Heers Formation
Encyclopedia
The Heers Formation is a geologic formation in the subsurface
of Belgium
. The formation consists of sand
and marl
and was deposited in the shallow sea that covered Belgium during the middle to late Selandian
age of the Paleocene
epoch
.
The formation is subdivided into two members: at the base green, glauconiferous
sand (Orp Member), on top calcareous clay
and marl in which plant fossil
s have been found (Gelinden Member). This sequence formed during a marine transgression. The Orp Member represents a near coastal marine environment, the Gelinden Member formed in shallow marine circumstances but further from the land.
The Heers Formation occurs in the subsurface of the northern and eastern parts of Flanders
. In Limburg
it reaches its maximal thickness at about 60 meters. The Heers Formation is stratigraphically on top of Cretaceous
and early Paleocene deposits, such as the Opglabbeek Formation
or the Houthem Formation
. The Heers Formation is almost everywhere overlain by the Hannut Formation
(clay, sand and limestone
from the late Paleocene).
The Orp and Gelinden members are also recognized in the Netherlands
(north of Belgium). Dutch stratigraphers see them as part of the Landen Formation
.
Subsurface
Subsurface is the seventh studio album by British progressive metal band Threshold. The album was released in August 2004, and received an Album of the Month award in several European music magazines....
of Belgium
Belgium
Belgium , officially the Kingdom of Belgium, is a federal state in Western Europe. It is a founding member of the European Union and hosts the EU's headquarters, and those of several other major international organisations such as NATO.Belgium is also a member of, or affiliated to, many...
. The formation consists of sand
Sand
Sand is a naturally occurring granular material composed of finely divided rock and mineral particles.The composition of sand is highly variable, depending on the local rock sources and conditions, but the most common constituent of sand in inland continental settings and non-tropical coastal...
and marl
Marl
Marl or marlstone is a calcium carbonate or lime-rich mud or mudstone which contains variable amounts of clays and aragonite. Marl was originally an old term loosely applied to a variety of materials, most of which occur as loose, earthy deposits consisting chiefly of an intimate mixture of clay...
and was deposited in the shallow sea that covered Belgium during the middle to late Selandian
Selandian
The Selandian is in the geologic timescale an age or stage in the Paleocene. It spans the time between and . It is preceded by the Danian and followed by the Thanetian. Sometimes the Paleocene is subdivided in subepochs, in which the Selandian forms the "Middle Paleocene".-Stratigraphic...
age of the Paleocene
Paleocene
The Paleocene or Palaeocene, the "early recent", is a geologic epoch that lasted from about . It is the first epoch of the Palaeogene Period in the modern Cenozoic Era...
epoch
Epoch (geology)
An epoch is a subdivision of the geologic timescale based on rock layering. In order, the higher subdivisions are periods, eras and eons. We are currently living in the Holocene epoch...
.
The formation is subdivided into two members: at the base green, glauconiferous
Glauconite
Glauconite is an iron potassium phyllosilicate mineral of characteristic green color with very low weathering resistance and very friable.It crystallizes with a monoclinic geometry...
sand (Orp Member), on top calcareous clay
Clay
Clay is a general term including many combinations of one or more clay minerals with traces of metal oxides and organic matter. Geologic clay deposits are mostly composed of phyllosilicate minerals containing variable amounts of water trapped in the mineral structure.- Formation :Clay minerals...
and marl in which plant fossil
Fossil
Fossils are the preserved remains or traces of animals , plants, and other organisms from the remote past...
s have been found (Gelinden Member). This sequence formed during a marine transgression. The Orp Member represents a near coastal marine environment, the Gelinden Member formed in shallow marine circumstances but further from the land.
The Heers Formation occurs in the subsurface of the northern and eastern parts of Flanders
Flanders
Flanders is the community of the Flemings but also one of the institutions in Belgium, and a geographical region located in parts of present-day Belgium, France and the Netherlands. "Flanders" can also refer to the northern part of Belgium that contains Brussels, Bruges, Ghent and Antwerp...
. In Limburg
Limburg (Belgium)
Limburg is the easternmost province of modern Flanders, which is one of the three main political and cultural sub-divisions of modern Belgium. It is located west of the river Meuse . It borders on the Dutch provinces of North Brabant and Limburg and the Belgian provinces of Liège, Flemish Brabant...
it reaches its maximal thickness at about 60 meters. The Heers Formation is stratigraphically on top of Cretaceous
Cretaceous
The Cretaceous , derived from the Latin "creta" , usually abbreviated K for its German translation Kreide , is a geologic period and system from circa to million years ago. In the geologic timescale, the Cretaceous follows the Jurassic period and is followed by the Paleogene period of the...
and early Paleocene deposits, such as the Opglabbeek Formation
Opglabbeek Formation
The Opglabbeek Formation is a geologic formation in the subsurface of the eastern part of Belgian Limburg. The formation consists of lagoonal and fluvial clay and sand and was deposited during the early Selandian...
or the Houthem Formation
Houthem Formation
The Houthem Formation, named after the Dutch town of Houthem, is a geological formation that crops out in the south of Belgian and Dutch Limburg. It has also been found in borings in the northeastern part of the Campine Basin...
. The Heers Formation is almost everywhere overlain by the Hannut Formation
Hannut Formation
The Hannut Formation is a geologic formation in the subsurface of northern Belgium. The formation consists of marine clay and silt, alternating with moer sandy layers. On top of this the lithology changes to limestone, siltstone and sandstone and the top of the formation is formed by a layer of...
(clay, sand and limestone
Limestone
Limestone is a sedimentary rock composed largely of the minerals calcite and aragonite, which are different crystal forms of calcium carbonate . Many limestones are composed from skeletal fragments of marine organisms such as coral or foraminifera....
from the late Paleocene).
The Orp and Gelinden members are also recognized in the Netherlands
Netherlands
The Netherlands is a constituent country of the Kingdom of the Netherlands, located mainly in North-West Europe and with several islands in the Caribbean. Mainland Netherlands borders the North Sea to the north and west, Belgium to the south, and Germany to the east, and shares maritime borders...
(north of Belgium). Dutch stratigraphers see them as part of the Landen Formation
Landen Formation
The Landen Formation is a lithostratigraphic unit in the subsurface of the Netherlands. This formation shares its name with the Belgian Landen Group, but the Belgian unit is thinner and has different definitions...
.
- 1988
- Formatie van Heers, in: : Voorstel lithostratigrafische indeling van het Paleogeen, Belgische Geologische Dienst, BrusselsCity of BrusselsThe City of Brussels is the largest municipality of the Brussels-Capital Region, and the official capital of Belgium by law....
, p. 52-58. (eds.); 2001: Paleogene and Neogene lithostratigraphic units (Belgium), Geologica Belgica 4(1-2), p. 135-152