Floor
Soil is the uppermost, living part of the earth's crust. The terms earth or soil are also used synonymously. Soils are very diverse - they can be wet or dry, sandy or loamy, rich or poor in humus, for example. The top two meters are of particular importance and therefore worth protecting. They form the basis for a rootable soil layer.
On this page
Soil is a precious and non-renewable resource. We must therefore treat it with care - for ourselves and for future generations.
Soil, inanimate matter?
Did you already know?
- More living creatures live in a handful of fertile soil than there are people on our planet.
- Around 60 percent of all animal and plant species on earth are found in the soil.
- More carbon is bound in the soil than in the global vegetation and atmosphere combined.
- Soil organisms are one of the most important sources for our health.
The soil is full of life!
Creatures that live in the soil are also known as "edaphones". These include tiny bacteria, fungi and microorganisms as well as insects, worms, spiders and even small mammals such as moles. One square meter of fertile soil contains up to a quadrillion bacteria (that's a one with 15 zeros!) in the uppermost soil layers alone. If all these were lined up in a row, they could reach around the earth 25 times. This "biodiversity" is crucial to ensuring that our soil remains fertile - and thus forms the basis of life for us humans and our environment.
Soil fulfills many important functions:
- Filter and protection for drinking water:
When rainwater seeps into the ground, it is cleaned in several layers as if by a natural filter system. In this way, the soil makes a significant contribution to the quality of our groundwater and drinking water. - Water storage:
Soils absorb rain, store it and gradually release the water again. This provides plants with water even during dry periods. At the same time, healthy soil reduces the risk of flooding because it acts like a natural sponge. - Nutrient reservoir:
Soils contain important minerals and trace elements. They release these to the plants - exactly when they are needed. - Carbon storage:
Soils are the most important terrestrial carbon store. Humus plays a central role in the storage of carbon. It itself consists largely of organic carbon and is created through the decomposition of organic material by soil organisms. This reduces the burden on the atmosphere and makes a significant contribution to climate protection. - Cooling function:
Overgrown soil acts like a natural air conditioning system: it cools through evaporation and heats up less than asphalt or concrete. This is why it is noticeably more pleasant in parks or forests on hot summer days. - Biological treasure trove:
We owe many of the active ingredients used in medicine today to soil organisms. For example, around 70% of all clinically used antibiotics come directly or indirectly from soil microbes.
Only healthy and intact soils can provide all these services in the long term. But soils are under pressure: they are losing their fertility, biodiversity and storage capacity due to over-fertilization, pollutants, intensive use, erosion, sealing, environmental contamination/contaminated sites and extreme weather events. Compaction and concrete surfaces considerably weaken their natural functions.
Soil of the year 2026: The archive floor
Soil formation reacts to changes in the environment and to human influences. It is also referred to as the "archive of natural and cultural history". As part of the annual "Soil of the Year" campaign, the focus in 2026 will be on the soil type "archive soil". The state of Hesse has taken over the patronage. Interested parties can find out about events on the website of the Hessian State Agency for Nature Conservation, Environment and Geology (HLNUG):
What does the Offenbach floor look like?
30 million years ago, today's Offenbach urban area was below sea level. Sediments were deposited. Floodplain landscapes came and went. When the water disappeared, trees and bushes grew and disappeared again. This resulted in what Offenbach's subsoil is known for today: layers of clay, loam, stone or sand lying next to and on top of each other. Clay in particular plays a special role here. There are different layers of clay in Offenbach, including the so-called Rupel clay. There is only general data about the soil in Offenbach - each plot of land must therefore be considered individually.
Here you can take a look at the floors in the city of Offenbach:
Further information
- Soil extraction permit
- Standard land values
- Topic page at HLNUG (opens in a new tab)
- Federal Environment Agency (opens in a new tab)
- Bundesverband Boden e.V. (opens in a new tab)
- Soil is valuable (opens in a new tab)
- Video clip floor (opens in a new tab)
- Soilcast - Soil, environment, climate (opens in a new tab)
Office for Environment and Climate
Stadt Offenbach am Main - Kaiserpalais
Kaiserstraße 39
63065 Offenbach
Notes on accessibility
Further information
KOMM parking garage, IHK Offenbach parking garage, Rathaus parking garage, public parking spaces on the banks of the Main
- +49 69 80652557
- +49 69 80652276
- umweltamtoffenbachde
- Further information
Opening hours
Monday - Friday:
09:00 - 12:00
and by appointment