Wauwilermoos pile dwelling settlement (Egolzwil 3)

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Wauwilermoos or Egolzwil 3 is one of the 111 serial sites of the UNESCO World Heritage Site Prehistoric pile dwellings around the Alps , of which are 56 located in Switzerland. [1] [2]

Prehistoric pile dwellings around the Alps series of stilt houses built near the Alps mountain range

Prehistoric pile dwellings around the Alps is a series of prehistoric pile-dwelling settlements in and around the Alps built from around 5000 to 500 B.C. on the edges of lakes, rivers or wetlands. 111 sites, located in Switzerland (56), Italy (19), Germany (18), France (11), Austria, and Slovenia (2) were added to UNESCO World Heritage Site list in 2011. In Slovenia, this was the first listed cultural world heritage site.

Contents

Geography

The site is located on the former Wauwilersee lakeshore in the municipalities of Egolzwil, Wauwil and Schötz in the Canton of Luzern in Switzerland. The settlement comprises 0.65 hectares (1.61 acres), and the buffer zone including the lake area comprises 56.82 hectares (140.41 acres) in all. [3]

Egolzwil Place in Lucerne, Switzerland

Egolzwil is a municipality in the district of Willisau in the canton of Lucerne in Switzerland.

Wauwil Place in Lucerne, Switzerland

Wauwil is a municipality in the district of Willisau in the canton of Lucerne in Switzerland.

Schötz Place in Lucerne, Switzerland

Schötz is a municipality in the district of Willisau in the canton of Lucerne in Switzerland. On 1 January 2013 the former municipality of Ohmstal merged into the municipality of Schötz.

To 20000 BC a branch of the Reuss glacier formed a valley whose deepest point was approximately 57 metres (187 ft) below the present surface. [4] [5] [6] At Schötz the glacier stopped, as shown by the impressive moraines. During the retreat of the glacier, meltwater jammed between the moraines. Thus in the Wauwilermoos plain three lakes were formed: Wauwilersee, Hagimoos and Mauensee; latter still exists. The meltwater outsourced enormous amounts of sand, so that the lakes never were particularly deep. The depth of Wauwilersee amounted only to about 15 metres (49 ft). To 17000 BC the area was finally free of ice, and soon first pioneer plants settled, such as dwarf birch and mountain avens on, typically for a post-glacial tundra landscape. To 14000 BC the silting up of the three lakes by sand, lake marl and peat began. As a result of climatic changes, the lake levels have been fluctuating over the course of the Stone Age era. So the water level rose several times, and the area covered by water was enlarged: on the one hand, the waves formed the beach ridges between Wauwil and Ettiswil, on the other hand, the radicals old Stone Age and middle Stone Age settlement sites were captured by the rising water, wiped and finally covered with lake sediments. The Neolithic lake dwellings also were covered with lake sediments. At the former Wauwilersee lake area, peat was mined between 1820 and about 1920, and the lake was drained around 1859. To date, the area is still drained in order to make it usable for agriculture. The moorlands in Wauwilermoos therefore disappeared except for small residual areas. Since July 2009 there is also a waterbird and migratory bird reserve of national importance, to protect migratory and waterfowl year-round living in Switzerland. [4]

Moraine Glacially formed accumulation of unconsolidated debris

A moraine is any glacially formed accumulation of unconsolidated glacial debris that occurs in both currently and formerly glaciated regions on Earth, through geomorphological processes. Moraines are formed from debris previously carried along by a glacier and normally consisting of somewhat rounded particles ranging in size from large boulders to minute glacial flour. Lateral moraines are formed at the side of the ice flow and terminal moraines at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines, till-covered areas with irregular topography, and medial moraines which are formed where two glaciers meet.

Tundra biome where the tree growth is hindered by low temperatures and short growing seasons

In physical geography, tundra is a type of biome where the tree growth is hindered by low temperatures and short growing seasons. The term tundra comes through Russian тундра from the Kildin Sami word тӯндар meaning "uplands", "treeless mountain tract". Tundra vegetation is composed of dwarf shrubs, sedges and grasses, mosses, and lichens. Scattered trees grow in some tundra regions. The ecotone between the tundra and the forest is known as the tree line or timberline.

Marl Lime-rich mud or mudstone which contains variable amounts of clays and silt

Marl or marlstone is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and silt. The dominant carbonate mineral in most marls is calcite, but other carbonate minerals such as aragonite, dolomite, and siderite may be present. Marl was originally an old term loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay and calcium carbonate, formed under freshwater conditions; specifically an earthy substance containing 35–65% clay and 65–35% carbonate. It also describes a habit of coralline red alga. The term is today often used to describe indurated marine deposits and lacustrine (lake) sediments which more accurately should be named 'marlstone'. Marlstone is an indurated rock of about the same composition as marl, more correctly called an earthy or impure argillaceous limestone. It has a blocky subconchoidal fracture, and is less fissile than shale. The term 'marl' is widely used in English-language geology, while the terms Mergel and Seekreide are used in European references.

Description

Egolzwil 3 is one of the earliest lake-dwelling settlements in Switzerland. Therefore, it contains an important archaeological Egolzwil culture reference assemblage. The houses in this region were built directly on the ground, as the well-preserved house floors with hearths prove. The village was inhabited only for six years, and thus shows a short but precisely defined episode within the Neolithic period. Moreover, it provides favourable preservation conditions for wood and other organic materials such as plants and bone. The remains of the settlements are an important site for palaeo-ecological studies on the Wauwil bog (German: Wauwilermoos). [3]

Excavations and finds

Wauwilermoos open-air museum Wauwilermoos 033.jpg
Wauwilermoos open-air museum
Wauwil arkeologia lernopado 054.jpg

After the draining of the lake in the mid-19th century, first Stone Age settlements have been found in the vast moorland. Due to the excavations that were carried out until 1929, the Wauwil plain became known as an archaeological region. A research based on scientific criteria began in the early 1930s with excavations in Schötz and at the Neolithic site Egolzwil E2 under the direction of Hans Reinerth. Emil Vogt started systematic excavations from 1950 to 1966 on the settlement sites E3, E4 and E5. After the excavations under René Wyss in 1965 and 1985–88, eleven Neolithic and 30 Mesolithic sites were known at the Wauwilermoos, at the beginning of the 21st century even more than 120 Stone Age sites. [7]

The Neolithic, the final division of the Stone Age, began about 12,000 years ago when the first development of farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The division lasted until the transitional period of the Chalcolithic from about 6,500 years ago, marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In Northern Europe, the Neolithic lasted until about 1700 BC, while in China it extended until 1200 BC. Other parts of the world remained broadly in the Neolithic stage of development, although this term may not be used, until European contact.

Mesolithic Prehistoric period, second part of the Stone Age

In Old World archaeology, Mesolithic is the period between the Upper Paleolithic and the Neolithic. The term Epipaleolithic is often used synonymously, especially for outside northern Europe, and for the corresponding period in the Levant and Caucasus. The Mesolithic has different time spans in different parts of Eurasia. It refers to the final period of hunter-gatherer cultures in Europe and Western Asia, between the end of the Last Glacial Maximum and the Neolithic Revolution. In Europe it spans roughly 15,000 to 5,000 BP; in Southwest Asia roughly 20,000 to 8,000 BP. The term is less used of areas further east, and not at all beyond Eurasia and North Africa.

The first settlements rose after the withdrawal of the Reuss glacier around 13000 BC at six sites. Late Paleolithic (approx. 12000-9000 BC) includes 46 sites situated on an old elevated shoreline of the former lake. These artifacts, among them many burins and typical back and wide lace tee scratches, are attributed to the Fürstein culture. The well-documented Egolzwil culture was named after the Wauwilermoos (E3) site, dated shortly after 4300 BC. In addition to the eponymous locality Egolzwil E3, there are four other settlement sites. The short-lived village was built at the ground level in the sedimentation zone of the lake. Its houses were made of timber ash, oak and alder. The interior was illuminated and heat by a centrally disposed fireplace. The hand-shaped ceramic consisted mainly of pots and bowls with two round-bowed handles and an average volume of 1.8 to 2.8 liters, along with some liquid containers (volume of 6-8 liters) and individual so-called Wauwilerbecher cups. Unique are sickles with a straight wooden handle and diagonally sweeping knives made of Silex that was fixed with birch tar, axe shafts, clubs, sticks, furrows, and a textile jewelry container with shells from the Mediterranean area. [7]

Paleolithic Prehistoric period, first part of the Stone Age

The Paleolithic or Palaeolithic is a period in human prehistory distinguished by the original development of stone tools that covers c. 99% of human technological prehistory. It extends from the earliest known use of stone tools by hominins c. 3.3 million years ago, to the end of the Pleistocene c. 11,650 cal BP.

Burin (lithic flake) type of Stone Age tool

In the field of lithic reduction, a burin is a type of handheld lithic flake with a chisel-like edge which prehistoric humans used for engraving or for carving wood or bone.

Silex is any of various forms of ground stone. In modern contexts the word refers to a finely ground, nearly pure form of silica or silicate.

Protection

As well as being part of the 56 Swiss sites of the UNESCO World Heritage Site Prehistoric pile dwellings around the Alps , the settlement is also listed in the Swiss inventory of cultural property of national and regional significance as a Class A object of national importance. [8] Hence, the area is provided as a historical site under federal protection, within the meaning of the Swiss Federal Act on the nature and cultural heritage (German: Bundesgesetz über den Natur- und Heimatschutz NHG) of 1 July 1966. Unauthorised researching and purposeful gathering of findings represent a criminal offense according to Art. 24. [9]

See also

Literature

Related Research Articles

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References

  1. "Prehistoric Pile Dwellings in Switzerland". Swiss Coordination Group UNESCO Palafittes (palafittes.org). Retrieved 2015-10-24.
  2. "World Heritage". palafittes.org. Retrieved 2015-10-24.
  3. 1 2 "Sites Switzerland: Egolzwil 3 (CH-LU-01)". palafittes.org. Retrieved 2015-10-24.
  4. 1 2 "Entstehung" (PDF) (in German). pfahlbausiedlung.ch. Retrieved 2015-10-26.
  5. "Eiszeiten und Klimawandel im Wehntal der vergangenen 500'000 Jahre" (in German). Mammutmuseum Niederweningen . Retrieved 2015-10-26.
  6. "Reussgletscher – Fussabdruck eines Kaltzeitgiganten" (PDF) (in German). University of Zurich . Retrieved 2015-10-26.
  7. 1 2 Jakob Bill (2013-08-26). "Wauwilermoos" (in German). HDS. Retrieved 2015-10-24.
  8. "A-Objekte KGS-Inventar" (PDF). Schweizerische Eidgenossenschaft, Amt für Bevölkerungsschutz. 2015-01-01. Retrieved 2015-10-24.
  9. "Bundesgesetz über den Natur- und Heimatschutz (NHG)" (PDF) (in German). Hochbaudepartement Stadt Zürich. 2014-10-12. Retrieved 2015-08-21.

Coordinates: 47°10′56.55″N8°0′59.36″E / 47.1823750°N 8.0164889°E / 47.1823750; 8.0164889