Geologically, the Cenozoic is the era when the continents moved into their current positions.

Geologically, the Biqa is the medial part of a depression that extends north to the western bend of the Orontes River in Syria and south to Jordan through Al Arabah to Al Aqabah, the eastern arm of the Red Sea.

Geologically, the island consists of gneiss and argillaceous schists, with no trace of fossils, showing that the island is, like the Falkland Islands, a surviving fragment of some greater land-mass now vanished, most probably indicating a former extension of the Andean system.

Geologically, the value of echinoderms is in their ossified skeletons, which are major contributors to many limestone formations, and can provide valuable clues as to the geological environment.

Geologically, a fjord ( or ; also spelt fiord ) is a long, narrow inlet with steep sides or cliffs, created in a valley carved by glacial activity.

Geologically the region is divided into the largely igneous and metamorphic west and sedimentary east, the dividing line slightly to the west of the River Exe.

Geologically, it is part of the Pottsville Escarpment.

Geologically, Lake Victoria is relatively young – about 400, 000 years old – and it formed when westward-flowing rivers were dammed by an upthrown crustal block.

Geologically, Pinellas is underlain by a series of limestone formations, the Hawthorne limestone and the Tampa limestone.

Geologically, the region is defined by coal-bearing layers from the upper Carboniferous period.

Geologically, recent faulting is indicated, however, by the apparent displacement of quaternary earth materials along the Big Valley fault.

Geologically speaking, Boston, NY is one of the more interesting places in the Greater Niagara region, for many glacial activities, over very many long years, caused sufficient pressure indentation to alter dramatically the landscape and even the water table.

Geologically, Ardmore is situated about 9 miles ( 16 km ) south of the Arbuckle Mountains, and is located at the eastern margin of the Healdton Basin, one of the most oil-rich regions of the United States.

Geologically, its terrain is almost completely flat levelled, which is the custom for south-western Skåne as a whole.

Geologically, the city lies on basalt flows that were heavily eroded by catastrophic flooding at the end of the Ice Age, so the city and environs is in the Channeled Scablands.

Geologically, the Firth of Forth is a fjord, formed by the Forth Glacier in the last glacial period.

Geologically it is mostly Pre-Cambrian rock, with some areas dated to Permian and Triassic periods.

Geologically, the town is situated on rock dated to the Carboniferous Period, consisting of coal measures and gritstones.

Geologically, the Thuringian Forest is defined by a belt of strongly uplifted and deformed metamorphic and igneous rock that divides the relatively flat sedimentary plains of the Thüringer Becken ( to the northeast ) from similar rock formations in the valley of the Werra ( to the southwest ).

Geologically, the aquifer is composed of limestone from the Cretaceous period, about 100 million years old.

Geologically, Nara Prefecture is bisected by the Japan Median Tectonic Line ( MTL ) running through its territory East-West, along Yoshino River.

Geologically speaking, a tea table is a rock formation that is a remnant of newer strata that have eroded away.

Geologically, the islands are not part of the Antillean arc.

Geologically, the rocks found at the two capes, and indeed over much of the peninsula, are part of the Table Mountain Group, and are formed of the same type of sandstones as Table Mountain itself.

It sits within the Wollongong Statistical District, which covers the local authority areas of Wollongong, Shellharbour and Kiama, extending from the town of Helensburgh in the north to Gerroa in the south Geologically, the city is located in the south-eastern part of the Sydney basin, which extends from Newcastle to Nowra.

Geologically the islands are part of the Luzon Volcanic Arc.

Geologically, the Gulf of Aqaba is an integral part of the Great Rift Valley that runs from East Africa through the Red Sea and northwards towards the rift valley containing the Dead Sea.

Geologically, the Balkan Mountains is a ' young ' part of the Alp-Himalayan chain which stretches across most of Europe and Asia.

Geologically, the range is considered a monocline ; part of a rifted volcanic margin.

Geologically, the group is part of the Australian continent, along with New Guinea, Tanimbar, Tasmania and Timor on the Indo-Australian Plate.

Geologically, the northern part of the county is in the Canadian Shield and the southern part is in the Great Lakes Basin.

Geologically the plateau is part of the extended plateau of the Great Plains in the Dakotas, and is separated from the main plateau to the west by the Missouri River Trench.

Geologically, the range is a part of the larger rugged Columbia River Plateau, located in the dry area of Oregon east of the Cascade Range.

Geologically, the Treskavica range is part of the Dinaric Alps and formed largely of secondary and tertiary sedimentary rock, mostly limestone and dolomite.

Geologically, the area is part of the Canadian shield.

Geologically, the Zanskar Range is part of the Tethys Himalaya, an approximately 100-km-wide synclinorium formed by strongly folded and imbricated, weakly metamorphosed sedimentary series.

Geologically they are part of the western slate zone ( greywacke zone ).

Geologically, the area is part of the larger Boston Basin and attaches to the relative lowland known as the Cambridge plain.

Geologically, the island is volcanic, being a part of a small crustal block on the Aleutian Arc that is being torn apart by oblique subduction.

Geologically the mountains are young, and with the exception of a few volcanic rocks in the extreme western part of the range, and a small exposure of the metamorphic Franciscan Formation north of Carpinteria, exclusively of sedimentary origin.

“ Geologically they are originally part of the main land at the edge of the great riff or fault which formed the depression to which the waters of Lake Superior collected .” When the glaciers melted, waves from the waters of Lake Superior caused erosion that formed the islands.

Geologically the fell forms part of the Thirlmere Member of the Lincomb Tarns Formation.

Geologically the summit of the fell forms part of the Deepdale Formation, ( principally volcaniclastic sandstone ) underlain by the dacitic lapilli-tuff of the Helvellyn Formation.