112-577: Aarwangen District is a constitutional district in the northeast corner of the canton of Bern in Switzerland , with its seat at Aarwangen . From 1 January 2010, the district lost its administrative power. Since 2010, it remains a fully recognised district under the law and the Constitution (Art.3 al.2) of the Canton of Berne. Its municipalities became part of the administrative region Emmental-Oberaargau . It
224-1304: A lesser extent in the Southern Hemisphere. They have different names, historically developed and depending on their geographic distributions: Fraser (in the Pacific Cordillera of North America), Pinedale (in the Central Rocky Mountains ), Wisconsinan or Wisconsin (in central North America), Devensian (in the British Isles), Midlandian (in Ireland), Würm (in the Alps ), Mérida (in Venezuela ), Weichselian or Vistulian (in Northern Europe and northern Central Europe), Valdai in Russia and Zyryanka in Siberia , Llanquihue in Chile , and Otira in New Zealand. The geochronological Late Pleistocene includes
336-584: A mutual defense league with Unterwalden . Bern responded with a military expedition to the Bernese Oberland , which ended in defeat for Unterwalden and its allies. By 1472, Bern was the patron of the Monastery. During the Protestant Reformation , the Monastery was secularized in 1528. The canons received a financial settlement and the properties were now managed by a Bernese bailiff . The tenants of
448-676: A potter's wheel, and was painted with multi-colored ornamentation. The transition to the Late Iron Age of the La Tène culture (450−1st century BCE) is indicated by a sudden change of style in the metalworking and ceramic industries. Numerous graves (from unknown settlements), along with the two oppida at Bern-Engehalbinsel and Jensberg by Studen , mark the population centers during the late Iron Age . Gold coins (from Melchnau ) along with silver and bronze coins first start to appear during this era. A sword with Greek characters that said Korisios
560-619: A program of city founding. The cities of Burgdorf , Murten , Thun and Bern were all founded by Berchtold V. When he died without an heir, the Zähringen lands went to the House of Kyburg , while the offices and fiefs reverted to the empire. During the High Middle Ages both the Aare valley and the Bernese Oberland were divided into a number of small counties, each with their own baron . Nobles from
672-513: A result of melting ice, the land has continued to rise yearly in Scandinavia, mostly in northern Sweden and Finland, where the land is rising at a rate of as much as 8–9 mm per year, or 1 m in 100 years. This is important for archaeologists, since a site that was coastal in the Nordic Stone Age now is inland and can be dated by its relative distance from the present shore. The term Würm
784-452: A single ice age given the continual presence of ice sheets near both poles. Glacials are somewhat better defined, as colder phases during which glaciers advance, separated by relatively warm interglacials . The end of the last glacial period, which was about 10,000 years ago, is often called the end of the ice age, although extensive year-round ice persists in Antarctica and Greenland . Over
896-762: A still lesser extent, glaciers existed in Africa, for example in the High Atlas , the mountains of Morocco , the Mount Atakor massif in southern Algeria , and several mountains in Ethiopia . Just south of the equator, an ice cap of several hundred square kilometers was present on the east African mountains in the Kilimanjaro massif , Mount Kenya , and the Rwenzori Mountains , which still bear relic glaciers today. Glaciation of
1008-594: Is derived from a river in the Alpine foreland, roughly marking the maximum glacier advance of this particular glacial period. The Alps were where the first systematic scientific research on ice ages was conducted by Louis Agassiz at the beginning of the 19th century. Here, the Würm glaciation of the LGP was intensively studied. Pollen analysis , the statistical analyses of microfossilized plant pollens found in geological deposits, chronicled
1120-465: Is one of the 26 cantons forming the Swiss Confederation . Its capital city, Bern , is also the de facto capital of Switzerland. The bear is the heraldic symbol of the canton, displayed on a red-yellow background. Comprising ten districts , Bern is the second-largest canton by both surface area and population. Located in west-central Switzerland, it is surrounded by eleven cantons. It borders
1232-634: Is ongoing. The glaciation and the current Quaternary Period both began with the formation of the Arctic ice cap . The Antarctic ice sheet began to form earlier, at about 34 Mya, in the mid- Cenozoic ( Eocene–Oligocene extinction event ), and the term Late Cenozoic Ice Age is used to include this early phase with the current glaciation. The previous ice age within the Quaternary is the Penultimate Glacial Period , which ended about 128,000 years ago,
SECTION 10
#17328722961141344-662: Is surrounded by the canton of Solothurn on the north, the canton of Aargau on the northeast, the canton of Lucerne on the east, the district of Trachselwald on the south, the district of Burgdorf on the southwest, and the district of Wangen on the west. The district includes the following 25 municipalities and has an area of 154 km (59 sq mi): 47°14′00″N 7°46′00″E / 47.2333°N 7.76667°E / 47.2333; 7.76667 Canton of Bern The canton of Bern , or Berne ( German : Kanton Bern ; French : canton de Berne ; Romansh : Chantun Berna ; Italian : Canton Berna ),
1456-623: Is usually considered the date of Bern's entrance into the Swiss Confederation; however, the alliance only indirectly tied Bern to Zürich and Lucerne. In 1358 the cash-strapped Count Peter II of Aarberg pawned the County of Aarberg to Bern. However, in 1367 he sold it, without repaying Bern, to his cousin Rudolf IV of Nidau. After Rudolf's death (1375) Bern acquired clear right to the Aarberg lands from
1568-724: The Burgdorferkrieg or Kyburgerkrieg ) allowed Bern to move against the Habsburgs in Aargau. After the Bernese laid siege to Burgdorf, Neu-Kyburg was forced to concede an unfavourable peace. Bern bought Thun and Burgdorf, the most important cities of Neu-Kyburg, and their remaining towns passed to Bern and Solothurn by 1408. The last of the Neu-Kyburgs, Berchtold, died destitute in Bern in 1417. In 1386,
1680-669: The Aare , the transition from the Gallo-Roman dominated population to a Germanic population in the Early Middle Ages happened relatively peacefully. One exception was the Battle of Wangen in 610, but elsewhere it generally was a slow process of cultural infiltration. By the 7th century, the Alamannic settlers had already taken most of the good locations southeast of the Aare and they began moving up
1792-758: The Austrians under Leopold of Habsburg invaded eastern Switzerland. When they besieged the city of Sempach , troops from Zürich, Lucerne and the Forest Cantons marched out and defeated the Austrians at the Battle of Sempach . While Bern was not involved at Sempach they took advantage of the Austrian weakness to march into the Oberland in 1386, followed by the Seeland (the region south of
1904-624: The Bäuerten (farming cooperative municipalities) and Talverbänden (rural alpine communities). However, throughout the Late Middle Ages, the Oberland, as a whole or in part, revolted several times against Bernese authority. The Evil League ( Böser Bund ) in 1445 fought against Bernese military service and taxes following the Old Zürich War , in 1528 the Oberland rose up in resistance to the Protestant Reformation and in 1641 Thun revolted. In
2016-558: The Cluniac Priory of Rüeggisberg (Lords of Rümligen in 1072), Münchenwiler (Wiler family in 1080), St. Peter's Island (Count of Hochburgund-Mâcon in the late 11th century), Hettiswil (1107), Röthenbach im Emmental (Lords of Rümligen or Signau), the Benedictine monastery at St. Johannsen in Erlach (Fenis family in 1100), Trub (Lords of Lützelflüh before 1130) and Rüegsau (possibly also
2128-768: The Helvetii were forced to return to their homes as foederati of the Romans. Under increasing Roman influence, the local economy and trade flourished. The main settlements lay at the foot of the Jura Mountains and on the Central Plateau . The existing roads were expanded, especially the Aventicum - Vindonissa and the Petinesca - Augusta Raurica roads. A fourth alpine pass, the Rawil pass ,
2240-733: The Holy Roman Empire , the canton of Bern entered an alliance with the Swiss Forest Cantons in 1323 and joined the Old Swiss Confederacy in 1353. Bern joined the Old Swiss Confederation in 1353. Between 1803 and 1814 it was one of the six directorial cantons of the Napoleonic Swiss Confederation . The earliest traces of a human presence in the area of the modern Canton is found in three caves in
2352-664: The Last glacial cycle , occurred from the end of the Last Interglacial to the beginning of the Holocene , c. 115,000 – c. 11,700 years ago, and thus corresponds to most of the timespan of the Late Pleistocene . The LGP is part of a larger sequence of glacial and interglacial periods known as the Quaternary glaciation which started around 2,588,000 years ago and
SECTION 20
#17328722961142464-585: The Lesotho Highlands and parts of the Drakensberg . The development of glaciers was likely aided in part due to shade provided by adjacent cliffs. Various moraines and former glacial niches have been identified in the eastern Lesotho Highlands a few kilometres west of the Great Escarpment , at altitudes greater than 3,000 m on south-facing slopes. Studies suggest that the annual average temperature in
2576-838: The Ottonian and Salian dynasties. The succession dispute following the death of Rudolph III in 1032 allowed the Salian kings to acquire the Kingdom of Upper Burgundy and with it the Aare valley. As a part of the Holy Roman Empire, the valley was involved when the Investiture Controversy broke out in 1056. In 1077, the Regent of Burgundy, Count Rudolf of Rheinfelden , declared himself as an anti-king against King Henry IV . The Bishops of Basel and Lausanne remained loyal to King Henry IV, and took
2688-697: The Owen Stanley Range , and the Saruwaged Range . Mount Giluwe in the Central Cordillera had a "more or less continuous ice cap covering about 188 km and extending down to 3200-3500 m". In Western New Guinea , remnants of these glaciers are still preserved atop Puncak Jaya and Ngga Pilimsit . Small glaciers developed in a few favorable places in Southern Africa during the last glacial period. These small glaciers would have been located in
2800-634: The Sense/Singine area ended without resolving anything. In 1334, Bern fought with the Barons of Weissenburg and occupied Wimmis and Unspunnen in the Oberland. Bern's victory allowed them to bring the Oberhasli region, its capital of Meiringen and Weissenburg under their control. Bern's continued expansion was at the expense of the feudal lords in the surrounding lands. In 1339 the Habsburgs, Kyburgs and Fribourg, marched against Bern with 17,000 men and besieged
2912-417: The Sierra Nevada in northern California . In northern Eurasia, the Scandinavian ice sheet once again reached the northern parts of the British Isles , Germany , Poland , and Russia, extending as far east as the Taymyr Peninsula in western Siberia. The maximum extent of western Siberian glaciation was reached by about 18,000 to 17,000 BP, later than in Europe (22,000–18,000 BP). Northeastern Siberia
3024-589: The Simmental region; Schnurenloch near Oberwil , Ranggiloch above Boltigen and Chilchlihöhle above Erlenbach . These caves were used at various times during the last ice age . The first open-air settlement in the area is an upper paleolithic settlement at Moosbühl in Moosseedorf. During the warmer climate of the mesolithic period, increasing forest cover restricted the movement of hunters, fishers and gatherers. Their temporary settlements were built along lake and marsh edges, which remained free of trees due to fluctuations in water level. Important mesolithic sites in
3136-479: The Swiss Plateau (the Bernese Mittelland) and the Alps (the Bernese Oberland ). The canton of Bern is bilingual , officially German - and French -speaking, and has a population (as of 31 December 2020) of 1,043,132. The largest city, Bern, is also the seat of the federal government of Switzerland. Other major cities are Thun and Biel/Bienne . The canton is also renowned for its numerous Alpine resort towns, notably Interlaken and Gstaad . Formerly part of
3248-469: The Upper Mississippi River , which in turn was formed during an earlier glacial period. In its retreat, the Wisconsin episode glaciation left terminal moraines that form Long Island , Block Island , Cape Cod , Nomans Land , Martha's Vineyard , Nantucket , Sable Island , and the Oak Ridges Moraine in south-central Ontario, Canada. In Wisconsin itself, it left the Kettle Moraine . The drumlins and eskers formed at its melting edge are landmarks of
3360-416: The Younger Dryas , began around 12,800 years ago and ended around 11,700 years ago, also marking the end of the LGP and the Pleistocene epoch. It was followed by the Holocene , the current geological epoch . The LGP is often colloquially referred to as the "last ice age", though the term ice age is not strictly defined, and on a longer geological perspective, the last few million years could be termed
3472-438: The bishopric of Basel , while the canton of Léman became the canton of Vaud and remained separate from Bern. Bern still remained the largest canton of the confederacy from 1815 to 1979, when parts of the Bernese Jura broke away to form the canton of Jura . In 1994 the Laufen District was transferred to the canton of Basel-Landschaft . The canton of Bern is mainly drained by the river Aare and its tributaries. The area of
Aarwangen District - Misplaced Pages Continue
3584-400: The grooves left by these glaciers can be easily observed. In southwestern Saskatchewan and southeastern Alberta, a suture zone between the Laurentide and Cordilleran ice sheets formed the Cypress Hills , which is the northernmost point in North America that remained south of the continental ice sheets. The Great Lakes are the result of glacial scour and pooling of meltwater at the rim of
3696-475: The isostatically depressed area, a temporary marine incursion that geologists dub the Yoldia Sea . Then, as postglacial isostatic rebound lifted the region about 9500 BP, the deepest basin of the Baltic became a freshwater lake, in palaeological contexts referred to as Ancylus Lake , which is identifiable in the freshwater fauna found in sediment cores. The lake was filled by glacial runoff, but as worldwide sea level continued rising, saltwater again breached
3808-418: The 10th century, the Aare valley came fully under the Second Kingdom of Burgundy . Under King Rudolph I and his son Rudolph II Burgundy's influence reached across most of modern Switzerland. They established royal courts at Bümpliz, Münsingen, Uetendorf, Wimmis, Kirchberg and Utzenstorf to allow them to govern the Aare valley. Later, the Aare valley moved toward closer ties with the Holy Roman Empire during
3920-416: The Aare to the regions of Lake Thun and Lake Brienz . All areas west of the Aare belonged to the romanised Burgundian kingdom, which became part of the Merovingian Frankish kingdom in the 534. During the Carolingian era , the political structure of the Franks had spread into parts of what became Switzerland. In 762/778 the County of Aargau was founded, followed in 861 by the County of Oberaargau and in 965
4032-411: The Aare valley were created over ruins of Roman villas and subsequent burial grounds in the 7th century (including Meikirch and Oberbipp). In Mett, the church was built over a 5th-century mausoleum, which was built over a 4th-century tomb. In 700, six sarcophagi were buried on St. Peter's Island next to a Roman temple complex. A wooden monastery was built over the complex in the 8th–9th century. During
4144-410: The Alpine foreland . Local ice fields or small ice sheets could be found capping the highest massifs of the Pyrenees , the Carpathian Mountains , the Balkan Mountains , the Caucasus , and the mountains of Turkey and Iran . In the Himalayas and the Tibetan Plateau , there is evidence that glaciers advanced considerably, particularly between 47,000 and 27,000 BP, but the exact ages, as well as
4256-440: The Bernese Oberland during the 13th and the beginning of the 14th century Interlaken Monastery grew to become the largest landholder in the region. The Monastery controlled the towns of Grindelwald , Lauterbrunnen and numerous farms along Lake Brienz . However, in 1350 a period of crises and conflicts led to a decline in the number of monks and nuns and increasing debt. In 1348, the people of Grindelwald and Wilderswil joined
4368-501: The Bernese invasions of Aargau in 1415 and Valais in 1418. The military losses and taxes following the Old Zürich War led Saanen to support the Evil League ( Böser Bund ) in 1445 against Bern. In 1475, during the Burgundian Wars , the mountain regions of Saanen and Pays-d'Enhaut , who were allied with Bern, attacked and burned the tower of Aigle Castle . They then gave Aigle town and the surrounding district to Bern in exchange for not having to pay one-third of their income to Bern. In
4480-503: The Bernese occupation was not popular amongst the population. In 1723, Major Abraham Davel led a revolt against Bern, in protest at what he saw as the denial of political rights of the French-speaking Vaudois by the German-speaking Bernese, and was subsequently beheaded. Inspired by the French Revolution , the Vaudois drove out the Bernese governor in 1798 and declared the Lemanic Republic . Vaud nationalists like Frédéric-César de La Harpe had called for French intervention in liberating
4592-433: The Bernese retook Grandson. After Charles' defeat at the Battle of Murten , Grandson became a shared territory between Bern and Fribourg. Each city appointed a vogt for five-year periods. Aigle and Grandson were the first French speaking regions in the Canton of Bern. During the Burgundian War in 1475, Saanen, together with troops from Château-d'Œx and the Simmental captured the Savoy district of Aigle for Bern. Saanen and
Aarwangen District - Misplaced Pages Continue
4704-434: The Canton are at Pieterlenmoos and Burgäschisee lake along with alpine valleys at Diemtig and Simmental. During the neolithic period, there were a number of settlements on the shores of Lake Biel , the Toteisbecken (Lobsigensee, Moossee, Burgäschisee and Inkwilersee) and along rivers ( Aare , Zihl ). Several of these sites are part of the Prehistoric Pile dwellings around the Alps , a UNESCO World Heritage Site . One of
4816-524: The Center for Arctic Gas Hydrate, Environment and Climate at the University of Tromsø , published a study in June 2017 describing over a hundred ocean sediment craters, some 3,000 m wide and up to 300 m deep, formed by explosive eruptions of methane from destabilized methane hydrates , following ice-sheet retreat during the LGP, around 12,000 years ago. These areas around the Barents Sea still seep methane today. The study hypothesized that existing bulges containing methane reservoirs could eventually have
4928-443: The Counts. In 1340 the Saanen valley concluded a peace treaty with the Simmental , which provided for arbitration in disputes. They entered into another treaty in 1393 with the Valais. In 1401, Count Rudolph of Gruyère entered into a treaty with Bern which included Saanen. Two years later Saanen and Château-d'Œx negotiated their own alliances with Bern. Due to the Bernese alliance, Saanen sent troops, under their own banner, to support
5040-504: The County of Bargen. The Treaty of Verdun in 843 put the border between Central and Eastern Frankish Empires at the Aare, and divided the Aare region in half. The population west of the Aare generally spoke a Romance language , while those to the east spoke a Germanic language . The region between the rivers Saane and Aare became the language border. Christianity spread slowly into the Aare valley. The dioceses of Lausanne , Basel , Sion , Chur and Constance were all established before
5152-474: The Greenland climate was dry during the LGP, with precipitation reaching perhaps only 20% of today's value. The name Mérida glaciation is proposed to designate the alpine glaciation that affected the central Venezuelan Andes during the Late Pleistocene. Two main moraine levels have been recognized - one with an elevation of 2,600–2,700 m (8,500–8,900 ft), and another with an elevation of 3,000–3,500 m (9,800–11,500 ft). The snow line during
5264-402: The Holy Roman Empire began to marry into the local noble families and a number of the Zähringen Ministerialis families (unfree knights in the service of a feudal overlord) moved into the Oberland. The nobles also began to found monasteries to spread their power into the Oberland. During the period between 1070 and 1150, at least ten large monasteries were founded by local nobles. These include;
5376-415: The Jura Mountains containing the Morat (Murten) , Neuchâtel and Bienne (Biel) lakes) in 1388 and the Aargau in 1389. In the peace agreement of 1389 Bern got Unterseen and the Upper Simme valley ( Simmental ) from the Habsburgs. In the same year, Fribourg accepted Berns acquisition of the Iselgaus, i.e. the area between Lake Biel and the Seeland. Over the next several decades Bern continued to expand to
5488-570: The LGP as the Devensian . Irish geologists, geographers, and archaeologists refer to the Midlandian glaciation, as its effects in Ireland are largely visible in the Irish Midlands . The name Devensian is derived from the Latin Dēvenses , people living by the Dee ( Dēva in Latin), a river on the Welsh border near which deposits from the period are particularly well represented. The effects of this glaciation can be seen in many geological features of England, Wales, Scotland, and Northern Ireland . Its deposits have been found overlying material from
5600-399: The Lords of Lützelflüh in first half of the 12th century), the Augustinian Collegiate church in Interlaken (Oberhofen family in 1130) and the Cistercian Frienisberg Abbey (Count Saugern around 1130). However, in 1191 the Oberland barons revolted against Berchtold V of Zähringen and many of the Oberland barons were killed in the battle of Grindelwald. During the 13th century a number of
5712-402: The Monastery who had expected the abolition of all owed debts, responded by rioting, which was suppressed by Bern. The lands around the northern shore of Lake Geneva and between Lake Neuchâtel were the next area into which Bern expanded. The region had originally been part of the Carolingian Empire . Then, in 1032 the Zähringens of Germany defeated the Burgundians, who were then replaced by
SECTION 50
#17328722961145824-505: The North American Laurentide ice sheet. At the height of glaciation, the Bering land bridge potentially permitted migration of mammals, including people, to North America from Siberia . It radically altered the geography of North America north of the Ohio River . At the height of the Wisconsin episode glaciation, ice covered most of Canada, the Upper Midwest , and New England , as well as parts of Montana and Washington . On Kelleys Island in Lake Erie or in New York's Central Park ,
5936-438: The Oberland with Bern, but it was not until the Act of Mediation , two years later, with the abolition of the Helvetic Republic and the partial restoration of the ancien régime , that the two cantons were reunited. Between 1803 and 1814 Bern was one of the six directorial cantons of the Napoleonic Swiss Confederation . With the post−Napoleonic Restoration of 1815 , Bern acquired the Bernese Jura with Biel/Bienne from
6048-410: The Polish River Vistula or its German name Weichsel). Evidence suggests that the ice sheets were at their maximum size for only a short period, between 25,000 and 13,000 BP. Eight interstadials have been recognized in the Weichselian, including the Oerel, Glinde, Moershoofd, Hengelo, and Denekamp. Correlation with isotope stages is still in process. During the glacial maximum in Scandinavia, only
6160-430: The Rheinfelden lands in Oberaargau and the upper Aare valley. After Rudolf's death in 1090, his lands went to his son, Berchtold II of Zähringen . He and his son, Berchtold III, tried to use these lands to expand their power. In 1127 the Zähringer were appointed Rector or delegate of the king in Burgundy. Their hopes for a new, independent Burgundy were dashed in 1156, and the last Zähringen count, Berchtold V, embarked on
6272-437: The Southern Hemisphere was less extensive. Ice sheets existed in the Andes ( Patagonian Ice Sheet ), where six glacier advances between 33,500 and 13,900 BP in the Chilean Andes have been reported. Antarctica was entirely glaciated, much like today, but unlike today the ice sheet left no uncovered area. In mainland Australia only a very small area in the vicinity of Mount Kosciuszko was glaciated, whereas in Tasmania glaciation
6384-452: The Wisconsin episode. It began about 30,000 years ago, reached its greatest advance 21,000 years ago, and ended about 10,000 years ago. In northwest Greenland, ice coverage attained a very early maximum in the LGP around 114,000. After this early maximum, ice coverage was similar to today until the end of the last glacial period. Towards the end, glaciers advanced once more before retreating to their present extent. According to ice core data,
6496-401: The area and French Revolutionary troops moved in, taking over the whole of Switzerland itself in the process and setting up the Helvetic Republic . In 1798, with the establishment of the Helvetic Republic, Bern was divided, the canton of Oberland with Thun as its capital and the canton of Léman with Lausanne as its capital were detached from what was left of the Canton of Bern. Within
6608-401: The area. Evidence of this trade include a hydria which was discovered in Grächwil. Burial rituals and social classes became more developed during this time. The so-called princely graves became more common, many of the burial mounds were over 30 m (98 ft) in diameter and 4 m (13 ft) high and richly outfitted with grave goods. In a grave mound in Bützberg the first burial in
6720-412: The best explored neolithic sites is at Twann (now Twann-Tüscherz ). In the Twannbach delta there were about 25 Cortaillod culture and Horgen culture villages that existed between 3800 and 2950 BC. One of the oldest examples of bread from Switzerland, a sourdough from 3560 to 3530 BC, came from one of these villages. A preserved Bronze Age dugout boat has been found on the dried out lake bed, it
6832-409: The border town of Laupen. To raise the siege, Bern raised a force of 6,000, consisting of Bernese, supported by the Forest Cantons, and other allies ( Simmental , Weissenbur and Oberhasli). The allied Bernese forces were victorious at the Battle of Laupen and Bern drew closer to the Swiss Forest Cantons. It entered into a permanent or eternal alliance with Uri, Schwyz and Unterwalden in 1353. This date
SECTION 60
#17328722961146944-421: The canton is commonly divided into six regions. The most populated area is the Bernese Mittelland on the plateau north of the Alps, with the capital city of Bern. The northmost part of the canton is the Bernese Jura bordering the Canton of Jura . The Bernese Oberland is the mountainous region which lies in the south of the canton. Last glacial period The Last Glacial Period ( LGP ), also known as
7056-441: The canton of Bern consists of lands acquired by the city of Bern mostly between the 14th and the 16th century during the original Swiss Confederacy period , both by conquest and purchase. Acquired districts, with dates of acquisition, include: In the Middle Ages, upwards mobility and access to public offices was relatively easy for successful traders and craftsmen, but Bernese society became ever more stratified and aristocratic as
7168-403: The cantons of Jura and Solothurn to the north. To the west lie the cantons of Neuchâtel , Fribourg , and Vaud . To the south lies the cantons of Valais . East of the canton of Bern lie the cantons of Uri , Nidwalden , Obwalden , Lucerne and Aargau . The geography of the canton includes a large share of all three natural regions of Switzerland: the Jura Mountains (the Bernese Jura ),
7280-402: The cathedral of Lausanne; but it was only decisively implemented when Bern put its full force behind it. Vaud was another French-speaking region in the mostly German-speaking canton, which caused several uprisings. Both Château-d'Œx and Saanen were part of the county of Gruyère . Both districts had quite a bit of independence and often entered into treaties against the will and best interests of
7392-483: The cities near Bern were granted the city right and appointed mayors and city councils. Bern became an imperial city . During the mid-13th century, the Empire's presence weakened in the Aare valley, forcing the local nobles to find allies to protect themselves. Bern entered into a number of treaties with its neighbors in the 13th century. In 1274, the Emperor Rudolph I of Habsburg , confirmed Bern's imperial immediacy. However, in 1285 he imposed an imperial tax which drove
7504-411: The city to support Rudolph's enemies. Although it withstood two sieges by the Emperor in 1288, after the defeat at Schosshalde in 1289 it had to pay taxes and a penalty. In 1298 Bernese forces won a victory at Oberwangen in Köniz against the County of Savoy and the Habsburg Austrian nobility. In 1300, the city acquired the four surrounding parishes of Bolligen, Vechigen, Stettlen and Muri, destroyed
7616-410: The counts of Savoy in 1218. Under the counts of Savoy the area was given political unity, and established as the Barony of Vaud . However, as the power of the Savoys declined at the beginning of the 15th century the land was occupied by troops from Bern . By 1536 the area was completely annexed. Reformation was started by co-workers of John Calvin , including Viret , who engaged in a famous debate at
7728-412: The detriment of the Habsburgs and Fribourg. They acquired the following towns: 1391 Simmenegg, 1399 Signau , 1400 Frutigen , 1407 Wangen , 1408 Trachselwald and Huttwil , 1412 Oltigen and in 1413 (together with Solothurn) Bipp and Bechburg. By 1400, Bern controlled the entire Bernese Oberland. Under their control, the five valleys of the Oberland enjoyed extensive rights and far-reaching autonomy in
7840-400: The dramatic changes in the European environment during the Würm glaciation. During the height of Würm glaciation, c. 24,000 – c. 10,000 BP, most of western and central Europe and Eurasia was open steppe-tundra, while the Alps presented solid ice fields and montane glaciers. Scandinavia and much of Britain were under ice. During the Würm, the Rhône Glacier covered
7952-430: The following year, he sold the town of Thun , its castle and the land surrounding Thun to Bern. Bern then granted the land back to Eberhard as a fief . Bern's support of Eberhard, their resulting expansion into the Oberland and their alliance with the Forest Cantons brought the city into conflict with the Habsburgs during the 14th century. The Gümmenenkrieg in 1333 between Bern and Fribourg over rights and influence in
8064-598: The formation of a single contiguous ice sheet on the Tibetan Plateau, is controversial. Other areas of the Northern Hemisphere did not bear extensive ice sheets, but local glaciers were widespread at high altitudes. Parts of Taiwan , for example, were repeatedly glaciated between 44,250 and 10,680 BP as well as the Japanese Alps . In both areas, maximum glacier advance occurred between 60,000 and 30,000 BP. To
8176-499: The last glacial advance was lowered approximately 1,200 m (3,900 ft) below the present snow line, which is 3,700 m (12,100 ft). The glaciated area in the Cordillera de Mérida was about 600 km (230 sq mi); this included these high areas, from southwest to northeast: Páramo de Tamá, Páramo Batallón, Páramo Los Conejos, Páramo Piedras Blancas, and Teta de Niquitao. Around 200 km (77 sq mi) of
8288-545: The last glacial maximum, the Patagonian ice sheet extended over the Andes from about 35°S to Tierra del Fuego at 55°S. The western part appears to have been very active, with wet basal conditions, while the eastern part was cold-based. Cryogenic features such as ice wedges , patterned ground , pingos , rock glaciers , palsas , soil cryoturbation , and solifluction deposits developed in unglaciated extra-Andean Patagonia during
8400-607: The late glacial (Weichselian) and the immediately preceding penultimate interglacial ( Eemian ) period. Canada was almost completely covered by ice, as was the northern part of the United States , both blanketed by the huge Laurentide Ice Sheet . Alaska remained mostly ice free due to arid climate conditions. Local glaciations existed in the Rocky Mountains and the Cordilleran ice sheet and as ice fields and ice caps in
8512-553: The local population merged with Roman beliefs and the Canton of Bern is home to a number of unique cult centers. They include the larger than life statues of gods (including enthroned Jupiter) at Petinesca, Engehalbinsel, and Thun-Allmendingen; and a number of stone inscriptions. At the beginning of the 5th century CE, Rome withdrew its troops from the Rhine garrisons, but allowed the Burgundians to settle on Helvetii lands in 443 CE. East of
8624-505: The lower Connecticut River Valley . In the Sierra Nevada , three stages of glacial maxima, sometimes incorrectly called ice ages , were separated by warmer periods. These glacial maxima are called, from oldest to youngest, Tahoe, Tenaya, and Tioga. The Tahoe reached its maximum extent perhaps about 70,000 years ago. Little is known about the Tenaya. The Tioga was the least severe and last of
8736-500: The main Wisconsin glacial advance. The upper level probably represents the last glacial advance (Late Wisconsin). The Llanquihue glaciation takes its name from Llanquihue Lake in southern Chile , which is a fan-shaped piedmont glacial lake. On the lake's western shores, large moraine systems occur, of which the innermost belong to the LGP. Llanquihue Lake's varves are a node point in southern Chile's varve geochronology . During
8848-479: The massive Missoula Floods . USGS geologists estimate that the cycle of flooding and reformation of the lake lasted an average of 55 years and that the floods occurred about 40 times over the 2,000-year period starting 15,000 years ago. Glacial lake outburst floods such as these are not uncommon today in Iceland and other places. The Wisconsin glacial episode was the last major advance of continental glaciers in
8960-569: The mound was followed by several later burials. Often, several grave mounds combined to become a necropolis, such as at Grossaffoltern , Ins , Bannwil , Langenthal and Bützberg. Most of the knowledge about the Hallstatt culture in the Canton comes from graves. The only discovered settlement is around Blanche Church in La Neuveville . The grave goods show that iron was forged into swords, daggers, spearheads, knives and wagon accessories. Gold, which
9072-502: The mountains of Southern Africa was about 6 °C colder than at present, in line with temperature drops estimated for Tasmania and southern Patagonia during the same time. This resulted in an environment of relatively arid periglaciation without permafrost , but with deep seasonal freezing on south-facing slopes. Periglaciation in the eastern Drakensberg and Lesotho Highlands produced solifluction deposits and blockfields ; including blockstreams and stone garlands. Scientists from
9184-490: The new canton of Oberland, historic borders and traditional rights were not considered. As there had been no previous separatist feeling amongst the conservative population, there was little enthusiasm for the new order. The situation in the canton of Léman was quite different. The French-speaking Vaudois had never felt like part of the German-speaking Canton of Bern. When they joined the Swiss Confederation in 1803, it
9296-586: The new faith made inroads into the valley. The Aare valley was bordered by three dioceses; Lausanne, Constance and Basel. However, the first Christian missionaries came into the valley from Alsace and other western areas. In 630 the Abbey of Luxeuil established the Abbey of Moutier-Grandval along the old transit route through the Pierre Pertuis Pass. By the 9th or 10th century, this abbey had property and influence all
9408-460: The other heirs. Throughout the 14th century, Bern entered into alliances and treaties with many of its neighbors, including members of the Swiss Confederation . Bern entered into a series of agreements with Biel/Bienne , which led to a conflict with Biel's ruler, Jean de Vienne , the Prince-Bishop of Basel , in 1367–68. The bishop marched south and destroyed Biel along with a number of towns in
9520-568: The past few million years, the glacial-interglacial cycles have been "paced" by periodic variations in the Earth's orbit via Milankovitch cycles . The LGP has been intensively studied in North America, northern Eurasia, the Himalayas , and other formerly glaciated regions around the world. The glaciations that occurred during this glacial period covered many areas, mainly in the Northern Hemisphere and to
9632-534: The power and wealth of the city grew. By the 17th century in the Early Modern period , citizenship had become an inherited prerogative, all political bodies elected one another and officials were elected for life. In effect, public offices were now the exclusive prerogative of the gnädige Herren , the "merciful lords", as the small number of noble families now ruling Bern came to be called. In 1605 there were 152 families that were qualified to rule, by 1691 that number
9744-719: The preceding Ipswichian stage and lying beneath those from the following Holocene , which is the current stage. This is sometimes called the Flandrian interglacial in Britain. The latter part of the Devensian includes pollen zones I–IV, the Allerød oscillation and Bølling oscillation , and the Oldest Dryas , Older Dryas , and Younger Dryas cold periods. Alternative names include Weichsel glaciation or Vistulian glaciation (referring to
9856-486: The proglacial rivers' shifting and redepositing gravels. Beneath the surface, they had profound and lasting influence on geothermal heat and the patterns of deep groundwater flow. The Pinedale (central Rocky Mountains) or Fraser (Cordilleran ice sheet) glaciation was the last of the major glaciations to appear in the Rocky Mountains in the United States. The Pinedale lasted from around 30,000 to 10,000 years ago, and
9968-517: The receding ice. When the enormous mass of the continental ice sheet retreated, the Great Lakes began gradually moving south due to isostatic rebound of the north shore. Niagara Falls is also a product of the glaciation, as is the course of the Ohio River, which largely supplanted the prior Teays River . With the assistance of several very broad glacial lakes, it released floods through the gorge of
10080-399: The same fate. During the last glacial period, Antarctica was blanketed by a massive ice sheet, much as it is today. The ice covered all land areas and extended into the ocean onto the middle and outer continental shelf. Counterintuitively though, according to ice modeling done in 2002, ice over central East Antarctica was generally thinner than it is today. British geologists refer to
10192-466: The sill about 8000 BP, forming a marine Littorina Sea , which was followed by another freshwater phase before the present brackish marine system was established. "At its present state of development, the marine life of the Baltic Sea is less than about 4000 years old", Drs. Thulin and Andrushaitis remarked when reviewing these sequences in 2003. Overlying ice had exerted pressure on the Earth's surface. As
10304-515: The southern Jura Mountains . During the Gugler war in 1375, there were several battles between Bernese troops and English mercenaries under Enguerrand de Coucy . By the 1370s, the Kyburgs (which still held Thun as a fief for Bern) were deeply in debt to Bern. On 11 November 1382, Rudolf II of Neu-Kyburg made an unsuccessful raid on Solothurn . The ensuing conflict with the Old Swiss Confederacy (known as
10416-521: The surrounding district enjoyed a great deal of independence during the 16th century. However, in 1555 the last Count of Gruyère lost both districts to Bern when his county went bankrupt. Bern took over the entire Saanen valley in the following year and introduced the Protestant Reformation. They incorporated the Pays-d'Enhaut with Château-d'Œx into the new Bernese district of Saanen. The area of
10528-476: The surrounding ice sheets. According to the sediment composition retrieved from deep-sea cores , even times of seasonally open waters must have occurred. Outside the main ice sheets, widespread glaciation occurred on the highest mountains of the Alpide belt . In contrast to the earlier glacial stages, the Würm glaciation was composed of smaller ice caps and mostly confined to valley glaciers, sending glacial lobes into
10640-588: The surrounding lands as collateral for a loan. In 1324, Bern acquired the pledged castle and lands. When the Emperor was unable to repay the loan, Laupen became the first bailiwick of Bern. In 1322, the brothers Eberhard II of Neu-Kyburg and Hartmann II of Neu-Kyburg started fighting with each other over who would inherit the family's lands around Thun. The fighting led to the " fratricide at Thun Castle " where Eberhard killed his brother Hartmann. To avoid punishment by his Habsburg overlords, Eberhard fled to Bern . In
10752-585: The threatening castles of Bremgarten and Belp and gave the Baron of Montenach Bernese citizenship. After the victory of Louis IV of Bavaria over the Habsburg Frederick the Fair in the battle of Mühldorf (Bavaria) in 1322, Bern entered an alliance with the anti-Habsburg Swiss Forest Cantons in 1323. Bern joined the Old Swiss Confederation in 1353. In 1310 Emperor Henry VII pledged Laupen Castle , Laupen and
10864-447: The total glaciated area was in the Sierra Nevada de Mérida , and of that amount, the largest concentration, 50 km (19 sq mi), was in the areas of Pico Bolívar , Pico Humboldt [4,942 m (16,214 ft)], and Pico Bonpland [4,983 m (16,348 ft)]. Radiocarbon dating indicates that the moraines are older than 10,000 BP, and probably older than 13,000 BP. The lower moraine level probably corresponds to
10976-586: The treaty of Fribourg from 1476, Fribourg received rights over the Aigle district, which they gave up to Bern in 1483. Bern rebuilt Aigle Castle in 1489 and made it the seat of the bailiwick of Aigle. Also in 1475, the Confederation attacked and captured Grandson Castle . In the next year, Charles the Bold retook the castle and executed the Bernese garrison. In 1476, at the Battle of Grandson , Charles' forces retreated and
11088-636: The way to Lake Biel and into the Balsthal valley. The first monastic cells of what would become the Abbey of Saint-Imier was also founded in 600. In the Seeland and Aare valleys, wooden churches were first built during the Merovingian period. The current churches in Kirchlindach, Oberwil bei Buren and Bleibach were all built above the ruins of these early churches. About 30 churches in the Bern and Solothurn portions of
11200-589: The western parts of Jutland were ice-free, and a large part of what is today the North Sea was dry land connecting Jutland with Britain (see Doggerland ). The Baltic Sea , with its unique brackish water , is a result of meltwater from the Weichsel glaciation combining with saltwater from the North Sea when the straits between Sweden and Denmark opened. Initially, when the ice began melting about 10,300 BP, seawater filled
11312-713: The whole western Swiss plateau, reaching today's regions of Solothurn and Aargau. In the region of Bern, it merged with the Aar glacier. The Rhine Glacier is currently the subject of the most detailed studies. Glaciers of the Reuss and the Limmat advanced sometimes as far as the Jura. Montane and piedmont glaciers formed the land by grinding away virtually all traces of the older Günz and Mindel glaciation, by depositing base moraines and terminal moraines of different retraction phases and loess deposits, and by
11424-675: Was added to the traditional three; the Grimsel , Brünig and Susten passes. In the Bernese Jura the Mont Raimeux and Pierre Pertuis passes opened. Under the Romans, many of the old fortified places were expanded and refortified. The old Helvetii oppidum at the Engehalbinsel became a Roman vicus , which was probably known as Brenodor or Brenodurum. At the foot of the Jens mountain, the fort Petinesca
11536-537: Was as the Canton of Vaud. Under the Helvetic Republic, Pays-d'Enhaut with Château-d'Œx became part of the Canton of Léman while Saanen and the rest of the district became part of the Canton of Oberland . When the Helvetic Republic collapsed in 1803, Saanen and its district became a district in the new Canton of Bern while Château-d'Oex and its district joined Vaud. The 1801 Malmaison Constitution proposed reuniting
11648-458: Was at its greatest extent between 23,500 and 21,000 years ago. This glaciation was somewhat distinct from the main Wisconsin glaciation, as it was only loosely related to the giant ice sheets and was instead composed of mountain glaciers, merging into the Cordilleran ice sheet. The Cordilleran ice sheet produced features such as glacial Lake Missoula , which broke free from its ice dam, causing
11760-650: Was built to guard the roads over the Jura Mountains. This was reinforced in the late-Roman era (368–369 CE) by a fortified bridge over the Thielle/Zihl river between Aegerten and Brügg. A number of Roman villas were built around the Canton. At Oberwichtrach both the main building ( pars urbana ) and the industrial section ( pars rustica ) of a Roman villa have been discovered. The villas at Münsingen, Toffen and Herzogenbuchsee have richly detailed Roman mosaics that are still partly visible. The religious practices of
11872-565: Was found at the Port site. At the oppidum at Bern-Engehalbinsel, there were studios for glass and ceramic production, and iron working achieved a high level of skill, along with craftsmen who worked in wood, leather and goldsmithing. There was a nearby place of worship in the Bremgarten wood, and cemeteries at Münsingen and Bern-Engehalbinsel. After the Roman era victory at Battle of Bibracte in 58 BCE,
11984-640: Was more severe than the Last Glacial Period in some areas such as Britain, but less severe in others. The last glacial period saw alternating episodes of glacier advance and retreat with the Last Glacial Maximum occurring between 26,000 and 20,000 years ago. While the general pattern of cooling and glacier advance around the globe was similar, local differences make it difficult to compare the details from continent to continent (see picture of ice core data below for differences). The most recent cooling,
12096-461: Was more widespread. An ice sheet formed in New Zealand, covering all of the Southern Alps, where at least three glacial advances can be distinguished. Local ice caps existed in the highest mountains of the island of New Guinea , where temperatures were 5 to 6 °C colder than at present. The main areas of Papua New Guinea where glaciers developed during the LGP were the Central Cordillera ,
12208-501: Was not covered by a continental-scale ice sheet. Instead, large, but restricted, icefield complexes covered mountain ranges within northeast Siberia, including the Kamchatka-Koryak Mountains. The Arctic Ocean between the huge ice sheets of America and Eurasia was not frozen throughout, but like today, probably was covered only by relatively shallow ice, subject to seasonal changes and riddled with icebergs calving from
12320-429: Was only 104, while towards the end of the 18th century there were only 69 such families. Meanwhile, the land ruled by the town was extending over more and more territory, so that finally it governed 52 bailiwicks. These offices became very lucrative as the Bernese territories grew. Patrician Landvögte , sheriffs , ruled the politically powerless countryside, often using armed force to put down peasant revolts . In Vaud
12432-620: Was part of lake village near Twann, a stone-lined well had been dug near the preserved boat in 1874. During the Early Iron Age changes in climate forced the Hallstatt culture (800–450 BCE) to abandon settlements along many waterways and in the valley floors and move to the plateaus and hills. With increased trade contacts across the Alps, the cultural influence of the Mediterranean region grew in
12544-469: Was probably collected from river sand, was made into diadems, rings and pendants. Thin bronze arm, leg and neck plates with geometric designs were often buried, especially in the graves at Allenlüften in Mühleberg, at Ins and at Bützberg. The jewelry that was buried included bracelets and rings which were also made of jet and lignite coal. At Münchringen, the grave pottery was both shaped by hand or thrown on
#113886