View allAll Photos Tagged faults
After developing a fault on the 29th October, B10BLE 62165 was swiftly donated to Scottish Fire & Rescue Service at Portlethen where it now rests.
I'm tryingt to upload more of my graphic design work at the moment.
So here is a poster I made/designed last year as a college project. It was for a fictious exhibition by an fictious artist. I made it all with cut out paper and just added in the finer details on illustrator afterwards.
.................................................................................
----------------------------------------------------------
click to activate the small icon of slideshow: the small triangle inscribed in the small rectangle, at the top right, in the photostream (it means the monitor);
or…. Press the “L” button to zoom in the image;
clicca sulla piccola icona per attivare lo slideshow: sulla facciata principale del photostream, in alto a destra c'è un piccolo rettangolo (rappresenta il monitor) con dentro un piccolo triangolo nero;
oppure…. premi il tasto “L” per ingrandire l'immagine;
www.worldphoto.org/sony-world-photography-awards/winners-...
www.fotografidigitali.it/gallery/2726/opere-italiane-segn...
………………………………………………………………………
Beach holidays were born in the 1700s in Great Britain, this social phenomenon was born in which bathers for the first time go to the beaches, certainly not as sunny as those bathed by the Mediterranean Sea, they are fully dressed; this "new fashion" is also encouraged by the belief of English doctors since the beginning of the eighteenth century (starting around 1720), that breathing the brackish sea air and bathing in cold sea water is healthy, invigorates the body and cure lung diseases (conviction even more strengthened by the discovery of oxygen by Antoine Lavoisier in 1778, which led to the greater diffusion and conviction of the theories on the health benefits of sea air, which was thought to be more oxygenated and pure), these theories push many people from Northern Europe suffering from severe lung diseases to spend long periods in southern Europe, often in the south of Italy, this explains why characters with extraordinary qualities come to Taormina to cure their tuberculosis. The photographer baron Wilhelm von Gloeden and the English lady Florence Trevelyan Trevelyan had the seawater brought with their mules from Isola Bella, but while W. Von Gloeden heated the sea water, the English noblewoman Lady Trevelian did not heat it, mindful of the teachings of the English medical school, this will cause her death from bronchopneumonia on 4 October 1907 (see my previous "photographic stories" about Taormina). In fact, "thalassotherapy" was born in Great Britain, together with the social and cultural phenomenon of frequenting bathing beaches (before the beginning of the 18th century, the sea and its beaches were lived, except for reasons of trade and fishing, in a dark and negative way, from the sea often came very serious dangers such as the sudden landings of ferocious pirates, or foreigners carrying very serious diseases could land). Thus the fashion of spending holidays by the sea was born in the English aristocracy and high bourgeoisie of the time, subsequently the habit of going to the sea spread to all levels of society, the railways that were built throughout Great Britain to 'beginning of the nineteenth century, made travel to the ocean accessible even to the lower classes, they too will frequent the seaside resorts, Blackpool becomes the first seaside resort in Great Britain completely frequented by the working classes thanks to the presence of low-cost bathing establishments; the great and definitive boom in seaside tourism will then take place in the 1950s and 1960s. This being the case, it should not be surprising to know that in Great Britain the beaches are more frequented than one might instinctively think due to a climate very different from the Mediterranean one, and that this socio-cultural phenomenon has been investigated at the photographic by photographers of the same Great Britain, of these I mention four names. An important photographer, who probably inspired subsequent photographers, was Tony Ray-Jones, who died prematurely in 1972, at the young age of 30, who was trying to create a “photographic memory” of the stereotypes of the English people; the famous photojournalist Martin Parr, who, although inspired by the previous one, differs from it for his way of doing “social satire” with his goal; finally, I would like to mention David Hurn and Simon Roberts, the latter with wider-ranging photographs, with photographs more detached from the individual. In Italy there are numerous photographers (I will mention only a few) who have made in their long career images captured in seaside resorts (generally we speaking of "beach photography" similar to "street photography"), photographs that are often unique in their style, such as that adopted by Franco Fontana, I mention Mimmo Jodice, Ferdinando Scianna (of whom I am honored to have known him personally), and Massimo Vitali, famous photographer (understood by some as "the photographer of the beaches"), especially for his beautiful photographs taken on the beaches (but not only), thanks to the presence of elevated fixed structures as a kind of mezzanine, built specifically in the bathing beaches for the realization of his photographs. This is my incipit, to introduce the theme I tackled, that of "beach photography", with a series of photographs taken mostly on the beaches of Eastern Sicily near Taormina and Giardini-Naxos, a few other photos were taken on the Sicilian island of Lipari (here, for example, I photographed the two beautiful and very sweet girls, from Germany, whom I thank again for offering themselves to my lens).
……………………………………………………………
Le vacanze al mare nascono nel ‘700 in Gran Bretagna, nasce questo fenomeno sociale nel quale i bagnanti per la prima volta si recano sulle spiagge, non certo assolate come quelle bagnate dal mar Mediterraneo, sono completamente vestiti; questa “nuova moda” è anche incoraggiata dalla convinzione dei medici inglesi fin dall’inizio del ‘700 (a partire dal 1720 circa), che respirare l’aria salmastra del mare e fare il bagno nell’acqua marina fredda sia salutare, rinvigorisca il corpo e curi le malattie polmonari (convinzione ancor più rafforzata dalla scoperta dell’ossigeno da parte di Antoine Lavoisier nel 1778, che portò alla maggiore diffusione e convinzione delle teorie sui benefici per la salute dell’aria di mare, che si pensava essere più ossigenata e pura), queste teorie spingono molte persone del Nord Europa affette da gravi malattie polmonari a trascorrere dei lunghi periodi nel sud Europa, spesso nel meridione d’Italia, questo spiega perché a Taormina giungono personaggi dalle qualità straordinarie per curare il proprio “mal sottile”, il barone fotografo Wilhelm von Gloeden e la lady inglese Florence Trevelyan Trevelyan si facevano portare coi muli l’acqua di mare proveniente dall’Isola Bella, però mentre W. Von Gloeden riscaldava l’acqua marina, la nobildonna inglese lady Trevelian non la riscaldava, memore degli insegnamenti della scuola medica inglese, questo causerà la sua morte per broncopolmonite il 4 ottobre del 1907 (vedi i miei precedenti “racconti fotografici” su Taormina). Infatti la “talassoterapia” nasce in Gran Bretagna, insieme al fenomeno sociale e culturale della frequentazione dei lidi balneari (prima dell’inizio del ‘700, il mare e le sue spiagge erano vissuti, tranne che per motivi di commercio e di pesca, in maniera oscura e negativa, dal mare spesso provenivano gravissimi pericoli come gli sbarchi improvvisi di feroci pirati, oppure potevano sbarcare stranieri portatori di gravissime malattie). Nell’aristocrazia e nell’alta borghesia inglese di allora nasce così la moda di trascorrere le vacanze al mare, successivamente l’abitudine di andare al mare si diffonde a tutti i livelli della società, le ferrovie che furono costruite in tutta la Gran Bretagna all’inizio dell’Ottocento, resero i viaggi verso l’oceano accessibili anche per i ceti più bassi, quelli più popolari e meno agiati, anch’essi frequenteranno le località balneari, Blackpool diviene la prima località balneare della Gran Bretagna completamente frequentata dalle classi popolari grazie alla presenza di stabilimenti balneari a basso costo; il grande e definitivo boom del turismo balneare si avrà poi negli anni ’50 e ’60. Stando così le cose, non ci si deve meravigliare nel sapere che in Gran Bretagna le spiagge sono più frequentate di quanto istintivamente si possa pensare a causa di un clima ben diverso da quello Mediterraneo, e che questo fenomeno socio-culturale sia stato indagato a livello fotografico da parte di fotografi della stessa Gran Bretagna, di questi cito quattro nomi. Un importante fotografo, che probabilmente ispirò i successivi fotografi, fu Tony Ray-Jones, scomparso prematuramente nel 1972, alla giovane età di 30 anni, il quale cercava di realizzare una “memoria fotografica” degli stereotipi del popolo inglese; il famoso fotoreporter Martin Parr, il quale pur ispirandosi al precedente, se ne differenzia per il suo modo di fare “satira sociale” col suo obiettivo; infine desidero menzionare David Hurn e Simon Roberts, quest’ultimo con fotografie di più ampio respiro, con fotografie più distaccate dal singolo individuo. In Italia numerosi sono i fotografi (ne cito solo qualcuno) che hanno realizzato nella loro lunga carriera immagini colte in località balneari (genericamente si parla di “beach photography” affine alla “street photography”), fotografie spesso uniche nel loro stile, come quello adottato da Franco Fontana, menziono Mimmo Jodice, Ferdinando Scianna (del quale mi onoro di averlo conosciuto personalmente), e Massimo Vitali, famoso fotografo (da alcuni inteso come “il fotografo delle spiagge”), soprattutto per le sue bellissime fotografie realizzate sui lidi (ma non solo), grazie alla presenza di strutture fisse sopraelevate a mò di soppalco, costruite appositamente nei lidi balneari per la realizzazione delle sue fotografie. Questo mio incipit, per introdurre il tema da me affrontato, quello della “beach photography”, con una serie di fotografie realizzate per la maggior parte sulle spiagge della Sicilia Orientale nei pressi di Taormina e Giardini-Naxos, qualche altra foto è stata realizzata nell’isola Siciliana di Lipari (qui ad esempio, ho fotografato le due belle e dolcissime ragazze, provenienti dalla Germania, che ringrazio nuovamente per essersi offerte al mio obiettivo).
……………………………………………..
(っ◔◡◔)っ ♥ Tariffs, DEI, Racism, Global Warming, Layoffs, Food Prices, eggs: since January 20th, this has been a sliding scale of added concerns that have been on our minds for the last few months. I'm remaining optimistic that tough times don't always last. Have faith, but don't be unprepared. ♥
Love is in the air, and so is Cupidelle!
✨ Made for Legacy & Reborn, this irresistibly sweet outfit is designed to make hearts flutter. Soft, flirty, and full of Valentine’s magic – it's the look that love stories are made of! 💕💋
💖 ENJOY 40% off on the IDOL set
& 60% off the FULL set! 💖
✨ TRY DEMO before you buy! ✨
LOVE is... MILOTA 💖 💖 💖
psst.... Join FACEBOOK giveaway
👆👆👆👆👆👆👆👆👆👆👆👆👆👆
There was probably some fault on the DVT which necessitated 87034 "William Shakespeare" to be on the southern end of this rake of Mk3 stock. It is seen howling through Rugeley Trent Valley on a sunny spring day, 1st March 2001. Eight years later, the loco was exported to Bulgaria, becoming 87034-5.
Sunsets along Whidbey Islands West coast are special. The West coast is exposed to the full energy of waves crashing down the Strait of Juan de Fuca which have cut high bluffs in the glacial drift that forms most of the island.
This is further north on the coast from the driftwood scene at Fort Ebey State Park but an occasional rain forest giant still rests on the beach.
The Olympic Mountains tower above the strait; shoved up by huge tectonic forces concentrated along the Hurricane Ridge fault.
This scene was about a mile from my daughters house. It was tough duty house sitting, taking care of my grand-dog but somebody had to do it...
S0A6520
In the late 1950s, Wolverhampton Council proposed a controversial and costly project to build a ring road around the town, to divert ‘through traffic’ away from the town centre. As with most towns in Britain, the huge increase in private car ownership was becoming a headache for the town’s planners.
As part of the town’s future road planning, it was decided that the building of the ‘Ring Road’ would also force the abandonment of the town’s trolleybus system, as the council wanted ‘no trolleybuses or trolleybus infrastructure’ to encounter the new Ring Road! This commitment would become a huge finical burden on the local rate-payers, so budgetary restraints were made where possible. Construction of the Ring Road began in 1961, but took almost three decades to complete.
Between June 1963 and March 1967, Wolverhampton Corporation Transport purchased 146 new double-deck motorbuses to replace the post-war trolleybus fleet. The financial enormity of funding the conversion program impacted on the quality of the new motorbus purchases, with savings having to be made. From 1965 – 1967, the Transport Department’s budget constraints forced them to opt for cheaper bus bodies to be fitted to the locally built Guy Arab V motorbus chassis that the council were duty-bound to purchase. Strachan (Coachbuilders) Ltd of Hamble, Hampshire became the new bus body supplier, but these budget built bus bodies for the Guy Arabs would soon prove to be sub-standard, resulting in short service lives due to structural fatigue.
On the demise of the town's last trolleybuses in March 1967, came the news that twelve high-capacity single-deck buses had been ordered. In July 1967, the ‘Transport Department’ took delivery of six AEC Swifts (708-713) and six Daimler Roadliners (714-719), all having Strachan built dual-doored bodies. This may have been seen as an extravagant purchase in lieu of the tax payers money recently spent on the trolleybus replacement fleet?
The buses appeared very modern looking, with large windows and spacious high-roofed interiors, being very similar in design to London Transport’s Strachan bodied ‘Red Arrow’ buses that had been new to the capital in 1966. The intension from the outset was to trial the concept of ‘pay-on-entry’ buses, with passengers paying the driver on boarding the bus.
The new buses were initially put to work on the No1 Tettenhall service to gauge public reaction to 'pay-on-entry, and assessing operational issues. However, after a few weeks the experiment was ended and crew-operated double-deckers reinstated to the route. Against all expectations, the costly experiment hadn’t been a success, having been met with mixed reactions from the travelling public who were not used to paying the driver on boarding, much preferring bus conductors to take their fares. It was also found that the ‘Cummins V6’ engined Daimler ‘Roadliners’ in particular, didn’t like the intense ‘stop and start’ work on this short urban service. Therefore a decision was made to redeploy these buses to rural services, such as the lengthy No17 and No31 routes to Bridgnorth in Shropshire. In this setting, the stops were fewer and the average speeds were higher, but as a cost saving measure the buses continued to be used as ‘pay-on-entry’ vehicles.
In October 1969, 708-719, along with the rest of the former Wolverhampton Corporation bus fleet, became part of the newly formed West Midlands PTE, whereupon they were renumbered 708N - 719N.
The first victim to early withdrawal was Roadliner 714N, which was lost to fire when working the No17 Bridgnorth service in November 1971. The following year, AEC Swifts 708, 711 were withdrawn and sold to Northampton Transport for further use.
The remaining buses continued to be allocated to Wolverhampton’s Bilston Garage, their duties staying much the same until the loss of the rural bus network in December 1973. The Midland Red taking over these services from WMPTE as part of a wider operational agreement between the two concerns.
Being relatively modern buses and suitable for one-man-operation, WMPTE continued to use the remaining Roadliners and Swifts, but with an eye to disposing of them when the opportunity arose as they did not fit the general fleet profile. Despite the Roadliners continuing to be mechanically troublesome, 716-719 received repaints into WMPTE livery in 1972 and 1973, and may have received body strengthen modifications in preparation? However, the AEC Swifts were never repainted out of their Wolverhampton colours.
Following the premature exit of 708N, 711N (pictured) and 714N, the next to go was Roadliner 715N in July 1973 suffering structural faults to its Strachan built body. It was sold for scrap in May 1974 still wearing WCT green and yellow.
The remaining AEC Swifts came out of service between 1973 to 1974, and the last Roadliners were finally withdrawn between the end of 1974 and January of 1975. Some of these buses found new owners, but all eventually ended up being scrapped with the exception of 719N. Today, 719(N) survives at the Transport Museum Wythall, restored into WCT livery.
The picture taken by the late Dave Everitt, show AEC Swift 711N pulling out onto Railway Drive, as it departs Victoria Square Bus Station for Cheslyn Hay in July 1970.
As for the previously mentioned ‘Ring Road’, that has further relevance to this picture, as part of its Eastern section runs right through the location where this picture was taken.
Image scanned from the original 35mm colour slide.
The tree-covered hill to the right is Duncan's Hill. Taken from the lowlands - but that distant hill in the middle of the shot is Birnam Hill in the Highlands. The Highland Boundary Fault runs along the next dip in the distance.
💘 Cupid's fault 2026 💘
Come visit us on February 2nd, 12:00 pm slt
Explore. Shop. Gift something special to your loved one… grab one for yourself too 😈 💝
💘 See more: www.access-sl.com/cupidsfault
Like & Follow ACCESS on FB: www.facebook.com/access.event.sl
Follow us on IG: @access_event
Cant wait for you to see it!
February 2-22nd, 2026
by ACCESS
At Bullseye®! we're all about quality and modularity! The Eastwood gives you just that with a big ass frame and a big ass calibre. This mean piece of machinery also comes with an over-barrel rail system, allowing you to really step up your game!
This fine firearm can be yours for only 3 easy payments of 1,000 credits! And as always, purchasing a Bullseye® gives you the Bullseye® Guarantee!*
And remember folks, nothing bucks like a Bullseye®!
*If your Bullseye®! explodes** in your hands and melts your forearms, simply handwrite us a letter and we'll refund your purchase***.
**It was probably your fault anyways.
***Shipping and taxes not included
Apparently, I'm still stuck in flashback mode. Here's a shot of the Bright Angel Fault section of The Grand Canyon. From 2007.
A slightly different take of “The Crack” just outside of the Subway. In actuality the crack is just a fault line outside of the Subway entrance. What makes this fault so interesting is the water flowing through it creating beautiful textures.
Often photographed closer up with pure emphasis on a portion of the crack I went for a more zoomed out framing showing the environment surround the crack. Before seeing it I had always thought the crack was located smack in the middle of the cascades. I was wrong. The crack is located next to a curved wall and the water is fed from a small cascading waterfall. I included some of the background trees to show the fall colors and a sense of distance. One thing I did notice was the lack of red maples in the area. The leaves surrounding the crack were already present when I had arrived and hence must have been placed there by prior photographers (not entirely natural but definitely adds some nice colors :).
Located at the top of Archangel Cascades the rock surrounding the crack was mostly all wet. I wanted to reduce some of the reflection but also keep some of it to show the wetness and to show some glimmer. I did in fact take the classic close up shots of it as well. I will save it for a later time.
Canon 5D Mark II
EF 24-70mm f/2.8L
Hoya Pro-1D polarizer
Hitech 0.3 soft ND grad
(IMG_3080)
We may throw the dice!
"We may throw the dice—but the Lord determines how they fall." Proverbs 16:33
If the fall of the dice is under the Lord's control—then whose is the arrangement of our whole life? If the simple casting of the dice is guided by Him—how much more the events of our entire life—especially when we are told by our blessed Savior, "The very hairs of your head are all numbered! Not a sparrow falls to the ground without your Father!" It would bring a holy calm over your mind, dear friend, if you were always to remember this. It would so relieve your mind from worry—that you would be the better able to walk in patience, calmness, and cheerfulness, as a Christian should.
When a man is anxious—he cannot pray with faith, or serve his Master. When you worry and fret about your lot and circumstances, you are meddling with Christ's business, and neglecting your own! You have been attempting "providing" work—and forgetting that it is yours to "obey". Be wise and attend to the obeying—and let Christ manage the providing.
Come and survey your Father's storehouse, and ask whether He will let you starve—while He has laid up so great an abundance in His garner! Look at His heart of mercy—and ask if that heart can ever prove unkind! Look at His inscrutable wisdom—and ask if that wisdom can ever be at fault. Above all, look to Jesus Christ your Intercessor, and ask yourself, while He pleads, can your Father deal ungraciously with you? If He remembers even sparrows, will He forget one of His poor children?
"Cast your burden upon the Lord—and He will take care of you. He will not permit the godly to slip and fall." Psalm 55:22
This reminds me of geologic diagrams of faulted rock strata. I did like the contrasting patterns here.
View from Gean House.
Ochil Hills (Scottish Gaelic: Monadh Ochail - from a Celtic word root, compare Old Welsh uchel meaning 'high') is a range of hills in Scotland north of the Forth valley bordered by the towns of Stirling, Alloa, Kinross, Auchterarder and Perth. The only major roads crossing the hills pass through Glen Devon/Glen Eagles and Glenfarg, the latter now largely replaced except for local traffic by the M90 Edinburgh-Perth motorway cutting through the eastern foothills. The hills are part of a Devonian lava extrusion whose appearance today is largely due to the Ochil Fault which results in the southern face of the hills forming an escarpment. The plateau is undulating with no prominent peak, the highest point being Ben Cleuch at 721 m The south-flowing burns have cut deep ravines including Dollar Glen, Silver Glen and Alva Glen, often only passable with the aid of wooden walkways. Historically, the hills, combined with the town being built at the lowest bridge-point on the River Forth, led to Stirling's importance as a main gateway to the Highlands. They also acted as a boundary to the Kingdom of Fife. Castle Campbell was built at the head of Dollar Glen in the late 15th century (an earlier castle on the site being called "Castle Gloom") mainly as a very visible symbol of the Campbell domination of the area. Sheriffmuir, the site of the 1715 battle of the Jacobite rising is on the northern slopes of the hills. In the early Industrial Revolution, several mill towns such as Tillicoultry, Alva and Menstrie (the Hillfoots Villages) grew up in the shadow of the Ochils to tap the water power. Some of the mills are open today as museums. en.wikipedia.org/wiki/Ochil_Hills
Alloa (Scottish Gaelic: Alamhagh, possibly meaning "rock plain") is a town in Clackmannanshire in the Central Lowlands of Scotland, on the north bank of the Firth of Forth close to the foot of the Ochil Hills 5.5 miles (8.9 km) east of Stirling and 7.9 miles (12.7 km) north of Falkirk. The town, formerly a burgh of barony, is the administrative centre of Clackmannanshire council. The economy relied heavily on trade through its port with mainland Europe, but competition from modern ports saw it close in 1970. The economy is now centred on retail and leisure after the closure of major industries; only one brewer and one glassmaker survive today. Alloa had a population of 18,989 at the 2001 census. Sir Robert Erskine was granted the lands of Alloa and its environs in 1368 for services to King David II and he and his descendants were good stewards, developing the estates and innovating. The Earl of Mar owned many of the coal mines, and Robert Bald, a local mining engineer, was contracted to provide water power from the Gartmorn Dam to operate the mines and other industries. Good water supplies and the availability of barley from the carselands encouraged George Younger to set up a brewery in the 1760s and he was soon followed by others. Alloa became one of Scotland's premier brewing centres. Unfortunately, the 6th Earl of Mar, who oversaw many far-reaching developments including substantial harbour improvements, a customs house and the building of the Gartmorn Dam, was forced to flee the country and forfeit his lands after disastrously backing the Jacobite cause in 1715. However, his brother was allowed to purchase the forfeited lands and future generations continued the tradition of creative industry by launching a glass-works in 1750 and laying one of Scotland's earliest railways (a waggonway) from the Sauchie mines to down to the harbour in around 1766. Before 1775, the colliers were attached to the properties in which they were born and were virtual serfs or slaves, supported by the master. After an Act of Parliament which abolished the system, the colliers could move between collieries at will, and they were supported in their needs by the Alloa Colliers' Fund or Friendly Society which was founded in 1775. Traces of the waggonway and the Gartmorn Dam can still be seen today, and although the dam is no longer used for energy production or water supply, it is well used for fishing and leisure purposes. The Clackmannashire Library was founded at Alloa in 1797 and it contained upwards of 1500 volumes. After the improvements were made to the harbour during the 18th century, Alloa thrived as a river port through which the products of Glasgow manufacture were exported to continental Europe. At that time, and until the 1950s, the main industry to the north and east of the town was coal mining. en.wikipedia.org/wiki/Alloa
A damaged blast from the distant past, an actual broken record, now only good for a little sliderization.
Some 45-rpm singles, such as this one, were pressed with cheaper polystyrene plastic than the polyvinyl chloride that gave the common phonograph record the “vinyl” nickname. Styrene 45s, as the plastic end product was called, wore out faster and were more fragile than vinyl; this particular disc was shipped in a bubble envelope instead of a corrugated-cardboard mailer, leading to the basis for what you see here.
Italien / Venetien- Gardasee
seen from Monte Baldo Massif near the cable car station
gesehen vom Monte Monte Baldo Massif in der Nähe der Seilbahnstation
Lake Garda (Italian: Lago di Garda [ˈlaːɡo di ˈɡarda] or (Lago) Benaco [beˈnaːko]; Eastern Lombard: Lach de Garda; Venetian: Ƚago de Garda; Latin: Benacus; Ancient Greek: Βήνακος) is the largest lake in Italy. It is a popular holiday location in northern Italy, about halfway between Brescia and Verona, and between Venice and Milan on the edge of the Dolomites. Glaciers formed this alpine region at the end of the last Ice Age. The lake and its shoreline are divided between the provinces of Verona (to the south-east), Brescia (south-west), and Trentino (north). The name Garda, which the lake has been referred to in documents dating to the 8th century, comes from the town of the same name. It is evolved from the Germanic word warda, meaning "place of guard", "place of observation" or "place of safety".
Geography
The northern part of the lake is narrower, surrounded by mountains, the majority of which belong to the Gruppo del Baldo. The shape is typical of a moraine valley, probably having been formed under the action of a Paleolithic glacier. Although traces of the glacier's actions are evident today, in more recent years it has been hypothesised that the glacier occupied a previously existing depression, created by stream erosion 5 to 6 million years ago.
The lake has numerous small islands and five main ones, the largest being Isola del Garda, where, in 1220 St. Francis of Assisi founded a monastery. In its place now stands a 19th-century building in the Venetian Gothic style. Nearby to the south is Isola San Biagio, also known as the Isola dei Conigli ("Island of the Rabbits"). Both are offshore of San Felice del Benaco, on the lake's western side. The three other main islands are Isola dell'Olivo, Isola di Sogno, and Isola di Trimelone, all farther north near the eastern side. The main tributary is the Sarca River, others include the Ponale River (fed by Lago di Ledro), the Varone/Magnone River (via the Cascate del Varone) and various streams from both mountainsides, while the only outlet is the Mincio River (79 metres (259 ft), at Peschiera). The subdivision is created by the presence of a fault submerged between Sirmione and Punta San Vigilio which is almost a natural barrier that hampers the homogenization between the water of the two zones.
If the water level of the Adige river is excessive, water is diverted to the lake through the Mori-Torbole tunnel.
History
Battle of Lake Benacus, in which Roman forces defeated the Alamanni on the shores of Lake Garda, in the year 268.
Battle between Milan and Venetian Republic in 1438 following the military engineering feat of galeas per montes.
Battle of Rivoli, in 1797 during the French campaign of Napoleon I in Italy against Austria.
Battle of Solferino in 1859, during the Italian Risorgimento. The terrible aftermath of this battle led to the Geneva Convention and the formation of the Red Cross.
The lake was the site of naval battles in 1866 between Italy and Austria.
As persuaded by the Nazis, Benito Mussolini established the capital of his Italian Social Republic in late 1943 in a villa in the town of Salò on its shores. It served as a nexus for military operations and communications for German troops who occupied northern Italy in late 1943 during World War II.
Mythology
According to the Greco-Roman mythology, the River Mincius was the child of the Lake Benacus.
(Wikipedia)
Monte Baldo (German: Waldberg) is a mountain range in the Italian Alps, located in the provinces of Trento and Verona. Its ridge spans mainly northeast-southwest, and is bounded from south by the highland ending at Caprino Veronese, from west by Lake Garda, from north by the valley joining Rovereto to Nago-Torbole and, from east, the Val d'Adige.
The name derives from the German Wald ("forest"); it appears for the first time in a German map in 1163. The Peace Trail (it: Sentiero della Pace), one of the most important long distance trails in Northern Italy, leads over the range. The ridge is reachable through a cable car from the nearby town of Malcesine, on the shore of Lake Garda.
Morphology
Mount Baldo is characterized by a geographical identity, a ridge parallel to Lake Garda, which stretches for 40 kilometres (25 miles), between the lake to the west and Val d'Adige to the east, and on the south it is bounded by plain Caprino and North Valley Loppio. Mount Baldo reaches its maximum elevation of 2,218 m with the Cima Valdritta, and its minimum elevation of 65 m on Lake Garda. Other prominent peaks in the range are Monte Altissimo di Nago (2,079 m), Cima del Longino (2,180 m), Cima delle Pozzette (2,132 m) and Punta Telegrafo (2,200 m).
(Wikipedia)
Der Gardasee (italienisch Lago di Garda oder Bènaco), einer der oberitalienischen Seen, ist der größte See Italiens, benannt nach der Gemeinde Garda am Ostufer. Sein antiker Name lautete von etwa 200 v. Chr. bis 800 n. Chr. Lacus benacus. Der Name soll von einer alten Gottheit namens Benacus abstammen. Der Gardasee wurde in der vergangenen Eiszeit durch einen Seitenast des Etschgletschers geformt, dessen Spuren man noch heute verfolgen kann, insbesondere durch die Endmoränen um das Südufer z. B. bei Lonato del Garda, Solferino, Valeggio sul Mincio und Custoza. Erste Besiedlungen des Seeufers datieren um das Jahr 2000 v. Chr.
Geographie
Lage
Der Gardasee liegt zwischen den Alpen im Norden und der Po-Ebene im Süden und ist daher ein Alpenrandsee. Der Norden des Sees gehört zur Region Trentino-Südtirol, der Westen zur Lombardei und der Osten zu Venetien. Damit teilen sich die drei Provinzen Trient (Norden), Verona (Osten) und Brescia (Westen) die Verwaltung.
Das nördliche Ufer des Sees ist von Zweitausendern der Gardaseeberge wie dem Monte Baldo umsäumt; das südliche Ufer liegt bereits in der norditalienischen Tiefebene.
In der Nähe des Sees befinden sich bekannte Weinbaugebiete:
Südlich von Desenzano del Garda liegt das Lugana-Gebiet
Östlich vom Gardasee finden sich die Gebiete des Bardolino- und des Soave-Weins
Ebenfalls östlich (zwischen dem Gardasee und Verona) liegt das Valpolicella-Gebiet
Zu- und Abflüsse
Der Gardasee wird hauptsächlich durch den Fluss Sarca gespeist. Dieser fließt am Nordende bei Torbole in den See. Als Mincio verlässt der Fluss bei Peschiera del Garda den Gardasee und fließt später in den Po. Neben den insgesamt 25 Zuflüssen gibt es noch einen künstlichen Zufluss in Form des 1959 fertiggestellten Etsch-Gardasee-Tunnels, dessen Tunnelausgang am südlichen Ortsausgang von Torbole liegt und der im Falle einer stark Hochwasser führenden Etsch geöffnet wird.
Pegel
Der Pegelnullpunkt liegt bei Peschiera del Garda bei 64,027 m s.l.m. Er unterliegt zum Teil starken saisonalen Schwankungen, da das Wasser des Gardasees über seinen Abfluss Mincio zur Bewässerung der intensiv landwirtschaftlich genutzten Flächen zwischen Verona und Mantua genutzt wird. Zum anderen sind die Schwankungen auch durch die Wasserentnahme für die Stromerzeugung im Oberlauf der Sarca bedingt.
Der Pegeltiefstand wurde in den Jahren 2003 und 2007 mit jeweils 8 cm unter Pegelnull erreicht, der Höchststand lag am 2. Juli 1879 bei 216 cm über Pegelnull. 1960 stand der Pegel bei 212 cm aufgrund der Öffnung des Etsch-Gardasee-Tunnels. Nicht festlegen lässt sich der Pegel von 1673 und 1746, als der Ort Desenzano del Garda überschwemmt wurde. Außer in Peschiera wird der Pegelstand auch in Riva del Garda und Torri del Benaco gemessen.
Inseln
Im See befinden sich fünf Inseln, die größte, Isola del Garda mit der Villa Borghese, liegt in der Nähe von Salò. Etwa zwei Kilometer südlich davon, ebenfalls in der Bucht von Manerba und San Felice, liegt die Isola San Biagio auch als „i Conigli“ (deutsch: die Kaninchen) bezeichnet. San Biagio ist ein beliebtes Ausflugsziel, das mit dem Boot oder zu Fuß vom Festland (je nach Wasserstand hüfttief oder trockenen Fußes) erreicht werden kann. Vor Assenza (zwischen Porto di Brenzone und Malcesine) liegt die Isola di Trimelone, diese ist allerdings militärisches Sperrgebiet. Etwas weiter nördlich von Trimelone liegt bei Malcesine im Val di Sogno die Isola del Sogno und nördlich davon die Isola dell’Olivo.
Geschichte
Aus der Bronzezeit stammen zahlreiche Pfahlbautensiedlungen, die direkt am Seeufer oder im unmittelbaren Hinterland des Gardasees errichtet wurden und seit 2011 zum UNESCO-Weltkulturerbe zählen.
Die Schlacht am Lacus Benacus (lateinisch für Gardasee) wurde im November des Jahres 268 an den Ufern des Gardasees in Norditalien zwischen Alamannen und Römern unter Kaiser Claudius Gothicus ausgetragen.
Unter den Signorie fiel der Gardasee zwischen dem 13. und 14. Jahrhundert unter den Einflussbereich der Scaliger, die zahlreiche Burgen insbesondere an den östlichen und südlichen Uferorten (Malcesine, Torri del Benaco, Lazise und Sirmione) errichteten. Im 15. Jahrhundert wurde der See und seine Uferorte zum Schauplatz im Kampf um die Vorherrschaft in Oberitalien zwischen dem Herzogtum Mailand unter den Viscontis und der Republik Venedig. Als militärische Glanzleistung zählte hierbei der Transport einer venezianischen Flotte vom Etschtal über die Berge nach Torbole im Jahr 1439, ein von der Republik Venedig als Galeas per montes bezeichnetes Unternehmen. Mit der im Frieden von Lodi 1454 festgelegten Grenze am Fluss Adda fiel der Gardasee endgültig unter den Einflussbereich der Dogenrepublik. Letztere baute insbesondere Peschiera am strategisch wichtigen Abfluss des Mincio zur Festung aus, die 2017 von der UNESCO zum Weltkulturerbe erklärt wurde.
Während des Spanischen Erbfolgekrieges zu Beginn des 18. Jahrhunderts versuchte General Vendôme mit seinen Truppen über das Nordufer in Richtung Norden vorzustoßen und hinterließ eine Spur der Verwüstung. Dabei wurden zahlreiche Burgen von den Franzosen zerstört, wie Castel Penede in Nago, die Burg von Arco oder Castel Drena, die als Ruinen erhalten sind. Am 19. April 1706 schlug Vendôme in der Schlacht bei Calcinato am Südufer des Sees die kaiserlichen Truppen unter dem Oberbefehl von Christian Detlev von Reventlow.
Die Schlacht bei Rivoli, die im Ersten Koalitionskrieg im Januar 1797 in der Nähe des Ortes Rivoli (südöstlich von Garda) stattfand, war ein Schlüsselerfolg der französischen Armee unter Napoleon Bonaparte im Italienfeldzug über ein zahlenmäßig überlegenes habsburgisches Heer unter Feldmarschall Alvinczy. Aufgrund des Vertrages von Pressburg vom 26. Dezember 1805, mit dem die Grafschaft Tirol zu Bayern fiel, gehörte die Nordspitze des Gardasees von Anfang 1806 bis Anfang 1810 als sogenannter Etschkreis zum Königreich Bayern und anschließend, wie der übrige See auch, zum Königreich Italien. Nach dem Wiener Kongress 1815 fiel der gesamte See dem Kaisertum Österreich zu und war Bestandteil des Königreichs Lombardo-Venetien.
Die Schlacht von Solferino am Südufer war die Entscheidungsschlacht im Sardinischen Krieg zwischen dem Kaisertum Österreich und dem Königreich Sardinien und dessen Verbündetem Frankreich unter Napoléon III. Durch die Niederlage der Österreicher bei Solferino am 24. Juni 1859 wurde der Weg zur Einigung Italiens frei gemacht. Die Grausamkeit der Schlacht und die Hilflosigkeit der verwundeten Soldaten veranlassten Henry Dunant (1828–1910) zur Gründung des Roten Kreuzes und führten zur Vereinbarung der Genfer Konvention von 1864.
Nach dem Verlust der Lombardei und dem dazugehörigen Westufer des Gardasees 1859, verlor Österreich 1866 nach dem Dritten Italienischen Unabhängigkeitskrieg mit Venetien auch das Ostufer, nur die Nordspitze, mit Riva del Garda, verblieb bis 1918 bei Österreich-Ungarn. Der See wurde in dieser Zeit auch „Gartsee“ genannt. Während des Ersten Weltkrieges verlief die Front direkt am Nordufer des Sees entlang, an dem zahlreiche Festungsanlagen errichtet worden waren.
Nach dem Sturz Mussolinis 1943 wurde auf Forderung der deutschen, nationalsozialistischen Regierung in Nord- und Mittelitalien die Marionettenregierung der faschistischen Italienischen Sozialrepublik (Repubblica Sociale Italiana, auch: Republik von Salò) unter Mussolinis Führung als Gegenregierung installiert, die im gleichnamigen Ort am Westufer des Gardasees ihren Regierungssitz hatte. Der Staat bestand zwischen dem 23. September 1943 und dem 25. April 1945. Am 30. April 1945 endete mit der Befreiung von Torbole und Riva durch die 10. US-Gebirgsdivision der Zweite Weltkrieg am Gardasee.
Tourismus
Der Gardasee ist ein beliebtes Reiseziel. Rund um den See gibt es Hotels, Pensionen, Ferienwohnungen und Campingplätze. Ein Großteil der Ferienunterkünfte ist von Ende März bis Anfang Oktober geöffnet. Die Hauptsaison ist Juli und speziell der August. In den Wintermonaten sind die meisten Hotels, Cafés und Restaurants geschlossen. 2018 gab es am Ufer 24 Millionen Übernachtungen.
Am Südufer des Sees befinden sich zahlreiche Freizeitparks wie das Gardaland oder das Canevaworld. Das Nordufer ist vor allem bei Kletterern, Mountainbikern und Surfern beliebt.
(Wikipedia)
Der Monte Baldo ist ein zwischen Gardasee und Etsch gelegener, etwa 30 Kilometer langer Bergrücken, der zum Gebirgszug der Gardaseeberge zählt.
Geographie
Eingegrenzt wird der Monte Baldo im Norden vom Loppiotal und Passo San Giovanni, im Osten vom Etschtal, im Westen vom Gardasee und im Süden von den Moränenhügel bei Rivoli Veronese und der Ebene bei Caprino Veronese.
Er hat keinen ausgezeichneten Gipfel, aber einige Spitzen: Monte Altissimo di Nago (2078 m), Cima del Longino (2180 m), Cima delle Pozzette (2132 m), Cima Valdritta (2218 m) und Punta Telegrafo (2200 m). Den tiefsten Einschnitt im Bergrücken des Monte Baldo bildet der Sattel Bocca di Navene auf 1425 m. Am Monte Baldo befinden sich außer dem Lago di Loppio am Nordende und dem Stausee Lago di Prà della Stua keine größeren stehenden Gewässer.
Der geologische Ursprung des Monte Baldo ist auf die Ablagerungen verschiedener Kalke im Mesozoikum im warmen Tethysmeer zurückzuführen, die bei der Entstehung der Alpen hochgefaltet wurden. Neben Sedimenten sind am Baldo darüber hinaus Spuren von Eruptivgesteinen wie Basalt und Tuff vorzufinden. Die heutige Form geht auf vier Eiszeiten zurück, die den Bergrücken geformt haben. Von der letzten Würmeiszeit finden sich noch einige Spuren, wie große abgeschliffene Felsplatten, Gletschertöpfe und Moränenhügel.
Tourenmöglichkeiten
Die Luftseilbahn Funivia Malcesine-Monte Baldo führt von Malcesine in zwei Teilstücken zur Bergstation Tratto Spino auf 1760 m s.l.m.. Sie bedient im Winter das angeschlossene Skigebiet und wird im Sommer von Wanderern und Radfahrern genutzt, die hier verschiedene Schotterpisten als Downhillstrecken nutzen. Auch als Startplatz für Gleitschirmflieger ist der Monte Baldo auf Grund seiner leichten Erreichbarkeit über die Seilbahn und der enormen Höhendifferenz (1680 m) zum Landeplatz in Malcesine äußerst beliebt. Regelmäßig werden hier Sicherheitstrainings über Wasser durchgeführt.
Von der Bergstation sind unter anderem die Schutzhütten Telegrafo im Süden und Altissimo im Norden zu erreichen, die beide über den Monte Baldo Höhenweg (italienisch Alta via del Monte Baldo) mit dem Tratto Spino verbunden sind.
(Wikipedia)
Kentmere Kenthene RC M.WT. Grad. 3 (normal) @ISO 3,
Shen Hao PTB45-B
Fuji 5,6/105 @f/45, 4s
Neutol 5:00 min
Adostop 2:00 min
Adofix 4:00 min
Lately found out that it was my fault to have a lot images overexposed: when cocking the shutter i moved the aperture tab...
A fault of mine in the past has been buying things more because I like them instead of worrying how they fit. Of course most of them if they are my size fit reasonably well anyway but other more personal things like shoes and underwear should be chosen to give maximum comfort. To be honest I haven't bothered much with bras anyway because I don't like wearing things if I don't need to and besides they either just make me feel padded and rigid or being squashed flat. But at last I came across a couple of super bras in the M&S sale this time that are not only comfortable they fit my breasts perfectly filling the cups and at last making me feel like a woman I try to be. It was on it's own but small so took a risk with this one as it wouldn't have been a problem had it been a 12 but I'm afraid it's just a 10 and I'm 14. So yes it's still not my size when it comes to straps so I will probably wear it for short spells like taking photos but if I grow to love it as I'm sure I will I then I can look out for it again as better fit and pay a little more lol. Well that's just the bra the alluring pants are new too and the colour might not be Jojo but knickers were going literally for pence.
Italien / Trentino - Gardasee
Cima Larici above Pregasina (Riva del Garda)
Cima Larici oberhalb von Pregasina (Riva del Garda)
Lake Garda (Italian: Lago di Garda [ˈlaːɡo di ˈɡarda] or (Lago) Benaco [beˈnaːko]; Eastern Lombard: Lach de Garda; Venetian: Ƚago de Garda; Latin: Benacus; Ancient Greek: Βήνακος) is the largest lake in Italy. It is a popular holiday location in northern Italy, about halfway between Brescia and Verona, and between Venice and Milan on the edge of the Dolomites. Glaciers formed this alpine region at the end of the last Ice Age. The lake and its shoreline are divided between the provinces of Verona (to the south-east), Brescia (south-west), and Trentino (north). The name Garda, which the lake has been referred to in documents dating to the 8th century, comes from the town of the same name. It is evolved from the Germanic word warda, meaning "place of guard", "place of observation" or "place of safety".
Geography
The northern part of the lake is narrower, surrounded by mountains, the majority of which belong to the Gruppo del Baldo. The shape is typical of a moraine valley, probably having been formed under the action of a Paleolithic glacier. Although traces of the glacier's actions are evident today, in more recent years it has been hypothesised that the glacier occupied a previously existing depression, created by stream erosion 5 to 6 million years ago.
The lake has numerous small islands and five main ones, the largest being Isola del Garda, where, in 1220 St. Francis of Assisi founded a monastery. In its place now stands a 19th-century building in the Venetian Gothic style. Nearby to the south is Isola San Biagio, also known as the Isola dei Conigli ("Island of the Rabbits"). Both are offshore of San Felice del Benaco, on the lake's western side. The three other main islands are Isola dell'Olivo, Isola di Sogno, and Isola di Trimelone, all farther north near the eastern side. The main tributary is the Sarca River, others include the Ponale River (fed by Lago di Ledro), the Varone/Magnone River (via the Cascate del Varone) and various streams from both mountainsides, while the only outlet is the Mincio River (79 metres (259 ft), at Peschiera). The subdivision is created by the presence of a fault submerged between Sirmione and Punta San Vigilio which is almost a natural barrier that hampers the homogenization between the water of the two zones.
If the water level of the Adige river is excessive, water is diverted to the lake through the Mori-Torbole tunnel.
History
Battle of Lake Benacus, in which Roman forces defeated the Alamanni on the shores of Lake Garda, in the year 268.
Battle between Milan and Venetian Republic in 1438 following the military engineering feat of galeas per montes.
Battle of Rivoli, in 1797 during the French campaign of Napoleon I in Italy against Austria.
Battle of Solferino in 1859, during the Italian Risorgimento. The terrible aftermath of this battle led to the Geneva Convention and the formation of the Red Cross.
The lake was the site of naval battles in 1866 between Italy and Austria.
As persuaded by the Nazis, Benito Mussolini established the capital of his Italian Social Republic in late 1943 in a villa in the town of Salò on its shores. It served as a nexus for military operations and communications for German troops who occupied northern Italy in late 1943 during World War II.
Mythology
According to the Greco-Roman mythology, the River Mincius was the child of the Lake Benacus.
(Wikipedia)
Der Gardasee (italienisch Lago di Garda oder Bènaco), einer der oberitalienischen Seen, ist der größte See Italiens, benannt nach der Gemeinde Garda am Ostufer. Sein antiker Name lautete von etwa 200 v. Chr. bis 800 n. Chr. Lacus benacus. Der Name soll von einer alten Gottheit namens Benacus abstammen. Der Gardasee wurde in der vergangenen Eiszeit durch einen Seitenast des Etschgletschers geformt, dessen Spuren man noch heute verfolgen kann, insbesondere durch die Endmoränen um das Südufer z. B. bei Lonato del Garda, Solferino, Valeggio sul Mincio und Custoza. Erste Besiedlungen des Seeufers datieren um das Jahr 2000 v. Chr.
Geographie
Lage
Der Gardasee liegt zwischen den Alpen im Norden und der Po-Ebene im Süden und ist daher ein Alpenrandsee. Der Norden des Sees gehört zur Region Trentino-Südtirol, der Westen zur Lombardei und der Osten zu Venetien. Damit teilen sich die drei Provinzen Trient (Norden), Verona (Osten) und Brescia (Westen) die Verwaltung.
Das nördliche Ufer des Sees ist von Zweitausendern der Gardaseeberge wie dem Monte Baldo umsäumt; das südliche Ufer liegt bereits in der norditalienischen Tiefebene.
In der Nähe des Sees befinden sich bekannte Weinbaugebiete:
Südlich von Desenzano del Garda liegt das Lugana-Gebiet
Östlich vom Gardasee finden sich die Gebiete des Bardolino- und des Soave-Weins
Ebenfalls östlich (zwischen dem Gardasee und Verona) liegt das Valpolicella-Gebiet
Zu- und Abflüsse
Der Gardasee wird hauptsächlich durch den Fluss Sarca gespeist. Dieser fließt am Nordende bei Torbole in den See. Als Mincio verlässt der Fluss bei Peschiera del Garda den Gardasee und fließt später in den Po. Neben den insgesamt 25 Zuflüssen gibt es noch einen künstlichen Zufluss in Form des 1959 fertiggestellten Etsch-Gardasee-Tunnels, dessen Tunnelausgang am südlichen Ortsausgang von Torbole liegt und der im Falle einer stark Hochwasser führenden Etsch geöffnet wird.
Pegel
Der Pegelnullpunkt liegt bei Peschiera del Garda bei 64,027 m s.l.m. Er unterliegt zum Teil starken saisonalen Schwankungen, da das Wasser des Gardasees über seinen Abfluss Mincio zur Bewässerung der intensiv landwirtschaftlich genutzten Flächen zwischen Verona und Mantua genutzt wird. Zum anderen sind die Schwankungen auch durch die Wasserentnahme für die Stromerzeugung im Oberlauf der Sarca bedingt.
Der Pegeltiefstand wurde in den Jahren 2003 und 2007 mit jeweils 8 cm unter Pegelnull erreicht, der Höchststand lag am 2. Juli 1879 bei 216 cm über Pegelnull. 1960 stand der Pegel bei 212 cm aufgrund der Öffnung des Etsch-Gardasee-Tunnels. Nicht festlegen lässt sich der Pegel von 1673 und 1746, als der Ort Desenzano del Garda überschwemmt wurde. Außer in Peschiera wird der Pegelstand auch in Riva del Garda und Torri del Benaco gemessen.
Inseln
Im See befinden sich fünf Inseln, die größte, Isola del Garda mit der Villa Borghese, liegt in der Nähe von Salò. Etwa zwei Kilometer südlich davon, ebenfalls in der Bucht von Manerba und San Felice, liegt die Isola San Biagio auch als „i Conigli“ (deutsch: die Kaninchen) bezeichnet. San Biagio ist ein beliebtes Ausflugsziel, das mit dem Boot oder zu Fuß vom Festland (je nach Wasserstand hüfttief oder trockenen Fußes) erreicht werden kann. Vor Assenza (zwischen Porto di Brenzone und Malcesine) liegt die Isola di Trimelone, diese ist allerdings militärisches Sperrgebiet. Etwas weiter nördlich von Trimelone liegt bei Malcesine im Val di Sogno die Isola del Sogno und nördlich davon die Isola dell’Olivo.
Geschichte
Aus der Bronzezeit stammen zahlreiche Pfahlbautensiedlungen, die direkt am Seeufer oder im unmittelbaren Hinterland des Gardasees errichtet wurden und seit 2011 zum UNESCO-Weltkulturerbe zählen.
Die Schlacht am Lacus Benacus (lateinisch für Gardasee) wurde im November des Jahres 268 an den Ufern des Gardasees in Norditalien zwischen Alamannen und Römern unter Kaiser Claudius Gothicus ausgetragen.
Unter den Signorie fiel der Gardasee zwischen dem 13. und 14. Jahrhundert unter den Einflussbereich der Scaliger, die zahlreiche Burgen insbesondere an den östlichen und südlichen Uferorten (Malcesine, Torri del Benaco, Lazise und Sirmione) errichteten. Im 15. Jahrhundert wurde der See und seine Uferorte zum Schauplatz im Kampf um die Vorherrschaft in Oberitalien zwischen dem Herzogtum Mailand unter den Viscontis und der Republik Venedig. Als militärische Glanzleistung zählte hierbei der Transport einer venezianischen Flotte vom Etschtal über die Berge nach Torbole im Jahr 1439, ein von der Republik Venedig als Galeas per montes bezeichnetes Unternehmen. Mit der im Frieden von Lodi 1454 festgelegten Grenze am Fluss Adda fiel der Gardasee endgültig unter den Einflussbereich der Dogenrepublik. Letztere baute insbesondere Peschiera am strategisch wichtigen Abfluss des Mincio zur Festung aus, die 2017 von der UNESCO zum Weltkulturerbe erklärt wurde.
Während des Spanischen Erbfolgekrieges zu Beginn des 18. Jahrhunderts versuchte General Vendôme mit seinen Truppen über das Nordufer in Richtung Norden vorzustoßen und hinterließ eine Spur der Verwüstung. Dabei wurden zahlreiche Burgen von den Franzosen zerstört, wie Castel Penede in Nago, die Burg von Arco oder Castel Drena, die als Ruinen erhalten sind. Am 19. April 1706 schlug Vendôme in der Schlacht bei Calcinato am Südufer des Sees die kaiserlichen Truppen unter dem Oberbefehl von Christian Detlev von Reventlow.
Die Schlacht bei Rivoli, die im Ersten Koalitionskrieg im Januar 1797 in der Nähe des Ortes Rivoli (südöstlich von Garda) stattfand, war ein Schlüsselerfolg der französischen Armee unter Napoleon Bonaparte im Italienfeldzug über ein zahlenmäßig überlegenes habsburgisches Heer unter Feldmarschall Alvinczy. Aufgrund des Vertrages von Pressburg vom 26. Dezember 1805, mit dem die Grafschaft Tirol zu Bayern fiel, gehörte die Nordspitze des Gardasees von Anfang 1806 bis Anfang 1810 als sogenannter Etschkreis zum Königreich Bayern und anschließend, wie der übrige See auch, zum Königreich Italien. Nach dem Wiener Kongress 1815 fiel der gesamte See dem Kaisertum Österreich zu und war Bestandteil des Königreichs Lombardo-Venetien.
Die Schlacht von Solferino am Südufer war die Entscheidungsschlacht im Sardinischen Krieg zwischen dem Kaisertum Österreich und dem Königreich Sardinien und dessen Verbündetem Frankreich unter Napoléon III. Durch die Niederlage der Österreicher bei Solferino am 24. Juni 1859 wurde der Weg zur Einigung Italiens frei gemacht. Die Grausamkeit der Schlacht und die Hilflosigkeit der verwundeten Soldaten veranlassten Henry Dunant (1828–1910) zur Gründung des Roten Kreuzes und führten zur Vereinbarung der Genfer Konvention von 1864.
Nach dem Verlust der Lombardei und dem dazugehörigen Westufer des Gardasees 1859, verlor Österreich 1866 nach dem Dritten Italienischen Unabhängigkeitskrieg mit Venetien auch das Ostufer, nur die Nordspitze, mit Riva del Garda, verblieb bis 1918 bei Österreich-Ungarn. Der See wurde in dieser Zeit auch „Gartsee“ genannt. Während des Ersten Weltkrieges verlief die Front direkt am Nordufer des Sees entlang, an dem zahlreiche Festungsanlagen errichtet worden waren.
Nach dem Sturz Mussolinis 1943 wurde auf Forderung der deutschen, nationalsozialistischen Regierung in Nord- und Mittelitalien die Marionettenregierung der faschistischen Italienischen Sozialrepublik (Repubblica Sociale Italiana, auch: Republik von Salò) unter Mussolinis Führung als Gegenregierung installiert, die im gleichnamigen Ort am Westufer des Gardasees ihren Regierungssitz hatte. Der Staat bestand zwischen dem 23. September 1943 und dem 25. April 1945. Am 30. April 1945 endete mit der Befreiung von Torbole und Riva durch die 10. US-Gebirgsdivision der Zweite Weltkrieg am Gardasee.
Tourismus
Der Gardasee ist ein beliebtes Reiseziel. Rund um den See gibt es Hotels, Pensionen, Ferienwohnungen und Campingplätze. Ein Großteil der Ferienunterkünfte ist von Ende März bis Anfang Oktober geöffnet. Die Hauptsaison ist Juli und speziell der August. In den Wintermonaten sind die meisten Hotels, Cafés und Restaurants geschlossen. 2018 gab es am Ufer 24 Millionen Übernachtungen.
Am Südufer des Sees befinden sich zahlreiche Freizeitparks wie das Gardaland oder das Canevaworld. Das Nordufer ist vor allem bei Kletterern, Mountainbikern und Surfern beliebt.
(Wikipedia)
PLEASE, NO invitations or self promotions, THEY WILL BE DELETED. My photos are FREE to use, just give me credit and it would be nice if you let me know, thanks.
To me this is the most vibrant display of colour in the fall.
The Aspy Fault runs inland for about 40 kilometres (24 miles) through Cape Breton Highlands National Park.
Land masses move and separate along fault lines, geologists can determine what land masses might once have been connected. Cape Breton may have been joined to Africa at one time.
« If you appreciate my work and would like to support me becoming an independent photographer, become a Patreon supporter at www.patreon.com/alexdehaas, or buy me a coffee at www.buymeacoffee.com/alexdehaas :) »
I love the beach when the sun goes down. It's tricky to photograph but the colour is so beautiful and soothing. I'm sure there are many photography faults with this but I love the glow and tranquility.
A remix of Varitshol Cairn's HR-53e Micro Faulter with a distinctly Imbrium Lunokhod Industries flavor. Designed to remain faithful to the original's compact profile while offering as many system customization options as possible.
Shoulders courtesy of A. Yates Industries's STOAT.
Feet/Lower leg configuration courtesy of Liu Sim's [EXOSUIT] Iǫtunn.
Hangar Post here: www.mobileframehangar.com/viewtopic.php?f=12&t=6724
===========================================================
Built for Mobile Frame Zero - a tabletop wargame.
Mobile Frame Hangar (MFZ Community Forums).
===========================================================