Geology of Oman
Encyclopedia
The geology of Oman includes varied landscapes which are a blend of its geological history, and its climate
over the past few million years. Rock outcrops in the Al Hajar Mountains
, the Huqf and Dhofar
are a point of interest for international geologists. The rock record spans about 825 million years and includes at least three periods when the country was covered by ice.
Oman
, located at the southeast corner of the Arabian plate
, is being pushed slowly northward, as the Red Sea
grows wider. The lofty Al Hajar Mountains and the drowned valleys of Musandam
are dramatic reminders of this. Generally speaking Oman is fairly quiescent tectonically. Musandan experiences occasional tremors as the Arabian Plate collides with the Eurasian Plate
.
During the Cretaceous
Period Oman was located adjacent to a subduction zone and a portion of the upper mantle
along with overlying seafloor volcanic rock
s were thrust
over the continental crust
. This obducted
sequence of ultramafic to mafic
rocks is the Semail ophiolite complex. The ophiolite is locally rich in copper
and chromite
orebodies
.
The interior plains of Oman are of young sedimentary rock
s, wadi gravels, dune sands and salt flats. Beneath them is a several kilometre thick stack of older sedimentary rocks that host the country’s hydrocarbon
resources. Ancient salt, which comes to the surface in several salt dome
s such as Qarat Kibrit, plays an important role in forming many of these oil and gas accumulations.
Climate
Climate encompasses the statistics of temperature, humidity, atmospheric pressure, wind, rainfall, atmospheric particle count and other meteorological elemental measurements in a given region over long periods...
over the past few million years. Rock outcrops in the Al Hajar Mountains
Al Hajar Mountains
The Hajjar Mountains in northeastern Oman and also the eastern United Arab Emirates are the highest mountain range in the eastern Arabian peninsula...
, the Huqf and Dhofar
Dhofar
The Dhofar region lies in Southern Oman, on the eastern border with Yemen. Its mountainous area covers and has a population of 215,960 as of the 2003 census. The largest town in the region is Salalah. Historically, it was the chief source of frankincense in the world. However, its frankincense...
are a point of interest for international geologists. The rock record spans about 825 million years and includes at least three periods when the country was covered by ice.
Oman
Oman
Oman , officially called the Sultanate of Oman , is an Arab state in southwest Asia on the southeast coast of the Arabian Peninsula. It is bordered by the United Arab Emirates to the northwest, Saudi Arabia to the west, and Yemen to the southwest. The coast is formed by the Arabian Sea on the...
, located at the southeast corner of the Arabian plate
Arabian Plate
The Arabian Plate is one of three tectonic plates which have been moving northward over millions of years and colliding with the Eurasian Plate...
, is being pushed slowly northward, as the Red Sea
Red Sea
The Red Sea is a seawater inlet of the Indian Ocean, lying between Africa and Asia. The connection to the ocean is in the south through the Bab el Mandeb strait and the Gulf of Aden. In the north, there is the Sinai Peninsula, the Gulf of Aqaba, and the Gulf of Suez...
grows wider. The lofty Al Hajar Mountains and the drowned valleys of Musandam
Musandam
Musandam Governorate is a governorate of Oman.Geographically, the Musandam peninsula juts into the Strait of Hormuz, the narrow entry into the Persian Gulf, from the Arabian Peninsula. The Musandam peninsula is an exclave of Oman, separated from the rest of the country by the United Arab Emirates...
are dramatic reminders of this. Generally speaking Oman is fairly quiescent tectonically. Musandan experiences occasional tremors as the Arabian Plate collides with the Eurasian Plate
Eurasian Plate
The Eurasian Plate is a tectonic plate which includes most of the continent of Eurasia , with the notable exceptions of the Indian subcontinent, the Arabian subcontinent, and the area east of the Chersky Range in East Siberia...
.
During the 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...
Period Oman was located adjacent to a subduction zone and a portion of the upper mantle
Mantle (geology)
The mantle is a part of a terrestrial planet or other rocky body large enough to have differentiation by density. The interior of the Earth, similar to the other terrestrial planets, is chemically divided into layers. The mantle is a highly viscous layer between the crust and the outer core....
along with overlying seafloor volcanic rock
Volcanic rock
Volcanic rock is a rock formed from magma erupted from a volcano. In other words, it is an igneous rock of volcanic origin...
s were thrust
Thrust fault
A thrust fault is a type of fault, or break in the Earth's crust across which there has been relative movement, in which rocks of lower stratigraphic position are pushed up and over higher strata. They are often recognized because they place older rocks above younger...
over the continental crust
Continental crust
The continental crust is the layer of igneous, sedimentary, and metamorphic rocks which form the continents and the areas of shallow seabed close to their shores, known as continental shelves. This layer is sometimes called sial due to more felsic, or granitic, bulk composition, which lies in...
. This obducted
Obduction
Obduction is the overthrusting of continental crust by oceanic crust or mantle rocks at a convergent plate boundary. It can occur during an orogeny, or mountain-building episode....
sequence of ultramafic to mafic
Mafic
Mafic is an adjective describing a silicate mineral or rock that is rich in magnesium and iron; the term is a portmanteau of the words "magnesium" and "ferric". Most mafic minerals are dark in color and the relative density is greater than 3. Common rock-forming mafic minerals include olivine,...
rocks is the Semail ophiolite complex. The ophiolite is locally rich in copper
Copper
Copper is a chemical element with the symbol Cu and atomic number 29. It is a ductile metal with very high thermal and electrical conductivity. Pure copper is soft and malleable; an exposed surface has a reddish-orange tarnish...
and chromite
Chromite
Chromite is an iron chromium oxide: FeCr2O4. It is an oxide mineral belonging to the spinel group. Magnesium can substitute for iron in variable amounts as it forms a solid solution with magnesiochromite ; substitution of aluminium occurs leading to hercynite .-Occurrence:Chromite is found in...
orebodies
Ore
An ore is a type of rock that contains minerals with important elements including metals. The ores are extracted through mining; these are then refined to extract the valuable element....
.
The interior plains of Oman are of young sedimentary rock
Sedimentary rock
Sedimentary rock are types of rock that are formed by the deposition of material at the Earth's surface and within bodies of water. Sedimentation is the collective name for processes that cause mineral and/or organic particles to settle and accumulate or minerals to precipitate from a solution....
s, wadi gravels, dune sands and salt flats. Beneath them is a several kilometre thick stack of older sedimentary rocks that host the country’s hydrocarbon
Hydrocarbon
In organic chemistry, a hydrocarbon is an organic compound consisting entirely of hydrogen and carbon. Hydrocarbons from which one hydrogen atom has been removed are functional groups, called hydrocarbyls....
resources. Ancient salt, which comes to the surface in several salt dome
Salt dome
A salt dome is a type of structural dome formed when a thick bed of evaporite minerals found at depth intrudes vertically into surrounding rock strata, forming a diapir....
s such as Qarat Kibrit, plays an important role in forming many of these oil and gas accumulations.