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Giebichenstein Boulder
The Giebichenstein near Stöckse, Germany, in the district of Nienburg, Lower Saxony, is one of the largest erratic boulders of northern Germany. It weighs around . A picture of the Giebichenstein is part of the emblem of the Stöckse municipality. There is the supposition that during Wolstonian Stage the stone was deposited by glaciers as a part of a moraine. Near the Giebichenstein there are the remains of a dolmen, and at the stone itself there were found the remains of a Stone Age The Stone Age was a broad prehistory, prehistoric period during which Rock (geology), stone was widely used to make stone tools with an edge, a point, or a percussion surface. The period lasted for roughly 3.4 million years and ended b ... hunter's camp. See also * List of individual rocks Historical geology Glaciology Rock formations of Lower Saxony Funnelbeaker culture Glacial erratics of Germany File:360-degree_view_of_the_Giebichenstein_(Stöckse,_October_2023).webm, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Giebichenstein Oktober 2023
Giebichenstein is a district (''Stadtteil'') in the north of Halle (Saale) on the eastern bank of the river Saale in the Saxony-Anhalt state of Germany. It is part of the ''Stadtbezirk Nord''. People * German physicist Eduard Grüneisen was born in Giebichenstein. * Georg Händel, father of famous composer George Frideric Handel, was town surgeon of Giebichenstein. * Georg Friedrich Meier, a German philosopher and aesthetician, died in Giebichenstein. * Hans Caspar von Krockow was the of Giebichenstein. Giebichenstein Castle The Giebichenstein Castle is situated in the north of Giebichenstein district, next to the Saale river. File:20150902-BurgGiebichenstein.jpg, Giebichenstein Castle, pictured in 2015 See also * Giebichenstein boulder, in Lower Saxony References {{authority control Halle (Saale) Districts of Saxony-Anhalt ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stöckse
Stöckse is a municipality in the district of Nienburg, in Lower Saxony, Germany. It is situated in the forest "Krähe" between Langendamm and Steimbke. Policy Municipality Stöckse The villages Stöckse and Wenden with district Lohe form the municipality (Gemeinde) Stöckse, part of collective municipality (Samtgemeinde) Steimbke. Municipal council The municipal council (Gemeinderat) Stöckse has 11 members elected and a mayor elected directly. Since the local elections on September 10, 2006, two parties and one selector's community (Wählergemeinschaft) represent it. *CDU - 6 seats *SPD - 2 seats *WG Stöckse - 3 seats Culture Theatre In Stöckse there is an open-air theatre. The stage is situated in a short part of forest in the city of Stöckse and accommodates 700 visitors. The audience is amused with comedies and stories in Low German, and a children's theatre themed "children play for children". Furthermore, the open-air theatre is a favoured aren ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nienburg (district)
Nienburg () is a districts of Germany, district (''Landkreis'') in Lower Saxony, Germany. It is bounded by (from the west and clockwise) the districts of Diepholz (district), Diepholz, Verden (district), Verden, Heidekreis, Hanover (district), Hanover and Schaumburg, and by the state of North Rhine-Westphalia (district of Minden-Lübbecke). History From the early Middle Ages to the end of the 16th century this region was the heart of the County of Hoya. The ruling family became extinct in 1582, and the central and southern parts of the county were annexed by the Principality of Lüneburg, Lüneburg branch of the duchy of Brunswick-Lüneburg. In 1705 the area of Nienburg and Hoya became subordinate to Electorate of Hanover, Hanover. In 1866 the Kingdom of Hanover was annexed by Prussia. The Prussian government established the districts of Nienburg and Stolzenau, which were merged in 1932. The earliest official mention of Nienburg/Weser dates from the year 1025, when Milo, the Cano ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glacial Erratic
A glacial erratic is a glacially deposited rock (geology), rock differing from the type of country rock (geology), rock native to the area in which it rests. Erratics, which take their name from the Latin word ' ("to wander"), are carried by glacial ice, often over distances of hundreds of kilometres. Erratics can range in size from pebbles to large boulders such as Okotoks Erratic, Big Rock (16,500 metric tons) in Alberta. Geologists identify erratics by studying the rocks surrounding the position of the erratic and the composition of the erratic itself. Erratics are significant because: *They can be transported by glaciers, and are thereby one of a series of indicators which mark the path of prehistoric Glacial motion, glacier movement. Their lithographic origin can be traced to the parent bedrock, allowing for confirmation of the ice flow route. *They can be transported by ice rafting, which allows quantification of the extent of glacial flooding resulting from ice dam failure ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wolstonian Stage
The Wolstonian Stage is a middle Pleistocene stage of the geological history of Earth from approximately 374,000 until 130,000 years ago. It precedes the Last Interglacial (also called the Eemian Stage) and follows the Hoxnian Stage in the British Isles. It is also approximately analogous to the Warthe and Saalian stages in northern Europe; the Riss glaciation in the Alps; and the Illinoian Stage in North America. The colder last part from around 194,000 years ago is called the Penultimate Glacial Period. It is equivalent to Marine isotope stages (MIS) 10 through 6. MIS 10, 8 and 6 were glacial periods and 9 and 7 were interglacials. It is named after Wolston in the English county of Warwickshire. Description The Wolstonian Stage is a middle Pleistocene stage of the geological history of Earth that precedes the Ipswichian Stage (Eemian Stage in Europe) and follows the Hoxnian Stage in the British Isles. The Wolstonian Stage apparently includes three periods of glac ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris (regolith and Rock (geology), rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines (till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French language, French , which in turn is derived from the Savoyard dialect, Savoyard Italian ('mound of e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dolmen
A dolmen, () or portal tomb, is a type of single-chamber Megalith#Tombs, megalithic tomb, usually consisting of two or more upright megaliths supporting a large flat horizontal capstone or "table". Most date from the Late Neolithic period (40003000 BCE) and were sometimes covered with earth or smaller stones to form a tumulus (burial mound). Small pad-stones may be wedged between the cap and supporting stones to achieve a level appearance. In many instances, the covering has eroded away, leaving only the stone "skeleton". In Sumba (Indonesia), dolmens are still commonly built (about 100 dolmens each year) for collective graves according to lineage. The traditional village of Wainyapu, Sumba, Wainyapu has some 1,400 dolmens. Etymology Celtic or French The word ''dolmen'' entered archaeology when Théophile Corret de la Tour d'Auvergne used it to describe megalithic tombs in his (1796) using the spelling ''dolmin'' (the current spelling was introduced about a decade later and h ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stone Age
The Stone Age was a broad prehistory, prehistoric period during which Rock (geology), stone was widely used to make stone tools with an edge, a point, or a percussion surface. The period lasted for roughly 3.4 million years and ended between 4000 Anno Domini, BC and 2000 BC, with the advent of metalworking. It therefore represents nearly 99.3% of human history. Though some simple metalworking of malleable metals, particularly the use of Goldsmith, gold and Coppersmith, copper for purposes of ornamentation, was known in the Stone Age, it is the melting and smelting of copper that marks the end of the Stone Age. In Western Asia, this occurred by about 3000 BC, when bronze became widespread. The term Bronze Age is used to describe the period that followed the Stone Age, as well as to describe cultures that had developed techniques and technologies for working copper alloys (bronze: originally copper and arsenic, later copper and tin) into tools, supplanting ston ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Individual Rocks
The following is a list of notable rocks and stones. See also * List of largest meteorites on Earth * List of longest natural arches * List of rock formations * List of rock formations that resemble human beings * List of rocks on Mars * Lists of rocks in Western Australia * List of menhirs, List of standing stones * Monoliths * Moon rocks * Stolen and missing Moon rocks * Stones of Scotland * Glacial erratic **Glacial erratic boulders of Estonia, of Estonia **Glacial erratics on and around Rügen, of Rügen **of Washington (state), Washington State, United States ***Glacial erratic boulders of Island County, Washington, of Island County, Washington ***Glacial erratic boulders of King County, Washington, of King County, Washington ***Glacial erratic boulders of Kitsap County, Washington, of Kitsap County, Washington ***Glacial erratic boulders of Snohomish County, Washington, of Snohomish County, Washington ***Glacial erratic boulders of the Puget Sound region, of the Puget Sound ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Historical Geology
Historical geology or palaeogeology is a discipline that uses the principles and methods of geology to reconstruct the geological history of Earth. Historical geology examines the vastness of geologic time, measured in billions of years, and investigates changes in the Earth, gradual and sudden, over this deep time. It focuses on geological processes, such as plate tectonics, that have changed the Earth's surface and subsurface over time and the use of methods including stratigraphy, structural geology, paleontology, and sedimentology to tell the sequence of these events. It also focuses on the evolution of life during different time periods in the geologic time scale. Historical development During the 17th century, Nicolas Steno was the first to observe and propose a number of basic principles of historical geology, including three key stratigraphic principles: the law of superposition, the principle of original horizontality, and the principle of lateral continuity. 18th-ce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Glaciology
Glaciology (; ) is the scientific study of glaciers, or, more generally, ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climatology, meteorology, hydrology, biology, and ecology. The impact of glaciers on people includes the fields of human geography and anthropology. The discoveries of water ice on the Moon, Mars, Europa (moon), Europa and Pluto add an extraterrestrial component to the field, which is referred to as "astroglaciology". Overview A glacier is a persistent body of dense ice, a form of rock) formed from snow falling and accumulating over a long period of time; glaciers move very slowly, either descending from high mountains, as in valley glaciers, or moving outward from centers of accumulation, as in continental glaciers. Areas of study within glaciology include glacial history and the reconstruction of past glaciation. A glaciologist is a person ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rock Formations Of Lower Saxony
Rock most often refers to: * Rock (geology), a naturally occurring solid aggregate of minerals or mineraloids * Rock music, a genre of popular music Rock or Rocks may also refer to: Places United Kingdom * Rock, Caerphilly, a location in Wales * Rock, Cornwall, a village in England * Rock, County Tyrone, a village in Northern Ireland * Rock, Devon, a location in England * Rock, Neath Port Talbot, a location in Wales * Rock, Northumberland, a village in England * Rock, Somerset, a location in England * Rock, West Sussex, a hamlet in Washington, England * Rock, Worcestershire, a village and civil parish in England United States * Rock, Kansas, an unincorporated community * Rock, Michigan, an unincorporated community * Rock, West Virginia, an unincorporated community * Rock, Rock County, Wisconsin, a town in southern Wisconsin * Rock, Wood County, Wisconsin, a town in central Wisconsin Elsewhere * Corregidor, an island in the Philippines also known as "The Rock" * Jamaica, a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
