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Concarena
The Concarena is a mountain in Lombardy, northern Italy. It is multi summited and its highest peak is the ''Cima della Bacchetta'', with a height of 2,549 m. The Concarena divides the mid Val Camonica and the Valle di Scalve, lying at its north-eastern tip (the southern one being the Pizzo Camino). Most of the mountain is located in the province of Brescia, with only the north-western areas part of the province of Bergamo. Other summits over 2,000 meters include the ''Cima dei Ladrinai'' (2,403 m), ''Monte Vaccio'' (2,338 m) and the ''Corno del Dente'' (2,303 m). The mountain is composed of carbonate rocks from the Triassic period (c. 225 million years ago). SOIUSA classification According to the SOIUSA (''International Standardized Mountain Subdivision of the Alps'') the mountain can be classified in the following way: * main part = Eastern Alps * major sector = Southern Limestone Alps * section = Bergamasque Alps and Prealps * subsection = Bergamas ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bergamasque Prealps
The Bergamasque Prealps () are a mountain range within the Alps. The range is located in Lombardy, in the north of Italy. Geography Administratively the range belongs to the Italian province of Bergamo and, to a lesser extent, to the provinces of Lecco and Brescia. The western slopes of the mountains are drained by the Adda, the central and eastern part of the range by Oglio and other minor rivers and streams, all of them tributaries of the Po. SOIUSA classification According to SOIUSA (''International Standardized Mountain Subdivision of the Alps'') the mountain range is an Alpine subsection, classified in the following way: * main part = Eastern Alps * major sector = Southern Limestone Alps * section = Bergamasque Alps and Prealps * subsection = Bergamasque Prealps * code = II/C-29.II Borders The Bergamo Prealps stretch between Lake Como (west) and Lake Iseo (east). They are separated from the Bergamo Alps (north) by some secondary valleys of Val Brembana, Val Seriana and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Val Camonica
Val Camonica (also ''Valcamonica'' or Camonica Valley, Eastern Lombard: ''Al Camònega'') is one of the largest valleys of the central Alps, in eastern Lombardy, Italy. It extends about from the Tonale Pass to Corna Trentapassi, in the commune of Pisogne near Lake Iseo. It has an area of about Area of the municipalities, excluding Val di Scalve and 118,323 inhabitants.Sum of ISTAT data of communes at 31 December 2007 The River Oglio runs through its full length, rising at Ponte di Legno and flowing into Lake Iseo between Pisogne and Costa Volpino. Almost all of the valley is included in the administrative territory of the province of Brescia, except for Lovere, Rogno, Costa Volpino and the Val di Scalve, which belong to the province of Bergamo. Since 1979, the rock drawings located along the valley are a UNESCO World Heritage Site, while the entire valley became a UNESCO World Biosphere Reserve in 2018. Etymology ''Val Camonica'' is derived from the Latin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pizzo Camino
Pizzo Camino (Pis Camì) is a mountain in the Bergamo Prealps, with a height of . It belongs to the massif dividing the upper Val di Scleve from the upper Val Camonica, together with the Concarena and the Cimone della Bagozza. It is on the boundaries between the provinces of Brescia and Bergamo. The summit is composed from limestone rocks, formed in the middle Triassic period from the former Tethys Ocean. The lower sides have instead a more sandstone-marl composition. SOIUSA classification According to the SOIUSA (''International Standardized Mountain Subdivision of the Alps'') the mountain can be classified in the following way: * main part = Eastern Alps * major sector = Southern Limestone Alps * section = Bergamasque Alps and Prealps * subsection = Bergamasque Prealps * supergroup = Prealpi Bergamasche Orientali * group = Gruppo Camino-Concarena * subgroup = Gruppo del Pizzo Camino * code In communications and information processing, code is a system of r ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains Of The Alps (2500–2999 M)
This page tabulates only the most prominent mountains of the Alps, selected for having a topographic prominence of ''at least'' , and all of them exceeding in height. Although the list contains 537 summits, some significant alpine mountains are necessarily excluded for failing to meet the stringent prominence criterion. The list of these most prominent mountains is continued down to 2500 m elevation at List of prominent mountains of the Alps (2500–2999 m) and down to 2000 m elevation on List of prominent mountains of the Alps (2000–2499 m). All such mountains are located in either France, Italy, Switzerland, Liechtenstein, Austria, Germany or Slovenia, even in some lower regions. Together, these three lists include all 44 ultra-prominent peaks of the Alps, with 19 ultras over 3000m on this page. For a definitive list of all 82 the highest peaks of the Alps, as identified by the International Climbing and Mountaineering Federation (UIAA), and often referred to as the ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
SOIUSA
Alps by SOIUSA. SOIUSA (an acronym for - English: ''International Standardized Mountain Subdivision of the Alps-ISMSA'') is a proposal for a new classification system of the Alps from the geographic and toponomastic point of view. It was designed by Sergio Marazzi, Italian researcher and author of the Orographic Atlas of the Alps ''SOIUSA''. His book was presented with the patronage of the Italian Alpine Club on 23 Jan 2006, but has yet to receive any formal acceptance. History The SOIUSA is an interpretation by Marazzi of the terrain of the Alps aiming to replace the traditional way the Alps were partitioned in Italy, the , which was adopted in 1926 by the Italian National Geographic Committee () after the IX Italian Geographic Congress (). SOIUSA takes into account the European geographic literature normalizing and standardizing the different national classification systems in use. It was publicly presented in a lecture organized by the Italian Alpine Club's Milan confere ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Lombardy
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
SOIUSA Code
SOIUSA code is the code used in the International Standardized Mountain Subdivision of the Alps (ISMSA or SOIUSA), a proposal by Italian Alpinist, Sergio Marazzi, to re- categorize the mountains and mountain ranges of the Alps. The proposal has been aired since 2005 but has yet to receive official recognition. SOIUSA groups' hierarchy SOIUSA divides the Alps in two main regions, the Western Alps and Eastern Alps. These two main regions are further divided in: *5 major sectors (SR); *36 sections (SZ); *132 subsections (STS); *333 supergroups (SPG); *870 groups (GR); *1625 subgroups (STG). Using this system, any Alpine mountain can be given a code which shows which region, sector, section, subsection, supergroup, group and subgroup it belongs to. Encoding SOIUSA code is built in the following way: * 2 main parts: ** Western Alps are identified by roman numeral I; ** Eastern Alps are identified by roman numeral II; * 5 major sectors: ** in Western Alps: *** South-western Alp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bergamasque Alps And Prealps
The Bergamasque Alps and Prealps (''Alpi e Prealpi Bergamasche'' in Italian) are a mountain range in the southern part of the Alps. They are located in Lombardy, in the northern part of Italy. Geography Administratively the range belongs to the Italian province of Bergamo and, marginally, to the provinces of Sondrio, Lecco and Brescia. The western slopes of the mountains are drained by the Adda, the central and western part of the range by Oglio and other minor rivers and streams, all of them tributaries of the Po . SOIUSA classification According to SOIUSA (''International Standardized Mountain Subdivision of the Alps'') the mountain range is an Alpine section, classified in the following way: * main part = Eastern Alps * major sector = Southern Limestone Alps * section = Bergamasque Alps and Prealps * code = II/C-29 Borders Bergamasque Alps and Prealps' borders are (clockwise): * Como lake (west); * river Adda, Aprica pass and Corteno valley (north); * val Camonica and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Southern Limestone Alps
The Southern Limestone Alps ( it, Alpi Sud-orientali, german: Südliche Kalkalpen), also called the Southern Calcareous Alps, are the ranges of the Eastern Alps south of the Central Eastern Alps mainly located in northern Italy and the adjacent lands of Austria and Slovenia. The distinction from the Central Alps, where the higher peaks are located, is based on differences in geological composition. The Southern Limestone Alps extend from the Sobretta- Gavia range in Lombardy in the west to the Pohorje in Slovenia in the east. Alpine Club classification Ranges of the Southern Limestone Alps according to the Alpine Club classification (from east to west): * Pohorje (1) * Kamnik–Savinja Alps (2) * Karawanks (3) * Julian Alps (4) * Gailtal Alps (5) * Carnic Alps (6) * Southern Carnic Alps (7) * Dolomites (8) * Fiemme Mountains (9) * Vicentine Alps (10) * Nonsberg Group (11) * Brenta Group (12) * Garda Mountains (13) * Ortler Alps (14) * Adamello-Presanella Alps ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Alps
Eastern Alps is the name given to the eastern half of the Alps, usually defined as the area east of a line from Lake Constance and the Alpine Rhine valley up to the Splügen Pass at the Alpine divide and down the Liro River to Lake Como in the south. The peaks and mountain passes are lower than the Western Alps, while the range itself is broader and less arched. Geography Overview The Eastern Alps include the eastern parts of Switzerland (mainly Graubünden), all of Liechtenstein, and most of Austria from Vorarlberg to the east, as well as parts of extreme Southern Germany (Upper Bavaria), northwestern Italy ( Lombardy), northeastern Italy (Trentino-Alto Adige/Südtirol, Veneto and Friuli-Venezia Giulia) and a good portion of northern Slovenia (Upper Carniola and Lower Styria). In the south the range is bound by the Italian Padan Plain; in the north the valley of the Danube River separates it from the Bohemian Massif. The easternmost spur is formed by the Vienna Woods ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carbonate Rock
Carbonate rocks are a class of sedimentary rocks composed primarily of carbonate minerals. The two major types are limestone, which is composed of calcite or aragonite (different crystal forms of CaCO3), and dolomite rock (also known as dolostone), which is composed of mineral dolomite (CaMg(CO3)2). Calcite can be either dissolved by groundwater or precipitated by groundwater, depending on several factors including the water temperature, pH, and dissolved ion concentrations. Calcite exhibits an unusual characteristic called retrograde solubility in which it becomes less soluble in water as the temperature increases. When conditions are right for precipitation, calcite forms mineral coatings that cement the existing rock grains together or it can fill fractures. Karst topography and caves develop in carbonate rocks because of their solubility in dilute acidic groundwater. Cooling groundwater or mixing of different groundwaters will also create conditions suitable for cave ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago (Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of arch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
