- published: 21 Mar 2012
- views: 99
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Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil)
Taphonomic signatures of brachiopod-dominated fossil assemblages from the Passagem Member (Middle Devonian: late early Givetian) are described in the present study. This rock unit (originally assigned to the Cabeças Formation, but actually related to the underlying Pimenteira Formation) is restricted to the eastern border of the Parnaíba Basin. It consists mostly of fine-grained sandstones with sigmoidal clinoform structures (bearing asymptotic cross-stratification and climbing ripples) and interbedded hummocky cross-stratified (HCS) parallel-sided, graded sandstone lobes. Three taphofacies - identified and characterized in four outcrops in the municipalities of Pimenteiras (Oiti and Rio Banguê), Picos (BR-316/km 305), and Sussuapara (Barreiro Branco), State of Piauí - are based on the qualitative and quantitative analysis of the taphonomic signatures of marine macrofossils and land plant debris. Their origin is associated with shallow-water turbidity currents (hyperpycnal flows) generated by a flood-dominated fluvio-deltaic system entering shallow marine settings. The taphonomic signatures of Taphofacies 1 indicate a proximal environment, consistent with distal mouth-bar deposits. This taphofacies, dominated by the brachiopod Pleurochonetes comstocki (Rathbun, 1874), comprises sandstones with asymptotic cross-stratification and climbing ripples. These deposits probably originated from the deceleration of medium-density, essentially unidirectional turbidity currents. Basinward of Taphofacies 1, Taphofacies 2 is considered to have accumulated via the deceleration of low-density turbidity currents in which the oscillatory component of the flow prevailed. This taphofacies is characterized by delta-front sandstone lobes with HCS, and is rich in terebratulid brachiopods. Lastly, Taphofacies 3 was generated by settlement from the upper part of the hyperpycnal flow, charged with fine-grained sediments, plant debris, and mica, and deposited as laterally extensive silt/sand couplets in more distal and marginal areas of the flow.
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years ago.
- published: 28 Jan 2016
- views: 79
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range[1], primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
- published: 21 Dec 2010
- views: 442
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
- published: 03 Dec 2012
- views: 2965
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stukje aangrenzend Frankrijk. Het is de westelijke uitloper van het Rijnlands leisteenplateau, een massief van leisteen, waartoe ook de Eifel, Hunsrück en de Taunus behoren. Het gebergte is een overblijfsel van de hercynische orogenese en werd 390 tot 300 miljoen jaar geleden gevormd.
The Ardennes (/ɑːrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geological features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage[1] of the Devonian (419.2 ± 3.2 to about 358 million years ago[2]) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half of the kingdom's total area). The eastern part of the Ardennes forms the northernmost third of the Grand Duchy of Luxembourg, also called "Oesling" (Luxembourgish: Éislek), and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
The trees and rivers of the Ardenne provided the underlying charcoal industry assets that enabled the great industrial period of Wallonia in the 18th and 19th centuries, when it was arguably the second great industrial region of the world, after England. The greater region maintained an industrial eminence into the 20th century after coal replaced charcoal in metallurgy.
Allied generals in World War II felt the region was impenetrable to massed vehicular traffic and especially armor, so the area was effectively "all but undefended" during the war, leading to the German Army twice using the region as an invasion route into Northern France and Southern Belgium via Luxembourg in the Battle of France and the later Battle of the Bulge.
- published: 08 Feb 2016
- views: 13
In this video you are travelling with me on a journey from France to Netherlands in October 2009.
The title: Long long journey... , is not really counting for this journey. Though it lasts more than ten hours to travel from France to Netherlands, travelling by train is very relaxing and exciting at the same time, reason for why these hours go as fast as the high speed of the luxurious trains. The new French trains are fast, very very modern and comfortable!
We drive through the Belgian Ardennes, in autumn: the trees have been coloured into warm red, orange and yellow ocher, and some have already lost all the leafs. On some moments you see "nothing" but some shrubs flashing by because of the high speed of the train, and because they are so close next to the rail road, or layers of the Ardennes' hill tops, where we are passing "through", and which have been opened up for the rail road. I decided not to cut those views out of the film, because it belongs to the reality, and... it is lovely to see the villages appear again after that...
Travelling by train offers the opportunity to meet people, to contact, to inform, to unite.
Travelling by train is one of the most excellent ecological ways to travel: that means that this way of travelling is supporting nature, environment, and so: mankind.
About Ecology:
http://en.wikipedia.org/wiki/Ecology
Ecology is a philosophy that includes all aspects of life - both physical and spiritual. 'Eco' is derived from the Greek word oikos, meaning to feel at home. To feel at home somewhere simply means 'to feel at ease, to be able to be yourself'.
From:
http://www.ecolonie.org
Nederlandse informatie over nationale en internationale treinreizen:
http://www.9292ov.nl/
http://www.nshispeed.nl/nl/internationale-treinplanner
Of bel:
voor internationale reizen: 0900-9296
voor reizen in Nederland: 0900-9292
Reizen in Nederland met het openbaar vervoer:
http://www.9292ov.nl/
About the Ardennes:
The Ardennes (Dutch: Ardennen) is a region of extensive forests, rolling hills and old mountains formed on the Givetian (Devonian) Ardennes mountains, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel.
In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
More: wiki
~
Enya:
http://www.youtube.com/view_play_list?p=97C2BCEC55EEA72F
~
Long long journey (lyrics)
City lights shine on the harbour,
night has fallen down,
through the darkness
and the shadow
I will still go on.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Where the road
runs through the valley,
where the river flows,
I will follow every highway
to the place I know.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Long, long journey
out of nowhere,
long, long way to go;
but what are sighs
and what is sadness
to the heart that's coming home?
(repeat)
- published: 19 Dec 2009
- views: 72749
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geophysical features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage, of the Devonian (419.2 ± 3.2 to about 358 Mya (million years ago)) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half the kingdom’s total area). The southern part of the Ardennes is the northern section of the Grand Duchy of Luxembourg and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
- published: 26 Oct 2014
- views: 29
Two children from the future travel to ancient times to witness major events in religious history.
- published: 18 Jun 2011
- views: 2005
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to the beginning of the Carboniferous Period, about 358.9 ± 0.4. It is named after Devon, England, where rocks from this period were first studied.
The Devonian period experienced the first significant adaptive radiation of terrestrial life. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the "Age of Fish". The first ray-finned and lobe-finned bony fish appeared, while the placoderms began dominating almost every known aquatic environment.
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
- published: 04 Oct 2014
- views: 869
location on Google Map
Givetian
The Givetian is one of two faunal stages in the Middle Devonian period. It lasted from 387.7 ± 0.8 million years ago to 382.7 ± 1.6 million years ago. It was preceded by the Eifelian stage and followed by the Frasnian stage. It is named after the town of Givet in France.
Name and definition
The Givetian stage was proposed in 1879 by French geologist Jules Gosselet and was accepted for the higher stage of the Middle Devonian by the Subcommission on Devonian Stratigraphy in 1981.
References
Coordinates: 31°14′15″N 4°21′15″W / 31.2375°N 4.3542°W / 31.2375; -4.3542
This page contains text from Wikipedia, the Free Encyclopedia -
https://wn.com/Givetian
This article is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License, which means that you can copy and modify it as long as the entire work (including additions) remains under this license.
This article is licensed under the Creative Commons Attribution-ShareAlike 3.0 Unported License, which means that you can copy and modify it as long as the entire work (including additions) remains under this license.
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2:36Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPGTafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil) Taphonomic signatures of brachiopod-dominated fossil assemblages from the Passagem Member (Middle Devonian: late early Givetian) are described in the present study. This rock unit (originally assigned to the Cabeças Formation, but actually related to the underlying Pimenteira Formation) is restricted to the eastern border of the Parnaíba Basin. It consists mostly of fine-grained sandstones with sigmoidal clinoform structures (bearing asymptotic cross-stratification and climbing ripples) and interbedded hummocky cross-stratified (HCS) parallel-sided, graded sandstone lobes. Three taphofacies - identified and characterized in four outcrops in the municipalities of Pimenteiras (Oiti and Rio Banguê), Picos (BR-316/km 305), and Sussuapara (Barreiro Branco), State of Piauí - are based on the qualitative and quantitative analysis of the taphonomic signatures of marine macrofossils and land plant debris. Their origin is associated with shallow-water turbidity currents (hyperpycnal flows) generated by a flood-dominated fluvio-deltaic system entering shallow marine settings. The taphonomic signatures of Taphofacies 1 indicate a proximal environment, consistent with distal mouth-bar deposits. This taphofacies, dominated by the brachiopod Pleurochonetes comstocki (Rathbun, 1874), comprises sandstones with asymptotic cross-stratification and climbing ripples. These deposits probably originated from the deceleration of medium-density, essentially unidirectional turbidity currents. Basinward of Taphofacies 1, Taphofacies 2 is considered to have accumulated via the deceleration of low-density turbidity currents in which the oscillatory component of the flow prevailed. This taphofacies is characterized by delta-front sandstone lobes with HCS, and is rich in terebratulid brachiopods. Lastly, Taphofacies 3 was generated by settlement from the upper part of the hyperpycnal flow, charged with fine-grained sediments, plant debris, and mica, and deposited as laterally extensive silt/sand couplets in more distal and marginal areas of the flow. -
0:17Eastmonosteus
EastmonosteusEastmonosteus
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years ago. -
2:29Short survival in the Ardennes
Short survival in the ArdennesShort survival in the Ardennes
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range[1], primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name. -
0:26Persian guys in Ardennen, Belgium, Summer 2012
Persian guys in Ardennen, Belgium, Summer 2012Persian guys in Ardennen, Belgium, Summer 2012
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. -
0:16Moodmasters video content: Woodmasters weekendje Ardennen
Moodmasters video content: Woodmasters weekendje ArdennenMoodmasters video content: Woodmasters weekendje Ardennen
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stukje aangrenzend Frankrijk. Het is de westelijke uitloper van het Rijnlands leisteenplateau, een massief van leisteen, waartoe ook de Eifel, Hunsrück en de Taunus behoren. Het gebergte is een overblijfsel van de hercynische orogenese en werd 390 tot 300 miljoen jaar geleden gevormd. The Ardennes (/ɑːrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geological features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage[1] of the Devonian (419.2 ± 3.2 to about 358 million years ago[2]) as were several other named ranges of the same greater range. Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half of the kingdom's total area). The eastern part of the Ardennes forms the northernmost third of the Grand Duchy of Luxembourg, also called "Oesling" (Luxembourgish: Éislek), and on the southeast the Eifel region continues into Rhineland-Palatinate (German state). The trees and rivers of the Ardenne provided the underlying charcoal industry assets that enabled the great industrial period of Wallonia in the 18th and 19th centuries, when it was arguably the second great industrial region of the world, after England. The greater region maintained an industrial eminence into the 20th century after coal replaced charcoal in metallurgy. Allied generals in World War II felt the region was impenetrable to massed vehicular traffic and especially armor, so the area was effectively "all but undefended" during the war, leading to the German Army twice using the region as an invasion route into Northern France and Southern Belgium via Luxembourg in the Battle of France and the later Battle of the Bulge. -
3:28Train travel ~ Long long journey ~ Enya
Train travel ~ Long long journey ~ EnyaTrain travel ~ Long long journey ~ Enya
In this video you are travelling with me on a journey from France to Netherlands in October 2009. The title: Long long journey... , is not really counting for this journey. Though it lasts more than ten hours to travel from France to Netherlands, travelling by train is very relaxing and exciting at the same time, reason for why these hours go as fast as the high speed of the luxurious trains. The new French trains are fast, very very modern and comfortable! We drive through the Belgian Ardennes, in autumn: the trees have been coloured into warm red, orange and yellow ocher, and some have already lost all the leafs. On some moments you see "nothing" but some shrubs flashing by because of the high speed of the train, and because they are so close next to the rail road, or layers of the Ardennes' hill tops, where we are passing "through", and which have been opened up for the rail road. I decided not to cut those views out of the film, because it belongs to the reality, and... it is lovely to see the villages appear again after that... Travelling by train offers the opportunity to meet people, to contact, to inform, to unite. Travelling by train is one of the most excellent ecological ways to travel: that means that this way of travelling is supporting nature, environment, and so: mankind. About Ecology: http://en.wikipedia.org/wiki/Ecology Ecology is a philosophy that includes all aspects of life - both physical and spiritual. 'Eco' is derived from the Greek word oikos, meaning to feel at home. To feel at home somewhere simply means 'to feel at ease, to be able to be yourself'. From: http://www.ecolonie.org Nederlandse informatie over nationale en internationale treinreizen: http://www.9292ov.nl/ http://www.nshispeed.nl/nl/internationale-treinplanner Of bel: voor internationale reizen: 0900-9296 voor reizen in Nederland: 0900-9292 Reizen in Nederland met het openbaar vervoer: http://www.9292ov.nl/ About the Ardennes: The Ardennes (Dutch: Ardennen) is a region of extensive forests, rolling hills and old mountains formed on the Givetian (Devonian) Ardennes mountains, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name. More: wiki ~ Enya: http://www.youtube.com/view_play_list?p=97C2BCEC55EEA72F ~ Long long journey (lyrics) City lights shine on the harbour, night has fallen down, through the darkness and the shadow I will still go on. Long, long journey through the darkness, long, long way to go; but what are miles across the ocean to the heart that's coming home? Where the road runs through the valley, where the river flows, I will follow every highway to the place I know. Long, long journey through the darkness, long, long way to go; but what are miles across the ocean to the heart that's coming home? Long, long journey out of nowhere, long, long way to go; but what are sighs and what is sadness to the heart that's coming home? (repeat) -
8:33Ardennes
ArdennesArdennes
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geophysical features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage, of the Devonian (419.2 ± 3.2 to about 358 Mya (million years ago)) as were several other named ranges of the same greater range. Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half the kingdom’s total area). The southern part of the Ardennes is the northern section of the Grand Duchy of Luxembourg and on the southeast the Eifel region continues into Rhineland-Palatinate (German state). This video is targeted to blind users. Attribution: Article text available under CC-BY-SA Creative Commons image source in video -
3:38Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
July 19th, 2014 vid credit to: Sherry Ho and Ly Li -
13:55The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
Two children from the future travel to ancient times to witness major events in religious history. -
16:38Devonian
DevonianDevonian
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to the beginning of the Carboniferous Period, about 358.9 ± 0.4. It is named after Devon, England, where rocks from this period were first studied. The Devonian period experienced the first significant adaptive radiation of terrestrial life. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the "Age of Fish". The first ray-finned and lobe-finned bony fish appeared, while the placoderms began dominating almost every known aquatic environment. This video is targeted to blind users. Attribution: Article text available under CC-BY-SA Creative Commons image source in video
-
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil) Taphonomic signatures of brachiopod-dominated fossil assemblages from the Passagem Member (Middle Devonian: late early Givetian) are described in the present study. This rock unit (originally assigned to the Cabeças Formation, but actually related to the underlying Pimenteira Formation) is restricted to the eastern border of the Parnaíba Basin. It consists mostly of fine-grained sandstones with sigmoidal clinoform structures (bearing asymptotic cross-stratification and climbing ripples) and interbedded hummocky cross-stratified (HCS) parallel-sided, graded sandstone lobes. Three taphofacies - identified and characterized in four outcrops in the municipalities of Pimentei...
published: 21 Mar 2012 -
Eastmonosteus
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years ago.
published: 28 Jan 2016 -
Short survival in the Ardennes
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range[1], primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
published: 21 Dec 2010 -
Persian guys in Ardennen, Belgium, Summer 2012
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
published: 03 Dec 2012 -
Moodmasters video content: Woodmasters weekendje Ardennen
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stukje aangrenzend Frankrijk. Het is de westelijke uitloper van het Rijnlands leisteenplateau, een massief van leisteen, waartoe ook de Eifel, Hunsrück en de Taunus behoren. Het gebergte is een overblijfsel van de hercynische orogenese en werd 390 tot 300 miljoen jaar geleden gevormd. The Ardennes (/ɑːrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geological features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Giveti...
published: 08 Feb 2016 -
Train travel ~ Long long journey ~ Enya
In this video you are travelling with me on a journey from France to Netherlands in October 2009. The title: Long long journey... , is not really counting for this journey. Though it lasts more than ten hours to travel from France to Netherlands, travelling by train is very relaxing and exciting at the same time, reason for why these hours go as fast as the high speed of the luxurious trains. The new French trains are fast, very very modern and comfortable! We drive through the Belgian Ardennes, in autumn: the trees have been coloured into warm red, orange and yellow ocher, and some have already lost all the leafs. On some moments you see "nothing" but some shrubs flashing by because of the high speed of the train, and because they are so close next to the rail road, or layers of the Ard...
published: 19 Dec 2009 -
Ardennes
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geophysical features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage, of the Devonian (419.2 ± 3.2 to about 358 Mya (million years ago)) as were several other named ranges of the same greater range. Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of sou...
published: 26 Oct 2014 -
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
July 19th, 2014 vid credit to: Sherry Ho and Ly Li
published: 23 May 2015 -
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
Two children from the future travel to ancient times to witness major events in religious history.
published: 18 Jun 2011 -
Devonian
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to the beginning of the Carboniferous Period, about 358.9 ± 0.4. It is named after Devon, England, where rocks from this period were first studied. The Devonian period experienced the first significant adaptive radiation of terrestrial life. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established. Fish reached substantial diversity during this time, leading the...
published: 04 Oct 2014
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
- Order: Reorder
- Duration: 2:36
- Updated: 21 Mar 2012
- views: 99
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil)
Taphonomic signatures of brachiopod-dom...
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil)
Taphonomic signatures of brachiopod-dominated fossil assemblages from the Passagem Member (Middle Devonian: late early Givetian) are described in the present study. This rock unit (originally assigned to the Cabeças Formation, but actually related to the underlying Pimenteira Formation) is restricted to the eastern border of the Parnaíba Basin. It consists mostly of fine-grained sandstones with sigmoidal clinoform structures (bearing asymptotic cross-stratification and climbing ripples) and interbedded hummocky cross-stratified (HCS) parallel-sided, graded sandstone lobes. Three taphofacies - identified and characterized in four outcrops in the municipalities of Pimenteiras (Oiti and Rio Banguê), Picos (BR-316/km 305), and Sussuapara (Barreiro Branco), State of Piauí - are based on the qualitative and quantitative analysis of the taphonomic signatures of marine macrofossils and land plant debris. Their origin is associated with shallow-water turbidity currents (hyperpycnal flows) generated by a flood-dominated fluvio-deltaic system entering shallow marine settings. The taphonomic signatures of Taphofacies 1 indicate a proximal environment, consistent with distal mouth-bar deposits. This taphofacies, dominated by the brachiopod Pleurochonetes comstocki (Rathbun, 1874), comprises sandstones with asymptotic cross-stratification and climbing ripples. These deposits probably originated from the deceleration of medium-density, essentially unidirectional turbidity currents. Basinward of Taphofacies 1, Taphofacies 2 is considered to have accumulated via the deceleration of low-density turbidity currents in which the oscillatory component of the flow prevailed. This taphofacies is characterized by delta-front sandstone lobes with HCS, and is rich in terebratulid brachiopods. Lastly, Taphofacies 3 was generated by settlement from the upper part of the hyperpycnal flow, charged with fine-grained sediments, plant debris, and mica, and deposited as laterally extensive silt/sand couplets in more distal and marginal areas of the flow.
wn.com/Tafofácies Do Membro Passagem, Bacia Do Parnaíba, Piauí.Mpg
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (State of Piauí, northeast Brazil)
Taphonomic signatures of brachiopod-dominated fossil assemblages from the Passagem Member (Middle Devonian: late early Givetian) are described in the present study. This rock unit (originally assigned to the Cabeças Formation, but actually related to the underlying Pimenteira Formation) is restricted to the eastern border of the Parnaíba Basin. It consists mostly of fine-grained sandstones with sigmoidal clinoform structures (bearing asymptotic cross-stratification and climbing ripples) and interbedded hummocky cross-stratified (HCS) parallel-sided, graded sandstone lobes. Three taphofacies - identified and characterized in four outcrops in the municipalities of Pimenteiras (Oiti and Rio Banguê), Picos (BR-316/km 305), and Sussuapara (Barreiro Branco), State of Piauí - are based on the qualitative and quantitative analysis of the taphonomic signatures of marine macrofossils and land plant debris. Their origin is associated with shallow-water turbidity currents (hyperpycnal flows) generated by a flood-dominated fluvio-deltaic system entering shallow marine settings. The taphonomic signatures of Taphofacies 1 indicate a proximal environment, consistent with distal mouth-bar deposits. This taphofacies, dominated by the brachiopod Pleurochonetes comstocki (Rathbun, 1874), comprises sandstones with asymptotic cross-stratification and climbing ripples. These deposits probably originated from the deceleration of medium-density, essentially unidirectional turbidity currents. Basinward of Taphofacies 1, Taphofacies 2 is considered to have accumulated via the deceleration of low-density turbidity currents in which the oscillatory component of the flow prevailed. This taphofacies is characterized by delta-front sandstone lobes with HCS, and is rich in terebratulid brachiopods. Lastly, Taphofacies 3 was generated by settlement from the upper part of the hyperpycnal flow, charged with fine-grained sediments, plant debris, and mica, and deposited as laterally extensive silt/sand couplets in more distal and marginal areas of the flow.
- published: 21 Mar 2012
- views: 99
Eastmonosteus
- Order: Reorder
- Duration: 0:17
- Updated: 28 Jan 2016
- views: 79
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years...
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years ago.
wn.com/Eastmonosteus
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. This creature comes from the Devonian Givetian about 387.7 million years ago.
- published: 28 Jan 2016
- views: 79
Short survival in the Ardennes
- Order: Reorder
- Duration: 2:29
- Updated: 21 Dec 2010
- views: 442
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mo...
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range[1], primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
wn.com/Short Survival In The Ardennes
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range[1], primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one. Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
- published: 21 Dec 2010
- views: 442
Persian guys in Ardennen, Belgium, Summer 2012
- Order: Reorder
- Duration: 0:26
- Updated: 03 Dec 2012
- views: 2965
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxe...
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
wn.com/Persian Guys In Ardennen, Belgium, Summer 2012
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Givetian (Devonian) Ardennes mountain range, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel. In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
- published: 03 Dec 2012
- views: 2965
Moodmasters video content: Woodmasters weekendje Ardennen
- Order: Reorder
- Duration: 0:16
- Updated: 08 Feb 2016
- views: 13
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stuk...
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stukje aangrenzend Frankrijk. Het is de westelijke uitloper van het Rijnlands leisteenplateau, een massief van leisteen, waartoe ook de Eifel, Hunsrück en de Taunus behoren. Het gebergte is een overblijfsel van de hercynische orogenese en werd 390 tot 300 miljoen jaar geleden gevormd.
The Ardennes (/ɑːrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geological features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage[1] of the Devonian (419.2 ± 3.2 to about 358 million years ago[2]) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half of the kingdom's total area). The eastern part of the Ardennes forms the northernmost third of the Grand Duchy of Luxembourg, also called "Oesling" (Luxembourgish: Éislek), and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
The trees and rivers of the Ardenne provided the underlying charcoal industry assets that enabled the great industrial period of Wallonia in the 18th and 19th centuries, when it was arguably the second great industrial region of the world, after England. The greater region maintained an industrial eminence into the 20th century after coal replaced charcoal in metallurgy.
Allied generals in World War II felt the region was impenetrable to massed vehicular traffic and especially armor, so the area was effectively "all but undefended" during the war, leading to the German Army twice using the region as an invasion route into Northern France and Southern Belgium via Luxembourg in the Battle of France and the later Battle of the Bulge.
wn.com/Moodmasters Video Content Woodmasters Weekendje Ardennen
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk België (een groot deel van Wallonië), Noord-Luxemburg en een klein stukje aangrenzend Frankrijk. Het is de westelijke uitloper van het Rijnlands leisteenplateau, een massief van leisteen, waartoe ook de Eifel, Hunsrück en de Taunus behoren. Het gebergte is een overblijfsel van de hercynische orogenese en werd 390 tot 300 miljoen jaar geleden gevormd.
The Ardennes (/ɑːrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geological features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage[1] of the Devonian (419.2 ± 3.2 to about 358 million years ago[2]) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half of the kingdom's total area). The eastern part of the Ardennes forms the northernmost third of the Grand Duchy of Luxembourg, also called "Oesling" (Luxembourgish: Éislek), and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
The trees and rivers of the Ardenne provided the underlying charcoal industry assets that enabled the great industrial period of Wallonia in the 18th and 19th centuries, when it was arguably the second great industrial region of the world, after England. The greater region maintained an industrial eminence into the 20th century after coal replaced charcoal in metallurgy.
Allied generals in World War II felt the region was impenetrable to massed vehicular traffic and especially armor, so the area was effectively "all but undefended" during the war, leading to the German Army twice using the region as an invasion route into Northern France and Southern Belgium via Luxembourg in the Battle of France and the later Battle of the Bulge.
- published: 08 Feb 2016
- views: 13
Train travel ~ Long long journey ~ Enya
- Order: Reorder
- Duration: 3:28
- Updated: 19 Dec 2009
- views: 72749
In this video you are travelling with me on a journey from France to Netherlands in October 2009.
The title: Long long journey... , is not really counting for t...
In this video you are travelling with me on a journey from France to Netherlands in October 2009.
The title: Long long journey... , is not really counting for this journey. Though it lasts more than ten hours to travel from France to Netherlands, travelling by train is very relaxing and exciting at the same time, reason for why these hours go as fast as the high speed of the luxurious trains. The new French trains are fast, very very modern and comfortable!
We drive through the Belgian Ardennes, in autumn: the trees have been coloured into warm red, orange and yellow ocher, and some have already lost all the leafs. On some moments you see "nothing" but some shrubs flashing by because of the high speed of the train, and because they are so close next to the rail road, or layers of the Ardennes' hill tops, where we are passing "through", and which have been opened up for the rail road. I decided not to cut those views out of the film, because it belongs to the reality, and... it is lovely to see the villages appear again after that...
Travelling by train offers the opportunity to meet people, to contact, to inform, to unite.
Travelling by train is one of the most excellent ecological ways to travel: that means that this way of travelling is supporting nature, environment, and so: mankind.
About Ecology:
http://en.wikipedia.org/wiki/Ecology
Ecology is a philosophy that includes all aspects of life - both physical and spiritual. 'Eco' is derived from the Greek word oikos, meaning to feel at home. To feel at home somewhere simply means 'to feel at ease, to be able to be yourself'.
From:
http://www.ecolonie.org
Nederlandse informatie over nationale en internationale treinreizen:
http://www.9292ov.nl/
http://www.nshispeed.nl/nl/internationale-treinplanner
Of bel:
voor internationale reizen: 0900-9296
voor reizen in Nederland: 0900-9292
Reizen in Nederland met het openbaar vervoer:
http://www.9292ov.nl/
About the Ardennes:
The Ardennes (Dutch: Ardennen) is a region of extensive forests, rolling hills and old mountains formed on the Givetian (Devonian) Ardennes mountains, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel.
In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
More: wiki
~
Enya:
http://www.youtube.com/view_play_list?p=97C2BCEC55EEA72F
~
Long long journey (lyrics)
City lights shine on the harbour,
night has fallen down,
through the darkness
and the shadow
I will still go on.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Where the road
runs through the valley,
where the river flows,
I will follow every highway
to the place I know.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Long, long journey
out of nowhere,
long, long way to go;
but what are sighs
and what is sadness
to the heart that's coming home?
(repeat)
wn.com/Train Travel ~ Long Long Journey ~ Enya
In this video you are travelling with me on a journey from France to Netherlands in October 2009.
The title: Long long journey... , is not really counting for this journey. Though it lasts more than ten hours to travel from France to Netherlands, travelling by train is very relaxing and exciting at the same time, reason for why these hours go as fast as the high speed of the luxurious trains. The new French trains are fast, very very modern and comfortable!
We drive through the Belgian Ardennes, in autumn: the trees have been coloured into warm red, orange and yellow ocher, and some have already lost all the leafs. On some moments you see "nothing" but some shrubs flashing by because of the high speed of the train, and because they are so close next to the rail road, or layers of the Ardennes' hill tops, where we are passing "through", and which have been opened up for the rail road. I decided not to cut those views out of the film, because it belongs to the reality, and... it is lovely to see the villages appear again after that...
Travelling by train offers the opportunity to meet people, to contact, to inform, to unite.
Travelling by train is one of the most excellent ecological ways to travel: that means that this way of travelling is supporting nature, environment, and so: mankind.
About Ecology:
http://en.wikipedia.org/wiki/Ecology
Ecology is a philosophy that includes all aspects of life - both physical and spiritual. 'Eco' is derived from the Greek word oikos, meaning to feel at home. To feel at home somewhere simply means 'to feel at ease, to be able to be yourself'.
From:
http://www.ecolonie.org
Nederlandse informatie over nationale en internationale treinreizen:
http://www.9292ov.nl/
http://www.nshispeed.nl/nl/internationale-treinplanner
Of bel:
voor internationale reizen: 0900-9296
voor reizen in Nederland: 0900-9292
Reizen in Nederland met het openbaar vervoer:
http://www.9292ov.nl/
About the Ardennes:
The Ardennes (Dutch: Ardennen) is a region of extensive forests, rolling hills and old mountains formed on the Givetian (Devonian) Ardennes mountains, primarily in Belgium and Luxembourg, but stretching into France (lending its name to the Ardennes département and the Champagne-Ardenne région), and geologically into the Eifel.
In Wallonia, the word 'Ardenne' in the singular is commonly used for the Belgian part of the region and in the plural for the French one.
Ardenne is the origin of the great industrial period of Wallonia, the second of the world (18th, 19th and 20th centuries). In France, the word 'Ardennes' in the plural, together with the definite article, is commonly used to refer to the French Department of that name.
More: wiki
~
Enya:
http://www.youtube.com/view_play_list?p=97C2BCEC55EEA72F
~
Long long journey (lyrics)
City lights shine on the harbour,
night has fallen down,
through the darkness
and the shadow
I will still go on.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Where the road
runs through the valley,
where the river flows,
I will follow every highway
to the place I know.
Long, long journey
through the darkness,
long, long way to go;
but what are miles
across the ocean
to the heart that's coming home?
Long, long journey
out of nowhere,
long, long way to go;
but what are sighs
and what is sadness
to the heart that's coming home?
(repeat)
- published: 19 Dec 2009
- views: 72749
Ardennes
- Order: Reorder
- Duration: 8:33
- Updated: 26 Oct 2014
- views: 29
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed...
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geophysical features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage, of the Devonian (419.2 ± 3.2 to about 358 Mya (million years ago)) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half the kingdom’s total area). The southern part of the Ardennes is the northern section of the Grand Duchy of Luxembourg and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
wn.com/Ardennes
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a region of extensive forests, rough terrain, rolling hills and ridges formed by the geophysical features of the Ardennes mountain range and the Moselle and Meuse River basins. Geologically, the range is a western extension of the Eifel and both were raised during the Givetian stage, of the Devonian (419.2 ± 3.2 to about 358 Mya (million years ago)) as were several other named ranges of the same greater range.
Primarily in Belgium and Luxembourg, but stretching into Germany and France (lending its name to the Ardennes department and the Champagne-Ardenne région), and geologically into the Eifel—the eastern extension of the Ardennes Forest into Bitburg-Prüm, Germany, most of the Ardenne proper consists of southeastern Wallonia, the southern and more rural part of the Kingdom of Belgium (away from the coastal plain but encompassing over half the kingdom’s total area). The southern part of the Ardennes is the northern section of the Grand Duchy of Luxembourg and on the southeast the Eifel region continues into Rhineland-Palatinate (German state).
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
- published: 26 Oct 2014
- views: 29
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
- Order: Reorder
- Duration: 3:38
- Updated: 23 May 2015
- views: 4779
July 19th, 2014
vid credit to:
Sherry Ho and Ly Li
July 19th, 2014
vid credit to:
Sherry Ho and Ly Li
wn.com/Hebe Dances And Immediately Regrets It At S.H.E. 2Gether 4Ever Encore In Kaohsiung (Eng Sub)
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
- Order: Reorder
- Duration: 13:55
- Updated: 18 Jun 2011
- views: 2005
Two children from the future travel to ancient times to witness major events in religious history.
Two children from the future travel to ancient times to witness major events in religious history.
wn.com/The Golden Laws (Engdub)1 Clip5 (Use Cc For Translation)
Two children from the future travel to ancient times to witness major events in religious history.
- published: 18 Jun 2011
- views: 2005
Devonian
- Order: Reorder
- Duration: 16:38
- Updated: 04 Oct 2014
- views: 869
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to th...
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to the beginning of the Carboniferous Period, about 358.9 ± 0.4. It is named after Devon, England, where rocks from this period were first studied.
The Devonian period experienced the first significant adaptive radiation of terrestrial life. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the "Age of Fish". The first ray-finned and lobe-finned bony fish appeared, while the placoderms began dominating almost every known aquatic environment.
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
wn.com/Devonian
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of the Silurian Period, about 419.2 ± 3.2 Mya (million years ago), to the beginning of the Carboniferous Period, about 358.9 ± 0.4. It is named after Devon, England, where rocks from this period were first studied.
The Devonian period experienced the first significant adaptive radiation of terrestrial life. Free-sporing vascular plants began to spread across dry land, forming extensive forests which covered the continents. By the middle of the Devonian, several groups of plants had evolved leaves and true roots, and by the end of the period the first seed-bearing plants appeared. Various terrestrial arthropods also became well-established. Fish reached substantial diversity during this time, leading the Devonian to often be dubbed the "Age of Fish". The first ray-finned and lobe-finned bony fish appeared, while the placoderms began dominating almost every known aquatic environment.
This video is targeted to blind users.
Attribution:
Article text available under CC-BY-SA
Creative Commons image source in video
- published: 04 Oct 2014
- views: 869
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2:36
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
Taphofacies analysis of late early Givetian fossil assemblages of the Parnaíba Basin (Stat...
published: 21 Mar 2012
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
Tafofácies do Membro Passagem, Bacia do Parnaíba, Piauí.MPG
- Report rights infringement
- published: 21 Mar 2012
- views: 99
0:17
Eastmonosteus
The set up of the Eastmanosteus sp. at the Mineral & Fossil Marketplace in Tucson, AZ. Th...
published: 28 Jan 2016
Eastmonosteus
Eastmonosteus
- Report rights infringement
- published: 28 Jan 2016
- views: 79
2:29
Short survival in the Ardennes
The Ardennes (pronounced /ɑrˈdɛn/; Dutch: Ardennen) is a region of extensive forests, roll...
published: 21 Dec 2010
Short survival in the Ardennes
Short survival in the Ardennes
- Report rights infringement
- published: 21 Dec 2010
- views: 442
0:26
Persian guys in Ardennen, Belgium, Summer 2012
Ardennen is a region of extensive forests, rolling hills and ridges formed within the Give...
published: 03 Dec 2012
Persian guys in Ardennen, Belgium, Summer 2012
Persian guys in Ardennen, Belgium, Summer 2012
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- published: 03 Dec 2012
- views: 2965
0:16
Moodmasters video content: Woodmasters weekendje Ardennen
De Ardennen (Frans: Ardenne, Waals: Årdene) vormen een bosrijk laaggebergte in oostelijk B...
published: 08 Feb 2016
Moodmasters video content: Woodmasters weekendje Ardennen
Moodmasters video content: Woodmasters weekendje Ardennen
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- published: 08 Feb 2016
- views: 13
3:28
Train travel ~ Long long journey ~ Enya
In this video you are travelling with me on a journey from France to Netherlands in Octobe...
published: 19 Dec 2009
Train travel ~ Long long journey ~ Enya
Train travel ~ Long long journey ~ Enya
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- published: 19 Dec 2009
- views: 72749
8:33
Ardennes
The Ardennes (/ɑrˈdɛn/; Luxembourgish: Ardennen; also known as Ardennes Forest) is a regio...
published: 26 Oct 2014
Ardennes
Ardennes
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- published: 26 Oct 2014
- views: 29
3:38
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
July 19th, 2014
vid credit to:
Sherry Ho and Ly Li
published: 23 May 2015
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
Hebe Dances and Immediately Regrets it at S.H.E. 2gether 4ever Encore in Kaohsiung (eng sub)
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- published: 23 May 2015
- views: 4779
13:55
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
Two children from the future travel to ancient times to witness major events in religious ...
published: 18 Jun 2011
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
The Golden Laws (EngDub)1_clip5 (Use CC for Translation)
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- published: 18 Jun 2011
- views: 2005
16:38
Devonian
The Devonian is a geologic period and system of the Paleozoic Era spanning from the end of...
published: 04 Oct 2014
Devonian
Devonian
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- published: 04 Oct 2014
- views: 869
Tafofácies do Membro Passagem, Bacia do Parnaíba, ...
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Persian guys in Ardennen, Belgium, Summer 2012...
Moodmasters video content: Woodmasters weekendje A...
Train travel ~ Long long journey ~ Enya...
Ardennes...
Hebe Dances and Immediately Regrets it at S.H.E. 2...
The Golden Laws (EngDub)1_clip5 (Use CC for Transl...
