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During the Permian , after the end of the uplifting, the Variscan mountains were heavily eroded, leaving only a relatively flat, truncated upland.
For a short time, and only partially, this was later flooded by the sea. This is a region of subsidence , which runs from the Trier Bay in the south to the Lower Rhine Bay in the north.
Through this zone existed at one time a sea link between north and south Central Europe. The remains of the sediments laid down at this time have survived to a greater extent in the Maubach- Mechernich Triassic Triangle in the north and in the Oberbettingen Triassic Graben in the area around Hillesheim and Oberbettingen.
In the Upper Cretaceous and during the Tertiary , the Eifel was inundated mainly from the north. Remains of Cretaceous rocks were discovered on the High Fens.
Scattered patches of Oligocene deposits can be found there and in the Western Eifel. From the Pliocene onwards, the Rhenish Massif, including the Eifel, experienced an uplift.
This led to the streams and rivers cutting into the gently rolling landscape resulting in the present appearance of the low mountain range with its flat plateaus and deeply incised valleys.
Due to numerous recent research projects, climate changes since the last ice age can be traced in detail in the Eifel region. It created numerous volcanic structures, lava flows and extensive layers of volcanic ejecta made of tuff and pumice , which have formed the basis of a significant mining activity for the extraction of building materials since Roman times.
Some of the hills are volcanic vents. The peculiar circle-shaped lakes maars of the volcanic regions formed in volcanic craters.
The first volcanic eruptions took place in the early Tertiary centred in the High Eifel and even before the volcanic activity of the Siebengebirge and Westerwald.
Volcanism in the western and eastern Eifel is, in contrast to that of the High Eifel, much more recent than that of the Siebengebirge and Westerwald.
In the eastern Eifel, volcanism began about , years ago in the area of today's Laacher See; it extended to the Neuwied Basin to the south, and crossed the Rhine to the east.
The quantity of basalt lavas, pumice tuffs and ash tuffs produced by the volcanoes was far greater here than in the western Eifel. East Eifel volcanism came to an end with a huge eruption, as a result of which the magma chamber emptied and collapsed, creating a caldera.
Today's Laacher See formed in the caldera. The ashes from the eruption can be detected today in deposits all over Central Europe and as far as Bornholm as a thin layer.
Volcanism is caused by magma , which either rises directly to the earth's surface from the upper regions of the earth's mantle or, in the majority of cases, gathers in a magma chamber, several tens of kilometres deep, at the base of the earth's crust , from which magma rises at irregular intervals and causes volcanic eruptions.
The Eifel is in the Atlantic climate zone with its relatively high precipitation; winters that are moderately cold and long with periods of snow; and summers that are often humid and cool.
A relatively dry and milder climate prevails in the wind and rain shadow of the High Eifel. Cold air from Siberia in the higher elevations of the Eifel has less of an impact on weather conditions, as the proximity of the Atlantic Ocean to the Eifel brings milder sea air to the Eifel even in winter.
Looking at the long-term averages, even the Snow Eifel only has snow cover for nine consecutive days in winter, as there are no longer lasting cold spells.
However, there is an average of 70 days of full snow cover because the frequency of snow at higher elevations is relatively high for comparison: The humid Atlantic climate can cause extreme variations though: The mean temperature in the coldest month January is The level of precipitation decreases significantly from west to east as a result of the rain shadow of the highlands.
The bioclimatic conditions in the Eifel are favourable. Heat stress and air humidity are rarely present in summer. The Eifel has a distinctly stimulating climate; the high elevations being considered as highly stimulating.
The Eifel is a clean air area with very low air-chemical pollution. On hot sunny days, there is sometimes an increased concentration of ground-level ozone.
At the time of the Roman Empire the whole mountain range between the rivers Rhine, Meuse and Moselle was called Arduenna silva "high forest".
Following the collapse of the West Roman Empire , the Frankish Empire emerged in the territories of present-day France and western Germany.
This was divided into gaue Lat.: Following the end of the Frankish Empire the name of the old gaue continued to be used in popular language.
Over the centuries an ever-larger region was referred to as the Eifel. The resulting root form Anfil or Anfali would then mean an "area that is not so level".
An - would then be a prefix and -fali , which is related to the Slavic polje "field" , means "plain" or "heath". Kaspers deduces from the surviving form in pago aquilinse the root form aku-ella, akwella and points to its development into the name "Eifel" in the following sequence: Akuella derives from the pre-German and means "land with summits" or "land with peaks".
Both propositions, like several others, are highly contentious. The most convincing proposal is that of Heinrich Dittmaier The second component corresponds to Ville , which is the name of a ridge between the Erft, Swist and Rhine today.
Unlike the modern word Ville the fricative consonant is hard in "Eifel". Responsible for that was probably a sound between ai- and -fil , which was assimilated by the f , possibly f , k , ch , d , t.
Dittmaier believes the missing sound was a k or ch , whereby "Eifel" originally went back to Aik-fil. However, the original, historical and even current vegetation of the present day Ville is dominated by oak mixed forest.
The meaning of "Ville" is also disputed. Dittmaier gives three possible explanations: Another proposal sees the name as even older and possibly of Celtic origin.
Near Cologne, an altar was found, which was dedicated to Matronae Aufaniae Celtic goddesses which were honoured by flowing water.
The thesis that the name "Eifel" was derived from this source is not conclusive, but it is persuasive; Eifel would then mean "land of water" or "watery mountains".
By the Old Stone Age , the Eifel was inhabited by people: Neanderthals and modern man. This is evinced by the Buchenloch and Magdalena Caves near Gerolstein.
The artifacts from the Magdalena Cave also show that the Eifel was visited by man even during the height of the last ice age.
Excavations show that iron was already being worked in the Eifel during the Iron Age. Near Bitburg there is an iron smelting site in which metal was smelted and worked in an almost industrial manner during the Roman period.
In Roman times, the Eifel was an important economic region. Its mineral resources lead, zinc spar , iron, limestone and stones for construction were mined, and trade benefited from long-distance Roman communication routes such as the Roman road from Trier to Cologne , which crossed the Eifel.
This explains the large number of castles, now lying in ruins, which had been built mainly for the purpose of guarding the border. Through skillful politics, several smaller principalities and abbey estates were able to acquire their independence, for example the House of Manderscheid-Blankenheim , the County of Salm-Reifferscheid and Prüm Abbey.
The mining and smelting works, with their demand for pit props and charcoal for smelting , the great demand for construction timber and firewood and the shipbuilding industry which was widespread until the 19th century, led to an almost complete deforestation of the woods.
In fact, around , the Eifel must be imagined as a landscape of meadows and heathland, where animals, especially flocks of sheep, grazed.
At the same time, the population was becoming increasingly impoverished because the poor arable land did not yield rich harvests.
Even after the decline of mining and smelting operations after the midth century, the situation of the population did not improve. In addition, the Eifel was a marching route for French troops to all kinds of theatres of war.
They demanded " forage money" from the local population, which just caused further impoverishment, as the records of Kottenheim show.
Prussian rule began in , but little changed in terms of social conditions: The Eifel, as a poor peripheral region of the empire "Prussian Siberia" , was only of interest for military reasons.
For Prussian officials and officers, mainly Protestants, a posting to the purely Catholic Eifel region was like a punishment sentence.
However, the landscape changed as Prussia carried out systematic reforestation, albeit with coniferous trees that were not typical of the region.
It can be said without exaggeration that two thirds of the entire population only enjoy meat once a year. Sfrecciamo verso un novembre pieno di Motorsport!
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