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    General considerations Distinctions between relative-age and absolute-age measurements Local relationships on a single outcrop or archaeological site can often be interpreted to deduce the sequence in which the materials were assembled. This then can be used to deduce the sequence of events and processes that took place or the history of that brief period of time as recorded in the rocks or soil. For example, the presence of recycled bricks at an archaeological site indicates the sequence in which the structures were built.

    Similarly, in geology, if distinctive granitic pebbles can be found in the sediment beside a similar granitic body, it can be inferred that the granite, after cooling, had been uplifted and eroded and therefore was not injected into the adjacent rock sequence.

    Although with clever detective work many complex time sequences or relative ages can be deduced, the ability to show that objects at two separated sites were formed at the same time requires additional information. A coin, vessel, or other common artifact could link two archaeological sites, but the possibility of recycling would have to be considered. It should be emphasized that linking sites together is essential if the nature of an ancient society is to be understood, as the information at a single location may be relatively insignificant by itself.

    Similarly, in geologic studies, vast quantities of information from widely spaced outcrops have to be integrated. Some method of correlating rock units must be found. In the ideal case, the geologist will discover a single rock unit with a unique collection of easily observed attributes called a marker horizon that can be found at widely spaced localities.

    Any feature, including colour variations, textures, fossil content, mineralogyor any unusual combinations of these can be used.


    It is only by correlations that the conditions on different parts of Earth at any particular stage in its history can be deduced. In addition, because sediment deposition is not continuous and much rock material has been removed by erosionthe fossil record from many localities has to be integrated before a complete picture of the evolution of life on Earth can be assembled.

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    Using this established record, geologists have been able to piece together events over the past million years, or about one-eighth of Earth history, during which time useful fossils have been abundant. The need to correlate over the rest of geologic time, to correlate nonfossiliferous units, and to calibrate the fossil time scale has led to the development of a specialized field that makes use of natural radioactive isotopes in order to calculate absolute ages. The precise measure of geologic time has proven to be the essential tool for correlating the global tectonic processes that have taken place in the past.

    Precise isotopic ages are called absolute ages, since they date the timing of events not relative to each other but as the time elapsed between a rock-forming event and the present. The same margin of error applies for younger fossiliferous rocks, making absolute dating comparable in precision to that attained using fossils.

    To achieve this precision, geochronologists have had to develop the ability to isolate certain high-quality minerals that can be shown to have remained closed to migration of the radioactive parent atoms they contain and the daughter atoms formed by radioactive decay over billions of years of geologic time.

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    In addition, they have had to develop special techniques with which to dissolve these highly refractory minerals without contaminating the small amount about one-billionth of a gram of contained lead and uranium on which the age must be calculated.

    Since parent uranium atoms change into daughter atoms with time at a known rate, their relative abundance leads directly to the absolute age of the host mineral.

    In fact, even in younger rocks, absolute dating is the only way that the fossil record can be calibrated. Without absolute ages, investigators could only determine which fossil organisms lived at the same time and the relative order of their appearance in the correlated sedimentary rock record. Unlike ages derived from fossils, which occur only in sedimentary rocks, absolute ages are obtained from minerals that grow as liquid rock bodies cool at or below the surface.

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    When rocks are subjected to high temperatures and pressures in mountain roots formed where continents collide, certain datable minerals grow and even regrow to record the timing of such geologic events. When these regions are later exposed in uptilted portions of ancient continents, a history of terrestrial rock-forming events can be deduced.

    Episodes of global volcanic activityrifting of continents, folding, and metamorphism are defined by absolute ages.

    The results suggest that the present-day global tectonic scheme was operative in the distant past as well. Continents move, carried on huge slabs, or plates, of dense rock about km 62 miles thick over a low-friction, partially melted zone the asthenosphere below. In the oceansnew seafloor, created at the globe-circling oceanic ridgesmoves away, cools, and sinks back into the mantle in what are known as subduction zones i.

    Where this occurs at the edge of a continent, as along the west coast of North and South America, large mountain chains develop with abundant volcanoes and their subvolcanic equivalents. These units, called igneous rockor magma in their molten form, constitute major crustal additions. By contrast, crustal destruction occurs at the margins of two colliding continents, as, for example, where the subcontinent of India is moving north over Asia. Great uplift, accompanied by rapid erosion, is taking place and large sediment fans are being deposited in the Indian Ocean to the south.

    Rocks of this kind in the ancient record may very well have resulted from rapid uplift and continent collision. When continental plates collide, the edge of one plate is thrust onto that of the other. The rocks in the lower slab undergo changes in their mineral content in response to heat and pressure and will probably become exposed at the surface again some time later.

    Rocks converted to new mineral assemblages because of changing temperatures and pressures are called metamorphic. Virtually any rock now seen forming at the surface can be found in exposed deep crustal sections in a form that reveals through its mineral content the temperature and pressure of burial. Such regions of the crust may even undergo melting and subsequent extrusion of melt magma, which may appear at the surface as volcanic rocks or may solidify as it rises to form granites at high crustal levels.

    Magmas produced in this way are regarded as recycled crust, whereas others extracted by partial melting of the mantle below are considered primary. Even the oceans and atmosphere are involved in this great cycle because minerals formed at high temperatures are unstable at surface conditions and eventually break down or weather, in many cases taking up water and carbon dioxide to make new minerals.

    If such minerals were deposited on a downgoing i. These components would then rise and be fixed in the upper crust or perhaps reemerge at the surface. Such hot circulating fluids can dissolve metals and eventually deposit them as economic mineral deposits on their way to the surface.

    Geochronological studies have provided documentary evidence that these rock-forming and rock-re-forming processes were active in the past.

    Seafloor spreading has been traced, by dating minerals found in a unique grouping of rock units thought to have been formed at the oceanic ridges, to million years ago, with rare occurrences as early as 2 billion years ago. Other ancient volcanic units document various cycles of mountain building.

    The source of ancient sediment packages like those presently forming off India can be identified by dating single detrital grains of zircon found in sandstone.

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    Magmas produced by the melting of older crust can be identified because their zircons commonly contain inherited older cores. Episodes of continental collision can be dated by isolating new zircons formed as the buried rocks underwent local melting.

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    Periods of deformation associated with major collisions cannot be directly dated if no new minerals have formed. The time of deformation can be bracketed, however, if datable units, which both predate and postdate it, can be identified. The timing of cycles involving the expulsion of fluids from deep within the crust can be ascertained by dating new minerals formed at high pressures in exposed deep crustal sections.

    In some cases, it is possible to prove that gold deposits may have come from specific fluids if the deposition time of the deposits can be determined and the time of fluid expulsion is known. Where the crust is under tension, as in Iceland, great fissures develop. These fissures serve as conduits that allow black lavacalled basaltto reach the surface.

    The portion that remains in a fissure below the surface usually forms a vertical black tubular body known as a dike or dyke. Precise dating of such dikes can reveal times of crustal rifting in the past. Dikes and lava, now exposed on either side of Baffin Bayhave been dated to determine the time when Greenland separated from North America—namely, about 60 million years ago.

    Combining knowledge of Earth processes observed today with absolute ages of ancient geologic analogues seems to indicate that the oceans and atmosphere were present by at least 4 billion years ago and that they were probably released by early heating of the planet.

    The continents were produced over time; the oldest preserved portions were formed approximately 4 billion years ago, but this process had begun about by 4. Absolute dating allows rock units formed at the same time to be identified and reassembled into ancient mountain belts, which in many cases have been disassociated by subsequent tectonic processes.

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    The most obvious of these is the Appalachian chain that occupies the east coast of North America and extends to parts of Newfoundland as well as parts of Ireland, England, and Norway. Relic oceanic crustformed between million and million years ago, was identified on both sides of the Atlantic in this chain, as were numerous correlative volcanic and sedimentary units.

    Evidence based on geologic description, fossil content, and absolute and relative ages leave no doubt that these rocks were all part of a single mountain belt before the Atlantic Ocean opened in stages from about million years ago. Determination of sequence Relative geologic ages can be deduced in rock sequences consisting of sedimentary, metamorphic, or igneous rock units.

    In fact, they constitute an essential part in any precise isotopic, or absolute, dating program. Such is the case because most rocks simply cannot be isotopically dated.

    Therefore, a geologist must first determine relative ages and then locate the most favourable units for absolute dating. It is also important to note that relative ages are inherently more precise, since two or more units deposited minutes or years apart would have identical absolute ages but precisely defined relative ages. While absolute ages require expensive, complex analytical equipment, relative ages can be deduced from simple visual observations. Steno's four laws of stratigraphy.

    Most methods for determining relative geologic ages are well illustrated in sedimentary rocks. These rocks cover roughly 75 percent of the surface area of the continents, and unconsolidated sediments blanket most of the ocean floor. They provide evidence of former surface conditions and the life-forms that existed under those conditions. The sequence of a layered sedimentary series is easily defined because deposition always proceeds from the bottom to the top.

    This principle would seem self-evident, but its first enunciation more than years ago by Nicolaus Steno represented an enormous advance in understanding. Known as the principle of superpositionit holds that in a series of sedimentary layers or superposed lava flows the oldest layer is at the bottom, and layers from there upward become progressively younger.

    On occasion, however, deformation may have caused the rocks of the crust to tilt, perhaps to the point of overturning them. Moreover, if erosion has blurred the record by removing substantial portions of the deformed sedimentary rock, it may not be at all clear which edge of a given layer is the original top and which is the original bottom. Identifying top and bottom is clearly important in sequence determination, so important in fact that a considerable literature has been devoted to this question alone.

    Many of the criteria of top—bottom determination are based on asymmetry in depositional features. Oscillation ripple marks, for example, are produced in sediments by water sloshing back and forth. When such marks are preserved in sedimentary rocks, they define the original top and bottom by their asymmetric pattern. Certain fossils also accumulate in a distinctive pattern or position that serves to define the top side. In wind-blown or water-lain sandstonea form of erosion during deposition of shifting sand removes the tops of mounds to produce what are called cross-beds.

    The truncated layers provide an easily determined depositional top direction. The direction of the opening of mud cracks or rain prints can indicate the uppermost surface of mudstones formed in tidal areas.

    When a section of rock is uplifted and eroded, as during mountain-building episodes, great volumes of rock are removed, exposing a variety of differently folded and deformed rock units. The new erosion surface must postdate all units, dikes, veins, and deformation features that it crosses. Even the shapes formed on the erosional or depositional surfaces of the ancient seafloor can be used to tell which way was up.

    A fragment broken from one bed can only be located in a younger unit, and a pebble or animal track can only deform a preexisting unit—i. In fact, the number of ways in which one can determine the tops of well-preserved sediments is limited only by the imagination, and visual criteria can be deduced by amateurs and professionals alike.

    One factor that can upset the law of superposition in major sediment packages in mountain belts is the presence of thrust faults. Such faultswhich are common in compression zones along continental edges, may follow bedding planes and then cross the strata at a steep angle, placing older units on top of younger ones.

    In certain places, the fault planes are only a few centimetres thick and are almost impossible to detect. Relative ages also can be deduced in metamorphic rocks as new minerals form at the expense of older ones in response to changing temperatures and pressures.

    In deep mountain roots, rocks can even flow like toothpaste in their red-hot state.
    Turkey The beach is the key to many a great holiday — from first childhood steps across the sand to teenage posturing and strolls en famille.

    But the perfect beach is rarely found by chance. The coasts of the Mediterranean and the Atlantic are fringed with an overwhelming array of beaches - many of which have been spoilt by concrete tower blocks and flocks of tourists.

    Head, instead, to one of these secret beaches - 52, one for every week of the year - chosen by our European experts in FranceItalySpainPortugalCroatiaGreece and Turkey. Beloved by locals, these sandy stretches are off the tourist track, and brimming with character. Rodas is the longest beach on the archipelago and the nicest. Visitors are limited to 2, a day; there are no hotels — only a campsite — and just a couple of basic restaurants.

    There are no bikes, let alone cars. Read the full review of Parador de Santiago de Compostela. Or you could stick to the beaches around Viveiro Bay, a teardrop-shaped inlet framed by hills. Groups of friends and families.

    The stylish Ego hotel, which has sea views. Llafranc on the Costa Brava Credit: Anyone seeking an unrowdy beach scene.

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    The Mas de Torrent, a luxurious country house hotel and spa, just a minute drive from Llafranc. Read the full review of Mas de Torrent. The colourful cliffs — rust, mustard, mauve, black, grey, white — that line the coast are dotted with watchtowers built over the past thousand years to fend off pirates and other invaders. Behind the beach is a landscape of prickly pear cacti and dwarf fan palms, with only the odd farm visible — you could be in Mexico. The colourful cliffs around Monsul are dotted with lookouts to ward off pirates Credit: Adventurous expats and locals looking for solitude.

    Hotel Carabeo, Nerja — with its top-rated restaurant, this nearby seven-room clifftop guesthouse is a gem. Read the full review of Hotel Carabeo. Es Grau, Menorca At Es Grau, on the north-east coast of Menorca, the Mediterranean stays at shin level for 40 metres out to sea, like a gigantic spa pool.

    Es Grau's shallow waters are ideal for young children Credit: The shallow water is ideal for small children, while teenagers love snorkelling, kayaking and paddle boarding around the bay. Read the full review of Torralbenc. Cala Pregonda, Menorca On the quiet north coast of Menorca, Pregonda is a long beach with reddish-gold sand and pink rocks. Tiny islands protect the bay, so the sea is still and crystalline.

    Solitude on Cala Pregonda Credit: Naeblys - Fotolia Read our expert guide to Menorca Who goes? People prepared to hike for half an hour along a track. Ses Sucreres is a stylishly converted traditional house with six rooms in Ferreries, five miles inland from Cala. Paths wind through the trees on the hillside if you fancy a bit of a hike. Read our expert guide to Majorca Who goes? Those wanting a low-key vibe. Cala Llombards, Majorca This cove on the south-east coast is a triangular strip of white sand framed by pine trees, with boat sheds perched on the rocks.

    Cala Llombards is popular with locals and people staying in nearby villas Credit: Locals and people staying in nearby villas. The shallow water makes it a good choice for small children.

    Cala Codolar, Ibiza The sand is a bit grey and coarse on this small beach, but the sea is a deep sapphire, so who cares? Sheltered by cliffs, Codolar is near the popular Cala Comte, in the west of the island, but is much less frenetic. The beach bar is refreshingly basic with reasonable prices — highly unusual in Ibiza.

    Read our expert guide to Ibiza and its beaches Who goes? This is a beach for families rather than fashionistas; no posing and preening here.
    W Barcelona, Catalonia You'll need a streak of fabulousness to feel really at home in the W — its bars and restaurants are peopled with model types, and its poolside areas can look like catalogue photo shoots on a busy afternoon.

    In contrast to this, and the dazzling lobby, the rooms themselves are a little subdued, but their all-glass fronts do afford spectacular views of the sea, the city or — if you're lucky, or pay a little more — both. Read the full review: Finca Cortesin, Casares, Malaga This is one of the smartest hotels in Spain but it is not remotely flashy. You walk into an atmosphere of soothing luxury with none of the hushed pomposity often prevalent in high end hotels. With lots of space both inside and out, huge pools, great restaurants, a superb spa and a top-level golf course, you can happily just check in and switch off for the duration.

    In the hills just off the coast between Estepona and Sotogrande, just below the pretty village of Casares, the hotel has sweeping views down to the Mediterranean and across the countryside. Finca Cortesin, Malaga Finca Cortesin is one of the smartest hotels in Spain but it is not remotely flashy. France We are reliably schizophrenic about the French.

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    They are both our next-door neighbours, and hereditary foes. Clearly, and like a classy courtesan, France is so damned seductive that she lures us away from fiercely-held principles. You can see how she might. The most diverse country in Europe runs from celebrated mountains to the continent's finest coast via everything else in-between. Beyond, the blue is endless contrasting splendidly with the white of the hotel. Land-side, the hotel is surrounded by a quiet residential zone half-way between the beaches and the city centre, two miles away.

    This is the sea-side for sybarites, who will get the full benefit of a glass of champagne on the terrace. Le Petit Nice, Marseille On a little rocky promontory, Le Petit Marseille is almost a bridge-head into the Med — which starts where the hotel terrace stops. Service is flawless with a no-holds-barred concierge. There is a heated infinity pool, five clay tennis courts, 33 cabanas and a boutique.

    Spa Eden-Roc by La Prairie has four treatment rooms, as well a sauna, steam room, gym and beauty salon. Almost all the 33 bright and airy rooms enjoy full-on sea views; many have more than one window, and most have balconies. Venture further inland, however, and you will find atmospheric villages and monasteries, world-class museums and a laid-back lifestyle pursued mostly in public. The style is minimalist modern, verging on stark, with only trickling water features and occasional shrubbery as relief.

    The fact of having just 74 rooms does lend an intimate, personal feel.

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    Facilities include an appealing spa with indoor swimming pool, two outdoor swimming pools, plus a popular roof terrace with two whirlpool tubs and sun-loungers. Lindos Blu, Rhodes The fact of having just 74 rooms does lend an intimate, personal feel at Lindos Blu.
    The enforcement of these laws, however, can be lax.

    Ever since the Czechoslovakian Velvet Revolution led to the creation of the two independent states Czech Republic and Slovakiaprostitution has been flourishing and has contributed its share to the region's booming tourist economy. It is widespread in Prague and areas near the Republic's western borders with Germany and Austria. Prague is a great place for mongering and this city has amazing selection of different kind of services such as brothels.

    Being new in town is never easy. Some brothels are totally rip-offs and some whorehouses are one of the best ones in the world. Nobody really gives a damn about prostitution in the Czech Republic. As long as there isn't other crimes involved, like drugs or violence, and as long as you aren't shameless about it, like disturbing your neighbors.

    Price for prostitute in Prague for 30 minutes of sex in a private apartment is around to CZK, while some women ask for less, such as CZK. Most prostitutes charge around CZK for a whole night. Prague is slowly becoming more and more known all over the world as a "New Amsterdam ". Both things "sex and drugs" which are tolerated in Amsterdam are also common in Prague.

    Prague is very popular party capital mostly for British guys, who will come there to host stag parties or just have a weekend get away party. Most of the time many of the guys from the bachelor party groups end up having sex with a prostitute and sometimes a prostitute is even included in the stag party packages which many companies sell to the tourists.

    Prague is a quite safe city. If you're walking alone or in drunk, do not show that you would be an easy target for pickpocketing or mugging. Leave your fancy watch and other unnecessary valuables in your hotel room at night time.


    Prague Female Escorts You can find a great variety of escorts in Prague. Information About Escorts There are almost escort websites for prostitution services in the Czech Republicup from 45 inwhich enable sex tourists to book their travel and appointments to buy sex acts before they leave home. Prague has the world's first online brothel, Big Sister, where customers get free sex with the sex acts being broadcast on the internet. Escort services are more expensive. These are services where the whore arrives at a destination selected by the customer.

    The price also depends on the distance; usually it is between and CZK per hour of sex. There are two well known Laufhaus brothels in Prague. A Laufhaus is a place where sex workers rent a room where they can serve clients. Usually prostitutes can arrange their working schedule and decide the pricing theirselves, but sometimes the schedules and prices are decided by the brothel owner.

    The clients walk through the corridors of the house hence the name: Red-light areas in Prague could be defined as areas with brothels or other sexual activities. Show Park Prague If you buy your entrance ticket on internet, it costs only 99 Koruna, at the door it is a little bit more. Once you find a girl you like in the Show Park, you can spend erotic moments in their cozy brothel rooms.

    Club advertises that it is largest adult entertainment complex in all of Europe with two facilities with a total of 81 rooms. Some girls sell extra services as well Bareback blow job, french kissing and anal sex in example. ShowPark Market is open for you everyday from You may go and visit rooms of some of the many beautiful girls at any time during opening hours. Current estimates indicate there are 10, to 25, prostitutes in the country.

    In Prague, the city's third district Praha 3immediately east of the center, is home to much of the city's sex industry.

    Prague's prostitutes are working in different type of places. Most common prostitutes' working places are brothels, massage parlors, streets and internet as escorts. There are lots of porn stars working also as prostitutes in Prague.

    Many world famous porn stars come from Czech Republic. Expect to pay several hundred euros for two hours if you decide to order a real porn star to your hotel room. All night will probably cost you thousands of euros. But if you're wealthy, Prague is one of the best cities in the world having sex with a real porn star! Street Hookers In the street of Prague, the sex prices are lower and the price to have sex with a street prostitute is around CZK and oral sex cost around CZK, but price may even be much lower — depending on the situation of the girl, how far she wants to go, and how badly she needs the money.

    Yet street prostitution is on the decrease in Prague as it gradually moves to apartments, brothels and clubs. You can find streetwalkers in Prague from these areas: There is some street action taking place at the town hall square during the nightime.

    Park between the Muzeum A metro and Muzeum Railway stops.

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    Mostly drug users and Roma gypsy sex workers. In the area around Narodnia and the pedestrian street Rijna leading toward Vaclawske you can usually spot street walkers. It's not that common anymore to see streetwalkers here as it used to be 20 years ago. But still some street action can be found. But especially in Wenceslas Square you also need to be very careful because there are so many scammers and pickpocketing happening.

    Hookers may approach you and grab your nuts and same time the other whore could steal your wallet or cellphone. From the statue to the railway station, dealers, beggars, prostitutes, and pickpockets are allowed to be there because they pay the police," "In the lower half of Wenceslas Square, the police don't want money; they are always changing and they can not be paid off.

    So the upper half profits from sex business and the lower half fights against it. Join to get 10 free private teasers and 9. You can choose any girl from our trusted Live Sex Cams!

    Live Sex Cams are booming at the moment. Webcam models can be found from all over the world and you can find girls, guys, trannies, couples and groups of different ages performing to you. Watching live sex shows is usually free, but if you buy some credits, you will have much better chances to see adult action as desired! It's possible also to hire a webcam model to a private chat room where you can ask the person to fulfill your fantasies.

    Adult Locations Prague is a great place to find adult action.

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