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Deutschlands größte Spielbank - taff - ProSiebenWith a capacity of 1. The wind farm builds on steel from Dillingen: Dillinger supplied approx. The first day at the company is a very special day for new trainees.
The eagerness to start training and this new phase of their lives was clearly palpable among the young people who started their future careers today at Dillinger and Saarstahl.
The fact sheet for the year with the key figures from the area of sustainability can now be found in our Download sector.
The spread of the coronavirus has increasing impact on the economy and presents the companies with major challenges.
Anyone aiming to set new standards in heavy plate has to go the whole way — from the "hot metal", via steelmaking, up to and including the treated finished plate.
Only in this way can all the decisive factors be controlled, optimised and perfectly harmonised with each other to achieve maximum production quality and supply reliability from start to finish.
We accept our responsibility to current and future generations of employees and stakeholders and we want to manufacture steel products in the most modern and sustainable way.
We are committed to the Paris Agreement and want to do our part for low-carbon steel production. The quality of our steels also very much depends on what our employees are made of.
People who take care, wholeheartedly and with the greatest skill, to ensure that — every time — we fulfil even the most demanding requirements, are the people who work at Dillinger — now, and tomorrow.
As a Dillinger customer, you can now use the E-Connect app on a smartphone or tablet to quickly and reliably identify a Dillinger heavy plate.
Our newsletter news dillinger will be informing you on new developments at Dillinger. You find the latest version as well as all previously published editions in the archive:.
Visit our Download sector and find the current publications such as our Delivery program as well as all the data sheets, certificates, annual reports and many more.
All fields of application at a glance: even if the product requirements are very demanding - the use of Dillinger heavy plates always offers our customers additional first class advantages.
Innovative top-quality steel products, total orientation around our customers' needs and unceasing technological development in close cooperation with our partners form the basis of our success - as they have for more than years.
Find out more What we do for the environment. Find out more Great oppor- tunities for a career at Dillinger.
The Dillinger Hütte steelworks is located here. Dillingen lies to the right of the Saar in the northern part of the Basin of Saarlouis and thus in the Saar-Nahe Basin.
The Basin of Saarlouis is bounded on the northwest, north and northeast by the heights of the Buntsandstein. They belong to the eastern edge of the Paris Basin and lead into the basin of the Prims.
The Prims coming from the Schwarzwalder Hochwald and emanates above the district of Pachten in the Saar. A few kilometers north of the territorial entity of Pachten the Saar unites with the Nied coming from Lorraine.
The alluvial deposits in the basin allow good agricultural use. The rock strata of the coal-saddle of Saarbrücken Carboniferous dive to the northwest and it comes to a superposition of younger rocks of the Rotliegend and the Triassic.
Dillingen lies on a plaice of the middle Buntsandstein. The rectangular plaice is stretched towards southeast-northwest and bounded to the south by the Carboniferous line of the municipalities of Ensdorf, Hülzweiler and Schwarzenholz.
In the southwest and northwest of this plaice of Buntsandstein lie the ridges of the upper Buntsandstein Röt Formation and the Muschelkalk between Berus, Siersburg and the valley of Haustadt.
The rocks of the lower Rotliegend and the carbon form the northeastern border area. The extended valley of the area Dillingen and Saarlouis lies in the area of the middle Buntsandstein , in which the valleys of the Saar and the Prims dug.
On this bas-relief with overlaying younger gravel blankets, the development area of Dillingen and Pachten spreads. In the middle Buntsandstein mainly crumbly, easily erodible sandstone formations are developed.
Above is the upper Buntsandstein Röt Formation , which is made up of firmer sandstones bound to parts of clay or carbonate. These were won in earlier times in numerous quarries as building material.
Above are Muschelkalk -Layers: The lowest shell limestone layer form sandy-clayey-limestone rocks. The middle limestone layer contains marl with gypsum and anhydrite.
The upper shell limestone layer is composed of massive limestones and platy limestones with layers of marl-layers. Above these solid subsoil rocks, sediment -terraces of the rivers Saar and Prims are deposited.
The different altitudes of these terraces bear testimony to different stages of the depression of the two rivers and the deposit of entrained crushed stones.
The youngest deposits form the meadow-clay of the two river valleys. In the territory of Dillingen is the confluence of the two river valleys of Saar and Prims.
The Prims finish their 91 kilometer run here. The terrain height at the mouth is m above sea level. East of the Saar occurs on both banks of Prims the middle Buntsandstein.
It is widely worn and forms a flat wavy stepped landscape. The areas are covered by broad terraced fields of gravel and clay. Almost all rocks occurring in the Dillingen area can be used economically.
The friable rocks of the middle Buntsandstein were mined as sand in pits or slope edges. The firmer sandstones of the upper Buntsandstein Röt Formation provided breakage and quarry stones.
Gravel was extracted from the terraces. Loam was used as brick material. The climate in Dillingen is moderately oceanic, but warm. There is significant rainfall throughout the year.
Even the driest month still shows high rainfall.
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Visit our Download sector and find the current publications such as our Delivery program as well as all the data sheets, certificates, annual reports and many more.
All fields of application at a glance: even if the product requirements are very demanding - the use of Dillinger heavy plates always offers our customers additional first class advantages.
Innovative top-quality steel products, total orientation around our customers' needs and unceasing technological development in close cooperation with our partners form the basis of our success - as they have for more than years.
Find out more What we do for the environment. Find out more Great oppor- tunities for a career at Dillinger. Find out more.
October EcoVadis, an international provider of business sustainability ratings, has again awarded the silver medal to Dillinger for its Corporate Social Responsibility CSR activities.
Press Release Steel for green energy: Hornsea One offshore wind farm builds on heavy plate from Dillinger October With a capacity of 1.
September The first day at the company is a very special day for new trainees. Sustainability Fact sheet September The fact sheet for the year with the key figures from the area of sustainability can now be found in our Download sector.
Corporate movie. Production at Dillinger Anyone aiming to set new standards in heavy plate has to go the whole way — from the "hot metal", via steelmaking, up to and including the treated finished plate.
Sustainability Report We accept our responsibility to current and future generations of employees and stakeholders and we want to manufacture steel products in the most modern and sustainable way.
Career at Dillinger The quality of our steels also very much depends on what our employees are made of. Do you know our new E-Connect app?
Learn more:. News dillinger: our Newsletter Our newsletter news dillinger will be informing you on new developments at Dillinger. New publications in our Download sector Visit our Download sector and find the current publications such as our Delivery program as well as all the data sheets, certificates, annual reports and many more.
It has about 20, inhabitants and is divided into the three districts Dillingen-city center, Pachten and Diefflen.
In terms of population, it is the second largest municipality in the district of Saarlouis. The Dillinger Hütte steelworks is located here.
Dillingen lies to the right of the Saar in the northern part of the Basin of Saarlouis and thus in the Saar-Nahe Basin. The Basin of Saarlouis is bounded on the northwest, north and northeast by the heights of the Buntsandstein.
They belong to the eastern edge of the Paris Basin and lead into the basin of the Prims. The Prims coming from the Schwarzwalder Hochwald and emanates above the district of Pachten in the Saar.
A few kilometers north of the territorial entity of Pachten the Saar unites with the Nied coming from Lorraine. The alluvial deposits in the basin allow good agricultural use.
The rock strata of the coal-saddle of Saarbrücken Carboniferous dive to the northwest and it comes to a superposition of younger rocks of the Rotliegend and the Triassic.
Dillingen lies on a plaice of the middle Buntsandstein. The rectangular plaice is stretched towards southeast-northwest and bounded to the south by the Carboniferous line of the municipalities of Ensdorf, Hülzweiler and Schwarzenholz.
In the southwest and northwest of this plaice of Buntsandstein lie the ridges of the upper Buntsandstein Röt Formation and the Muschelkalk between Berus, Siersburg and the valley of Haustadt.
The rocks of the lower Rotliegend and the carbon form the northeastern border area. The extended valley of the area Dillingen and Saarlouis lies in the area of the middle Buntsandstein , in which the valleys of the Saar and the Prims dug.
On this bas-relief with overlaying younger gravel blankets, the development area of Dillingen and Pachten spreads.
In the middle Buntsandstein mainly crumbly, easily erodible sandstone formations are developed. Above is the upper Buntsandstein Röt Formation , which is made up of firmer sandstones bound to parts of clay or carbonate.
These were won in earlier times in numerous quarries as building material. Above are Muschelkalk -Layers: The lowest shell limestone layer form sandy-clayey-limestone rocks.
The middle limestone layer contains marl with gypsum and anhydrite. The upper shell limestone layer is composed of massive limestones and platy limestones with layers of marl-layers.
Above these solid subsoil rocks, sediment -terraces of the rivers Saar and Prims are deposited. The different altitudes of these terraces bear testimony to different stages of the depression of the two rivers and the deposit of entrained crushed stones.
The youngest deposits form the meadow-clay of the two river valleys. In the territory of Dillingen is the confluence of the two river valleys of Saar and Prims.
The Prims finish their 91 kilometer run here. The terrain height at the mouth is m above sea level. East of the Saar occurs on both banks of Prims the middle Buntsandstein.
It is widely worn and forms a flat wavy stepped landscape. The areas are covered by broad terraced fields of gravel and clay.
Almost all rocks occurring in the Dillingen area can be used economically. The friable rocks of the middle Buntsandstein were mined as sand in pits or slope edges.
The firmer sandstones of the upper Buntsandstein Röt Formation provided breakage and quarry stones. Gravel was extracted from the terraces.
Loam was used as brick material. The climate in Dillingen is moderately oceanic, but warm.






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