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100-593: The area is part of the Pomeranian coast. The Zingst Peninsula forms an eastward-running spit , nearly 20 km (12 mi) in length, and has a width of just 2 to 4 km (1.2 to 2.5 mi). Zingst separates the Baltic Sea from the lagoon of Barther Bodden , which is part of the Darss-Zingst Bodden Chain , a large estuary . The shallow waters of the inlet are a major stopover for

200-512: A cliff face compress air in cracks on the cliff face. This exerts pressure on the surrounding rock, and can progressively splinter and remove pieces. Over time, the cracks can grow, sometimes forming a cave . The splinters fall to the sea bed where they are subjected to further wave action. Attrition occurs when waves cause loose pieces of rock debris ( scree ) to collide with each other, grinding and chipping each other, progressively becoming smaller, smoother and rounder. Scree also collides with

300-487: A sandblasting effect. This effect helps to erode, smooth and polish rocks. The definition of erosion is grinding and wearing away of rock surfaces through the mechanical action of other rock or sand particles. According to the IPCC, sea level rise caused by climate change will increase coastal erosion worldwide, significantly changing the coasts and low-lying coastal areas. Hydraulic action occurs when waves striking

400-471: A final solution to erosion. Seawalls can also deprive public access to the beach and drastically alter the natural state of the beach. Groynes also drastically alter the natural state of the beach. Some claim that groynes could reduce the interval between beach nourishment projects though they are not seen as a solution to beach nourishment. Other criticisms of seawalls are that they can be expensive, difficult to maintain, and can sometimes cause further damage to

500-475: A horrific case of coastal erosion is due to an increase in the frequency and the intensity of storms it experienced. These natural events had destroyed the Hampton Pier, Hernecliffe Gardens, a set of villas, several roads, and many other structures that once lay on Hampton-On-Sea. After this destruction, in 1899 they started building a sea wall to protect the rest of the remaining land and buildings. However,

600-421: A more permanent solution than soft-erosion control methods. Seawalls and groynes serve as semi-permanent infrastructure. These structures are not immune from normal wear-and-tear and will have to be refurbished or rebuilt. It is estimated the average life span of a seawall is 50–100 years and the average for a groyne is 30–40 years. Because of their relative permanence, it is assumed that these structures can be

700-633: A population of about 3,200. At the former National People's Army training area in the Sundisch meadows from 1970-1992 various experiments were conducted using high-altitude research rockets. In the early 1970s, five Polish Meteor 1E sounding rockets were launched from here. From 21 October 1988, Soviet MMR06 -M rockets were launched. Even after the Wende , trials continued. Between 14 February 1992 and 10 April 1992, 19 Russian MMR06-M rockets were fired from Zingst. Although further rockets were available,

800-548: A rate of over 100 feet per year, earning the area the nickname "Washaway Beach". Much of the original town has collapsed into the ocean. The area is said to be the fastest-eroding shore of the United States' West Coast. Measures were finally taken to slow the erosion, with substantial slowing of the process noted in 2018. Fort Ricasoli , a historic 17th century fortress in Malta is being threatened by coastal erosion, as it

900-558: A relatively low population density , with its largest cities being Gdańsk and Szczecin . Outside its urban areas, it is characterized by farmland, dotted with numerous lakes, forests, and small towns. In the west of Pomerania lie several islands, the largest of which are Rügen , the largest island in Germany; Usedom /Uznam, and Wolin , the largest island in Poland. The region has a rich and complicated political and demographic history at

1000-576: A solution that keeps in mind environmental justice . Typically, there has been low public support for "retreating". However, if a community does decide to relocate their buildings along the coast it is common that they will then turn the land into public open space or transfer it into land trusts in order to protect it. These relocation practices are very cost-efficient, can buffer storm surges, safeguard coastal homes and businesses, lower carbon and other pollutants, create nursery habitats for important fish species, restore open space and wildlife, and bring back

1100-430: A strip the historical Greater Poland ( Tuczno , Człopa , Mirosławiec , Wałcz , and Czaplinek ), or even a small part of Pomerelia ( Biały Bór ); in turn the other one comprises only approximately northern two-thirds of Pomerelia but also parts of historical Malbork Land and Upper Prussia known under the ethnographic designation of Powiśle and constituting the westernmost strip of historical Prussia ; and finally,

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1200-667: A universally accepted definition, since it may refer either to combined Hither and Farther Pomerania only (in German contemporary and historical usage ) or to Hither and Farther Pomerania combined with Pomerelia (in Polish contemporary and historical usage). As a consequence, the term "West Pomerania" is ambiguous, since it may refer to either Hither Pomerania (in German usage and historical usage based on German terminology ), or to combined Hither and Farther Pomerania (in Polish usage and historical usage based on German terminology). In parallel,

1300-697: A whole new range of solutions to coastal erosion, not just structural solutions. Solutions that have potential include native vegetation, wetland protection and restoration, and relocation or removal of structures and debris. The solutions to coastal erosion that include vegetation are called "living shorelines". Living shorelines use plants and other natural elements. Living shorelines are found to be more resilient against storms, improve water quality, increase biodiversity, and provide fishery habitats. Marshes and oyster reefs are examples of vegetation that can be used for living shorelines; they act as natural barriers to waves. Fifteen feet of marsh can absorb fifty percent of

1400-551: A width of 2 to 4 km (1.2 to 2.5 mi) the Zingst stretches eastwards from the adjacent peninsula of Darß . It is bounded to the north by the Baltic and to the south by the lagoons of Barther Bodden und Grabow , that belong to the Darss-Zingst Bodden Chain . The island of Großer Werder , which once lay off the eastern coast of Zingst, has now become attached as a peninsula as a result of sanding up. The land bridge to Darß to

1500-421: A year, 1917, directly due to earlier dredging of shingle in the bay in front of it. The California coast, which has soft cliffs of sedimentary rock and is heavily populated, regularly has incidents of house damage as cliffs erodes. Devil's Slide , Santa Barbara , the coast just north of Ensenada , and Malibu are regularly affected. The Holderness coastline on the east coast of England, just north of

1600-590: Is 7.9. Precipitation is a relatively low 600 millimetres (24 in) per year. The average humidity is very high as a result of its coastal location. As a result the number of dull days is 146. The Osterwald forest is the only raised bog in Mecklenburg-Western Pomerania , but it has been partially dried out as a result of human intervention. The tree species here include birch , English oak , beech and pine . Other trees introduced by humans include alder , spruce and firs . A feature

1700-584: Is a historical region on the southern shore of the Baltic Sea in Central Europe , split between Poland and Germany . The central and eastern part belongs to the West Pomeranian , Pomeranian and Kuyavian-Pomeranian voivodeships of Poland, while the western part belongs to the German states of Mecklenburg-Western Pomerania and Brandenburg . Pomerania's historical border in the west

1800-511: Is due to waves causing erosion of the primarily sedimentary material on which the buildings foundations sit. Dunwich , the capital of the English medieval wool trade, disappeared over the period of a few centuries due to redistribution of sediment by waves. Human interference can also increase coastal erosion: Hallsands in Devon , England, was a coastal village washed away over the course of

1900-532: Is included within the modern West Pomeranian Voivodeship, but its easternmost parts (the Słupsk area) now constitute the northwest of Pomeranian Voivodeship. Farther Pomerania in turn comprises several other historical subregions, most notably the former Principality of Cammin , the Nowogard County, and the Słupsk and Sławno Land . The Lębork and Bytów Land is considered a part of Pomerelia ( Kashubia ) by

2000-439: Is removed from the foreshore depends on the power of the waves crossing the beach . This energy must reach a critical level to remove material from the debris lobe. Debris lobes can be very persistent and can take many years to completely disappear. Beaches dissipate wave energy on the foreshore and provide a measure of protection to the adjoining land. The stability of the foreshore, or its resistance to lowering. Once stable,

2100-587: Is suffering from this problem as well. Hampton-on-Sea is located in Kent, England. It was at one time very popular for its oyster fishing and was very reliant on the sea. Hampton-on-Sea has undergone the effects of coastal erosion since before the 1800s. Hampton-on-Sea's coastal erosion worsened with the increase in global warming and climate change. Global warming is causing a rise in sea level, more intense and frequent storms, and an increase in ocean temperature and precipitation levels. Another reason Hampton-on-Sea had such

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2200-556: Is the redwoods , planted in 1955. Amongst the animal population are tawny owl , red kite and short-eared owl . Pine martens are also common. East of the Prerowstrom, surrounded by countryside and the Freesenbruch, is the town of Barth (population 8,000), which was created by the unification of the settlements of Pahlen, Hanshagen and Rothem ho. Hanshagen and Pahlen date to the 13th century. The nearby town of Zingst has

2300-658: Is the Mecklenburg-Western Pomeranian border Urstromtal , which now constitutes the border between the Mecklenburgian and Pomeranian part of Mecklenburg-Western Pomerania, while it is bounded by the Vistula River in the east. The easternmost part of Pomerania is alternatively known as Pomerelia , consisting of four sub-regions: Kashubia inhabited by ethnic Kashubians , Kociewie , Tuchola Forest and Chełmno Land . Pomerania has

2400-601: Is the loss or displacement of land, or the long-term removal of sediment and rocks along the coastline due to the action of waves , currents , tides , wind-driven water, waterborne ice, or other impacts of storms. The landward retreat of the shoreline can be measured and described over a temporal scale of tides, seasons, and other short-term cyclic processes. Coastal erosion may be caused by hydraulic action, abrasion , impact and corrosion by wind and water, and other forces, natural or unnatural. On non-rocky coasts, coastal erosion results in rock formations in areas where

2500-410: Is transported in a west-to-east direction, and the beach at Zingst loses 40 cm annually. The loss was mainly caused by storm surges, so this process is now severely weakened. Zingst exhibits a North Mecklenburg coastal climate. The annual average temperature is 7.8 °C (46.0 °F). The number of frosty days is 11.1 and the number of hot summer days (temperatures over 25 °C (77 °F))

2600-462: The Lebensraum policy. The Stutthof concentration camp with numerous subcamps was located in the region. There were also numerous Nazi prisons, forced labour camps, and multiple prisoner-of-war camps , including the large Stalag II-B and Stalag II-D , for Polish, French , Belgian, Dutch, Serbian, Italian , American, Canadian, Australian, New Zealander and other Allied POWs. Połczyn-Zdrój

2700-403: The bodden with the Baltic Sea. A road now connects Zingst and Darß, running along a 100 m (330 ft)-wide isthmus . The soils of Zingst consist almost entirely of sand. The sand is white in colour, which makes it popular with sunbathers and tourists. Dunes border the Baltic Sea and enclose low ground about half a metre below sea level. The low-lying land results in boggy conditions in

2800-779: The Central European Plain . Its southern, hilly parts belong to the Baltic Ridge, a belt of terminal moraines formed during the Pleistocene . Within this ridge, a chain of moraine-dammed lakes constitutes the Pomeranian Lake District . The soil is generally rather poor, sometimes sandy or marshy. The western coastline is jagged, with many peninsulas (such as Darß – Zingst ) and islands (including Rügen , Usedom , and Wolin ) enclosing numerous bays ( Bodden ) and lagoons (the biggest being

2900-456: The Communist regimes implemented during the post-war era; since then, Pomerania is democratically governed . Pomeranian dialect and traditions still live in the country of Brazil in a colony where the language is still spoken. The arrival of Pomerania immigrants with Germans and Italians helped form the state of Espírito Santo since the early 1930s. Their importance and respect are one of

3000-675: The Gestapo carried out arrests of Polish leaders, activists, entrepreneurs, and even some staff of the Consulate of Poland in Szczecin. In September 1939, Germany invaded Poland starting World War II . The first battle of the war, at Westerplatte , was fought in the region. Afterwards the Polish part of Pomerania was annexed by Germany, and made part of the Reichsgau Danzig-West Prussia . The Nazis deported

3100-557: The Humber Estuary , is one of the fastest eroding coastlines in Europe due to its soft clay cliffs and powerful waves. Groynes and other artificial measures to keep it under control has only accelerated the process further down the coast, because longshore drift starves the beaches of sand, leaving them more exposed. The white cliffs of Dover have also been affected. The coastline of North Cove, Washington has been eroding at

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3200-646: The Kashubians in Pomerelia . In the German part of Pomerania, Standard German dominates. The historical German dialects of Pomerania are, however, Low German . The Pomeranian dialects were all part of the East Low German subgroup: Mecklenburgisch-Vorpommersch in the west, Central Pomeranian (Mittelpommersch) in Central Pomerania around Szczecin (then Stettin), and East Pomeranian in

3300-696: The Lagoon of Szczecin ). The eastern coastline is smooth. Łebsko and several other lakes were formerly bays, but have been cut off from the sea. The easternmost coastline along the Gdańsk Bay (with the Bay of Puck ) and Vistula Lagoon , has the Hel Peninsula and the Vistula peninsula jutting out into the Baltic. The Pomeranian region has the following administrative divisions: The bulk of Farther Pomerania

3400-560: The Little Kashubian Tricity with a population of 120,158 people (2012), formed by the City of Wejherowo (population 50,310 in 2012) and the towns (urban gminas) of Rumia (population 49,230 in 2020) and Reda (population 26,011 in 2019). The area also includes two smaller towns of Żukowo and Pruszcz Gdański belonging to the eponymous urban-rural gminas, and a number of rural gminas. Altogether, there are 16 cities in

3500-1035: The National Museum in Szczecin , the Museum of the Puck Region , and the Museum of Maritime Fisheries in Świnoujście. Other notable museums include the Museum of the National Anthem ( Muzeum Hymnu Narodowego ) in Będomin at the birthplace of Józef Wybicki , author of the lyrics of the national anthem of Poland , and the Copernicus House in Toruń , birthplace of famed astronomer Nicolaus Copernicus . The Diocesan Museum in Pelplin contains one of

3600-515: The Osterwald . Beyond that are the Sund Meadows ( Sundischen Wiesen ) named after Stralsund. The easternmost point of the peninsula is Pramort . The original island of Zingst is, geologically, a very young landscape. Its formation process began with the end of Weichselian glaciation , about 12,000 years ago. This left behind a Young Drift landscape. As a result of the melting ice sheet,

3700-675: The Stone and Bronze Age , Baltic peoples , Germanic peoples and Veneti during the Iron Age and, in the Dark Ages , West Slavic tribes and Vikings . Starting in the 10th century, early Polish rulers subdued the region, successfully integrating the eastern part with Poland, while the western part fell under the suzerainty of Denmark and the Holy Roman Empire in the late 12th century. Gdańsk , established during

3800-957: The University of Szczecin , the University of Gdańsk and the Nicolaus Copernicus University in Toruń , the oldest of which, the University of Greifswald , was founded when Greifswald belonged to Duchy of Pomerania , thus being one of the oldest universities in the world . The technical universities are the Gdańsk University of Technology , West Pomeranian University of Technology in Szczecin, and Koszalin University of Technology . The Stralsund University of Applied Sciences (Hochschule Stralsund) in Stralsund has around 2,400 students. Agriculture primarily consists of raising livestock, forestry, fishery, and

3900-570: The former eastern territories of Germany and Poles of German ethnicity from Pomerelia were expelled . Between 1945 and 1948, millions of ethnic Germans (Volksdeutsche) and German citizens (Reichsdeutsche), were removed from former German territory now governed by Poland and other Eastern European countries. Many German civilians were sent to internment and labor camps where they were used as forced labor as part of German reparations to countries in Eastern Europe. The death toll attributable to

4000-540: The Amber Museums in Gdańsk and Jarosławiec , and the Museum of Gingerbread in Toruń. There are around 40 museums in the district of Vorpommern-Rügen , the most notable of which are: In the district of Vorpommern-Greifswald are located around 30 museums, among which: There are four traditional (non-profiled and multi-faculty, public research ) universities in the region, namely the University of Greifswald ,

4100-533: The Baltic in the north, the Alte Straminke, an old sea inlet with its surrounding marshes, in the east, and the channel of Zingster Strom in the south. The village is barely above sea level, so that it has to be protected from storm floods by dykes. Further east, on the Zingster Strom, is the village of Müggenburg. East of the village of Zingst lies a large forest, very rich in wildlife, called

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4200-566: The Eastern seaboard of the United States. Locations such as Florida have noticed increased coastal erosion. In reaction to these increases Florida and its individual counties have increased budgets to replenish the eroded sands that attract visitors to Florida and help support its multibillion-dollar tourism industries. There are three common forms of coastal erosion control methods. These three include: soft-erosion controls, hard-erosion controls, and relocation. Hard-erosion control methods provide

4300-758: The German population in the Duchy of Pomerania adopted the Protestant reformation in 1534, the Polish (along with Kashubian ) population remained with the Roman Catholic Church . The Thirty Years' War severely ravaged and depopulated narrow Pomerania; few years later this same happened to Pomerelia ( the Deluge ). With the extinction of the Griffin house during the same period, the Duchy of Pomerania

4400-1116: The Guardhouse no. 1 at Westerplatte (a branch of the Museum of Gdańsk), the Museum of Coastal Defence in Hel , the Stutthof Museum in Sztutowo with the branch Piaśnica Museum in Wejherowo , the Museum of the Pomeranian Wall and World War II in Szczecinek , and the Armory Museum in Kłanino . There are also aquaria: the Gdynia Aquarium and the Seal Sanctuary in Hel . Perhaps more unusual museums include

4500-1090: The Museum of Sopot, the Emigration Museum in Gdynia, the Museum of Polish Navy in Gdynia, the Museum of Kociewie in Starogard Gdański, the Museum of Kashubian and Pomeranian Literature and Music in Wejherowo, the Kashubian Museum in Kartuzy, the Central Pomerania Museum in Słupsk , the Darłowo Museum, the Koszalin Museum, the Museum of Polish Arms in Kołobrzeg, the Museum of Archeology and History in Stargard,

4600-440: The Polish historiography, and of Farther Pomerania by the German historiography. Parts of Pomerania and surrounding regions have constituted a euroregion since 1995. The Pomerania euroregion comprises Hither Pomerania and Uckermark in Germany, West Pomerania in Poland, and Scania in Sweden. In Lechitic languages the prefix "po-" means along ; unlike the word "po", which means after . Pomorze , therefore, means Along

4700-523: The Pomeranian Jews to a reservation near Lublin . The Polish population suffered heavily during the Nazi oppression ; more than 40,000 died in executions, death camps, prisons and forced labour , primarily those who were teachers, businessmen, priests, politicians, former army officers, and civil servants. Thousands of Poles and Kashubians suffered expulsion , their homes taken over by the German military and civil servants, as well as some Baltic Germans resettled there between 1940 and 1943 in accordance with

4800-503: The Pomeranian universities. Since the late 19th century, tourism has been an important sector of the economy, primarily in the numerous seaside resorts along the coast. The Polish Świnoujście LNG terminal is located in Pomerania. Sports enjoying either great popularity or success in Pomerania are football , basketball , speedway , handball , volleyball and rugby union . Most popular and accomplished football teams are Arka Gdynia , Lechia Gdańsk and Pogoń Szczecin , based in

4900-404: The Prerower Strom channel between the Darß and Zingst was artificially closed. Towards the end of the 20th century the former island of Great Werder became connected to the Zingst as the strait between them silted up. This area is a windwatt . The process of land formation continues at the eastern end of the peninsula today. Zingst lies between the accretion zones of Darßer Ort and Bock. Sediment

5000-466: The Sea . This construction is similar to toponyms Pogórze ( Along the Mountains ), Polesie ( Along the Forest ), Porzecze ( Along the River ), etc. Pomerania was first mentioned in an imperial document of 1046, referring to a Zemuzil dux Bomeranorum ( Zemuzil , Duke of the Pomeranians). Pomerania is mentioned repeatedly in the chronicles of Adam of Bremen (c. 1070) and Gallus Anonymous (ca. 1113). The territorial designation "Pomerania" lacks

5100-414: The base of the cliff face, chipping small pieces of rock from the cliff or have a corrasion (abrasion) effect, similar to sandpapering. Solution is the process in which acishutds contained in sea water will dissolve some types of rock such as chalk or limestone. Abrasion , also known as corrasion , occurs when waves break on cliff faces and slowly erode it. As the sea pounds cliff faces it also uses

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5200-655: The beach if built improperly. As we learn more about hard erosion controls it can be said for certain that these structural solutions cause more problems than they solve. They interfere with the natural water currents and prevent sand from shifting along coasts, along with the high costs to install and maintain them, their tendency to cause erosion in adjacent beaches and dunes, and the unintended diversion of stormwater and into other properties. Natural forms of hard-erosion control include planting or maintaining native vegetation, such as mangrove forests and coral reefs. Soft erosion strategies refer to temporary options of slowing

5300-432: The broad-sense Pomerania, understood as comprising also Pomerelia . Their list is presented below and includes the 14 municipalities in Poland electing a city mayor ( Polish : prezydent miasta ) instead of a town mayor ( Polish : burmistrz ), with 9 of them holding the status of a city with powiat rights ( Polish : miasto na prawach powiatu , an independent city ), as well as the 2 municipalities in Germany holding

5400-531: The coastline contains rock layers or fracture zones with varying resistance to erosion. Softer areas become eroded much faster than harder ones, which typically result in landforms such as tunnels , bridges , columns , and pillars . Over time the coast generally evens out. The softer areas fill up with sediment eroded from hard areas, and rock formations are eroded away. Also erosion commonly happens in areas where there are strong winds, loose sand , and soft rocks. The blowing of millions of sharp sand grains creates

5500-556: The cultivation of cereals , sugar beets , and potatoes. Industrial food processing is increasingly relevant in the region. Key producing industries are shipyards , mechanical engineering facilities (i.e. renewable energy components), and sugar refineries , along with paper and wood fabricators. Service industries today are an important economical factor in Pomerania, most notably with logistics, information technology, life science , biotechnology , health care, and other high-tech branches often clustering around research facilities of

5600-431: The cultural signatures of the area. The Brazilian city of Pomerode (in the state of Santa Catarina ) was founded by Pomeranian Germans in 1861 and is considered the most typically German of all the German towns of southern Brazil. The German part of Western Pomerania is inhabited by German Pomeranians . In other parts, Poles are the dominant ethnic group since the territorial changes of Poland after World War II , and

5700-455: The culture of these coastal communities. Storms can cause erosion hundreds of times faster than normal weather. Before-and-after comparisons can be made using data gathered by manual surveying, laser altimeter , or a GPS unit mounted on an ATV. Remote sensing data such as Landsat scenes can be used for large scale and multi year assessments of coastal erosion. Moreover, geostatistical models can be applied to quantify erosion effects and

5800-421: The descendants of émigrées, most notably in the Americas (e.g. Argentina, Brazil, Chile and Canada). Slovincian was spoken at the Farther Pomeranian –Pomerelian frontier, but is now extinct. At least 50 museums in Poland cover the history of Pomerania, the most important of them being the District Museum in Toruń , the Museum in Grudziądz, the National Museum in Gdańsk , the National Maritime Museum, Gdańsk ,

5900-495: The early 14th century the Teutonic Knights invaded and annexed Pomerelia from Poland into their monastic state , which already included historical Prussia . As a result of the Teutonic rule, in German terminology the name of Prussia was also extended to conquered Polish lands like Gdańsk Pomerania , although it was not inhabited by Baltic Prussians but Lechitic Poles. Meanwhile, the Ostsiedlung started to turn Slavic narrow Pomerania into an increasingly German-settled area;

6000-399: The east. The regions east of the Piaśnica river are not considered Pomeranian according to German terminology, but either West Prussian or Pomerelian. Danzig German was hence classified as Low Prussian , like the dialects of East Prussia ( Königsberg ). Those parts of Pomerania that remained German after 1945 are almost entirely located in the Mecklenburgisch-Vorpommersch area. Only

6100-443: The effects of erosion. These options, including Sandbag and beach nourishment , are not intended to be long-term solutions or permanent solutions. Another method, beach scraping or beach bulldozing allows for the creation of an artificial dune in front of a building or as means of preserving a building foundation. However, there is a U.S. federal moratorium on beach bulldozing during turtle nesting season, 1 May – 15 November. One of

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6200-548: The energy of incoming waves. Relocation of infrastructure any housing farther away from the coast is also an option. The natural processes of both absolute and relative sea level rise and erosion are considered in rebuilding. Depending on factors such as the severity of the erosion, as well as the natural landscape of the property, relocation could simply mean moving inland by a short distance or relocation can be to completely remove improvements from an area. A coproduction approach combined with managed retreat has been proposed as

6300-427: The expelled Pomeranians found refuge there, later many moved on to other German regions and abroad. Today German Hither Pomerania forms the eastern part of the state of Mecklenburg-Vorpommern , while the Polish part is divided mainly between the West Pomeranian , Pomeranian voivodeships, with their capitals in Szczecin and Gdańsk . During the 1980s, the Solidarity and Die Wende ("the change") movements overthrew

6400-420: The finest collections of medieval art in Poland, and the country's sole copy of the Gutenberg Bible . Medieval open-air museums are the Grodzisko in Sopot and Skansen in Wolin . There are also the Dar Pomorza , ORP Błyskawica and SS Sołdek museum ships . Several museums devoted to World War II history are located in Polish Pomerania, including the Museum of the Second World War in Gdańsk,

6500-461: The flight and expulsions is disputed, with low-range estimates in the hundreds of thousands (see: Flight and expulsion of Germans (1944–1950) ). The area was resettled primarily with Poles of Polish ethnicity, (some themselves expellees from former eastern Poland ) and some Poles of Ukrainian ethnicity (resettled under Operation Vistula ) and few Polish Jews . Most of Hither or Western Pomerania ( Vorpommern ) remained in Germany, and most of

6600-399: The foreshore should widen and become more effective at dissipating the wave energy, so that fewer and less powerful waves reach beyond it. The provision of updrift material coming onto the foreshore beneath the cliff helps to ensure a stable beach. The adjacent bathymetry , or configuration of the seafloor, controls the wave energy arriving at the coast, and can have an important influence on

6700-450: The former Swedish parts were reorganized into the Prussian Province of Pomerania , while Pomerelia was made part of the Province of West Prussia . With Prussia, both provinces joined the newly constituted German Empire in 1871. Under German rule, the Polish minority suffered discrimination and oppressive measures aimed at eradicating its culture. Following the German Empire's defeat in World War I, however, eastern Pomerania/ Pomerelia

6800-444: The function of a natural storm beach , may be a soft-erosion control alternative in high energy environments such as open coastlines. Over the years beach nourishment has become a very controversial shore protection measure: It has the potential to negatively impact several of the natural resources. Some large issues with these beach nourishment projects are that they must follow a wide range of complex laws and regulations, as well as

6900-400: The high expenses it takes to complete these projects. Just because sand is added to a beach does not mean it will stay there. Some communities will bring in large volumes of sand repeatedly only for it to be washed away with the next big storm. Despite these factors, beach nourishment is still used often in many communities. Lately, the U.S. Army Corps of Engineers emphasized the need to consider

7000-416: The historical ones with Mecklenburg and Brandenburg . As a consequence, the common understanding of the terms has started to be used more and more frequently in the sense of the current administrative units. Settlement in the area called Pomerania for the last 1,000 years started by the end of the Vistula Glacial Stage , some 13,000 years ago. Archeological traces have been found of various cultures during

7100-500: The historical region of Hither Pomerania today, while the Szczecin metropolitan area reaches even further. Pomerelia is dominated by the Tricity metropolitan area (Pomeranian Voivodeship) with its population in 2012 estimated at least at 1,035,000 and the area at 1,332,51 km , encompassing the Tricity itself with a population of 748,986 combining the eponymous three cities of Gdańsk (population 460,427), Gdynia (population 248,726) and Sopot (population 38,217), as well as

7200-665: The historically Brandenburgian headwaters of the Uecker river ( Prenzlau ). In Mecklenburg-Vorpommern , however, the dominating Low German standard version is the Mecklenburgisch-Vorpommersch dialect, and Central Pomeranian texts are often rewritten. East Pomeranian, Low Prussian , and Standard German were dominating east of the Oder-Neisse line before most of its speakers were expelled after World War II . Kashubian and East Low German are also spoken by

7300-505: The interior of the peninsula, and these bogs offer habitat to a wide variety of wildlife. The ruins of a Slavic fort, the 'Hertesburg,' are on the Zingst peninsula near Zingst municipality. The peninsula of Zingst or the Zingst is the easternmost part of the Fischland-Darß-Zingst peninsula that lies between the city of Rostock and town of Stralsund on the southern Baltic Sea coast. With a length of just under 20 km and

7400-466: The intersection of several cultures. Pomerania is the area along the Bay of Pomerania of the Baltic Sea between the rivers Recknitz , Trebel , Tollense and Augraben in the west and Vistula in the east. It formerly reached perhaps as far south as the Noteć river, but since the 13th century its southern boundary has been placed further north. Most of the region is coastal lowland, being part of

7500-594: The late 12th-early 13th century, the Griffin Duchy of Pomerania stayed with the Holy Roman Empire and the Principality of Rugia with Denmark, while Pomerelia, under the ruling of Samborides , was a part of Poland. Pomerania, during its alliance in the Holy Roman Empire , shared borders with West Slavic state Oldenburg, as well as Poland and the expanding Margraviate of Brandenburg . In

7600-488: The launch of MMR06-M rockets on Zingst had to be stopped in April 1992 because the army needed to clear the site to make the out of bounds area safe. 54°25′N 12°40′E  /  54.417°N 12.667°E  / 54.417; 12.667 Pomerania Pomerania ( Polish : Pomorze [pɔˈmɔʐɛ] ; German : Pommern [ˈpɔmɐn] ; Pòmòrskô ; Swedish : Pommern )

7700-574: The migratory European crane . In spring and autumn, up to 3,000 birds gather here on their migration route to and from Spain. Most of the estuary and the eastern end of the peninsula are part of the Western Pomerania Lagoon Area National Park . Until the early 1870s, Zingst was an island, separated from Darß by the Prerowstrom , a narrow inlet. A storm tide in 1874 closed the inlet, which had connected

7800-416: The most common methods of soft erosion control is beach nourishment projects. These projects involve dredging sand and moving it to the beaches as a means of reestablishing the sand lost due to erosion. In some situations, beach nourishment is not a suitable measure to take for erosion control, such as in areas with sand sinks or frequent and large storms. Dynamic revetment , which uses loose cobble to mimic

7900-475: The natural temporal and spatial evolution of tracked coastal coastal profiles. The results can be used to determine the required temporal and spatial distances between the measured profiles for ecomic tracking. A place where erosion of a cliffed coast has occurred is at Wamberal in the Central Coast region of New South Wales where houses built on top of the cliffs began to collapse into the sea. This

8000-473: The rate of cliff erosion. Shoals and bars offer protection from wave erosion by causing storm waves to break and dissipate their energy before reaching the shore. Given the dynamic nature of the seafloor, changes in the location of shoals and bars may cause the locus of beach or cliff erosion to change position along the shore. Coastal erosion has been greatly affected by the rising sea levels globally. There has been great measures of increased coastal erosion on

8100-402: The rate of reaction by removing the reacted material. The ability of waves to cause erosion of the cliff face depends on many factors. The hardness (or inversely, the erodibility ) of sea-facing rocks is controlled by the rock strength and the presence of fissures , fractures , and beds of non-cohesive materials such as silt and fine sand . The rate at which cliff fall debris

8200-706: The regions between the Zarow river in the west and the Oder river in the east are historically part of the Central Pomeranian dialect region: the southern shores of the Szczecin Lagoon ( Ueckermünde ), the towns along the Uecker and Randow rivers, and those parts of Pomerania that are now in Brandenburg ( Gartz and the northern districts of Schwedt/Oder ). Central Pomeranian is also spoken along

8300-531: The reign of Mieszko I of Poland has since become Poland's main port (apart from periods of Poland losing control over the region). In the 12th century, the Duchy of Pomerania (western part), as a vassal state of Poland, became Christian under saint Otto of Bamberg ( the Apostle of the Pomeranians ); at the same time Pomerelia (eastern part) became a part of diocese of Włocławek within Poland. Since

8400-823: The remaining Wends and Polish people, often known as Kashubians , continued to settle within Pomerelia. In 1325 the line of the princes of Rügen died out, and the principality was inherited by the Griffins . In 1466, with the Teutonic Order 's defeat in the Thirteen Years' War , Pomerelia became again part of the Polish Crown and formed the Pomeranian Voivodeship within the provinces of Royal Prussia and Greater Poland . While

8500-410: The remaining one third of Pomerelia forms part of województwo kujawsko-pomorskie ( Kuyavian-Pomeranian Voivodeship ), a further regional unit, in this case bearing a name accurately reflecting historical heterogeneity of its territory. Similarity but to lesser extent, borders of the combined German districts Vorpommern-Rügen and Vorpommern-Greifswald deviate significantly in numerous locations from

8600-559: The resulting Polonization . Kashubians , descendants of the medieval West Slavic Pomeranians , are numerous in rural Pomerelia . German Hither Pomerania had a population of about 470,000 in 2012 (districts of Vorpommern-Rügen and Vorpommern-Greifswald combined) – while the Polish districts of Hither Pomerania had a population of about 580,000 in 2012 ( Szczecin and Świnoujście cities with powiat rights , Police County , as well as Goleniów Wolin and Międzyzdroje gminas combined). So overall, about 1.15 million people live in

8700-562: The salt water inflow from the North Sea reduced greatly and, since then, the Baltic Sea has slowly become less salty. Coastal erosion (abrasion, dispersal and deposition) has extended the original islands in the course of time to their present form. About 1,500 years ago, the ever-lengthening spits cut off the bays lying behind them, forming a string of lagoons known as the Darss-Zingst Bodden Chain. Finally, in 1874,

8800-414: The scree from other wave actions to batter and break off pieces of rock from higher up the cliff face which can be used for this same wave action and attrition. Corrosion or solution/chemical weathering occurs when the sea's pH (anything below pH 7.0) corrodes rocks on a cliff face. Limestone cliff faces, which have a moderately high pH, are particularly affected in this way. Wave action also increases

8900-426: The sea wall did not offer much help: buildings continued to be affected by the erosion. Then a storm came and broke the sea wall, it then flooded the land behind it. These events cause many land investors to back out. Eventually, Hampton-on-Sea had to be abandoned because the erosion overtook so much of the land. By 1916 Hampton-on-Sea had been completely abandoned. By the 1920s only a couple of structures still stood. It

9000-440: The status of a district-belonging city (German: Große kreisangehörige Stadt ), as no city of the German part of Pomerania holds currently any higher status, such as a partially of fully independent city (German: Große selbständige Stadt , Kreisfreie Stadt , or Stadtkreis ), or a city-state (German: Stadtstaat ). Polish is the dominating language in the Polish part of Pomerania. Kashubian dialects are also spoken by

9100-491: The term "East Pomerania" may similarly carry different meanings, referring either to Farther Pomerania (in German usage and historical usage based on German terminology ), or to Pomerelia (in Polish usage and historical usage based on German terminology). As a further complication, the borders of the eponymous administrative units have been drawn disregarding mostly the historical ones. The Polish unit called województwo zachodniopomorskie ( West Pomeranian Voivodeship ) includes

9200-492: The three largest cities. Among the most successful Polish basketball teams are the Arka Gdynia men's and women's teams. Other popular men's clubs are Czarni Słupsk , Spójnia Stargard , Trefl Sopot , Wilki Morskie Szczecin , Polpharma Starogard Gdański . The most successful speedway club is KS Toruń , while other popular teams are Wybrzeże Gdańsk and GKM Grudziądz . Coastal erosion Coastal erosion

9300-521: The underlying land lifted and the hollows were filled with water and the predecessor to the Baltic Sea, Lake Ancylus , was created. The tops of the ridges remained exposed as islands. The major outline of the coasts in the southern area of the Baltic Sea were formed by the Littorina transgression , about 7,000 to 2,500 years ago. About 5,000 years ago, the sea reached its present level and the cores of today's Darß and Zingst became islands. 4,500 years ago,

9400-459: The west is only about 100 m (330 ft) wide and right on the Baltic Sea. At this spot in 1874 the inlet of Prerower Strom , which had hitherto lined the lagoon and the Baltic, was artificially closed following the 1872 Baltic Sea flood . Only since that time has Zingst no longer been an island. The settlement heart of the village of Zingst lies between the Freesenbruch in the west,

9500-562: The whole Polish part of Hither Pomerania, but only the western two-thirds of Farther Pomerania, with the remaining easternmost one-third ( Słupsk , Ustka , and Miastko ) has been part of the województwo pomorskie ([East-] Pomeranian Voivodeship ). The former regional unit stretches however far more south than the historical region, to include the northern part of the historical Neumark ( Dębno , Chojna , Trzcińsko-Zdrój , Myślibórz , Nowogródek Pomorski , Lipiany , Barlinek , Pełczyce , Suchań , Choszczno , Recz , and Drawno ), as well as

9600-410: Was built on a fault in the headland which is prone to erosion. A small part of one of the bastion walls has already collapsed since the land under it has eroded, and there are cracks in other walls as well. In El Campello , Spain, the erosion and failure of a Roman fish farm excavated from rock during the first century B.C. was exacerbated by the construction of a close sport harbour. Hampton-on-Sea

9700-589: Was divided between the Swedish Empire and Brandenburg-Prussia in 1648 , while Pomerelia remained in with the Polish Crown. Prussia gained the southern parts of Swedish Pomerania in 1720, invaded and annexed Pomerelia from Poland in 1772 and 1793, and gained the remainder of Swedish Pomerania in 1815 , after the Napoleonic Wars . The former Brandenburg-Prussian Pomerania and

9800-618: Was expanded to include northern parts of the former Province of Posen–West Prussia (part of historic Greater Poland ). Under the Nazi government , the persecution of Poles in the German-controlled part of Pomerania intensified. In January 1939, Germany resumed expulsions of Poles and many were also forced to flee. The Sturmabteilung , Schutzstaffel , Hitler Youth and Bund Deutscher Osten launched attacks on Polish institutions, schools and activists. From May to August 1939,

9900-500: Was returned to the rebuilt Polish state, while German-majority Gdańsk/Danzig was transformed into the independent Free City of Danzig . In the interbellum, the border with Poland and the creation of what German propaganda called the " Polish Corridor " were often contested in Germany. Irredentist claims towards Poland were one of the factors contributing to the rise of the Nazi Party in Germany. In 1938 Germany's Province of Pomerania

10000-645: Was the location of a Germanisation camp for kidnapped Polish children . The Polish resistance movement was active both in the pre-war Polish part and the pre-war German part of Pomerania. After Nazi Germany 's defeat in World War II, the German–Polish border was shifted west to the Oder–Neisse line , and all of Pomerania was in the Soviet Occupation Zone . The German inhabitants of

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