Adigrat Sandstone
   HOME

TheInfoList



OR:

The Adigrat Sandstone formation in north
Ethiopia Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the ...
, in a wide array of reddish colours, comprises
sandstone Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) ...
s with coarse to fine grains, and locally conglomerates, silt- and
claystone Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too sm ...
s. Given the many
lateritic Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by ...
palaeosols and locally fossil wood fragments, the formation is interpreted as a deposit in estuarine, lacustrine-deltaic or continental environments. The upper limit of Adigrat Sandstone is of Middle-Late
Jurassic The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The J ...
age (around 160 million years or Ma ago) whereas the lower boundary is
Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
(200 Ma). There are numerous rock-hewn churches in this formation.


Name and definition

The name “Adigrat Sandstone” was coined by geologist
William Thomas Blanford William Thomas Blanford (7 October 183223 June 1905) was an English geologist and naturalist. He is best remembered as the editor of a major series on '' The Fauna of British India, Including Ceylon and Burma''. Biography Blanford was born ...
, who accompanied the
British Expedition to Abyssinia The British Expedition to Abyssinia was a rescue mission and punitive expedition carried out in 1868 by the armed forces of the British Empire against the Ethiopian Empire (also known at the time as Abyssinia). Emperor Tewodros II of Ethiopia, t ...
in 1868. The formation is named after the town of
Adigrat Adigrat (, ''ʿaddigrat'', also called ʿAddi Grat) is a city and separate woreda in Tigray Region of Ethiopia. It is located in the Misraqawi Zone at longitude and latitude , with an elevation of above sea level and below a high ridge to the we ...
, on the route of the invading British army. So far the nomenclature was not proposed for recognition to the
International Commission on Stratigraphy The International Commission on Stratigraphy (ICS), sometimes referred to unofficially as the "International Stratigraphic Commission", is a daughter or major subcommittee grade scientific daughter organization that concerns itself with stratigra ...
.


Stratigraphic context

The Adigrat Sandstone has been deposited upon a
Triassic The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period ...
planation surface. The age of the Adigrat Sandstone is not well-defined and sedimentation has probably started at different times in different areas. Recent investigations using fossils determined a
Late Triassic The Late Triassic is the third and final epoch (geology), epoch of the Triassic geologic time scale, Period in the geologic time scale, spanning the time between annum, Ma and Ma (million years ago). It is preceded by the Middle Triassic Epoch ...
to
Middle Jurassic The Middle Jurassic is the second epoch of the Jurassic Period. It lasted from about 174.1 to 163.5 million years ago. Fossils of land-dwelling animals, such as dinosaurs, from the Middle Jurassic are relatively rare, but geological formations co ...
age.


Environment

A large part of the formation was deposited in a shallow sea, as indicated by the presence of fossils typical of brackish water and shallow marine environment (such as
bivalves Bivalvia (), in previous centuries referred to as the Lamellibranchiata and Pelecypoda, is a class of marine and freshwater molluscs that have laterally compressed bodies enclosed by a shell consisting of two hinged parts. As a group, bival ...
,
foraminifera Foraminifera (; Latin for "hole bearers"; informally called "forams") are single-celled organisms, members of a phylum or class of amoeboid protists characterized by streaming granular Ectoplasm (cell biology), ectoplasm for catching food and ot ...
, and marine crocodiles). The sedimentary structures also suggest tidal environments and storm deposits. Other sediment and also sedimentary structures indicate that parts of the sands were deposited in a continental environment.


Lithology

The Adigrat Sandstone comprises thick sequences of cross-bedded sandstone with minor intercalations of
siltstone Siltstone, also known as aleurolite, is a clastic sedimentary rock that is composed mostly of silt. It is a form of mudrock with a low clay mineral content, which can be distinguished from shale by its lack of fissility.Blatt ''et al.'' 1980, p ...
and
claystone Mudrocks are a class of fine-grained siliciclastic sedimentary rocks. The varying types of mudrocks include siltstone, claystone, mudstone, slate, and shale. Most of the particles of which the stone is composed are less than and are too sm ...
and sometimes
dolomite Dolomite may refer to: *Dolomite (mineral), a carbonate mineral *Dolomite (rock), also known as dolostone, a sedimentary carbonate rock *Dolomite, Alabama, United States, an unincorporated community *Dolomite, California, United States, an unincor ...
. The sandstones consist essentially of
quartz Quartz is a hard, crystalline mineral composed of silica (silicon dioxide). The atoms are linked in a continuous framework of SiO4 silicon-oxygen tetrahedra, with each oxygen being shared between two tetrahedra, giving an overall chemical form ...
, but hold also some
feldspar Feldspars are a group of rock-forming aluminium tectosilicate minerals, also containing other cations such as sodium, calcium, potassium, or barium. The most common members of the feldspar group are the ''plagioclase'' (sodium-calcium) feldsp ...
. The grains are cemented by silica and clay minerals. The thickness of the Adigrat Sandstone increases from north to south: maximum values (600 metres) are west of the Mekelle Outlier at the edge of
Kola Tembien Kola Tembien (, "Lower Tembien") is a woreda in Tigray Region, Ethiopia. It is named in part after the former province of Tembien. Part of the Mehakelegnaw Zone, Kola Tembien is bordered on the south by Abergele, on the west by the Tekezé River ...
and Dogu’a Tembien districts.


Life

In the Adigrat Sandstone,
fossil wood Fossil wood, also known as fossilized tree, is wood that is preserved in the fossil record. Over time the wood will usually be the part of a plant that is best preserved (and most easily found). Fossil wood may or may not be petrified, in ...
fragments and
trace fossils A trace fossil, also known as an ichnofossil (; from el, ἴχνος ''ikhnos'' "trace, track"), is a fossil record of biological activity but not the preserved remains of the plant or animal itself. Trace fossils contrast with body fossils, ...
have been recorded. In addition, remains of
vertebrate Vertebrates () comprise all animal taxa within the subphylum Vertebrata () ( chordates with backbones), including all mammals, birds, reptiles, amphibians, and fish. Vertebrates represent the overwhelming majority of the phylum Chordata, ...
animals, such as non-marine amphibians and reptiles, have been found.


Geographical extent

The formation outcrops widely in north
Ethiopia Ethiopia, , om, Itiyoophiyaa, so, Itoobiya, ti, ኢትዮጵያ, Ítiyop'iya, aa, Itiyoppiya officially the Federal Democratic Republic of Ethiopia, is a landlocked country in the Horn of Africa. It shares borders with Eritrea to the ...
, particularly in the gorges formed by the Tekezze River and its affluents. In extends further to the southeast towards Soqota and to the northeast towards Gheralta,
Adigrat Adigrat (, ''ʿaddigrat'', also called ʿAddi Grat) is a city and separate woreda in Tigray Region of Ethiopia. It is located in the Misraqawi Zone at longitude and latitude , with an elevation of above sea level and below a high ridge to the we ...
and central
Eritrea Eritrea ( ; ti, ኤርትራ, Ertra, ; ar, إرتريا, ʾIritriyā), officially the State of Eritrea, is a country in the Horn of Africa region of Eastern Africa, with its capital and largest city at Asmara. It is bordered by Ethiopia ...
.


The Rock-Hewn Churches in Adigrat Sandstone

Most of the rock-hewn
monolithic church A monolithic church or rock-hewn church is a church made from a single block of stone. Because freestanding rocks of sufficient size are rare, such edifices are usually hewn into the ground or into the side of a hill or mountain. They can be of ...
es in the
Tigray region The Tigray Region, officially the Tigray National Regional State, is the northernmost regional state in Ethiopia. The Tigray Region is the homeland of the Tigrayan, Irob, and Kunama people. Its capital and largest city is Mekelle. Tigray is ...
are in Adigrat Sandstone. These churches are located in the districts
Hawzen Hawzen ( Ge'ez: ሓውዜን) is a town in northern Ethiopia. Located in the Misraqawi (Eastern) Zone of the Tigray Region (or ''kilil''), this town has a latitude and longitude of with an elevation of 2105 meters above sea level. Its market da ...
,
Kola Tembien Kola Tembien (, "Lower Tembien") is a woreda in Tigray Region, Ethiopia. It is named in part after the former province of Tembien. Part of the Mehakelegnaw Zone, Kola Tembien is bordered on the south by Abergele, on the west by the Tekezé River ...
and Dogu’a Tembien. The precise ages of these churches are not well defined but they would mostly have been excavated between the 10th and 15th centuries. According to local belief, the carving of the churches was started by missionaries who came from the Mediterranean to Ethiopia (known as the ‘ Nine Saints’) during the fifth or sixth century. They promoted
monasticism Monasticism (from Ancient Greek , , from , , 'alone'), also referred to as monachism, or monkhood, is a religious way of life in which one renounces worldly pursuits to devote oneself fully to spiritual work. Monastic life plays an important role ...
, hence the remote and inaccessible locations of many rock-hewn churches. The tradition continues until today, as new rock-hewn churches are being excavated. Although design and structure vary, most rock churches consist of a hall with basilica architecture holding three naves, often vestibule, domes, pillars, vast ceilings and archways. Ceilings and walls may be decorated with colourful frescoes and rock carvings. Most of these mediaeval churches are still in use today as
Orthodox Orthodox, Orthodoxy, or Orthodoxism may refer to: Religion * Orthodoxy, adherence to accepted norms, more specifically adherence to creeds, especially within Christianity and Judaism, but also less commonly in non-Abrahamic religions like Neo-pa ...
village churches. The mediaeval
Siqurto foot tunnel The Siqurto foot tunnel crosses beneath the Imba Tsiyon ridge, which forms the water divide between the Giba and Weri'i basins. The ridge is part of the Mugulat Mountains, Tigray, Ethiopia, Design and construction The tunnel was hewn in th ...
has also been excavated in Adigrat Sandstone.


Geomorphology

The Adigrat Sandstone is intersected by an orthogonal network of joints. In thick and homogeneous sandstone, there is a distance of tens of metres between major joints. As the uplift of the Ethiopian Highlands during the Caenozoic resulted deep incision of the rivers, a remarkable
Grand Canyon The Grand Canyon (, yuf-x-yav, Wi:kaʼi:la, , Southern Paiute language: Paxa’uipi, ) is a steep-sided canyon carved by the Colorado River in Arizona, United States. The Grand Canyon is long, up to wide and attains a depth of over a m ...
-like structural relief has been created, holding
mesas A mesa is an isolated, flat-topped elevation, ridge or hill, which is bounded from all sides by steep escarpments and stands distinctly above a surrounding plain. Mesas characteristically consist of flat-lying soft sedimentary rocks capped by a ...
,
buttes __NOTOC__ In geomorphology, a butte () is an isolated hill with steep, often vertical sides and a small, relatively flat top; buttes are smaller landforms than mesas, plateaus, and tablelands. The word ''butte'' comes from a French word mea ...
, and pinnacles up to 300 metres high, beneath the main escarpment. The rectangular shape of these relief forms indicates that their formation has been influenced by intersecting joints. A dominant process in cliff formation is rockfall. Variations of slope steepness along the escarpments are due to the distinctive
bedding Bedding, also known as bedclothes or bed linen, is the materials laid above the mattress of a bed for hygiene, warmth, protection of the mattress, and decorative effect. Bedding is the removable and washable portion of a human sleeping environm ...
of the rocks and to variability in rock type: on thick sequences of homogeneous sandstone vertical faces have developed, while intercalations of thinly bedded fine-grained sediments lead to steps in the slopes. Caverns and
apses In architecture, an apse (plural apses; from Latin 'arch, vault' from Ancient Greek 'arch'; sometimes written apsis, plural apsides) is a semicircular recess covered with a hemispherical vault or semi-dome, also known as an '' exedra''. ...
have formed along bedding planes and along curved joints. These natural cavities have sometimes been expanded into larger caves by the inhabitants of the area.


References

{{reflist Geologic formations of Eritrea Geologic formations of Ethiopia Triassic System of Africa Jurassic System of Africa Sandstone formations Shallow marine deposits Formations