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Jewish apologetics came many centuries later; it is considerably younger than Greek, Christian, and even Moslem apologetics, tracing its origins to as late as the Middle Ages. One of the pioneers and an acknowledged champion of Jewish apologetics was the prominent poet Yehuda Halevi, who wrote the Kuzari tract in the 11th century. Halevi’s apologetic technique relies on the standard Hellenistic scholastic system, perfected for centuries by Christian and Moslem philosophers, but Halevi undoubtedly made a valuable addition to this field. With this in mind he developed a series of interesting arguments in defense of Judaism, arguments which retain their popular appeal to this day. Among other esteemed achievements Halevi is the alleged inventor of an elegant scholastic technique which was named the “Kuzari principle” in honor of the tract wherein it was applied. Essentially, this technique is designed to prove the authenticity of the assertions made by Judaism on the strength of their existence alone, that is, without discussing their content. According to Halevi, a historical theory that lays claim to an uninterrupted process whereby its mass tradition was formed and transmitted is rendered authentic by the very fact of this claim. Without a doubt, the Kuzari principle regardless of whether it is true or false is applicable to Judaism; at the same time, it should apply to many other historical theories. This dual applicability creates a multitude of fascinating logical problems.

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Minoan eruption

Get daily news updates directly to your inbox Subscribe Thank you for subscribingWe have more newsletters Show me See our privacy notice Could not subscribe, try again laterInvalid Email has long had a reputation for being a rich man’s destination and the yachts in the harbours and five-star resorts around the island still convey that image. But there are plenty of cheaper options and with its short flying time, sandy beaches, shallow waters and a distinctly Italian feel it makes for an ideal destination for family fun or a romantic trip for two.

THE NORTH THE three main cities, and points of entry by air, are at opposite ends of the island but are all on the coast, allowing for water-based activities combined with fine dining and all the facilities of urban living. The main attraction of Alghero, in the north, is the 16th Century Old Town, still surrounded by the original wall and several defensive towers.

Walking along the rampart route offers wonderful coastal views as well as a vast choice of elegant restaurants and authentic ice-cream bars from which to watch the stunning sunsets. The walkway then leads to the port, a popular mooring point for millionaires’ yachts as well as smaller, more humble boats.

Jun 02,  · One of the highlights of Santorini is the archaeological site of Akrotiri, discovered in under a thick blanket of pumice. This remarkably well-preserved Minoan site, dating back to the Bronze Age, reveals the advanced lifestyle of the early Greeks.

The formation of islands by rising sea levels can be likened to a population bottleneck whose magnitude and duration is determined by island area and time since isolation, respectively. The Holocene landbridge islands of the Aegean Sea Greece were formed since the last glacial maximum and constitute an ideal system for disentangling the effects of island area, age and geographic isolation on genetic variability.

Of the many reptile species inhabiting this island system, the Aegean wall lizard Podarcis erhardii is an excellent indicator of fragmentation history due to its widespread distribution and poor over-water dispersal abilities. In this study, we utilize a detailed record of Holocene fragmentation to investigate the effects of island history on wall lizard mitochondrial and nuclear microsatellite diversity.

Findings show that the spatial distribution of mitochondrial haplotypes reflects historical patterns of fragmentation rather than geographic proximity per se. In keeping with neutral bottleneck theory, larger and younger islands retain more nuclear genetic variation than smaller, older islands. Conversely, there is no evidence of an effect of isolation by distance or effect of distance to the nearest larger landmass on genetic variability, indicating little gene flow between islands.

Lastly, population-specific measures of genetic differentiation are inversely correlated with island area, suggesting that smaller islands exhibit greater divergence due to their greater susceptibility to drift. Taken together, these results suggest that both island area and time since isolation are important predictors of genetic variation and that these patterns likely arose through the progressive fragmentation of ancestral diversity and the ensuing cumulative effects of drift.

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The Minoan eruption of Thera, also referred to as the Thera eruption or Santorini eruption, was a major catastrophic volcanic eruption with a Volcanic Explosivity Index VEI of 6 or 7 and a dense-rock equivalent DRE of 60 km3 14 cu mi , 1 2 which is estimated to have occurred in the mid-second millennium BCE. The eruption was one of the largest volcanic events on Earth in recorded history.

The volcano ejected up to four times as much as the well-recorded eruption by Krakatoa in

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About this holiday Based in Perissa on the southeast coast, framed by dramatic scenery and peppered with white-washed villas, we can take a break from the world at home, soaking up the warm Mediterranean rays. Our hotel is situated just 80 metres from the unique and stunning black sand beach of Perissa which holds a Blue Flag award and, as it lies next to the Profitis Ilias mountain, it is protected from the summer Aegean winds.

Mr Drosos, his family and the staff at the hotel are sure to extend us a warm welcome. Being exclusive to Solos we will have their undivided attention, helping us to make the most of our stay at this charming family-run residence. We have easy access to the promenade running parallel to the beach which is lined with plenty of shops, bars, restaurants and traditional tavernas.

As this is all within easy reach, it makes sense to have our board basis at the Villa Masitrali as bed and breakfast. The southernmost of the Cyclades, a group of islands that spreads most of the way across the Mediterranean from Athens in the north to Crete in the south, it enjoys great weather from early spring to late autumn. The island is like no other; its dramatic crescent shape was created from a huge volcanic eruption thousands of years ago.

A wide range of optional excursions are on offer if you choose to leave Perissa and explore further afield. Choose from a fullday tour of the island or jump on transfer to Oia to witness the wonderful sunset.

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Mount Teide Weekend – Tenerife paul gamlingay 03 February This trip should not be underestimated if weather conditions are poor. We had km winds and driving snow at the top Long days but excellent fun I would probably rate the trip at a 7. Remember to take micro… Read more spikes just in case as these are not something you would normally associate with Tenerife. The guide, Cao, and the on-site team were excellent.

The current stone spire crowning the tower, dating from , was erected after a major fire caused by a thunderstorm. The original spire, entirely Gothic, was built of American mahogany, had a pyramidal structure, and was the tallest tower in Spain.

The entire contents of that provisional application are incorporated herein by reference. The PC is clearly capable of doing a whole lot more than what we use it for. Essentially, for many the PC became a replacement for the typewriter, and it is still largely a word processor. The other initial application that drove PC adoption was the spreadsheet.

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Volcanic craters on Santorini today Background Geological evidence shows the Thera volcano erupted numerous times over several hundred thousand years before the Minoan eruption. In a repeating process, the volcano would violently erupt, then eventually collapse into a roughly circular seawater-filled caldera , with numerous small islands forming the circle. The caldera would slowly refill with magma, building a new volcano, which erupted and then collapsed in an ongoing cyclical process.

The northern part of the caldera was refilled by the volcanic ash and lava, then collapsed again. This was up to four times what was thrown into the stratosphere by Krakatoa in , a well-recorded event. The Thera volcanic events and subsequent ashfall probably sterilized the island, as occurred on Krakatoa. This layer has three distinct bands that indicate the different phases of the eruption. The thinness of the first ash layer, along with the lack of noticeable erosion of that layer by winter rains before the next layer was deposited, indicate that the volcano gave the local population a few months’ warning.

Since no human remains have been found at the Akrotiri site , this preliminary volcanic activity probably caused the island’s population to flee. It is also suggested that several months before the eruption, Santorini experienced one or more earthquakes, which damaged the local settlements. Archaeological evidence indicated burial of man-made structures with limited damage. Man-made structures not buried during Minoan A were completely destroyed.

The third phase was also characterized by the initiation of caldera collapse. This phase was characterized by the completion of caldera collapse, which produced tsunami.

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Volcanic craters on Santorini today Advertisements Background Geological evidence shows the Thera volcano erupted numerous times over several hundred thousand years before the Minoan eruption. In a repeating process, the volcano would violently erupt, then eventually collapse into a roughly circular seawater-filled caldera , with numerous small islands forming the circle. The caldera would slowly refill with magma, building a new volcano, which erupted and then collapsed in an ongoing cyclical process.

Immediately prior to the Minoan eruption, the walls of the caldera formed a nearly continuous ring of islands with the only entrance lying between Thera and the tiny island of Aspronisi. The northern part of the caldera was refilled by the volcanic ash and lava, then collapsed again.

Apr 24,  · Team SoloMid’s jungler Santorin tells us about his favorite TV shows, his closest friend on the team, and what he misses about Denmark. Follow us on Twitter.

Mykonos or Santorini where should I go? You can get a ferry to Mykonos from Athens from two ports. From Piraeus port and from Rafina port. How long does the trip last between Athens and Mykonos? From Piraeus port you have two choices the speed boat that will take you to Mykonos in 2h 30m and the regular boat that needs approximately 5 hours to reach Mykonos port.

From Rafina port you again have two choices the speed boat that needs around 2h 15m and the regular boat that will take you to Mykonos in 4h 30m. If you get sea sickness easily then you should take the regular boat because when there is wind the journey will be tough. Santorini How much does it cost to go from Athens to Mykonos and vice versa? Can I fly to Mykonos or Santorini?

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Abstract The notion of personalized medicine has developed from the application of the discipline of pharmacogenetics to clinical medicine. Regulatory authorities differ in their approach to these issues. Evidence emerging subsequently has generally revealed the pharmacogenetic information included in the label to be premature. Lack of efficacy or an adverse drug reaction is frequently related to non-genetic factors.

Phenoconversion, arising from drug interactions, poses another often neglected challenge to any potential success of personalized medicine by mimicking genetically-determined enzyme deficiency.

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The volcanic rocks in these areas are mainly basalt and andesite through dacite, with a dominant calc-alkaline to rare tholeiitic tendency. Primitive mantle-normalized multi-element variations exhibit enrichment of large-ion lithophile elements and to a lesser extent, of light rare earth elements, as well as depletion of high field strength elements, thus revealing that volcanic rocks evolved from a parental magma derived from an enriched mantle source. Sr, Nd and Pb isotopic systematics imply that the volcanic rocks are derived from a subduction-modified subcontinental lithospheric mantle.

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Before dinner this evening, gather with your travelling companions for a welcome drink. Day 2 – Santorini Santorini is a picture-perfect island perched on what is left of a sunken volcanic caldera. It really is one the most beautiful of the Greek islands, boasting steep mountain paths and hillsides scattered with whitewashed villages and blue-domed churches. Spend a free day exploring in the company of your travelling companions or enjoying the facilities at your hotel, which include a spa and two pools.

Day 3 – Caldera Islands cruise Today we include a cruise around Santorini and its neighbouring islands — a fantastic way to savour their immense beauty. Our first stop will be Nea Kameni, a lava island where you can take a walk to the edge of the crater of its still-active volcano to see whirls of steam rising from the ground. Next we sail to Palea Kameni, another islet formed by molten rock. Here you can bathe in hot sulphur springs or simply enjoy the exceptional views.

Our final stop is Thirassia, an island which was once part of Santorini.

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