performing Arts is a performing arts center in downtown Kansas City, Missouri, USA, at 16th and Broadway, near the Power & Light District, the T-Mobile Center and the Crossroads Arts District. Its construction was a major part of the ongoing redevelopment of downtown Kansas City.

 

The Center was created as a 501(c)(3) non-profit organization. Unlike some other major civic construction projects, no taxpayer funds went into its construction. The City of Kansas City contributed to and operates a parking garage adjacent to the Kauffman Center.

 

It is the performance home to the Kansas City Symphony, the Lyric Opera of Kansas City, and the Kansas City Ballet which in the past performed at the Lyric Theatre, eight blocks north of the center. The Kauffman Center houses two unique performance venues: Muriel Kauffman Theatre and Helzberg Hall.

 

According to its website, the Kauffman Center's mission is "to enrich the lives of communities throughout the region, country and world by offering extraordinary and diverse performing arts experiences". Not only do notable performances take place almost weekly, but the Center is a place where the KC community comes together and celebrates the city's rich arts culture. The Kauffman Center seeks to fulfill this mission by offering a wide selection of performances, and also by offering specific programs to connect with the youth in the Kansas City area.

A notable capture during a fleeting visit to Singapore in October 1992 was this prototype Alexander-bodied Mercedes-Benz 0305, the forerunner of a large fleet to operate in the City state, all of which had their bodywork assembled locally. SBS 5541Z, seen here on North Bridge Road, was, I believe, shipped from the UK as a complete vehicle.

 

This image is copyright and must not be reproduced or downloaded without the permission of the photographer.

  

Chiesa Hallgrímskirkja

L'interno è estremamente semplice e spoglio.

L'unica particolarità notevole è un organo a 5275 canne.

 

Hallgrímskirkja Church

The interior is extremely simple and bare.

The only notable peculiarity is a 5275 pipe organ.

 

IMG_4616m

A famous notable person of North Brookfield was George Michael Cohan (July 3, 1878 – November 5, 1942) an American entertainer, playwright, composer, lyricist, actor, singer, dancer and theatrical producer. (James Cagney played Cohan in the 1942 biopic Yankee Doodle Dandy receiving the Academy Award for Best Actor for his performance.)

 

As a child, George M. Cohan and his family toured most of the year and spent summer vacations from the vaudeville circuit at his grandmother's home in North Brookfield, Massachusetts, where Cohan befriended baseball player Connie Mack. The family generally gave a performance at the town hall there each summer, and Cohan had a chance to gain some more normal childhood experiences, like riding his bike and playing sandlot baseball.

 

Cohan's memories of those happy summers inspired his 1907 musical 50 Miles from Boston, which is set in North Brookfield and contains one of his most famous songs, "Harrigan". As Cohan matured through his teens, he used the quiet summers there to write. When he returned to the town in the cast of Ah, Wilderness! in 1934, he told a reporter "I've knocked around everywhere, but there's no place like North Brookfield."

This photo won a 'Notable' award this week in 'Bird Guides', which is tough to get, as the best bird photographers in the UK post there. :)

 

Taken at RSPB Greylake in Somerset, UK.

 

My nature blog;

carlbovisnaturephotography.blogspot.co.uk/2016/11/water-r...

Sanssouci, Postdam, Brandenburg, Deutschland.

 

Sanssouci (del francés sans souci= «sin preocupaciones»​) es el nombre de un conjunto de edificios y jardines que incluyen el antiguo palacio de verano oficial de Federico II el Grande, rey de Prusia, en Potsdam, cerca de Berlín. Se trata de una de las obras cumbres del estilo Rococó, y es también notable por los numerosos templetes y pabellones diseminados por el parque que rodea el conjunto.

 

El Palacio de Sanssouci combina la arquitectura del siglo XVIII con una arquitectura paisajística.​ Bajo la dirección de Georg Wenzeslaus von Knobelsdorff, se edificó entre de 1745 y 1747 un palacete de una sola planta del estilo de un “maison de plaisance” según las indicaciones del rey.​ El edificio comprende dos alas laterales que ocupa casi toda la parte superior de la terraza. Las alas del palacio cuentan con filas de árboles en su lado norte y terminan en sendas glorietas enrejadas, decoradas con adornos dorados.

 

Bajo su cúpula se encuentra el Salón de Mármol oval en el que pudo celebrarse la legendaria tertulia organizada por el soberano prusiano, deseoso de compartir sus inquietudes musicales y filosóficas con invitados como Voltaire. La decoración interior es, en su mayor parte, originaria desde el siglo XVIII.

 

Federico II residió en el Palacio habitualmente.​ Sin embargo, después de su muerte en 1786, este se mantuvo vacío y descuidado hasta mediados del siglo XIX.

 

Sanssouci (from the French sans souci = "carefree") is the name of a group of buildings and gardens that include the former official summer palace of Frederick II the Great, King of Prussia, in Potsdam, near Berlin. It is one of the top works of the Rococo style, and it is also notable for the many pavilions and pavilions scattered throughout the park that surrounds the complex.

 

Sanssouci Palace combines 18th century architecture with landscape architecture Under the direction of Georg Wenzeslaus von Knobelsdorff, between 1745 and 1747 a one-storey mansion in the style of a “maison de plaisance” was built according to the indications The building comprises two lateral wings that occupy almost the entire upper part of the terrace. The wings of the palace have rows of trees on their north side and end in gazebos gated, decorated with gold ornaments.

 

Under its dome is the oval Marble Hall where the legendary gathering organized by the Prussian sovereign, eager to share his musical and philosophical concerns with guests like Voltaire, could be held. The interior decoration is, for the most part, original from the 18th century.

 

Frederick II regularly resided in the Palace, however after his death in 1786 it remained empty and neglected until the mid-19th century.

The most notable change on the 7th was to London's 4th busiest bus route, the 140. Initially I was cautious of the idea of splicing up such a integral service however I was pleasantly surprised, the 10 or so VWHs already have USBS for the X140 and branding is on the way, the drivers were very vocal explaining what the route was over the intercom. The best bit about this route however... It is quick and only after getting off an X140 and onto a 140 I realised just how sodding slow they are. Could certainly do with more of these expresses. X36 springs to mind as something that would be well used.

El Mosteiro dos Jerónimos és un monestir manuelí, testimoni de la riquesa del descobriment portuguès. Es troba al barri de Belém, Lisboa, a l'entrada del riu Tejo. És el punt més àlgid de l'estil manuelí i el conjunt monàstic més notable del segle XVI a Portugal i una de les principals esglésies saló d'Europa.

 

En destaca el seu claustre, completat el 1544, i la porta sud d'un complex disseny geomètric, davant del riu Tejo. Els elements decoratius són plens de símbols de l'art de la navegació i les escultures de plantes i animals exòtics. El monument és considerat Patrimoni de la Humanitat per la UNESCO i 7 de juliol del 2007, va ser escollit com una de les set meravelles de Portugal.

 

Encarregat pel rei Manuel I de Portugal, poc després que Vasco da Gama hagués tornat del viatge a l'Índia, fou finançat en gran part pels beneficis del comerç d'espècies. Escollí la ubicació al costat del riu a Santa Maria de Belém el 1502 i començà a treballar amb diversos arquitectes i constructors, entre ells Diogo de Boitaca (el pla original i l'aplicació) i João de Castilho (cúpules de la nau i el transsepte - amb una xarxa de venes en forma d'estrella - pilars, porta sud, sagristia i façana), que substitueix la primera el 1516/17. En el regnat de Don Joan III s'hi va afegir el cor.

 

El seu nom ve del fet que fou lliurat a l'orde de Sant Jeroni, que s'hi va establir fins al 1834. Sobrevisqué al terratrèmol del 1755, però va ser malmès per les tropes franceses enviades per Napoleó Bonaparte a principis del segle XIX.

 

Inclou, entre d'altres, les tombes dels reis Manuel I de Portugal i la seva esposa, Maria d'Aragó i de Castella, Joan III de Portugal i la seva dona, Caterina d'Habsburg, Sebastià I de Portugal i Enric I de Portugal, i també les de Vasco da Gama de Luís Vaz de Camões, d'Alexandre Herculano i Fernando Pessoa.

 

Després del 1834, amb l'expulsió dels ordes religiosos, el monestir dels Jerònims va ser donat a l'església parroquial de Santa Maria de Belém.

 

En una extensió construïda el 1850 es troba el Museu Arqueològic Nacional i el Museu Marítim es troba a l'ala oest.

 

Fou seu, el 1983, de la XVII Exposició europea d'Art, de la Ciència i la Cultura.

 

Pàgina a la UNESCO World Heritage List.

 

Aquesta imatge ha jugat a A place from Flickr.

 

A Google Maps.

Notable, this shoot, because I got to shoot with my buddy, Ian, who I'd not seen in far too long, as he'd taken it upon himself to move far far far away (nashville), considering not at all my feelings in the matter.

 

So it was nice, we used to shoot together regularly, always a blast seeing what he comes up with, often hanging out on the periphery while I shoot, zipping in and out, ending up with all kinds of awesome.

 

Like this: ianbroyles.tumblr.com/post/38011151044/lou

 

It's not even that we were shooting together, or that we were sharing ideas, it was just an atmosphere created by having a good friend along for the ride, sharing in the conversation with Brittany, it's a different energy, a fuller dynamic.

Bupaya Pagoda is a notable pagoda located in Bagan (formerly Pagan), in Myanmar, at a bend on the right bank of the Ayeyarwady River. The small pagoda, which has a bulbous shaped dome, is widely believed to have been built by the third King of Pagan, Pyusawhti who ruled from 168 to 243 AD. It is one of the most notable shrines among the thousands of new or ruined Pagodas in Pagan, which is located about 90 miles (140 km) south of Mandalay.

 

Many celestial objects are beautiful – swirling spiral galaxies or glittering clusters of stars are notable examples. But some of the most striking scenes are created during the death throes of intermediate-mass stars, when great clouds of superheated gas are expelled into space. These dying breaths form planetary nebulas like NGC 6302, captured here in this image from the NASA/ESA Hubble Space Telescope.

 

Known perhaps more appropriately as the Bug or Butterfly Nebula, this complex nebula lies roughly 3800 light-years away from us within the Milky Way. It was formed when a star around five times the mass of our Sun became a red giant, ejected its outer layers, and became intensely hot. Its distinctive shape classifies it as a bipolar nebula, where fast-moving gas can escape more easily from the poles of the dying star than from around its equator. This creates a lobed structure reminiscent of an hourglass or, as in this case, a giant cosmic butterfly.

 

While this image is beautiful in its own right, the mix of colours actually tells us a lot about physical conditions within the nebula.

 

The red edges of the butterfly wings represent areas that emit light from the element nitrogen, due to the relatively low temperatures there. Conversely the white splashes closer to the nebula's centre pinpoint light emitted by the element sulphur, marking regions of higher temperature and colliding gases closer to the central star.

 

This hot gas was expelled from the star and collided with slower-moving gas in its path, creating rippling shock waves through the nebula. An example of such a shock wave can be seen in the well-defined white blob towards the top right of the image.

 

Other colours identify emission from oxygen, helium and hydrogen gases. The observations making up this composite image were taken in optical and ultraviolet light on 27 July 2009, using Hubble's Wide Field Camera 3. The Principal Investigators for the observing programme are K. Noll , H. Bond and B. Balick.

 

This image was originally released in September 2009 on the NASA Hubblesite.

 

Credit: NASA/ESA/Hubble SM4 ERO Team

Schweiz / Berner Oberland - Eiger, Mönch und Jungfrau

 

seen on the way from Allmendhubel to Grütschalp

 

gesehen auf dem Weg vom Allmendhubel zur Grütschalp

 

The Eiger (German pronunciation: [ˈaɪ̯ɡɐ]) is a 3,967-metre (13,015 ft) mountain of the Bernese Alps, overlooking Grindelwald and Lauterbrunnen in the Bernese Oberland of Switzerland, just north of the main watershed and border with Valais. It is the easternmost peak of a ridge crest that extends across the Mönch to the Jungfrau at 4,158 m (13,642 ft), constituting one of the most emblematic sights of the Swiss Alps. While the northern side of the mountain rises more than 3,000 m (10,000 ft) above the two valleys of Grindelwald and Lauterbrunnen, the southern side faces the large glaciers of the Jungfrau-Aletsch area, the most glaciated region in the Alps. The most notable feature of the Eiger is its nearly 1,800-metre-high (5,900 ft) north face of rock and ice, named Eiger-Nordwand, Eigerwand or just Nordwand, which is the biggest north face in the Alps.] This huge face towers over the resort of Kleine Scheidegg at its base, on the eponymous pass connecting the two valleys.

 

The first ascent of the Eiger was made by Swiss guides Christian Almer and Peter Bohren and Irishman Charles Barrington, who climbed the west flank on August 11, 1858. The north face, the "last problem" of the Alps, considered amongst the most challenging and dangerous ascents, was first climbed in 1938 by an Austrian-German expedition.The Eiger has been highly publicized for the many tragedies involving climbing expeditions. Since 1935, at least 64 climbers have died attempting the north face, earning it the German nickname Mordwand, literally "murder(ous) wall"—a pun on its correct title of Nordwand (North Wall).

 

Although the summit of the Eiger can be reached by experienced climbers only, a railway tunnel runs inside the mountain, and two internal stations provide easy access to viewing-windows carved into the rock face. They are both part of the Jungfrau Railway line, running from Kleine Scheidegg to the Jungfraujoch, between the Mönch and the Jungfrau, at the highest railway station in Europe. The two stations within the Eiger are Eigerwand (behind the north face) and Eismeer (behind the south face), at around 3,000 metres. The Eigerwand station has not been regularly served since 2016.

 

Etymology

 

The first mention of Eiger, appearing as "mons Egere", was found in a property sale document of 1252, but there is no clear indication of how exactly the peak gained its name. The three mountains of the ridge are commonly referred to as the Virgin (German: Jungfrau – translates to "virgin" or "maiden"), the Monk (Mönch), and the Ogre (Eiger; the standard German word for ogre is Oger). The name has been linked to the Latin term acer, meaning "sharp" or "pointed".

 

Geographic setting and description

 

The Eiger is located above the Lauterbrunnen Valley to the west and Grindelwald to the north in the Bernese Oberland region of the canton of Bern. It forms a renowned mountain range of the Bernese Alps together with its two companions: the Jungfrau (4,158 m (13,642 ft)) about 5.6 kilometres (3.5 mi) southwest of it and the Mönch (4,107 m (13,474 ft)) about in the middle of them. The nearest settlements are Grindelwald, Lauterbrunnen (795 m (2,608 ft)) and Wengen (1,274 m (4,180 ft)). The Eiger has three faces: north (or more precisely NNW), east (or more precisely ESE), and west (or more precisely WSW). The northeastern ridge from the summit to the Ostegg (lit.: eastern corner, 2,709 m (8,888 ft)), called Mittellegi, is the longest on the Eiger. The north face overlooks the gently rising Alpine meadow between Grindelwald (943 m (3,094 ft)) and Kleine Scheidegg (2,061 m (6,762 ft)), a mountain railways junction and a pass, which can be reached from both sides, Grindelwald and Lauterbrunnen/Wengen – by foot or train.

 

Politically, the Eiger (and its summit) belongs to the Bernese municipalities of Grindelwald and Lauterbrunnen. The Kleine Scheidegg (literally, the small parting corner) connects the Männlichen-Tschuggen range with the western ridge of the Eiger. The Eiger does not properly form part of the main chain of the Bernese Alps, which borders the canton of Valais and forms the watershed between the Rhine and the Rhône, but constitutes a huge limestone buttress, projecting from the crystalline basement of the Mönch across the Eigerjoch. Consequently, all sides of the Eiger feed finally the same river, namely the Lütschine.

 

Eiger's water is connected through the Weisse Lütschine (the white one) in the Lauterbrunnen Valley on the west side (southwestern face of the Eiger), and through the Schwarze Lütschine (the black one) running through Grindelwald (northwestern face), which meet each other in Zweilütschinen (lit.: the two Lütschinen) where they form the proper Lütschine. The east face is covered by the glacier called Ischmeer, (Bernese German for Ice Sea), which forms one upper part of the fast-retreating Lower Grindelwald Glacier. These glaciers' water forms a short creek, which is also confusingly called the Weisse Lütschine, but enters the black one already in Grindelwald together with the water from the Upper Grindelwald Glacier. Therefore, all the water running down the Eiger converges at the northern foot of the Männlichen (2,342 m (7,684 ft)) in Zweilütschinen (654 m (2,146 ft)), about 10 kilometres (6.2 mi) northwest of the summit, where the Lütschine begins its northern course to Lake Brienz and the Aare (564 m (1,850 ft)).

 

Although the north face of the Eiger is almost free of ice, significant glaciers lie at the other sides of the mountain. The Eiger Glacier flows on the southwestern side of the Eiger, from the crest connecting it to the Mönch down to 2,400 m (7,900 ft), south of Eigergletscher railway station, and feeds the Weisse Lütschine through the Trümmelbach. On the east side, the Ischmeer–well visible from the windows of Eismeer railway station–flows eastwards from the same crest then turns to the north below the impressive wide Fiescherwand, the north face of the Fiescherhörner triple summit (4,049 m (13,284 ft)) down to about 1,600 m (5,200 ft) of the Lower Grindelwald Glacier system.

 

The massive composition of the Eiger, Mönch, and Jungfrau constitutes an emblematic sight of the Swiss Alps and is visible from many places on the Swiss Plateau and the Jura Mountains in the northwest. The higher Finsteraarhorn (4,270 m (14,010 ft)) and Aletschhorn (4,190 m (13,750 ft)), which are located about 10 kilometres (6.2 mi) to the south, are generally less visible and situated in the middle of glaciers in less accessible areas. As opposed to the north side, the south and east sides of the range consist of large valley glaciers extending for up to 22 kilometres (14 mi), the largest (beyond the Eiger drainage basin) being those of Grand Aletsch, Fiesch, and Aar Glaciers, and is thus uninhabited. The whole area, the Jungfrau-Aletsch protected area, comprising the highest summits and largest glaciers of the Bernese Alps, was inscribed as a UNESCO World Heritage Site in 2001.

 

In July 2006, a piece of the Eiger, amounting to approximately 700,000 cubic metres of rock, fell from the east face. As it had been noticeably cleaving for several weeks and fell into an uninhabited area, there were no injuries and no buildings were hit.

 

Climbing history

 

While the summit was reached without much difficulty in 1858 by a complex route on the west flank, the battle to climb the north face has captivated the interest of climbers and non-climbers alike. Before it was successfully climbed, most of the attempts on the face ended tragically and the Bernese authorities even banned climbing it and threatened to fine any party that should attempt it again. But the enthusiasm which animated the young talented climbers from Austria and Germany finally vanquished its reputation of unclimbability when a party of four climbers successfully reached the summit in 1938 by what is known as the "1938" or "Heckmair" route.

 

The climbers that attempted the north face could be easily watched through the telescopes from the Kleine Scheidegg, a pass between Grindelwald and Lauterbrunnen, connected by rail. The contrast between the comfort and civilization of the railway station and the agonies of the young men slowly dying a short yet uncrossable distance away led to intensive coverage by the international media.

 

After World War II, the north face was climbed twice in 1947, first by a party of two French guides, Louis Lachenal and Lionel Terray, then by a Swiss party consisting of H. Germann, with Hans and Karl Schlunegger.

 

First ascent

 

In 1857, a first recorded attempt was made by Christian Almer, Christian Kaufmann, Ulrich Kaufmann guiding the Austrian alpinist Sigismund Porges. They did manage the first ascent of neighboring Mönch instead. Porges, however, successfully made the second ascent of the Eiger in July 1861 with the guides Christian Michel, Hans and Peter Baumann.

 

The first ascent was made by the western flank on August 11, 1858 by Charles Barrington with guides Christian Almer and Peter Bohren. On the previous afternoon, the party walked up to the Wengernalp hotel. From there they started the ascent of the Eiger at 3:30 a.m. Barrington describes the route much as it is followed today, staying close to the edge of the north face much of the way. They reached the summit at about noon, planted a flag, stayed for some 10 minutes and descended in about four hours. Barrington describes the reaching of the top, saying, "the two guides kindly gave me the place of first man up." After the descent, the party was escorted to the Kleine Scheidegg hotel, where their ascent was confirmed by observation of the flag left on the summit. The owner of the hotel then fired a cannon to celebrate the first ascent. According to Harrer's The White Spider, Barrington was originally planning to make the first ascent of the Matterhorn, but his finances did not allow him to travel there as he was already staying in the Eiger region.

 

Mittellegi ridge

 

Although the Mittellegi ridge had already been descended by climbers (since 1885) with the use of ropes in the difficult sections, it remained unclimbed until 1921. On the 10th of September of that year, Japanese climber Yuko Maki, along with Swiss guides Fritz Amatter, Samuel Brawand and Fritz Steuri made the first successful ascent of the ridge. The previous day, the party approached the ridge from the Eismeer railway station of the Jungfrau Railway and bivouacked for the night. They started the climb at about 6:00 a.m. and reached the summit of the Eiger at about 7:15 p.m., after an over 13 hours gruelling ascent. Shortly after, they descended the west flank. They finally reached Eigergletscher railway station at about 3:00 a.m. the next day.

 

Attempts on the north face

 

1935

 

In 1935, two young German climbers from Bavaria, Karl Mehringer and Max Sedlmeyer, arrived at Grindelwald to attempt the ascent of the north face. After waiting some time for the weather to improve, they set off, reaching the height of the Eigerwand station before stopping for their first bivouac. The following day, facing greater difficulties, they gained little height. On the third day, they made hardly any vertical gain. That night, the weather deteriorated, bringing snow and low cloud that shrouded the mountain from the observers below. Avalanches began to sweep the face. Two days later, the weather briefly cleared, and the two men were glimpsed a little higher and about to bivouac for the fifth night, before clouds descended again. A few days later, the weather finally cleared, revealing a completely white north face.: 225  Weeks later, the German World War I ace Ernst Udet went searching for the missing men with his aircraft, eventually spotting one of them frozen to death in what became known as the "Death Bivouac". Sedlmeyer's body was found at the foot of the face the following year by his brothers Heinrich and Martin Meier, who were part of a group looking for the victims of the 1936 climbing disaster. Mehringer's remains were found in 1962 by Swiss climbers below the "Flat Iron" (Bügeleisen) at the lefthand end of the second ice field. 

 

1936

 

The next year ten young climbers from Austria and Germany came to Grindelwald and camped at the foot of the mountain. Before their attempts started one of them was killed during a training climb, and the weather was so bad during that summer that, after waiting for a change and seeing none on the way, several members of the party gave up. Of the four that remained, two were Bavarians, Andreas Hinterstoisser and Toni Kurz, and two were Austrians, Willy Angerer and Edi Rainer. When the weather improved they made a preliminary exploration of the lowest part of the face. Hinterstoisser fell 37 metres (121 ft) but was not injured. A few days later the four men finally began the ascent of the face. They climbed quickly, but on the next day, after their first bivouac, the weather changed; clouds came down and hid the group to the observers. They did not resume the climb until the following day, when, during a break, the party was seen descending, but the climbers could be seen only intermittently from the ground. The group had no choice but to retreat, since Angerer had suffered serious injuries from falling rock. The party became stuck on the face when they could not recross the difficult Hinterstoisser Traverse, from which they had taken the rope they had first used to climb it. The weather then deteriorated for two days. They were ultimately swept away by an avalanche, which only Kurz survived, hanging on a rope. Three guides started on an extremely perilous rescue attempt. They failed to reach him but came within shouting distance and learned what had happened. Kurz explained the fate of his companions: one had fallen down the face, another was frozen above him, and the third had fractured his skull in falling and was hanging dead on the rope.

 

In the morning the three guides came back, traversing the face from a hole near the Eigerwand station and risking their lives under incessant avalanches. Toni Kurz was still alive but almost helpless, with one hand and one arm completely frozen. Kurz hauled himself off the cliff after cutting loose the rope that bound him to his dead teammate below and climbed back onto the face. The guides were not able to pass an unclimbable overhang that separated them from Kurz. They managed to give him a rope long enough to reach them by tying two ropes together. While descending, Kurz could not get the knot to pass through his carabiner. He tried for hours to reach his rescuers who were only a few metres below him. Then he began to lose consciousness. One of the guides, climbing on another's shoulders, was able to touch the tip of Kurz's crampons with his ice-axe but could not reach higher. Kurz was unable to descend further and, completely exhausted, died slowly.

 

1937

 

An attempt was made in 1937 by Mathias Rebitsch and Ludwig Vörg. Although the attempt was unsuccessful, they were nonetheless the first climbers who returned alive from a serious attempt on the face. They started the climb on 11 August and reached a high point of a few rope lengths above Death Bivouac. A storm then broke and after three days on the wall they had to retreat. This was the first successful withdrawal from a significant height on the wall.

 

First ascent of the north face

 

The north face was first climbed on July 24, 1938 by Anderl Heckmair, Ludwig Vörg, Heinrich Harrer and Fritz Kasparek in a German–Austrian party. The party had originally consisted of two independent teams: Harrer (who did not have a pair of crampons on the climb) and Kasparek were joined on the face by Heckmair and Vörg, who had started their ascent a day later and had been helped by the fixed rope that the lead team had left across the Hinterstoisser Traverse. The two groups, led by the experienced Heckmair, decided to join their forces and roped together as a single group of four. Heckmair later wrote: "We, the sons of the older Reich, united with our companions from the Eastern Border to march together to victory."

 

The expedition was constantly threatened by snow avalanches and climbed as quickly as possible between the falls. On the third day a storm broke and the cold was intense. The four men were caught in an avalanche as they climbed "the Spider," the snow-filled cracks radiating from an ice-field on the upper face, but all possessed sufficient strength to resist being swept off the face. The members successfully reached the summit at four o'clock in the afternoon. They were so exhausted that they only just had the strength to descend by the normal route through a raging blizzard.

 

Other notable events

 

1864 (Jul 27): Fourth ascent, and first ascent by a woman, Lucy Walker, who was part of a group of six guides (including Christian Almer and Melchior Anderegg) and five clients, including her brother Horace Walker[

1871: First ascent by the southwest ridge, 14 July (Christian Almer, Christian Bohren, and Ulrich Almer guiding W. A. B. Coolidge and Meta Brevoort).

1890: First ascent in winter, Ulrich Kaufmann and Christian Jossi guiding C. W. Mead and G. F. Woodroffe.

1924: First ski ascent and descent via the Eiger glacier by Englishman Arnold Lunn and the Swiss Fritz Amacher, Walter Amstutz and Willy Richardet.

1932: First ascent of the northeast face ("Lauper route") by Hans Lauper, Alfred Zürcher, Alexander Graven and Josef Knubel

1970: First ski descent over the west flank, by Sylvain Saudan.

1986: Welshman Eric Jones becomes the first person to BASE jump from the Eiger.

1988: Original Route (ED2), north face, Eiger (3970m), Alps, Switzerland, first American solo (nine and a half hours) by Mark Wilford.

1991: First ascent, Metanoia Route, North Face, solo, winter, without bolts, Jeff Lowe.

1992 (18 July): Three BMG/UIAGM/IFMGA clients died in a fall down the West Flank: Willie Dunnachie; Douglas Gaines; and Phillip Davies. They had ascended the mountain via the Mittellegi Ridge.

2006 (14 June): François Bon and Antoine Montant make the first speedflying descent of the Eiger.

2006 (15 July): Approximately 700,000 cubic metres (20 million cubic feet) of rock from the east side collapses. No injuries or damage were reported.

2015 (23 July): A team of British Para-Climbers reached the summit via the West Flank Route. The team included John Churcher, the world's first blind climber to summit the Eiger, sight guided by the team leader Mark McGowan. Colin Gourlay enabled the ascent of other team members, including Al Taylor who has multiple sclerosis, and the young autistic climber Jamie Owen from North Wales. The ascent was filmed by the adventure filmmakers Euan Ryan & Willis Morris of Finalcrux Films.

 

Books and films

 

The 1959 book The White Spider by Heinrich Harrer describes the first successful ascent of the Eiger north face.

The Climb Up To Hell, 1962, by Jack Olson, an account of the ill-fated 1957 attempted climb of the north face by an Italian four-man team and the dramatic rescue of the sole survivor mounted by an international all-volunteer group of rescuers.

Eiger Direct, 1966, by Dougal Haston and Peter Gillman, London: Collins, also known as Direttissima; the Eiger Assault

The 1971 novel The Ice Mirror by Charles MacHardy describes the second attempted ascent of the Eiger north face by the main character.

The 1972 novel The Eiger Sanction is an action/thriller novel by Rodney William Whitaker (writing under the pseudonym Trevanian), based around the climbing of the Eiger. This was then made into the 1975 film The Eiger Sanction starring Clint Eastwood and George Kennedy. The Eiger Sanction film crew included very experienced mountaineers (e.g., Mike Hoover, Dougal Haston, and Hamish MacInnes, see Summit, 52, Spring 2010) as consultants, to ensure accuracy in the climbing footage, equipment and techniques.

The Eiger, 1974, by Dougal Haston, London: Cassell

The 1982 book Eiger, Wall of Death by Arthur Roth is an historical account of first ascents of the north face.

The 1982 book Traverse of The Gods by Bob Langley is a World War II spy thriller where a group escaping from Nazi Germany is trapped and the only possible exit route is via the Nordwand.

Eiger, 1983, a documentary film by Leo Dickinson of Eric Jones' 1981 solo ascent of the north face.

Eiger Dreams, 1990, a collection of essays by Jon Krakauer, begins with an account of Krakauer's own attempt to climb the north face.

Eiger: The Vertical Arena (German edition, 1998; English edition, 2000), edited by Daniel Anker, a comprehensive climbing history of the north face authored by 17 climbers, with numerous photographs and illustrations.

The IMAX film The Alps features John Harlin III's climb up the north face in September 2005. Harlin's father, John Harlin II, set out 40 years earlier to attempt a direct route (the direttissima) up the 6,000-foot (1,800 m) face, the so-called "John Harlin route". At 1300 m, his rope broke, and he fell to his death. Composer James Swearingen created a piece named Eiger: Journey to the Summit in his memory.

The 2007 docu/drama film The Beckoning Silence featuring mountaineer Joe Simpson, recounting—with filmed reconstructions—the ill-fated 1936 expedition up the north face of the Eiger and how Heinrich Harrer's book The White Spider inspired him to take up climbing. The film followed Simpson's eponymous 2003 book. Those playing the parts of the original climbing team were Swiss mountain guides Roger Schäli (Toni Kurz), Simon Anthamatten (Andreas Hinterstoisser), Dres Abegglen (Willy Angerer) and Cyrille Berthod (Edi Rainer). The documentary won an Emmy Award the subsequent year.

The 2008 German historical fiction film Nordwand is based on the 1936 attempt to climb the Eiger north face. The film is about the two German climbers, Toni Kurz and Andreas Hinterstoisser, involved in a competition with an Austrian duo to be the first to scale the north face of Eiger.

The 2010 documentary Eiger: Wall of Death by Steve Robinson.

 

(Wikipedia)

 

The Mönch (German pronunciation: [ˈmœnç] German: "monk") at 4,110 metres (13,480 ft) is a mountain in the Bernese Alps, in Switzerland. Together with the Eiger and the Jungfrau, it forms a highly recognisable group of mountains, visible from far away.

 

The Mönch lies on the border between the cantons of Valais and Bern, and forms part of a mountain ridge between the Jungfrau and Jungfraujoch to the west, and the Eiger to the east. It is west of Mönchsjoch, a pass at 3,650 metres (11,980 ft), Mönchsjoch Hut, and north of the Jungfraufirn and Ewigschneefäld, two affluents of the Great Aletsch Glacier. The north side of the Mönch forms a step wall above the Lauterbrunnen valley.

 

The Jungfrau railway tunnel runs right under the summit, at an elevation of approximately 3,300 metres (10,830 ft).

 

The summit was first climbed on record on 15 August 1857 by Christian Almer, Christian Kaufmann (1831-1861), Ulrich Kaufmann and Sigismund Porges.

 

(Wikipedia)

 

The Jungfrau (YOONG-frow, German pronunciation: [ˈjʊŋˌfʁaʊ̯], transl. "maiden, virgin"), at 4,158 meters (13,642 ft) is one of the main summits of the Bernese Alps, located between the northern canton of Bern and the southern canton of Valais, halfway between Interlaken and Fiesch. Together with the Eiger and Mönch, the Jungfrau forms a massive wall of mountains overlooking the Bernese Oberland and the Swiss Plateau, one of the most distinctive sights of the Swiss Alps.

 

The summit was first reached on August 3, 1811, by the Meyer brothers of Aarau and two chamois hunters from Valais. The ascent followed a long expedition over the glaciers and high passes of the Bernese Alps. It was not until 1865 that a more direct route on the northern side was opened.

 

The construction of the Jungfrau Railway in the early 20th century, which connects Kleine Scheidegg to the Jungfraujoch, the saddle between the Mönch and the Jungfrau, made the area one of the most-visited places in the Alps. Along with the Aletsch Glacier to the south, the Jungfrau is part of the Jungfrau-Aletsch area, which was declared a World Heritage Site in 2001.

 

Etymology

 

The name Jungfrau ("maiden, virgin"), which refers to the highest of the three prominent mountains overlooking the Interlaken region, along with the Mönch ("monk") and the Eiger ("ogre"), is most likely derived from the name Jungfrauenberg given to Wengernalp, the alpine meadow directly facing the huge northern side of the Jungfrau, across the Trummelbach gorge. Wengernalp was so named for the nuns of Interlaken Monastery, its historical owner. Contrary to popular belief, the name did not originate from the appearance of the snow-covered mountain, the latter looking like a veiled woman.

 

The "virgin" peak was heavily romanticized as "goddess" or "priestess" in late 18th to 19th century Romanticism. Its summit, considered inaccessible, remained untouched until the 19th century. After the first ascent in 1811 by Swiss alpinist Johann Rudolf Meyer, the peak was jokingly referred to as "Mme Meyer" (Mrs. Meyer).

 

Geographic setting

 

Politically, the Jungfrau (and its massif) is split between the municipalities of Lauterbrunnen (Bern) and Fieschertal (Valais). It is the third-highest mountain of the Bernese Alps after the nearby Finsteraarhorn and Aletschhorn, respectively 12 and 8 km (7.5 and 5 mi) away. But from Lake Thun, and the greater part of the canton of Bern, it is the most conspicuous and the nearest of the Bernese Oberland peaks; with a height difference of 3,600 m (11,800 ft) between the summit and the town of Interlaken. This, and the extreme steepness of the north face, secured for it an early reputation for inaccessibility.

 

The Jungfrau is the westernmost and highest point of a gigantic 10 km (6.2 mi) wall dominating the valleys of Lauterbrunnen and Grindelwald. The wall is formed by the alignment of some of the biggest north faces in the Alps, with the Mönch (4,107 m or 13,474 ft) and Eiger (3,967 m or 13,015 ft) to the east of the Jungfrau, and overlooks the valleys to its north by a height of up to 3 km (1.9 mi). The Jungfrau is approximately 6 km (3.7 mi) from the Eiger; with the summit of the Mönch between the two mountains, 3.5 km (2.2 mi) from the Jungfrau. The Jungfraujoch is the saddle between the Jungfrau and the Mönch and the Eigerjoch is the saddle between the Mönch and the Eiger. The wall is extended to the east by the Fiescherwand and to the west by the Lauterbrunnen Wall, although it follows different directions from the Jungfrau and the Eiger.

 

The difference of altitude between the deep valley of Lauterbrunnen (800 m or 2,600 ft) and the summit is particularly visible from the area of Mürren. From the valley floor, west of the massif, the altitude gain is more than 3 km (1.9 mi) for a horizontal distance of 4 km (2.5 mi).

 

The landscapes around the Jungfrau are extremely contrasted. In contrast to the vertiginous precipices of its northwest, the mountain's southeastern side emerges from the upper snows of the Jungfraufirn, one of the main feeders of the Aletsch Glacier, at around 3,500 meters (11,500 ft). The 20-kilometer-long (12 mi) valley of Aletsch on the southeast is completely uninhabited, and is surrounded by neighboring valleys with similar landscapes. The area as a whole constitutes the largest glaciated area not just in the Alps, but in Europe as well.

 

Climbing history

 

In 1811, the brothers Johann Rudolf (1768–1825) and Hieronymus Meyer, sons of Johann Rudolf Meyer (1739–1813), the head of a rich merchant family of Aarau, along with several servants and a porter picked up at Guttannen, first reached the Valais by way of the Grimsel, and crossed the Beich Pass, a glacier pass over the Oberaletsch Glacier, to the head of the Lötschen valley. There, they added two local chamois hunters, Alois Volken and Joseph Bortis, to their party and traversed the Lötschenlücke before reaching the Aletschfirn (the west branch of the Aletsch Glacier), where they established the base camp, north of the Aletschhorn. After the Guttannen porter was sent back alone over the Lötschenlücke, the party finally reached the summit of the Jungfrau by the Rottalsattel on August 3. They then recrossed the two passes named to their point of departure in Valais, and went home again over the Grimsel.

 

The journey was a most extraordinary one for the time, and some persons threw doubts at its complete success. To settle these, another expedition was undertaken in 1812. In this the two sons, Rudolf (1791–1833) and Gottlieb (1793–1829), of Johann Rudolf Meyer, played the chief parts. After an unsuccessful attempt, defeated by bad weather, in the course of which the Oberaarjoch was crossed twice (this route being much more direct than the long detour through the Lötschental), Rudolf, with the two Valais hunters (Alois Volker and Joseph Bortis), a Guttannen porter named Arnold Abbühl, and a Hasle man, bivouacked on a depression on the southeast ridge of the Finsteraarhorn. Next day (August 16) the whole party attempted the ascent of the Finsteraarhorn from the Studer névé on the east by way of the southeast ridge, but Meyer, exhausted, remained behind. The following day the party crossed the Grünhornlücke to the Aletsch Glacier, but bad weather then put an end to further projects. At a bivouac, probably just opposite the present Konkordia Hut, the rest of the party, having come over the Oberaarjoch and the Grünhornlücke, joined the Finsteraarhorn party. Gottlieb, Rudolf's younger brother, had more patience than the rest and remained longer at the huts near the Märjelensee, where the adventurers had taken refuge. He could make the second ascent (September 3) of the Jungfrau, the Rottalsattel being reached from the east side as is now usual, and his companions being the two Valais hunters.

 

The third ascent dates from 1828, when several men from Grindelwald, headed by Peter Baumann, planted their flag upon the summit. Next came the ascent by Louis Agassiz, James David Forbes, Heath, Desor, and Duchatelier in 1841, recounted by Desor in his Excursions et Séjours dans les Glaciers. Gottlieb Samuel Studer published an account of the next ascent made by himself and Bürki in 1842.

 

In 1863, a party consisting of three young Oxford University graduates and three Swiss guides successfully reached the summit and returned to the base camp of the Faulberg (located near the present position of the Konkordia Hut) in less than 11 hours (see the section below, The 1863 Ascent). In the same year Mrs Stephen Winkworth became the first woman to climb the Jungfrau. She also slept overnight in the Faulberg cave prior to the ascent as there was no hut at that time.

 

Before the construction of the Jungfraujoch railway tunnel, the approach from the glaciers on the south side was very long. The first direct route from the valley of Lauterbrunnen was opened in 1865 by Geoffrey Winthrop Young, H. Brooke George with the guide Christian Almer. They had to carry ladders with them in order to cross the many crevasses on the north flank. Having spent the night on the rocks of the Schneehorn (3,402 m or 11,161 ft) they gained next morning the Silberlücke, the depression between the Jungfrau and Silberhorn, and thence in little more than three hours reached the summit. Descending to the Aletsch Glacier they crossed the Mönchsjoch, and passed a second night on the rocks, reaching Grindelwald next day. This route became a usual until the opening of the Jungfraujoch.

 

The first winter ascent was made on 23 January 1874, by Meta Brevoort and W. A. B. Coolidge with guides Christian and Ulrich Almer. They used a sled to reach the upper Aletsch Glacier, and were accompanied by Miss Brevoort's favorite dog, Tschingel.

 

The Jungfrau was climbed via the west side for the first time in 1885 by Fritz and Heinrich von Allmen, Ulrich Brunner, Fritz Graf, Karl Schlunegger and Johann Stäger—all from Wengen. They ascended the Rottal ridge (Innere Rottalgrat) and reached the summit on 21 September. The more difficult and dangerous northeast ridge that connects the summit from the Jungfraujoch was first climbed on 30 July 1911 by Albert Weber and Hans Schlunegger.

 

In July 2007, six Swiss Army recruits, part of the Mountain Specialists Division 1, died in an accident on the normal route. Although the causes of the deaths was not immediately clear, a report by the Swiss Federal Institute for Snow and Avalanche Research concluded that the avalanche risk was unusually high due to recent snowfall, and that there was "no other reasonable explanation" other than an avalanche for the incident.

 

The 1863 Ascent

 

The Führerbuch of the Alpine guide Peter Baumann records an ascent of the Jungfrau made by himself with three men from England in July 1863. The foreign climbers were long thought to have been John Tyndall, J.J. Hornby and T.H. Philpott, until in 1958 the records were checked by the Alpine Club and the following conclusion was reached:

 

On July 23, 1963, Phillpotts, with James Robertson and H.J. Chaytor, climbed the Jungfrau (the entry shown in A.J. 32. 227 was wrongly transcribed by Montagnier, who says ‘T.H. Philpott’ for J.S. Phillpotts). The entry in Peter Baumann’s Führerbuch (facsimile in A.C. archives) says that the trio crossed the Strahlegg Pass and the Oberaarjoch, and then climbed the Jungfrau from the Eggishorn.

 

Tyndall, Hornby and Philpott were well-known Alpinists, but there is no record of their having attempted the Jungfrau in 1863. Robertson, Chaytor and Phillpotts were novices; they had recently graduated from Oxford University where they had all been keen members of the Oxford University Boat Club.

 

William Robertson (1839–1892), the leader of the expedition (wrongly called ‘James’ in the Note quoted above), was an Australian by birth, and the first non-British national to take part in the Oxford and Cambridge Boat Race. He later became a barrister and member of parliament in Australia. He and H.J. Chaytor (possibly the father of the medievalist Henry John Chaytor) were both members of the victorious Oxford team in the 1861 Boat Race. James Surtees Phillpotts (1839–1930) was the third member of the team; he would later become headmaster of Bedford School. The trio had three Swiss guides, Peter Baumann, Peter Kaufmann ("Grabipeter", father of Peter Kaufmann the younger) and Rubi.

 

A description of the ascent of the Jungfrau is contained in a letter dated Sunday 26 July which Phillpotts wrote to his friend Alexander Potts (later to become the first headmaster of Fettes College). The letter is now in the possession of the Alpine Club. The following extracts are from that letter.

 

The Virgin certainly did not smile on the poor "fools who rushed in" on her sacred heights, i.e. in plain British, we had the treadmill slog, the biting wind, the half frost-bitten feet and the flayed faces that generally attend an Alpine ascent.

 

We got to the Faulberg hole about dark, and enjoyed the coffee the longman (Kauffmann) made, as one would in a hole in a rock in a cold evening. The "Faulberg Nachtlager" consists of two holes and a vestibule to the upper hole. The Upper Hole in which we lodged just contained Chay[tor], the Guv [Robertson] and myself, stretched at full length on a little hay over a hard rock mattress, convex instead of concave at the point where one likes to rest one's weight. Chaytor was in the middle, and as we were very close was warm and slept. The Guv and I courted Nature's soft nurse in vain. At two we got up and methodically put our feet into the stocks, i.e. our boots, breakfasted and shivered, then started (unwashed of course, as the cold gave us malignant hydrophobia) a little after 3:30.

 

The hole was about 150 feet [46 m] up one of the loose stone cliffs one now knows so well. So we groped our way down it and over the moraine – the stars still lingering, as day was just dawning. We could not start at 1:30, the proper time, as there was no moon and we wanted light as we had to tramp the glacier at once. Rubi led, and off we went, roped and in Indian file, in the old treadmill way over the slippery plowed-field-like snow that lay on the upper glacier, for a pull without a check of one or two hours.

 

At last we came to the region of bergschrunds and crevasses. They seemed to form at first an impassable labyrinth, but gradually the guides wound in and out between the large rifts, which were exquisitely lovely with their overhanging banks of snow and glittering icicles, and then trod as on pins and needles over a snowbridge here and there, or had to take a jump over the more feasible ones – and we found ourselves at the foot of the mountain; trudged up on the snow which ought to have been crisp but was even then more or less fresh fallen and sloppy; had to creep over about three crevasses, and after a tiresome pull, dragging one leg after another out of ankle or knee deep snow, we got on a crest of snow at right angles to the slope we had just come up. That slope with its crevasses on one side, and on the other a shorter and much steeper one which led in a few steps to a precipice.

 

All along this crest went a snakelike long crevasse, for which we had continually to sound, and go first one side and then the other; then we got to the foot of the saddle. Some twenty or thirty steps, some cut, some uncut, soon took us up a kind of hollow, and we got on a little sloping plateau of some six feet [1.8 m] large, where we left the grub and the knapsack, keeping my small flask of cognac only. Then up a steep ice slope, very steep I should say, down which the bits of ice cut out of the steps hopped and jumped at full gallop and then bounded over to some bottomless place which we could not see down. Their pace gave one an unpleasant idea of the possible consequence of a slip.

 

Here we encountered a biting bitter wind. Peter Baumann cut magnificent steps, at least he and Rubi did between them, the one improving on the other's first rough blows. After Rubi came Chaytor with Kauffmann behind him, then the Guv, and then myself, the tail of the string. Each step was a long lift from the last one, and as the snow was shallow they had to be cut in the ice which was like rock on this last slope.

 

Suddenly there burst upon us, on lifting our heads over the ridge, the green and cheerful valleys of Lauterbrunnen and Interlaken, of Grindelwald and a distant view of others equally beautiful stretching on for ever in one vast panorama. On the other side in grim contrast there was a wild and even awful scene. One gazed about one and tried in vain to see to the bottom of dark yawning abysses and sheer cliffs of ice or rock.

 

Tourism

 

Named after the Jungfrau, the Jungfrau Region of the Bernese Oberland is a major tourist destination in the Alps and includes a large number of railways and other facilities. While the mountain peak was once difficult to access, the Jungfrau Railway, a rack railway, now goes to the Jungfraujoch railway station at 3,454 m (11,332 ft), therefore providing an easy access to the upper Aletsch Glacier and a relatively short access to the Jungfrau itself, the height difference between the station and the summit being only 704 metres and the horizontal distance being slightly less than 2 kilometres. As a result, in the popular mind, the Jungfrau has become a mountain associated with the Bernese Oberland and Interlaken, rather than with Upper Valais and Fiesch.

 

In 1893, Adolf Guyer-Zeller conceived of the idea of a railway tunnel to the Jungfraujoch to make the glaciated areas on its south side more accessible. The building of the tunnel took 16 years and the summit station was not opened before 1912. The goal was in fact to reach the summit of the Jungfrau with an elevator from the highest railway station, located inside the mountain. The complete project was not realized because of the outbreak of the World War I. Nevertheless, it was at the time one of the highest railways in the world and remains today the highest in Europe and the only (non-cable) railway on Earth going well past the perennial snow-line.

 

The Jungfrau Railway leaves from Kleine Scheidegg, which can be reached from both sides by trains from Grindelwald, and Lauterbrunnen via Wengen. The train enters the Jungfrau Tunnel running eastward through the Eiger just above Eigergletscher, which is, since 2020, also accessible by aerial tramway from Grindelwald. Before arriving at the Jungfraujoch, it stops for a few minutes at two other stations, Eigerwand (on the north face of the Eiger) and Eismeer (on the south side), where passengers can see through the holes excavated from the mountain. The journey from Kleine Scheidegg to Jungfraujoch takes approximately 50 minutes including the stops; the downhill return journey taking only 35 minutes.

 

A large complex of tunnels and buildings has been constructed at the Jungfraujoch, referred to as the "Top of Europe". There are several restaurants and bars, shops, multimedia exhibitions, a post office, and a research station with dedicated accommodation facilities. An elevator enables access to the top of the Sphinx and its observatory, at 3,571 m (11,716 ft), the highest viewing platform of the area. Outside, at the level of the Jungfraujoch, there is a ski school, and the "Ice Palace", a collection of elaborate ice sculptures displayed inside the Aletsch Glacier. Another tunnel leads to the east side of the Sphinx, where one can walk on the glacier up to the Mönchsjoch Hut, the only hotel infrastructure in the area.

 

Apart from the Jungfraujoch, many facilities have been built in the Jungfrau Region, including numerous mountain railways. In 1908, the first public cable car in the world, the Wetterhorn Elevator, opened at the foot of the Wetterhorn, but was closed seven years later. The Schilthorn above Mürren, the Männlichen above Wengen, and the Schynige Platte above Wilderswil, offer good views of the Jungfrau and the Lauterbrunnen valley. On the south side, the Eggishorn above Fiesch also offers views of the Jungfrau, across the Aletsch Glacier.

 

Climbing routes

 

The normal route follows the traces of the first climbers, but the long approach on the Aletsch Glacier is no longer necessary. From the area of the Jungfraujoch the route to the summit takes only a few hours. Most climbers start from the Mönchsjoch Hut. After a traverse of the Jungfraufirn the route heads to the Rottalsattel (3,885 m or 12,746 ft), from where the southern ridge leads to the Jungfrau. It is not considered a very difficult climb but it can be dangerous on the upper section above the Rottalsattel, where most accidents happen. The use of the Jungfrau Railway instead of the much more gradual approach from Fiesch (or Fieschertal), via the Konkordia Hut, can cause some acclimatization troubles as the difference of altitude between the railway stations of Interlaken and Jungfraujoch is almost 3 km (1.9 mi).

 

(Wikipedia)

 

Der Eiger ist ein Berg in den Berner Alpen mit einer Höhe von 3967 m ü. M. Er ist dem Hauptkamm der Berner Alpen etwas nördlich vorgelagert und steht vollständig auf dem Territorium des Schweizer Kantons Bern. Zusammen mit Mönch und Jungfrau, deren Gipfel auf der Grenze zum Kanton Wallis liegen, dominiert der Eiger die Landschaft des zentralen Berner Oberlandes. Die etwa 3000 Meter über dem Tal aufragenden Nordflanken dieser Berge stellen die Schauseite einer der bekanntesten je als ein «Dreigestirn» bezeichneten Gipfel-Dreiergruppen in den Alpen dar.

 

Insbesondere die Nordwand des Eigers fasziniert sowohl Bergsteiger als auch Alpin-Laien. Durch dramatische Begehungsversuche und gelungene Begehungen dieser Wand wurde der Eiger weltweit bekannt und immer wieder ins Blickfeld der Öffentlichkeit gerückt – nicht zuletzt, da die gesamte Wand von Grindelwald und der Bahnstation Kleine Scheidegg aus einsehbar ist. Die Jungfraubahn mit ihrem Tunnel durch den Eigerfels ist seit ihrer Eröffnung im Jahr 1912 ein Touristenmagnet.

 

Namensherkunft

 

Die erste urkundliche Erwähnung des Eigers stammt aus dem Jahre 1252 – dies ist die zweitfrüheste urkundliche Erwähnung eines Schweizer Bergs nach dem Bietschhorn (1233). Am 24. Juli 1252 wurde in einer Verkaufsurkunde zwischen Ita von Wädiswyl und der Propstei Interlaken ein Grundstück mit den Worten «ad montem qui nominatur Egere» (dt.: Bis zum Berg, der Eiger genannt wird) abgegrenzt. Ein halbes Jahrhundert später wird der Eiger in einem Belehnungsbrief erstmals in deutscher Sprache erwähnt: «under Eigere».

 

Für die Herkunft des Namens gibt es drei gängige Erklärungen. Eine erste ist der althochdeutsche Name Agiger oder Aiger, wie der erste Siedler unterhalb des Eigers geheissen haben soll. Der Berg über dessen Weiden wurde deshalb Aigers Geissberg oder auch nur Geissberg genannt. Hieraus entwickelten sich dann im Laufe der Zeit die direkten Vorgänger der heutigen Bezeichnung. Die Herkunft des Namens könnte auch von dem lateinischen Wort acer kommen, woraus sich im Französischen aigu entwickelte. Beide Worte haben die Bedeutung scharf beziehungsweise spitz – in Anlehnung an die Form des Eigers. Die dritte Erklärung stammt von der früher gebräuchlichen Schreibweise Heiger, was sich aus dem Dialektausdruck «dr hej Ger» entwickelt haben könnte (hej bedeutet hoch, Ger war ein germanischer Wurfspiess). Wiederum wäre hier die Form des Eigers ausschlaggebend für seine Bezeichnung.

 

Im Zusammenhang mit dem Eiger wird auch des Öfteren die Namensähnlichkeit mit dem Oger, einem menschenähnlichen Unhold, genannt. In Anlehnung an das Dreigestirn «Eiger–Mönch–Jungfrau» gibt es die Erzählung, der Unhold Eiger wolle seine lüsternen Pranken auf die Jungfrau legen, woran er aber vom fröhlichen Mönch gehindert werde. Zu dieser Geschichte sind in Grindelwald alte Karikaturen und neuere Postkarten zu kaufen.

 

Lage und Umgebung

 

Der Eiger erhebt sich direkt südwestlich von Grindelwald (Amtsbezirk Interlaken). Die bekannte Nordwand ist genaugenommen eine Nordwestwand. Neben dieser existiert in der berühmten «Eiger-Nordansicht» auch noch die Nordostwand. Sie bildet die Basis für den scharfen Mittellegigrat, der vom Unteren Grindelwaldgletscher zum Gipfel zieht. Auf der gegenüberliegenden Seite begrenzt der Westgrat die Nordwand. Ihm folgt die Westflanke, in welcher sich der Eigergletscher und der Klein Eiger befinden. An diesen schliessen sich der Südwestgrat und noch ein Stück östlicher der Südgrat an, der wiederum die Südostwand begrenzt, welche bis zum Mittellegigrat reicht. Südöstlich des Eigers liegt der Grindelwald-Fieschergletscher.

 

In der Umgebung des Eigers befinden sich einige Viertausender des Aarmassivs. Im Osten ist er umgeben von Schreckhorn (4078 m ü. M.) und Lauteraarhorn (4042 m ü. M.), im Südosten vom Grossen Fiescherhorn (4049 m ü. M.), und im Südwesten ist der Mönch (4107 m ü. M.) durch das Nördliche und Südliche Eigerjoch vom Eiger getrennt. Zusammen mit dem Mönch und der Jungfrau (4158 m ü. M.) bildet der Eiger das «Dreigestirn», bei dem der Eiger den nordöstlichen und die Jungfrau den südwestlichen Endpunkt bildet. Entgegen der steil abfallenden Nordseite des Berges befindet sich im Süden des Eigers die Hochfläche und Gletscherwelt der Berner Alpen. Seit Ende 2001 gehört der Eiger zum Gebiet des UNESCO-Weltnaturerbes Schweizer Alpen Jungfrau-Aletsch.

 

Geologie

 

Der Eiger ist ein Teil des helvetischen Systems, das im Grossraum um den Thunersee die Decken des Alpennordrandes bildet. In einer späten Phase der alpidischen Gebirgsfaltung wurden die helvetischen Kalk-Sedimente von ihrer kristallinen Basis abgeschürft und in Form einer Abscherungsdecke nach Nordwesten verschoben. Während des Faltungsprozesses in der Alpenentstehung brachen die Kalkbänke auf und Kluft- sowie Faltensysteme entstanden, die später mit ausgefälltem Calcit geschlossen wurden. Wichtigste Bestandteile der Sedimente sind der Schrattenkalk der Kreidezeit und der Malmkalk. Als Füll- und Schmiermaterial dienten Mergel und Tonschiefer.

 

Die klar erkennbare Faltung des Helvetikums mit seinen gebänderten, plattigen Kalkschichten zeigt sich auch am Eiger. Das Massiv des Eigers besteht komplett aus Kalk der helvetischen Zone und schliesst die Flyschschichten und die Molasse des Grindelwaldbeckens steil nach Süden hin ab. Weil der Talkessel von Grindelwald so reich gegliedert ist, finden hier die verschiedensten Tiere einen Lebensraum.[6] Südlich des Eigers schliesst sich das Aarmassiv mit seinem Innertkirchner-Lauterbrunner-Kristallin an. Teilweise hat sich dieses über die Sedimente des Eiger geschoben. Im Bereich des Mönchs treffen die Sedimente auf Altkristallin. Die typischen Gesteine des helvetischen Systems im Bereich des Eigers entstanden während des Jura, dem mittleren Zeitabschnitts des Mesozoikums. Der vorherrschende Kalk ist dabei mit verschiedenen Gesteinen durchmischt. Es zeigen sich Mergel-Kalke und -Schiefer, Ton-Schiefer, Eisenoolith sowie kalkige Sandsteine.

 

Die Kalkschichten des Eigers lagern auf Gneis und sind um 60–70° nach Norden geneigt. Geprägt wurde die heutige Form des Eigers durch die Eiszeiten. Während der Riss-Kaltzeit reichte die Vergletscherung bis an den Fuss der Nordwand. In der Würm-Kaltzeit war die Mächtigkeit des Eises um 200 Meter geringer. Durch die Bewegung der Gletscher wurde die Erdoberfläche umgestaltet. Vom Eis überlagerte Landschaften wurden abgeschliffen, wohingegen unbedeckte Bereiche durch Verwitterung und andere Formen der Erosion verändert wurden. Mit dem Rückzug des Eises änderten sich auch die Druckverhältnisse im Gestein, was sich durch Entlastungsbewegungen formgebend auswirkte. Prägend für den Eiger und seine Form war die allseitige Umlagerung von Eismassen, welche für einen recht gleichmässigen und markanten Abrieb aller Wände sorgte. Darüber hinaus war die Nordwand durch ihre Exposition den Abtragungsprozessen wie Frostverwitterung mehr ausgesetzt.

 

Felssturz

 

2006 ereignete sich am Eiger ein grosser Bergsturz, der öffentliches Interesse auf sich zog. An der Ostseite des Berges, unterhalb des Mittellegigrates, war durch Felsbewegungen ein rund 250 Meter langer Spalt entstanden, der eine Breite von etwa 7 Metern erreichte.Danach senkten sich die äusseren Teile mehrere Zentimeter pro Tag ab. Eine Ursache dieser Felsabspaltung könnte sowohl das massive Eindringen von Schmelzwasser in den Felsen gewesen sein, als auch eine Instabilität des Gesteins durch den Rückgang des Gletschers unterhalb des Felsabbruchs infolge der globalen Erwärmung. Am 13. Juli 2006 um 19:24 Uhr stürzten rund 500'000 Kubikmeter Felsbrocken auf den Unteren Grindelwaldgletscher. Über der Gemeinde Grindelwald schwebte stundenlang eine Staubwolke. Bereits am Nachmittag desselben Tages war die sogenannte «Madonna vom Eiger» zu Tal gestürzt. Hierbei handelte es sich um einen ungefähr 30 Meter hohen schlanken Felsturm mit rund 600 Kubikmeter Volumen.

 

Seit diesen Ereignissen wird die Felsnase (Gesamtvolumen: ungefähr eine Million Kubikmeter Gestein), aus der die Gesteinsmasse abbrach, von der Universität Lausanne beobachtet. Die Beobachtungen ergaben, dass sich die Nase von Juli 2007 bis August 2008 auf einer nach Osten geneigten Gleitfläche um 15 Meter talwärts bewegte. Zusätzlich kippte die Gesteinsmasse um zwei Grad nach Nordosten. Die Kluft zwischen Berg und Felsbrocken betrug im August 2008 50 Meter. Immer wieder brechen Gesteinsteile ab und stürzen zu Tal. Gebremst und stabilisiert wird die Masse vom Gletschereis, in das die Felsnase gleitet. Dies verhindert, dass die Nase als kompakte Masse zu Tal stürzt. So gilt es als wahrscheinlicher, dass der Gesteinsblock in sich selbst zusammenfallen wird.

 

(Wikipedia)

 

Der Mönch ist ein 4107 m ü. M. hoher Berg der Berner Alpen in der Schweiz. Zusammen mit dem Eiger und der Jungfrau bildet er eine markante, von weit her sichtbare Dreiergruppe, ein sogenanntes „Dreigestirn“.

 

Seine Erstbesteigung fand am 15. August 1857 durch Christian Almer, Christian Kaufmann, Ulrich Kaufmann und Sigismund Porges statt.

 

Südöstlich des Mönch liegt die Mönchsjochhütte, eine 3657 m ü. M. hoch gelegene Berghütte wenig oberhalb des oberen Mönchsjochs, das den Mönch vom Trugberg trennt.

 

Höhenbestimmung

 

1935 wurde die Höhe des Mönchs mit 4099 m ü. M. bestimmt. Diese Zahl ist noch heute häufig in der Literatur zu finden. 1993 ergaben jedoch Messungen per Luftfotogrammetrie eine Höhe von 4107 m ü. M.. Daraufhin wurde der Wert auf der Landeskarte der Schweiz korrigiert. Mit einer Messung per GPS ermittelte man 1997 eine Höhe von 4109,4 m ü. M.; und bei einer erneuten luftfotogrammetrischen Messung von 1999 resultierte sogar eine Höhe von 4110 m ü. M.. Diese neuen Messwerte wurden jedoch nicht auf den amtlichen Karten berücksichtigt. Für diese abweichenden Werte sind nicht nur Messfehler verantwortlich, sondern auch die Tatsache, dass der Mönch eine Kuppe aus Firn besitzt, welche in den letzten Jahren gewachsen ist.

 

Name

 

Am Fusse des Mönchs befinden sich Alpweiden, auf welchen früher Wallache, sogenannte „Münche“, gesömmert wurden. So hat man den über den Münchenalpen gelegenen Berg Münchenberg genannt und schliesslich nur noch Münch oder Mönch.

 

Routen

 

Südarm des Ostgrates (Normalroute)

 

Schwierigkeit: ZS-, mit II. UIAA-Grad Felskletterei

Zeitaufwand: 2½–3½ Std. von der Mönchsjochhütte, 3–4 Std. vom Jungfraujoch

Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)

Talort: Grindelwald (1034 m ü. M.)

 

Südwestgrat

 

Schwierigkeit: ZS-, mit III-. UIAA-Grad Felskletterei

Zeitaufwand: 3–4 Stunden

Ausgangspunkt: Jungfraujoch (3454 m ü. M.)

Talort: Grindelwald (1034 m ü. M.)

 

Nordostarm des Ostgrates

 

Schwierigkeit: ZS, mit III+. UIAA-Grad Felskletterei

Zeitaufwand: 4–5 Stunden

Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)

Talort: Grindelwald (1034 m ü. M.)

 

Nordostgrat

 

Schwierigkeit: ZS

Zeitaufwand: 4–5 Stunden

Ausgangspunkt: Mönchsjochhütte (3657 m ü. M.)

Talort: Grindelwald (1034 m ü. M.)

 

Nordwestbollwerk (Nollen)

 

Schwierigkeit: S

Zeitaufwand: 6–10 Stunden

Ausgangspunkt: Guggihütte (2791 m ü. M.)

Talort: Kleine Scheidegg (2061 m ü. M.)

 

(Wikipedia)

 

Die Jungfrau ist ein Berg in der Schweiz. Sie ist mit 4158 m ü. M. der dritthöchste Berg der Berner Alpen und bildet zusammen mit Eiger und Mönch eine markante Dreiergruppe, ein sogenanntes «Dreigestirn».

 

Am 13. Dezember 2001 wurde die Jungfrau zusammen mit südlich angrenzenden Gebieten als Schweizer Alpen Jungfrau-Aletsch in die Liste als UNESCO-Weltnaturerbe aufgenommen.

 

Lage und Umgebung

 

Über den Jungfrau-Gipfel verläuft die Grenze zwischen den Kantonen Bern und Wallis. Der Berg ist ausserordentlich vielgestaltig. Im Norden und Nordwesten, auf ihrer „weiblichen“ Schauseite (vgl. Foto) sind ihr Wengen-Jungfrau, Schneehorn, das Silberhorn, das Chly Silberhoren und der „Schwarzmönch“ vorgelagert sowie die zerrissenen Kühlauenen- und Giessengletscher. Im Westen erhebt sie sich fast eisfrei volle 3250 Meter über dem hinteren Lauterbrunnental. Es ist dies (nach dem Mont Blanc) der zweithöchste direkte Abhang in den Alpen. Ihre Südwand erhebt sich über dem versteckten Rottalgletscher und ihre Ostwand über den Firnen am Jungfraujoch.

 

Die Pläne, auf die Jungfrau eine Bergbahn zu bauen, wurden aufgrund finanzieller Schwierigkeiten nicht realisiert. Die ursprünglich bis unter den Gipfel geplante Jungfraubahn wurde bis 1912 mit Endstation Jungfraujoch fertiggestellt.

 

Auf dem untersten Absatz des Nordostgrats haben die PTT einen Funk-Umsetzer auf 3777 m ü. M. installiert.

 

Geologie

 

Die Jungfrau liegt im nördlichen Randbereich des Aarmassivs, eines der sogenannten Zentralmassive der Schweizer Alpen. Ihre höheren Lagen (Silberhorn, Wengen-Jungfrau und Hauptgipfel) sowie ihre Westflanke bis hinunter zum oberen Ende des Lauterbrunnentals sind weit überwiegend aus kristallinem Grundgebirge (prä-triassische Gneise, Glimmerschiefer u. ä.) der Helvetischen Zone aufgebaut. Die Nordwestflanke hingegen, der ganze «Vorbau» (Schwarzmönch, Rotbrett und Schneehorn) besteht aus sedimentärem, überwiegend jurassischem und kretazischem Deckgebirge des Helvetikums. Eine Besonderheit der Jungfrau ist, dass dort zwischen dem prinzipiell autochthonen Gipfel-Kristallin und dessen Deckschichten ein Überschiebungs-kontakt besteht; somit ist das Grundgebirge geringfügig auf sein Deckgebirge überschoben worden.

 

Name

 

Der Name Jungfrau dürfte sich von der Wengernalp am Fusse des Berges ableiten, die – nach den Besitzerinnen, den Nonnen vom Kloster Interlaken – früher Jungfrauenberg genannt wurde. Einer anderen Quelle zufolge leitet sich der Name vom Aussehen des Nordhanges des Berges ab, der aus der Ferne dem Schleier eines Mädchens ähneln soll.

 

Nach dem Berg ist die Jungfrau-Region benannt, die Tourismusorganisation der Orte Grindelwald, Wengen, Mürren und Lauterbrunnen, ausserdem die Jungfraubahn Holding AG, die neben der Jungfraubahn selbst auch die anderen Bergbahnen in der Region betreibt.

 

Besteigungsgeschichte

 

Bergsteiger auf dem Gipfel im Jahr 1878

Erstbesteiger waren Johann Rudolf Meyer und sein Bruder Hieronymus mit den Führern Joseph Bortis und Alois Volken, die am 3. August 1811 vom Lötschental her den Berg von Süden erklommen hatten. Sie folgten ungefähr der heutigen Normalroute. Der Volksmund taufte daraufhin die bis dahin unberührte Jungfrau «Madame Meyer».

 

1874 erfolgte die Winter-Erstbesteigung durch die Alpinistin Margaret Claudia Brevoort.

 

Die Jungfrau gilt, obwohl leicht erreichbar, als unfallträchtiger Berg. Bei einem der schwersten Unglücke stürzten am 12. Juli 2007 sechs Rekruten der Gebirgsspezialisten-Rekrutenschule Andermatt vom Rottalsattel 1000 Meter auf den darunterliegenden Rottalgletscher in den Tod, nachdem sie eine Lawine ausgelöst hatten. Das urteilende Militärgericht ging von einem falsch eingeschätzten, heimtückischen Lawinenrisiko aus und sprach in der Folge die verantwortlichen Bergführer frei.

 

Routen

 

Rottalsattel und Südostgrat (Normalroute)

 

Schwierigkeit: ZS-

Zeitaufwand: 4–5 Std. von der Mönchsjochhütte, 3½–4½ Std. vom Jungfraujoch

Ausgangspunkt: Mönchsjochhütte (3657 m)

Talort: Grindelwald (1034 m)

 

Innere Rottalgrat

 

Schwierigkeit: ZS

Zeitaufwand: 6–7 Stunden

Ausgangspunkt: Rottalhütte (2755 m)

Talort: Stechelberg (919 m)

 

Nordwestgrat oder „Rotbrettgrat“

 

Schwierigkeit: S

Zeitaufwand: 8–12 Stunden

Ausgangspunkt: Silberhornhütte (2663 m)

Talort: Stechelberg (919 m)

 

Nordostgrat

 

Schwierigkeit: S+, mit IV. UIAA-Grad Felskletterei

Zeitaufwand: 8–10 Stunden

Ausgangspunkt: Jungfraujoch (3454 m)

Talort: Grindelwald (1034 m)

 

Kunst

 

Erwähnt ist die Jungfrau unter anderem bei Friedrich Schiller, Wilhelm Tell, Vers 628 (1804). Lord Byrons Drama Manfred (1817) spielt am Fuss und auf dem Gipfel des Massivs. Ferdinand Hodler hat die Jungfrau mehrfach gemalt, darunter die perspektivisch verfremdete «Jungfrau über dem Nebelmeer». Alex Diggelmann gab 1958 eine Lithographienmappe unter dem Titel Die Jungfrau, mein Berg heraus. Stephan Bundi gestaltete 2005 eine Schweizer Gedenkmünze mit dem Bergmotiv.

 

Im Januar 2012 wurde zum 100-jährigen bestehen der Jungfraubahn eine übergrosse Schweizer Flagge vom Lichtkünstler Gerry Hofstetter an den Gipfel projiziert. Zeitweise waren neben dem Schweizer Kreuz auch ein Porträt des Zürcher Unternehmers Adolf Guyer-Zeller sowie ein Bild von einem der Züge zu sehen.

 

(Wikipedia)

Whitley Bay is a seaside town in the North Tyneside borough in Tyne and Wear, England. It was formerly governed as part of Northumberland and has been part of Tyne and Wear since 1974. It is part of the wider Tyneside built-up area, being around 10 miles (16 km) east of Newcastle upon Tyne. Two notable landmarks are the Spanish City (a domed building on the seafront) and St. Mary's Lighthouse, the latter on a small island near the town.

 

Whitley was first mentioned around 1100 when King Henry I conferred it with other possessions on the Priory of Tynemouth being referred to in ancient documents and maps before that date as Witelei, Wyteley, Hwyteleg, Witelithe, Wheteley, Wytheleye, Whitlaw, Whitlathe and Whitlag. Whitley is also referred to in the charters of King Henry II, King Richard I and King John, confirming to the priors their possessions and liberties.

 

Whitley was connected with the Crusades when Pope Nicholas IV granted to Edward I the first-fruits and tenths of all ecclesiastical possessions for six years to defray the expenses of an expedition to the Holy Land. A valuation was made of the spiritual and temporal goods of the Priory on 26 March 1292, when the yearly rents from Whitley were returned as 20 shillings, and the tithes as 9 marks.

 

About the beginning of the 14th century, the manor of Whitley was held from the Prior of Tynemouth by a singular feudal service called the Conveyes which seems to have originated from John de Whitley. Richard de Emeldon, eighteen times Mayor of Newcastle and seven times its representative in Parliament, was the Lord of the Manor of Whitley in 1333.

 

On 9 April 1345, Edward III granted Gilbert de Whitley a licence to crenellate his manor house at Whitley. To crenellate a house was to place battlements on it. Before this could be done, the sanction of the Crown was often sought. Although battlements were often largely symbolic, in this instance it is probably an indication of the degree of insecurity felt even this far south during the Edwardian wars with Scotland. The licence and crenellations were an indication of status. Only 2% of the small tower houses of the sort Gilbert built had licences. The 'sanction' of the crown was a sought-after bonus, but not a requirement.

 

After the Dissolution of the Monasteries, Whitley was held under the Crown for a time. By a grant of Edward VI dated 8 December 1551, it came into the hands of Dudley, Earl of Warwick who was created Duke of Northumberland. It remained in the Percy family until 1632 after which time the area appeared to be let at a yearly rental to various holders until it came into the possession of the Duke of Somerset on his marriage in 1682 with Elizabeth, the heiress of Joscelyn, the 11th Earl of Northumberland. Whitley subsequently passed by inheritance to her granddaughter Elizabeth Seymour who had married Sir Hugh Smithson, a Yorkshire baronet, afterwards created Duke of Northumberland. Whitley has since been retained by descendants and the present Duke of Northumberland is the Lord of the Manor and principal landowner.

 

Monkseaton, which forms the greater part of the north west of the district, is also very old and its industries were common with those of Whitley being chiefly coalmining and limestone quarrying.

 

From the late 19th century and into the 20th century, the adverse effects of the decline of local coal mining and dependent industries in the area were ameliorated by the emergence of Whitley as a seaside holiday resort. The opening of the North Tyne Loop railway line in 1882, connecting the coastal villages to Newcastle, benefited the tourism industry. The line, now followed by the present Metro system, included a new railway station in the centre of the town, and another at Monkseaton. Both stations remain in use as Metro stations. Whitley Bay remains a popular holiday resort, with a caravan park operated by Parkdean Resorts for both holidaymakers and holiday home owners.

 

The parish church is St. Paul's Church. It was provided by the Duke of Northumberland when the parish of Tynemouth was divided in 1860 and it was consecrated in 1864.

 

The Whitley and Monkseaton Local Board was established in 1873. The district of the Local Board became the Urban District of Whitley and Monkseaton.

 

The town was known as Whitley until the 1890s, by which time confusion with Whitby, in North Yorkshire, regularly caused mail to be misdirected. The final straw came in September 1901 when a former resident died in Edinburgh and his body was to be buried in St Paul's churchyard, Whitley. Unfortunately, the body was mistakenly transported to Whitby, thereby delaying the funeral. When the council asked residents for suggestions of a new name, the most popular choice was Whitley Bay. Though since known officially as Whitley Bay, many residents still refer to the town as 'Whitley'.

 

On 1 January 1944, the Whitley and Monkseaton Urban District became the Whitley Bay Urban District and on 5 March 1954 it was granted a Royal Charter of Incorporation as the Borough of Whitley Bay. The charter was presented by The Princess Royal at a ceremony in the town on 14 April 1954.

 

The Local Government Act 1972 abolished the borough, with Hartley in the north of the borough becoming a part of Blyth Valley district in Northumberland, and the majority of the town including Whitley Bay and Monkseaton forming part of the Metropolitan Borough of North Tyneside in the Tyne and Wear area. The town is in the constituency of Tynemouth.

Cribyn is a notable peak in Wales' Brecon Beacons National Park, standing at 795 meters (2,608 feet). It's part of a prominent ridge that includes Pen y Fan and Corn Du. The mountain's steep northern and eastern faces result from glacial erosion during the last ice age. Popular walking routes, such as the Llanfrynach and Cribyn Circular Walk, provide scenic paths to the summit, showcasing the rugged beauty of the area.

 

View from Pen y Fan.

Oribi Loop

 

Burchell's Zebra

 

Steppenzebra

 

Golden Gate Highlands National Park is located in Free State, South Africa, near the Lesotho border. It covers an area of 340 km2 (130 sq mi). The park's most notable features are its golden, ochre, and orange-hued, deeply eroded sandstone cliffs and outcrops, especially the Brandwag rock. Another feature of the area is the numerous caves and shelters displaying San rock paintings. Wildlife featured at the park includes mongooses, eland, zebras, and over 100 bird species. It is the Free State's only national park, and is more famous for the beauty of its landscape than for its wildlife. Numerous paleontology finds have been made in the park, including dinosaur eggs and skeletons.

 

"Golden Gate" refers to the sandstone cliffs found on either side of the valley at the Golden Gate dam. In 1875, a farmer called J.N.R. van Reenen and his wife stopped here as they travelled to their new farm in Vuurland. He named the location "Golden Gate" when he saw the last rays of the setting sun fall on the cliffs.

 

In 1963, 47.92 km2 (11,840 acres) were proclaimed as a national park, specifically to preserve the scenic beauty of the area. In 1981, the park was enlarged to 62.41 km2 (15,420 acres), and in 1988, it was enlarged to 116.33 km2 (28,750 acres). In 2004, the park was announced to be joining with the neighbouring QwaQwa National Park. The amalgamation of QwaQwa National Park was completed in 2007, increasing the park's area to 340 km2 (84,000 acres).

 

The park is 320 km (200 mi) from Johannesburg and is close to the villages of Clarens and Kestell, in the upper regions of the Little Caledon River. The park is situated in the Rooiberge of the eastern Free State, in the foothills of the Maluti Mountains. The Caledon River forms the southern boundary of the park, as well as the border between the Free State and Lesotho. The highest peak in the park (and also in the Free State) is Ribbokkop at 2,829 m (9,281 ft) above sea level.

 

The park is located in the eastern highveld region of South Africa, and experiences a dry, sunny climate from June to August. It has showers, hail, and thunderstorms between October and April. It has thick snowfalls in the winter. The park has a relatively high rainfall of 800 mm (31 in) per year.

 

The park is an area of rich highveld and montane grassland flora. It has more than 60 grass species and a large variety of bulbs and herbs. Each of these species has its own flowering time, meaning that veld flowers can be seen throughout the summer. The park also has Afromontane forests and high-altitude Austro-Afro alpine grassland, which is scarce in South Africa. The ouhout (Leucosidea sericea), an evergreen species, is the most common tree in the park. Ouhout is a favourite habitat of beetles and 117 species occur on these trees in the park. The Lombardi poplars and weeping willows in the park are introduced species, but are kept because of their cultural and historic connection with the eastern Free State. Other exotic species in the park, for example wattle and bluegum, are systematically eradicated.

 

Instead of reintroducing one of the "big five" into the park, the sungazer lizard and water mongoose were reintroduced. Twelve species of mice, 10 species of carnivores, and 10 antelope species have been recorded in the park. The grey rhebuck and the mountain reedbuck were present when the park was established.

 

The geology of the park provides very visual "textbook" examples of Southern Africa's geological history. The sandstone formations in the park form the upper part of the Karoo Supergroup. These formations were deposited during a period of aeolian deposition towards the end of the Triassic Period. At the time of deposition, the climate of the area the park covers was becoming progressively drier until arid desert conditions set in, resulting in a land of dunes and sandy desert, with occasional scattered oases. The deposition of the sandstones ended when lava flowed out over the desert 190 million years ago.

 

The following sequence of geological formations is visible in the park (starting from the bottom): the Molteno Formation, Elliott Formation, Clarens Formation, and Drakensberg Formation. The yellow-brown Golden Gate and Brandwag cliffs are made up of the Clarens formation. The layers in this formation are 140 to 160 m (460 to 520 ft) thick. The Drakensberg formation comprises the basaltic lava that flowed over the desert. It forms the mountain summits in the park. On Ribbokkop, it is 600 m (2,000 ft) thick. The Elliot Formation is a red mudstone where many dinosaur fossils have been found.

 

The oldest dinosaur embryos ever discovered were found in the park in 1978. The eggs were from the Triassic Period (220 to 195 million years ago) and had fossilised foetal skeletons of Massospondylus, a prosauropod dinosaur. More examples of these eggs have since been found in the park. Other fossils found in the park include those of advanced cynodontia (canine toothed animals), small thecodontia (animals with teeth set firmly in the jaw), and bird-like and crocodile-like dinosaurs.

 

Accommodation in the park is available at Glen Reenen and Brandwag Rest camps. Caravan and camp sites with all amenities are available at Glen Reenen camp. The hotel was formerly part of Brandwag camp, but since its recent refurbishment, it is managed separately by SANParks as Golden Gate Hotel. The nearest town to Golden Gate Highlands National Park is Clarens (17 km to the west), but Phuthaditjhaba is also easily reached by a good tar road, driving through the access gate to the east of the park.

 

This park will be included into the Maloti-Drakensberg Transfrontier Conservation Area, Peace Park.

 

(Wikipedia)

 

Burchell's zebra (Equus quagga burchellii) is a southern subspecies of the plains zebra. It is named after the British explorer and naturalist William John Burchell. Common names include the bontequagga, Damaraland zebra, and Zululand zebra (Gray, 1824). Burchell's zebra is the only subspecies of zebra which may be legally farmed for human consumption.

 

Like most plains zebras, females and males are relatively the same size, standing 1.1 to 1.4 meters (3.75 to 4.6 feet) at the shoulder. They weigh between 485 to 550 pounds. Year-round reproduction observed in this subspecies in Etosha National Park, Namibia, concludes synchronization of a time budget between males and females, possibly explaining the lack of sexual dimorphism.

 

Damara zebras are described as being striped on the head, the neck, and the flanks, and sparsely down the upper segments of the limbs then fading to white. One or two shadow stripes rest between the bold, broad stripes on the haunch. This main, distinguishing characteristic sets the Zuzuland Zebra apart from the other subspecies. Gray (1824), observed a distinct dorsal line, the tail only bristly at the end, and the body distinctly white. The dorsal line is narrow and becomes gradually broader in the hinder part, distinctly margined with white on each side.

 

Like most plains zebras, Burchells live in small family groups. These can be either harem or bachelor groups, with harem groups consisting of one stallion and one to six mares and their most recent foals, and bachelor groups containing two to eight unattached stallions. The males in bachelor herds are often the younger or older stallions of the population, as they are most likely not experienced enough or strong enough to defend breeding rights to a group of females from challengers. These small groups often congregate together in larger herds around water and food sources, but still maintain their identity as family units while in the population gatherings.

 

Formerly, the Burchell's zebra range was centered north of the Vaal/Orange river system, extending northwest via southern Botswana to Etosha and the Kaokoveld, and southeast to Swaziland and KwaZulu-Natal. Now extinct in the middle portion, it survives at the northwestern and southeastern ends of the distribution.

 

Burchell's zebra migrates the longest distance of any terrestrial animal in Africa, traveling 160 miles one way. They migrate from the Chobe River in Namibia to Nxai Pan National Park in Botswana. Their migration follows a straight north–south route almost entirely within the Kavango–Zambezi Transfrontier Conservation Area (KAZA).

 

Like other plains zebras, Burchell's zebras must have populated the African plains in impressive numbers. Associations of thousands have been reported. The wild herds were thought to have disappeared by 1910, and the last known captive individual died in the Berlin Zoo in 1918. As European settlement spread northward from the Cape to colonial southern Rhodesia, this subspecies was thought to have been hunted to extinction.

 

However, Groves and Bell concluded in their 2004 publication that "the extinct true Burchell's zebra" is a phantom. Careful study of the original zebra populations in Zululand and Swaziland, and of skins harvested on game farms in Zululand and Natal, has revealed that a certain small proportion shows similarity to what now is regarded as typical burchellii. The type localities of the two subspecies Equus quagga burchellii (Burchell's zebra) and Equus quagga antiquorum (Damaraland zebra) are so close to each other that they suggest that the two are in fact one, and therefore the older of the two names should take precedence over the younger. They therefore say that the correct name for the southernmost subspecies must be burchellii, not antiquorum.[9] The subspecies Equus quagga burchellii still exists in KwaZulu-Natal and in Etosha. Equus quagga burchellii can be found in a number of zoos in the United States including the following: the Cincinnati Zoo, Columbus Zoo, Naples Zoo, Nashville Zoo, Woodland Park Zoo, etc.

 

(Wikipedia)

 

Der Golden-Gate-Highlands-Nationalpark (englisch Golden Gate Highlands National Park) liegt in Südafrika, im Südosten des Freistaates nahe der Grenze zu Lesotho, und zeichnet sich besonders durch seine malerischen Felslandschaften aus. Orange oder ocker gefärbte Sandsteinfelsen ragen über das bergige Grasland auf. Außerdem gibt es Felsmalereien der San.

 

Der nördliche Eingang zum Park liegt bei dem Künstlerdorf Clarens.

 

(Wikipedia)

 

Das Steppenzebra (Equus quagga) oder Pferdezebra ist ein Zebra aus der Familie der Pferde (Equidae) und gehört zur Ordnung der Unpaarhufer (Perissodactyla). Es stellt heute die häufigste Zebra-Art in Afrika dar und ist vom Nordosten bis in den Süden des Kontinents verbreitet. Es lebt gesellig in kleinen Herdenverbänden und ernährt sich hauptsächlich von Gräsern. Im Gegensatz zu den anderen heutigen Pferdearten kommt es auch in teilweise geschlossenen Landschaften vor. Der Bestand, dessen größte Population heute in der Serengeti lebt, gilt als nicht gefährdet. Es werden sechs rezente Unterarten unterschieden, die sich meistens deutlich in der Streifenzeichnung voneinander abheben.

 

(Wikipedia)

Restormel Castle lies by the River Fowey near Lostwithiel in Cornwall, England, UK. It is one of the four chief Norman castles of Cornwall, the others being Launceston, Tintagel and Trematon. The castle is notable for its perfectly circular design. Although once a luxurious residence of the Earl of Cornwall, the castle was all but ruined by the 16th century. It was briefly reoccupied and fought over during the English Civil War but was subsequently abandoned. Now in the care of English Heritage, it is open to the public.

Situated in the upper reaches of Himalayan Mountain range in Leh district of Jammu and Kashmir, the most notable feature of the lake is the ever changing hues of the lake.

 

Situated at a height of about 13,900 ft, the name Pangong is a derivative of the Tibetan word Banggong Co meaning "long, narrow, enchanted lake". One third of the lake is in India while the remaining two thirds lies in Tibet, which is controlled by China. Majority of the streams which fill the lake are located on the Tibetan side.

 

Pangong Tso is about five hours drive from Leh in Ladakh region of Jammu & Kashmir. The route passes through beautiful Ladakh countryside, over Chang La, the third highest motorable mountain pass (5289 m) in the world.

 

The first glimpse of the serene, bright blue waters is the most amazing experience.

During winter the lake freezes completely, despite being saline This slat water, beautiful ocean like lake is about 5 KM wide at its broadest point and about 134 KM long with about 60% of the length extending into Tibet. During winters the lake freezes completely, which itself is a great experience to witness if you have seen the other colors of the lake. Being very near to the Line of Actual Control, one need to get Inner Line Permit to visit Pangong Tso.The beautiful multi shades of blue color offered by this lake along with a picturesque landscape around gives this place a stunning look.

 

This place is a must to see if you ever visit Leh. They even provide camping options as well as home stays in case one plans to spend a night out there.

Early newspaper articles capture notable events around Ouray. Most descriptions of the history of Ouray describe a town that was the center of mining and society in an area of vast mineral wealth. It is easy to forget that the town was still part of the Wild West, and was sometimes subject to the same lawlessness that impacted many frontier towns.

 

June 25, 1897 A MOST DARING ROBBERY

Ora Jones and an unknown companion entered Chase’s saloon today and after drinking leveled the guns at the customers, picked up sacks containing five hundred dollars, and escaped on horses.

 

October 3, 1899 - A STAGE STOPPED - ROBBERS OVERLOOKED A BOX FILLED WITH BULLION

Two masked men stopped the Sneffels' stage one mile this side of the Camp Bird mills, eight miles from Ouray this afternoon. They were after the daily shipment of gold bullion from the Camp Bird mine, and unloaded the mail and baggage looking for it. However, they overlooked the box containing $12,000 worth of gold, representing two days' production of the mine.

The mails were left untouched and the passengers were not molested. Sheriff Edgar was notified, and, with a posse, overtook the holdups near Yankee Boy basin. After a brisk exchange of shots the officers retired to secure reinforcements. Several other parties are in pursuit.

 

July 30, 1910 - FINANCIER WITH REVOLVER ROUTS STAGE ROBBERS

An attempt to hold up a stage coach of eight easterners was frustrated last night by the coolness and nerve of Samuel McCurdy of Pittsburg, a retired financier, who opened fire with an automatic pistol.

The party was returning from an outing in the mountains in an old-fashioned stage coach driven by A.L. Stewart, a veteran stage driver, when two bandits stepped into the road and ordered Stewart to stop.

 

February 27, 1921 - ANGRY MINERS TRY TO LYNCH MURDERER

A mob of more than 200 miners smashed down the door to the Ouray county jail at Ouray, Colorado, last night and Invaded the jail in an attempt to lynch Billy Nagle, a miner, who had confessed, according to the sheriff, that he had killed Fred Jacobs, superintendent of the White Cloud mine at Ironton and Hindmarch Hill.

Nogle had been removed from the jail by Sheriff Roy Laird a short time before, smuggled through a coal chute, and brought to Montrose in an automobile.

  

Syracuse is a historic city in Sicily, the capital of the province of Syracuse. The city is notable for its rich Greek history, culture, amphitheatres, architecture, and as the birthplace of the preeminent mathematician and engineer Archimedes. This 2,700-year-old city played a key role in ancient times, when it was one of the major powers of the Mediterranean world. Syracuse is located in the southeast corner of the island of Sicily, right by the Gulf of Syracuse next to the Ionian Sea.

 

The city was founded by Ancient Greek Corinthians and Teneans and became a very powerful city-state. Syracuse was allied with Sparta and Corinth and exerted influence over the entirety of Magna Graecia, of which it was the most important city. Described by Cicero as "the greatest Greek city and the most beautiful of them all", it equaled Athens in size during the fifth century BC. It later became part of the Roman Republic and Byzantine Empire. After this Palermo overtook it in importance, as the capital of the Kingdom of Sicily. Eventually the kingdom would be united with the Kingdom of Naples to form the Two Sicilies until the Italian unification of 1860.

 

In the modern day, the city is listed by UNESCO as a World Heritage Site along with the Necropolis of Pantalica. In the central area, the city itself has a population of around 125,000 people. The inhabitants are known as Siracusans. Syracuse is mentioned in the Bible in the Acts of the Apostles book at 28:12 as Paul stayed there.

 

Perfection notable

The Basilica of San Michele Maggiore is a church of Pavia, one of the most striking example of Lombard-Romanesque style. It dates from the 11th and 12th centuries.

A first church devoted to St. Michael Archangel was built, at the desire of King Grimoald between 662 and 671, on the location of the Lombard Palace chapel (to this period belongs the lower section of the bell tower), but it was destroyed by a fire in 1004. Recent archeological evidence shows pre-Lombard origins of the basilica from the fifth century, like the Ostrogoth silverware found in 1968 and now preserved in the Pavia Civic Museums. The current construction was begun in the late 11th century (crypt, choir and transept) and was completed by 1130. The vaults of the nave, originally with two grossly squared groin-vaulted spans, were replaced in 1489 by the design of master architect Agostino de Candia in four rectangular spans, and the structure was created by his father the renown Pavia master mason Iacopo da Candia.

The basilica was the seat of numerous important events, including the coronations of Berengar I (888), Guy III (889), Louis III (900), Rudolph II (922), Hugh (926), Berengar II and his son Adalbert (950), Arduin (1002), Henry II (1004) and Frederick Barbarossa (1155).[4]

San Michele Maggiore can be considered the prototype of other important medieval churches in Pavia such as San Pietro in Ciel d'Oro and San Teodoro. However, it differentiates from latter in the use of sandstone instead of bricks, and for the Latin cross plan with a nave and two aisles and a much-extended transept. San Michele's transept, provided with a true façade, a false apse and a barrel vault different from the rest of the church, constitutes a nearly independent section of the edifice. Also, its length (38 m, compared to the 55 m of the whole basilica), contributes to this impression.

At the crossing of nave and transept is the octagonal dome, a 30 m-high asymmetrical structure supported on squinches, in the Lombard-Romanesque style. It is reportedly the earliest example of this form in Lombardy. The façade is decorated by numerous sandstone sculptures, of religious or profane themes; they are however now much deteriorated. The façade has five double and two single mullioned windows and a cross, which are a 19th-century reconstruction of what was thought be the original scheme. Bas reliefs in horizontal bands portray human, animal and fantastic figures. Over the minor portals are portrayed St. Ennodius, bishop of Pavia, and St. Eleucadius, archbishop of Ravenna. In the lunettes are angels which, according to a caption sculpted there, have the role of ambassadors of the faithful's words into heaven.Bronze doors, coloured mosaics, geometric designs, bronze pilasters.

The nave has four spans. The aisles have matronaea with statical function. The four chapels in correspondence of the second and four spans of the aisles are a later addition. under the apse, which has a large 16th-century fresco, is the high altar (1383) housing the remains of Sts. Ennodius and Eleucadius. The presbytery has fragments of a notable pavement mosaic with the Labours of the Months and mythological themes.In the transept there is a crucifix in silver leaf, just over 2 m high and commissioned by the abbess of the monastery of Santa Maria Teodote Raingarda in the second half of the 10th century, it arrived in the basilica of San Michele after the suppression of the monastery in 1799.

The cross of the Abbess Raingarda, 10th century.

Altar of the Virgin: the altarpiece, depicting the Virgin between Saints Rocco and Sebastian was executed by Guglielmo Caccia in 1601. In the left arm of the transept there is the altar of Santa Lucia, whose altarpiece, depicting the martyrdom of the saint, is the work of Guglielmo Caccia and the baroque altar of Sant'Anna, rich in Baroque stucco, which houses a painting representing the Virgin and Child, St. Joseph and St. Anne by the Novara painter Pietro Antonio de Pietri. The crypt, with a nave and two aisles, is located immediately under the altar: it houses beautifully decorated capitals and the monument of the Blessed Martino Salimbene (1491).

 

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We're Here! : *Umbrella*

 

Running out of ideas for your 365 project? Join We're Here!

 

Strobist: AB1600 with 60X30 softbox behind umbrella. AB800 with Softlighter II camera left. Triggered by Cybersync.

 

View Large and on Black

  

It would have been perfect without the giant cruise ships in the harbor.

  

Notable residents from Wikipedia

King Richard I of England (1157-1199), in 1190[11]

Pope Gregory XI (1330-1378), in 1377

Henry Herbert (1831-1890), British Politician

Guy de Maupassant (1850-1893), French writer

Guglielmo Marconi (1874-1937), Italian engineer, inventor of radio

Giuseppe Amisani (1879-1941), Italian painter

Michele Cascella (1892-1989), Italian painter

Rex Harrison (1908-1990), American actor

Lilli Palmer (1914-1986), German actress, wife of Rex Harrison

 

en.wikipedia.org/wiki/Portofino

 

Follow me in Instagram. I'm a newbie out there. www.instagram.com/juliasumangil/

 

Italien / Piemont - Nationalpark Val Grande

 

On the way from the Capella Fina to the Rifugio Pian Cavallone.

 

Auf dem Weg von der Capella Fina zum Rifugio Pian Cavallone.

 

Val Grande National Park (Italian: Parco Nazionale della Val Grande) is a protected area located in Piedmont, in the north of Italy, at the border with Switzerland. It is most notable for landscapes of the High Alps.

 

Geography

 

The park is located in Province of Verbano-Cusio-Ossola and is shared between ten municipalities: Aurano, Beura-Cardezza, Caprezzo, Cossogno, Valle Cannobina, Intragna, Malesco, Miazzina, Premosello-Chiovenda, San Bernardino Verbano, Santa Maria Maggiore, Trontano, and Vogogna.

 

The park lies entirely in the drainage basin of the Po River. It is located between the valley of Vigezzo in the north, the Cannobina valley in the northwest, the valley of Ossola in the southwest, and Lake Maggiore in the southeast. The park is not populated and is often described as "the largest wilderness in the Alps"

 

Val Grande and Val Pogallo, two principal valleys inside the park, with the former running southeast and the latter running south, feed the two major rivers in the park. These valleys join into Torrente San Bernardino, a tributary of Lake Maggiore. The majority of the area of the park is forested.

 

History

 

Shepherds populated Val Grande since at least the 13th century, and the timber production was active since the 15th century. However, at the end of World War II all population left the area, following the actions of German troops against the Italian resistance in the area in June 1944. The idea to create a national park in Val Grande dates back to 1953. In 1967, the area was designated a Strict Nature Reserve and became the first conservation area with this status in the Italian Alps. In 1974, the Association Italia Nostra developed a detailed plan to establish a national park, and, in the 1980s, the preparation started. The park was established on March 2, 1992. On June 24, 1998 the area of the park was extended.

 

Tourism

 

As of 2012, the park had three visitor centers (located in Santa Maria Maggiore, Cossogno, and Premosello-Chiovenda), two museums, and a number of nature itineraries, which should be followed accompanied by a guide.

 

(Wikipedia)

 

Der Nationalpark Val Grande (italienisch Parco nazionale della Val Grande) ist ein Nationalpark in den norditalienischen Alpen, nahe der Schweiz. Er liegt zwischen dem Lago Maggiore und dem Val d’Ossola in der piemontesischen Provinz Verbano-Cusio-Ossola und ist 146 km² groß.

 

Im westlichen Teil des Parks liegt seine namengebende Kernzone, das schwer zugängliche Val Grande. Der östliche Teil besteht aus dem offeneren Val Pogallo und einigen angrenzenden Gebieten.

 

Das Gebiet des Felsenmassivs Pedum wurde 1967 zur Riserva naturale integrale (Totalreservat) erklärt. Nach mehreren Initiativen lokaler Gruppen und des Umweltministers in den 1980er Jahren wurde schließlich 1992 der Parco Nazionale della Valgrande geschaffen.

 

Die einzigen Ortschaften im Nationalpark sind Cicogna im Val Pogallo und Colloro am südwestlichen Rand des Parks. Der größte Teil des Nationalparks war nie ganzjährig bewohnt. Es wurde jedoch intensive Almwirtschaft betrieben, bis in die 1950er Jahre auch Waldwirtschaft. Nach dem Zweiten Weltkrieg wurden bis in die 1970er Jahre sämtliche Almen aufgegeben, im Val Grande selbst bis 1969. Nachdem der Verbiss durch die Weidetiere fehlt, wandeln sich die ehemaligen Almen allmählich zur Wildnis.

 

Erst nach Gründung des Nationalparks begann ein bescheidener Tourismus. Abgesehen von etlichen frei zugänglichen Steinhäusern ist kaum touristische Infrastruktur vorhanden. Außer den Zufahrten nach Cicogna und Colloro existieren keine ausgebauten Straßen.

 

Geographie

 

Val Grande

 

Das Val Grande ist etwa 25 Kilometer lang, der größte Teil davon ist unbewohnt und liegt im Nationalpark Val Grande (Parco Nazionale della Valgrande). Der Hauptfluss des Val Grande ist der Torrente San Bernardino, er entspringt am Monte Togano (2301 m s.l.m.) und fließt in Intra/Verbania in den Lago Maggiore (193 m s.l.m.). Sieben stark bewaldete und ursprüngliche Seitentäler bilden den oberen Teil des Val Grande. Mancherorts finden sich noch Überreste der einstigen Alpwirtschaft.

 

Im Zentrum des oberen Val Grande steht der Pizzo Mottac (1802 m s.l.m.). An dessen Fuß liegen die Alpen In La Piana und Gabbio. Der mittlere Bereich ist eine wilde Schlucht ohne Wanderweg. Steile Wälder und Felsbänder prägen diesen Abschnitt. Der unterste Teil des Val Grande ist ab Ponte Casletto mit einer schmalen Straße, die nach Cicogna führt, erschlossen. Darin liegen die Ortschaften Rovegro, Cossogno, Santino, Unchio und Trobaso.

 

Das Val Grande gilt als das größte Wildnisgebiet im Alpenraum.

 

Die Vegetation besteht in den Tälern aus Kastanien- und Buchenwäldern. Bis 1800 m s.l.m. reicht dichter Bewuchs. Darüber findet sich Grasheide mit Erlensträuchern in geschützten Lagen.

 

Die Seitentäler des oberen Val Grande heißen Val Gabbio, Val Serena, Valle Rossa, Val Ragozzale, Val Portaiola, Val Biordo und Vallone di Loc. Im mittleren Val Grande heißen die Seitentäler Val Fredda, Val Piana und Val Cauri.

 

Val Pogallo

 

Beim Ponte Casletto treffen sich Val Pogallo und Val Grande. Das Val Pogallo ist bewohnt und besser erschlossen. Zur Blütezeit der Holzwirtschaft wurde ein teils mit großen Steinplatten sehr gut ausgebauter Weg von Cicogna aus erbaut. Dieser Weg wurde später nach dem Gründer der Holzgesellschaft und vielseitigen Industriellen Carlo Sutermeister benannt und wird als Strada Sutermeister bezeichnet. Gerne nutzen ihn als einen der schönsten leichten Wege Wanderer von Cicogna aus. Das einstige Holzfällerdorf Pogallo war zwischenzeitlich komplett verfallen. Nach und nach wurden viele der Steinhäuser wieder instand gesetzt. Mitglieder des Vereines Associazzione Amici di Pogallo pflegen das Dorf, das von Cicogna aus über eine 1,5 Stunden lange Wanderung erreichbar ist. Der Weg ist ein Sentiero Natura mit Infotafeln des Nationalparkes und führt auch an einer Badestelle vorbei.

 

Geschichte

 

Zur Römerzeit scheint das Val Grande besiedelt gewesen zu sein. Ab dem 13. Jahrhundert begannen die Bewohner der umliegenden Täler die Alpwirtschaft auf das Val Grande auszudehnen.

 

Mit der Industrialisierung ergab sich eine Abwanderung aus den Bergtälern und die Alpwirtschaft wurde bereits stellenweise aufgegeben. Im Val Grande wurde 1969 die letzte Alp der Natur überlassen.

 

Im mittleren und unteren Val Grande hinterließ die Holzwirtschaft in der ersten Hälfte des 20. Jahrhunderts ihre Spuren, als ein verzweigtes Netz von Seilbahnen errichtet wurde. In dieser Zeit wurden in Pogallo, Orfalecchio, Arca und an anderen Orten Wohn- und Wirtschaftsgebäude errichtet.

 

Während des Zweiten Weltkriegs gründeten antifaschistische Partisanen die Repubblica dell’Ossola. Nachdem alliierte Truppen bereits Rom eingenommen hatten, wurden die Partisanen von Soldaten Mussolinis und der deutschen Wehrmacht vertrieben und zogen sich ins Gebiet des Val Grande zurück. Im Juli 1944 unternahm die deutsche SS mit Einheiten der faschistischen Repubblica Sociale Italiana eine Durchkämmung (Rastrellamento), um gegen Kämpfer der Resistenza in den Bergen vorzugehen. Dabei wurden ca. 500 Menschen getötet. Darunter wurden viele Opfer grausamer Hinrichtungen der Faschisten.

 

Wie die Zeitzeugin Antonietta Chiovini berichtete, wurden auf dem kargen Gipfel bei der Kapelle von Marona von der Waffen-SS zwölf Partisanen gestellt, die den Feind von der eigenen Brigade ablenken wollten. Um Munition zu sparen, wurden die jungen Männer halbtot geschlagen, bevor sie den Abhang hinunter gestoßen wurden.

 

Beim Beschuss der Bergsiedlungen wurden viele Gebäude und die zum Abtransport gefällter Bäume dienenden Seilbahnen zerstört. Der Verlust der Infrastruktur trug zum Rückzug des Menschen aus dem Gebiet um das Val Grande bei.

 

Wanderrouten

 

Im oberen Teil existiert ein gut ausgebauter und markierter Weg von Malesco über die Alpe Scaredi, In La Piana, Gabbio und Alpe della Colma nach Premosello (in diesen erwähnten Alpen stehen kostenlose und sehr einfach eingerichtete Hütten zur Verfügung). Abseits dieser Route gibt es nur wenige und schlechter erkennbare markierte Wege. Die meisten alten Pfade sind verschwunden. Mobilfunkempfang gibt es fast im gesamten oberen Val Grande nicht.

 

(Wikipedia)

"St. Peter Cathedral is a large Roman Catholic cathedral located on Baraga Avenue in Marquette, Michigan. As the mother church of the Diocese of Marquette, it is one of the most notable marks of Catholic presence in the Upper Peninsula. The cathedral was listed on the National Register of Historic Places in 2012.

 

The current church is nothing like it first was, when a Jesuit priest named Father Jean-Baptiste Menet began holding services on the site in a small log cabin. Upon Bishop Frederic Baraga’s visit to the site, it was determined that a larger, more prominent church should be built, and that eventually the see should be moved to Marquette from Sault Ste. Marie. Construction began in 1864, with Baraga himself laying the cornerstone. Two years later he dedicated the building, but he did not live to see his beloved cathedral catch fire.

 

Some have suggested that this first fire, on October 2, 1879, was caused by Irish arsonists who were enraged that Father John Kenny had been removed as pastor. Though the building was destroyed, the congregation's resolve was fervent as ever, and plans were made to continue meeting in the basement before a new cathedral could be erected. It took nine winters to complete the new building.

 

The church also faced another tragic fire which destroyed everything except the sandstone walls: a few minutes after four a.m. on November 3, 1935, the building again erupted in flames. The parish celebrated Mass in high school auditorium for several months until the cathedral could be restored.

 

Extensive work and money was put into its reconstruction and beautification, including elaborate marble work and Romanesque columns, as well as an extended nave and domes on the tops of the steeples. This church is one of around 200, including at least three other cathedrals, that incorporates the work of architectural sculptor Corrado Parducci.

 

Marquette (/mɑːrˈkɛt/ mar-KEHT) is a city in Marquette County in the U.S. state of Michigan. The population was 20,629 at the 2020 United States Census, which makes it the largest city in the Upper Peninsula. It also serves as the county seat of Marquette County. Located on the shores of Lake Superior, the city is a major port, known primarily for shipping iron ore. The city is partially surrounded by Marquette Charter Township, but the two are administered autonomously.

 

Marquette is the home of Northern Michigan University. In 2012, Marquette was listed among the 10 best places to retire in the United States by CBS MoneyWatch.

 

The land around Marquette was known to French missionaries of the early 17th century and the trappers of the early 19th century. Development of the area did not begin until 1844, when William Burt and Jacob Houghton (the brother of geologist Douglass Houghton) discovered iron deposits near Teal Lake west of Marquette. In 1845, Jackson Mining Company, the first organized mining company in the region, was formed.

 

The village of Marquette began on September 14, 1849, with the formation of a second iron concern, the Marquette Iron Company. Three men participated in organizing the firm: Robert J. Graveraet, who had prospected the region for ore; Edward Clark, agent for Waterman A. Fisher of Worcester, Massachusetts, who financed the company, and Amos Rogers Harlow. The village was at first called New Worcester, with Harlow as the first postmaster. On August 21, 1850, the name was changed to honor Jacques Marquette, the French Jesuit missionary who had explored the region. A second post office, named Carp River, was opened on October 13, 1851 by Peter White, who had gone there with Graveraet at age 18. Harlow closed his post office in August 1852. The Marquette Iron Company failed, while its successor, the Cleveland Iron Mining Company, flourished and had the village platted in 1854. The plat was recorded by Peter White. White's office was renamed as Marquette in April 1856, and the village was incorporated in 1859. It was incorporated as a city in 1871.

 

During the 1850s, Marquette was linked by rail to numerous mines and became the leading shipping center of the Upper Peninsula. The first ore pocket dock, designed by an early town leader, John Burt, was built by the Cleveland Iron Mining Company in 1859. By 1862, the city had a population of over 1,600 and a soaring economy.

 

In the late 19th century, during the height of iron mining, Marquette became nationally known as a summer haven. Visitors brought in by Great Lakes passenger steamships filled the city's hotels and resorts.

 

South of the city, K. I. Sawyer Air Force Base was an important Air Force installation during the Cold War, host to B-52H bombers and KC-135 tankers of the Strategic Air Command, as well as a fighter interceptor squadron. The base closed in September 1995, and is now the county's Sawyer International Airport.

 

Marquette continues to be a shipping port for hematite ores and, today, enriched iron ore pellets, from nearby mines and pelletizing plants. About 7.9 million gross tons of pelletized iron ore passed through Marquette's Presque Isle Harbor in 2005.

 

The Roman Catholic Bishop Frederic Baraga is buried at St. Peter Cathedral, which is the center for the Diocese of Marquette.

 

Lakeview Arena, an ice hockey rink in Marquette won the Kraft Hockeyville USA contest on April 30, 2016. The arena received $150,000 in upgrades, and hosted the Buffalo Sabres and Carolina Hurricanes on October 4, 2016 in a preseason NHL contest. Buffalo won the game 2-0." - info from Wikipedia.

 

Now on Instagram.

Notable red rock landscape seen from the Brin Mesa Trail in rural Sedona, northern Arizona.

BR Class 455/8 unit 5812 at London Victoria, forming a Central Division service. Also notable in this March 22nd 1985 scene are 73128 heading a VSOE charter train, Class 411 unit 1585, and Class 421/1 unit 7329. A Gatwick Express Class 73/1 is also visible on the left under the overall roof. Unit 5812 was allocated to Wimbledon depot at this time, before its transfer to Selhurst depot in 1986. The Class 455/8s were built between 1982 and 1984 by British Rail Engineering Ltd.'s Holgate Road, York, carriage works. They eventually replaced those 4-SUB and 4-EPB units still remaining in service. Additionally, the Class 508 units, placed on loan from new, were subsequently cascaded to the Merseyrail system, with one TSO from each 4-car unit being retained and reformed into the new Class 455/7 units introduced in 1984, distinctive by their lower roof profiling. During privatisation, 5812 was taken over by Connex South Central in October 1996, and Southern from August 2001, after which 'mid-life' refurbishments eventually took place between 2004-2006. The last Southern Class 455/8s were taken out of service in May 2022. Unit 5812 was one of the last units to be despatched for scrap, at Sims Metals, Newport Docks, being dragged there by GBRf 66726, along with unit 5836, on 11th August 2022, just three months after its final day in traffic.

 

© Gordon Edgar - All rights reserved. Please do not use my images without my explicit permission

As seen at the State Library of NSW.

One of the most notable historic landmarks in Cincinnati is the Carew Tower, which is a part of a larger complex that fills almost the entire block between 4th Street, 5th Street, Vine Street, and Race Street in Downtown Cincinnati. Constructed between 1927 and 1930, the Art Deco-Style complex was designed by the firms W.W. Ahlschlager & Associates and Delano & Aldrich, and was developed by John J. Emery to replace the old Mabley & Carew Department Store and the Hotel Emery, and provide high-quality hotel accommodation, as well as top-notch office space in downtown. The complex includes the 49-floor, 574-foot (175 meter)-tall Carew Tower, which was the city’s tallest building from 1930 until 2010, and the Cincinnati Hilton Netherland Plaza Hotel, one of the finest accommodations in the city. The building is considered to be a prototype for large-scale mixed-use development as was later seen with Rockefeller Center in New York City, as well as the basis for the design of the Empire State Building. The tower features the city’s most notable observation deck atop the 49th floor, which allows for spectacular views of the city, the Ohio River, and Northern Kentucky. The complex features ornate Art Deco ornamentation throughout, most notably around the entryways, in the Palm Court, Lobby, and Continental Room of the Hotel, and the lobby of the tower. The complex originally included a third tower with an advanced mechanical automated car storage system, something unseen and unheard of today outside of the world’s largest cities, which later fell out of favor as self-service parking garages were built in the mid-20th Century, eventually being demolished in 1980. Today, the Carew Tower and Netherland Plaza Hotel are listed as National Historic Landmarks, owing to their artistic merit, design, and history, having been designated in 1994. The complex is one of twelve national historic landmarks in the city, and is one of the city’s most significant places.

The chapter house is notable for its octagonal shape, slender central pillar and decorative medieval frieze. It was redecorated in 1855-9 by William Burges. The frieze circles the interior above the stalls and depicts scenes and stories from the books of Genesis and Exodus, including Adam and Eve, Noah, the Tower of Babel, and Abraham, Isaac and Jacob. (Wikipedia)

Nikon 1 V2

INSTRUCTIONS AVAILABLE TO BUILD THIS MODEL AND OTHER CITROEN TA VERSIONS

 

The Citroen Traction Avant is notable for being one of the singularly most innovative cars in history. Unfortunately it is overshadowed in this respect by its immediate successor, the equally innovative Citroen DS - a car with arguably more radical appearance.

 

The Traction Avant, as the name implies, was one of the very first front wheel drive (FWD) vehicles. Not the very first, but the vehicle that largely popularised the configuration to the marketplace.

 

The configuration placed the engine inline, behind the front axle, with the gearbox ahead of the axle (this layout was also used on the Citroen DS and Renault R4, R16 and first generation R5).

 

The Traction Avant was also one of the first monocoque (or unibody) cars - a method which allowed mass reduction and a lowering of the vehicle profile.

 

The Traction Avant was first launched in 1934 in the 7CV and 11CV taxation classes with 4-cylinder engines. Over time further versions were added. Long wheelbase, Wagon, convertible and Coupe bodystyles. Six-cylinder, and prototype V8-engine editions.

 

Distant Heavily Cropped Shot

Pectoral Sandpiper PESA (Calidris melanotos)

 

Maber Flats

Saanichton Peninsula BC

ebird.org/checklist/S105933454

 

DSCN1757

According to info available on ebird - VERY Early

 

1st record of a PESA in March for all of British Columbia or other Western- Alberta, Saskatchewan, Manitoba [any province or portion of Canada going west until Southern Ontario]

 

No previous record of a PESA in the month of April for Greater Victoria

 

And only 2 previous records for April for Vancouver Island closer to (almost) a month later

 

28th Apr 1998 (1)

& 25th Apr 2015 (2)

ebird.org/checklist/S27440456

ebird.org/canada/checklist/S40094698

  

****

Other note:

We here in Victoria area usually get low numbers of this species in the spring compared to than in the fall

Bupaya Pagoda is a notable pagoda located in Bagan (formerly Pagan), in Myanmar, at a bend on the right bank of the Ayeyarwady River. The small pagoda, which has a bulbous shaped dome, is widely believed to have been built by the third King of Pagan, Pyusawhti who ruled from 168 to 243 AD. It is one of the most notable shrines among the thousands of new or ruined Pagodas in Pagan, which is located about 90 miles (140 km) south of Mandalay.

The Alhambra is a palace and fortress complex located in Granada, Andalusia, Spain. It is one of the most famous monuments of Islamic architecture and one of the best-preserved palaces of the historic Islamic world, in addition to containing notable examples of Spanish Renaissance architecture.

The complex was begun in 1238 by Muhammad I Ibn al-Ahmar, the first Nasrid emir and founder of the Emirate of Granada, the last Muslim state of Al-Andalus. It was built on the Sabika hill, an outcrop of the Sierra Nevada which had been the site of earlier fortresses and of the 11th-century palace of Samuel ibn Naghrillah. Later Nasrid rulers continuously modified the site. The most significant construction campaigns, which gave the royal palaces much of their definitive character, took place in the 14th century during the reigns of Yusuf I and Muhammad V. After the conclusion of the Christian Reconquista in 1492, the site became the Royal Court of Ferdinand and Isabella (where Christopher Columbus received royal endorsement for his expedition), and the palaces were partially altered. In 1526, Charles V commissioned a new Renaissance-style palace in direct juxtaposition with the Nasrid palaces, but it was left uncompleted in the early 17th century. After being allowed to fall into disrepair for centuries, with its buildings occupied by squatters, the Alhambra was rediscovered following the defeat of Napoleon I, whose troops destroyed parts of the site. The rediscoverers were first British intellectuals and then other American and Northern European Romantic travelers. The most influential of them was Washington Irving, whose Tales of the Alhambra (1832) brought international attention to the site. The Alhambra was one of the first Islamic monuments to become the object of modern scientific study and has been the subject of numerous restorations since the 19th century. It is now one of Spain's major tourist attractions and a UNESCO World Heritage Site.

During the Nasrid era, the Alhambra was a self-contained city separate from the rest of Granada below. It contained most of the amenities of a Muslim city such as a Friday mosque, hammams (public baths), roads, houses, artisan workshops, a tannery, and a sophisticated water supply system. As a royal city and citadel, it contained at least six major palaces, most of them located along the northern edge where they commanded views over the Albaicín quarter. The most famous and best-preserved are the Mexuar, the Comares Palace, the Palace of the Lions, and the Partal Palace, which form the main attraction to visitors today. The other palaces are known from historical sources and from modern excavations. At the Alhambra's western tip is the Alcazaba fortress. Multiple smaller towers and fortified gates are also located along the Alhambra's walls. Outside the Alhambra walls and located nearby to the east is the Generalife, a former Nasrid country estate and summer palace accompanied by historic orchards and modern landscaped gardens.

The architecture of the Nasrid palaces reflects the tradition of Moorish architecture developed over previous centuries. It is characterized by the use of the courtyard as a central space and basic unit around which other halls and rooms were organized. Courtyards typically had water features at their center, such as a reflective pool or a fountain. Decoration was focused on the inside of the building and was executed primarily with tile mosaics on lower walls and carved stucco on the upper walls. Geometric patterns, vegetal motifs, and Arabic inscriptions were the main types of decorative motifs. Additionally, "stalactite"-like sculpting, known as muqarnas, was used for three-dimensional features like vaulted ceilings.

The evidence for a Roman presence is unclear but archeologists have found remains of ancient foundations on the Sabika hill. A fortress or citadel, probably dating from the Visigothic period, existed on the hill in the 9th century. The first reference to the Qal‘at al-Ḥamra was during the battles between the Arabs and the Muladies during the rule of ‘Abdallah ibn Muhammad (r. 888–912). According to surviving documents from the era, the red castle was quite small, and its walls were not capable of deterring an army intent on conquering. The first reference to al-Ḥamrāʼ came in lines of poetry attached to an arrow shot over the ramparts, recorded by Ibn Hayyan.

"Deserted and roofless are the houses of our enemies;

Invaded by the autumnal rains, traversed by impetuous winds;

Let them within the red castle (Kalat al hamra) hold their mischievous councils;

Perdition and woe surround them on every side."

At the beginning of the 11th century, the region of Granada was dominated by the Zirids, a Sanhaja Berber group and offshoot of the Zirids who ruled parts of North Africa. When the Caliphate of Córdoba collapsed after 1009 and the Fitna (civil war) began, the Zirid leader Zawi ben Ziri established an independent kingdom for himself, the Taifa of Granada. The Zirids built their citadel and palace, known as the al-Qaṣaba al-Qadīma, on the hill now occupied by the Albaicín neighborhood. It was connected to two other fortresses on the Sabika and Mauror hills to the south. On the Darro River, between the Zirid citadel and the Sabika hill, was a sluice gate called Bāb al-Difāf ("Gate of the Tambourines"),[a] which could be closed to retain water if needed. This gate was part of the fortification connecting the Zirid citadel with the fortress on the Sabika hill and it also formed part of a coracha (from Arabic qawraja), a type of fortification allowing soldiers from the fortress to access the river and bring back water even during times of siege. The Sabika hill fortress, also known as al-Qasaba al-Jadida ("the New Citadel"), was later used for the foundations of the current Alcazaba of the Alhambra. Under the Zirid kings Habbus ibn Maksan and Badis, the most powerful figure in the kingdom was the Jewish administrator known as Samuel ha-Nagid (in Hebrew) or Isma'il ibn Nagrilla (in Arabic). Samuel built his own palace on the Sabika hill, possibly on the site of the current palaces, although nothing remains of it. It reportedly included gardens and water features.

The period of the Taifa kingdoms, during which the Zirids ruled, came to an end with the conquest of al-Andalus by the Almoravids from North Africa during the late 11th century. In the mid-12th century they were followed by the Almohads. After 1228 Almohad rule collapsed and local rulers and factions emerged again across the territory of Al-Andalus. With the Reconquista in full swing, the Christian kingdoms of Castile and Aragon – under kings Ferdinand III and James I, respectively – made major conquests across al-Andalus. Castile captured Cordoba in 1236 and Seville in 1248. Meanwhile, Ibn al-Ahmar (Muhammad I) established what became the last and longest reigning Muslim dynasty in the Iberian peninsula, the Nasrids, who ruled the Emirate of Granada. Ibn al-Ahmar was a relatively new political player in the region and likely came from a modest background, but he was able to win the support and consent of multiple Muslim settlements under threat from the Castilian advance. Upon settling in Granada in 1238, Ibn al-Ahmar initially resided in the old citadel of the Zirids on the Albaicin hill, but that same year he began construction of the Alhambra as a new residence and citadel. According to an Arabic manuscript since published as the Anónimo de Madrid y Copenhague,

This year, 1238 Abdallah ibn al-Ahmar climbed to the place called "the Alhambra". He examined it, marked the foundations of a castle and left someone in charge of directing the work, and before that year had passed, the construction of the ramparts was completed; water was brought in from the river and a channel carrying the water was built (...)

During the reign of the Nasrid Dynasty, the Alhambra was transformed into a palatine city, complete with an irrigation system composed of aqueducts and water channels that provided water for the complex and for other nearby countryside palaces such as the Generalife. Previously, the old fortresses on the hill had been dependent on rainwater collected from the cistern near the Alcazaba and on what could be brought up from the Darro River below. The creation of the Sultan's Canal, which brought water from the mountains to the east, solidified the identity of the Alhambra as a palace-city rather than a defensive and ascetic structure. This first hydraulic system was expanded afterwards and included two long water channels and several sophisticated elevation devices to bring water onto the plateau.

Later Nasrid rulers after Ibn al-Ahmar continuously modified the site. Along with the fragile materials themselves, which needed regular repairs, this makes the exact chronology of its development difficult to determine. The only elements preserved from the time of Ibn al-Ahmar are some of the fortification walls, particularly the Alcazaba at the western end of the complex. Ibn al-Ahmar did not have time to complete any major new palaces and he may have initially lived in one of the towers of the Alcazaba, before later moving to a modest house on the site of the current Palace of Charles V. The oldest major palace for which some remains have been preserved is the structure known as the Palacio del Partal Alto, in an elevated location near the center of the complex, which probably dates from the reign of Ibn al-Ahmar's son, Muhammad II (r. 1273–1302). To the south was the Palace of the Abencerrajes, and to the east was another private palace, known as the Palace of the Convent of San Francisco, both of which were probably also originally constructed during the time of Muhammad II. Muhammad III (r. 1302–1309) erected the Partal Palace, parts of which are still standing today, as well as the Alhambra's main (congregational) mosque (on the site of the current Church of Santa Maria de la Alhambra). The Partal Palace is the earliest known palace to be built along the northern walls of the complex, with views onto the city below. It is also the oldest Nasrid palace still standing today.

Isma'il I undertook a significant remodeling of the Alhambra. His reign marked the beginning of the "classical" period of Nasrid architecture, during which many major monuments in the Alhambra were begun and decorative styles were consolidated. Isma'il decided to build a new palace complex just east of the Alcazaba to serve as the official palace of the sultan and the state, known as the Qaṣr al-Sultan or Dār al-Mulk. The core of this complex was the Comares Palace, while another wing of the palace, the Mexuar, extended to the west. The Comares Baths are the best-preserved element from this initial construction, as the rest of the palace was further modified by his successors. Near the main mosque Isma'il I also created the Rawda, the dynastic mausoleum of the Nasrids, of which only partial remains are preserved. Yusuf I (r. 1333–1354) carried out further work on the Comares Palace, including the construction of the Hall of Ambassadors and other works around the current Mexuar. He also built the Alhambra's main gate, the Puerta de la Justicia, and the Torre de la Cautiva, one of several small towers with richly-decorated rooms along the northern walls.

Muhammad V's reign (1354–1391, with interruptions) marked the political and cultural apogee of the Nasrid emirate as well as the apogee of Nasrid architecture. Particularly during his second reign (after 1362), there was a stylistic shift towards more innovative architectural layouts and an extensive use of complex muqarnas vaulting. His most significant contribution to the Alhambra was the construction of the Palace of the Lions to the east of the Comares Palace in an area previously occupied by gardens. He also remodeled the Mexuar, created the highly-decorated "Comares Façade" in the Patio del Cuarto Dorado, and redecorated the Court of the Myrtles, giving these areas much of their final appearance. After Muhammad V, relatively little major construction work occurred in the Alhambra. One exception is the Torre de las Infantas, which dates from the time of Muhammad VII (1392–1408). The 15th century saw the Nasrid dynasty in decline and in turmoil, with few significant construction projects and a more repetitive, less innovative style of architecture.

The last Nasrid sultan, Muhammad XII of Granada, surrendered the Emirate of Granada in January 1492, without the Alhambra itself being attacked, when the forces of the Catholic Monarchs, King Ferdinand II of Aragon and Queen Isabella I of Castile, took the surrounding territory with a force of overwhelming numbers. Muhammad XII moved the remains of his ancestors from the complex, as was verified by Leopoldo Torres Balbás in 1925, when he found seventy empty tombs. The remains are now likely to be located in Mondújar in the principality of Lecrín.

After the conquest, the Alhambra became a royal palace and property of the Spanish Crown. Isabella and Ferdinand initially took up residence here and stayed in Granada for several months, up until 25 May 1492. It was during this stay that two major events happened. On 31 March the monarchs signed the Alhambra Decree, which ordered the expulsion of all Jews in Spain who refused to convert. Christopher Columbus, who had also been present to witness the surrender of Granada, presented his plans for an expedition across the Atlantic to the monarchs in the Hall of Ambassadors and on 17 April they signed the contract which set the terms for the expedition which landed in the Americas later that year.

The new Christian rulers began to make additions and alterations to the palace complex. The governorship of the Alhambra was entrusted to the Tendilla family, who were given one of the Nasrid palaces, the Palacio del Partal Alto (near the Partal Palace), to use as family residence. Iñigo López de Mendoza y Quiñones (d. 1515), the second Count of Tendilla, was present in Ferdinand II's entourage when Muhammad XII surrendered the keys to the Alhambra and he became the Alhambra's first Spanish governor. For almost 24 years after the conquest he made repairs and modifications to its fortifications in order to better protect it against gunpowder artillery attacks. Multiple towers and fortifications – such as the Torre de Siete Suelos, the Torre de las Cabezas, and the Torres Bermejas – were built or reinforced in this period, as seen by the addition of semi-round bastions. In 1512 the Count was also awarded the property of Mondéjar and subsequently passed on the title of Marquis of Mondéjar to his descendants.

Charles V (r. 1516–1556) visited the Alhambra in 1526 with his wife Isabella of Portugal and decided to convert it into a royal residence for his use. He rebuilt or modified portions of the Nasrid palaces to serve as royal apartments, a process which began in 1528 and was completed in 1537. He also demolished a part of the Comares Palace to make way for a monumental new palace, known as the Palace of Charles V, designed in the Renaissance style of the period. Construction of the palace began in 1527 but it was eventually left unfinished after 1637.

The governorship of the Tendilla-Mondéjar family came to an end in 1717–1718, when Philip V confiscated the family's properties in the Alhambra and dismissed the Marquis of Mondéjar, José de Mendoza Ibáñez de Segovia (1657–1734), from his position as mayor (alcaide) of the Alhambra, in retaliation for the Marquis opposing him in the War of the Spanish Succession. The departure of the Tendilla-Mondéjar family marked the beginning of the Alhambra's most severe period of decline. During this period the Spanish state dedicated few resources to it and its management was taken over by self-interested local governors who lived with their families inside the neglected palaces.

Over subsequent years the Alhambra was further damaged. Between 1810 and 1812 Granada was occupied by Napoleon's army during the Peninsular War. The French troops, under the command of Count Sebastiani, occupied the Alhambra as a fortified position and caused significant damage to the monument. Upon evacuating the city, they attempted to dynamite the whole complex to prevent it from being re-used as a fortified position. They successfully blew up eight towers before the remaining fuses were disabled by Spanish soldier José Garcia, whose actions saved what remains today. In 1821, an earthquake caused further damage.

Restoration work was undertaken in 1828 by the architect José Contreras, endowed in 1830 by Ferdinand VII. After the death of Contreras in 1847, it was continued by his son Rafael (died 1890) and his grandson Mariano Contreras (died 1912). In 1830 Washington Irving lived in Granada and wrote his Tales of the Alhambra, first published in 1832, which spurred international interest in southern Spain and in its Islamic-era monuments like the Alhambra (an apartment of which he decorated in New England style). Other artists and intellectuals, such as John Frederick Lewis and Owen Jones, helped make the Alhambra into an icon of the era with their writings and illustrations during the 19th century.

Pavilion in the Court of the Lions in 19th-century photo, showing the "oriental" dome added by Rafael Contreras in 1859, later removed by Leopoldo Torres Balbás

The Contreras family members continued to be the most important architects and conservators of the Alhambra up until 1907. During this period they generally followed a theory of "stylistic restoration", which favoured the construction and addition of elements to make a monument "complete" but not necessarily corresponding to any historical reality. They added elements which they deemed to be representative of what they thought was an "Arabic style", emphasizing the Alhambra's purported "Oriental" character. For example, in 1858–1859 Rafael Contreras and Juan Pugnaire added Persian-looking spherical domes to the Court of the Lions and to the northern portico of the Court of the Myrtles, even though these had nothing to do with Nasrid architecture.

In 1868 a revolution deposed Isabella II and the government seized the properties of the Spanish monarchy, including the Alhambra. In 1870 the Alhambra was declared a National Monument of Spain and the state allocated a budget for its conservation, overseen by the Provincial Commission of Monuments. Mariano Contreras, the last of the Contreras architects to serve as director of conservation of the Alhambra, was appointed as architectural curator in April 1890. His tenure was controversial and his conservation strategy attracted criticism from other authorities. In September 1890 a fire destroyed a large part of the Sala de la Barca in the Comares Palace, which highlighted the site's vulnerability. A report was commissioned in 1903 which resulted in the creation of a "Special Commission" in 1905 whose task was to oversee conservation and restoration of the Alhambra, but the commission ultimately failed to exercise control due to friction with Contreras. In 1907 Mariano Contreras was replaced with Modesto Cendoya, whose work was also criticized. Cendoya began many excavations in search of new artifacts but often left these works unfinished. He restored some important elements of the site, like the water supply system, but neglected others. Due to continued friction with Cendoya, the Special Commission was dissolved in 1913 and replaced with the Council (Patronato) of the Alhambra in 1914, which was charged again with overseeing the site's conservation and Cendoya's work. In 1915 it was linked directly to the Directorate-General of Fine Arts of the Ministry of Public Education (later the Ministry of National Education). Like Mariano Contreras before him, Cendoya continued to clash with the supervisory body and to obstruct their control. He was eventually dismissed from his post in 1923.

The Alcazaba before and after 20th-century restoration work

After Cendoya, Leopoldo Torres Balbás was appointed as chief architect from 1923 to 1936. The appointment of Torres Balbás, a trained archeologist and art historian, marked a definitive shift to a more scientific and systematic approach to the Alhambra's conservation. He endorsed the principles of the 1931 Athens Charter for the Restoration of Monuments, which emphasized regular maintenance, respect for the work of the past, legal protection for heritage monuments, and the legitimacy of modern techniques and materials in restoration so long as these were visually recognizable. Many of the buildings in the Alhambra were affected by his work. Some of the inaccurate changes and additions made by the Contreras architects were reversed. The young architect "opened arcades that had been walled up, re-excavated filled-in pools, replaced missing tiles, completed inscriptions that lacked portions of their stuccoed lettering, and installed a ceiling in the still unfinished palace of Charles V". He also carried out systematic archeological excavations in various parts of the Alhambra, unearthing lost Nasrid structures such as the Palacio del Partal Alto and the Palace of the Abencerrajes which provided deeper insight into the former palace-city as a whole.

The work of Torres Balbás was continued by his assistant, Francisco Prieto Moreno, who was the chief architectural curator from 1936 to 1970. In 1940 a new Council of the Alhambra was created to oversee the site, which has remained in charge ever since. In 1984 the central government in Madrid transferred responsibility for the site to the Regional Government of Andalusia and in 1986 new statutes and documents were developed to regulate the planning and protection of the site. In 1984 the Alhambra and Generalife were also listed as a UNESCO World Heritage Site. The Alhambra is now one of the most popular tourist destinations in Spain. Research, archeological investigations, and restoration works have also remained ongoing into the 21st century.

 

Notable for also wearing an OEM Citroen bodykit, but it seems like this rare (seems to be less facelift 3 doors in Europe) model is no longer around.

L'Estany de Banyoles, Banyoles, Girona.

 

L'Estany de Banyoles es el lago más grande de Catalunya, en la provincia de Girona. Es el principal símbolo de la ciudad de Banyoles. El lago y su cuenca lacustre son considerados el conjunto cárstico más extenso de España, constituyendo un sistema medioambiental de notable valor.

 

Situado en el oeste del término municipal de Banyoles, fue declarado por la Generalitat de Catalunya como zona integrante del Plan de Espacios de Interés Natural. En 2003 se incluyó en la lista Ramsar de Zonas Húmedas de Importancia Internacional, solicitándose por varios colectivos la instauración de un Parque Natural.

 

L'Estany de Banyoles es de origen tectónico y cárstico. Se formó en la época cuaternaria, hace unos 250 000 años. Los movimientos tectónicos producidos por la formación de los Pirineos abrieron la falla del Ampurdán. La erosión y otros fenómenos geológicos crearon la zona lacustre.

 

El primer Estany de Banyoles tenía una extensión muy superior a la actual, inundando las riberas unos 6 u 8 metros por encima del nivel actual de las aguas.

 

Las pesquerías son pequeñas construcciones que se encuentran en las aguas del lago en la orilla oriental y declaradas Bien Cultural de Interés Nacional (en la categoría de Jardín Histórico) por la Generalitat de Catalunya.

 

En total hay 20 pesquerías, cada una con un nombre particular. Su construcción comenzó a mediados del siglo XIX hasta 1931, y durante estos años han sido renovados y acondicionados.

 

Inicialmente, el papel de la pesquería era mantener el material para la pesca. Posteriormente, muchos de ellos aumentaron la superficie para poder almacenar un bote. Finalmente, con la llegada de la práctica del deporte y el ascenso de la burguesía banyolina, se adaptaron para poder nadar e incluso quedarse.

 

L'Estany de Banyoles is the largest lake in Catalonia, in the province of Girona. It is the main symbol of the city of Banyoles. The lake and its lacustrine basin are considered the most extensive karst complex in Spain, constituting an environmental system of remarkable value.

 

Located in the west of the municipality of Banyoles, it was declared by the Generalitat de Catalunya as an integral part of the Plan of Spaces of Natural Interest. In 2003 it was included in the Ramsar list of Wetlands of International Importance, requesting by several groups the establishment of a Natural Park.

 

L'Estany de Banyoles is of tectonic and karstic origin. It was formed in the Quaternary era, about 250,000 years ago. The tectonic movements produced by the formation of the Pyrenees opened the Ampurdán fault. Erosion and other geological phenomena created the lacustrine zone.

 

The first Estany de Banyoles had a much higher extension than the current, flooding the banks about 6 or 8 meters above the current level of water.

 

The fishery are small constructions that are found in the water of the lake on the east bank and declared Cultural Good of National Interest (in the category of Historic Garden) by the Generalitat de Catalunya.

 

In total there are 20 the fishery, each with a particular name. Its construction began in the mid-nineteenth century until 1931, and over these years they have been renovated and conditioned.

 

Initially, the role of the fishery was to keep the material for fishing. Subsequently, many of them increased the surface in order to be able to store a boat. Finally, with the arrival of the practice of sport and the rise of the banyolina bourgeoisie, they adapted to be able to swim and even to stay.

KT-22 is a notable peak located in Olympic Valley, California, renowned for its challenging terrain and steep slopes, making it a favorite among advanced skiers and snowboarders. The peak is named after the adjacent ski lift, KT-22, and offers a variety of expert-level runs, including moguls, chutes, and cliff drops. With its stunning views of Lake Tahoe and the surrounding Sierra Nevada mountains, KT-22 is not only a premier destination for winter sports but also a scenic gem in the region.

1957 was chiefly notable for the introduction of one of GM's most memorable designs, the Series 70 Eldorado Brougham.

 

Announced in December 1956 and released around March 1957, the Eldorado Brougham was a hand built, limited car derived from the Park Avenue and Orleans show cars of 1953-54. Designed by Ed Glowacke, it featured the first appearance of quad headlights and totally unique trim. The exterior ornamentation included wide, ribbed lower rear quarter beauty panels extending along the rocker sills and rectangularly sculptured side body "cove" highlighted with five horizontal windsplits on the rear doors. Tail styling treatments followed the Eldorado pattern. This four-door hardtop with rear-hinged rear doors was an ultra-luxury car that cost an astonishing $13,074 — twice the price of any other 1957 Eldorado and more than the Rolls-Royce Silver Cloud of the same year. It featured a stainless steel roof, air suspension, the first automatic two-position "memory" power seats, a dual four-barrel V-8, low profile tires with thin white-walls, automatic trunk opener, Cruise Control, high pressure cooling system, polarized sun visors,electric antenna, automatic-release parking brake, electric door locks, dual heating system, silver magnetized glovebox, drink tumblers, cigarette and tissue dispensers, lipstick and cologne, ladies compact with powder puff, mirror and matching leather notebook, comb and mirror, Arpège atomizer with Lanvin perfume, automatic starter with restart function, Autronic Eye, drum-type electric clock, power windows, forged aluminum wheels and air conditioning.

 

Buyers of Broughams had a choice of 44 full leather interior and trim combinations and could select such items as Mouton, Karakul or lambskin carpeting. There were serious difficulties with the air suspension. Some owners found it cheaper to have the system removed and replaced with conventional coil springs.

 

The 1957 Eldorado Brougham joined the Sixty Special and the Series 75 as the only Cadillac models with Fleetwood bodies although Fleetwood script or crests did not appear anywhere on the exterior of the car, and so this would also mark the first time in 20 years that that a Fleetwood bodied car was paired with the Brougham name. The 1957-58 Eldorado Brougham also marked the return of the Cadillac Series 70, if only briefly. Only 400 Eldorado Broughams were sold in 1957.

IN ENGLISH BELOW THE LINE

 

Foto feta amb una Rolleiflex Old Standard fabricada el 1936; objectiu Carl Zeiss Tessar f3.5 / 75mm + filtre groc; pelicula Kentmere Pan 100.

 

El castell de Cardona és un dels més importants de la historia de Catalunya, pel seus vincles amb els vescomtes de Cardona, el control de les mines de sal, i els setges borbonics durant la guerra de Successió, notablement el de 1711 i el de 1713-1714, on només es rendí després de la caiguda de Barcelona.

 

Vaig fer aquesta fotografia des d'on ara hi ha el mirador del camp de futbol, però on aproximadament es situà una de les principals bateries de setge franceses el 1711. Però el setge fou una derrota pels borbonics, majoritariament francesos.

 

ca.wikipedia.org/wiki/Castell_de_Cardona

  

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Picture taken with my Rolleiflex Old Standard made in 1936; Carl Zeiss Tessar f3.5 75mm lens + yellow filter; Kentmere Pan 100 film.

 

The castle of Cardona, above the city of the same name, seen from the football field viewpoint. In this plain there was one of the largest French siege batteries in 1711. But their guns could barely reach the mighty lower walls.

 

It's one of the key fortresses in Catalonia, with a lot of history in medieval and modern times, most notably it's control of the salt mines and the borbonic sieges of 1711 and 1713-1714 during the War of the Spanish Succession, where it was the last standing spot of Catalan resistance, only surrendering a week after the fall of Barcelona.

 

en.wikipedia.org/wiki/Castle_of_Cardona