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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.
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Geologically and speaking
Geologically speaking, an increase in sediment load will over time increase the slope of the river, so these two conditions can be considered synonymous ; and, consequently, a variation of slope can model a variation in sediment load.
Geologically speaking, a tea table is a rock formation that is a remnant of newer strata that have eroded away.
Geologically speaking, Inwood Hill Park is quite diverse, with marble, schist, and limestone all prevalent in the area.
Geologically speaking, the whole area was originally under water, and, when the land rose, the chalk Wolds were formed from the skeletons and shells covering the sea floor.
Geologically speaking, Glen Coe is the remains of an ancient supervolcano that erupted with a force of VEI-8.
However, in an interview with Time magazine, Boris Behncke, a German researcher at the University of Catania's department of geological sciences in Sicily, said: Geologically speaking, it's a possibility, But geology has a very long time scale ... We really should not be too worried.
Geologically speaking, Fripp Island is considered to be a barrier island.
Geologically and Boston
Geologically, the area is part of the larger Boston Basin and attaches to the relative lowland known as the Cambridge plain.
Geologically and is
Geologically, the Cenozoic is the era when the continents moved into their current positions.
Geologically, Dominica is part of the rugged Lesser Antilles volcanic arc.
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, 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 and one
Geologically, it is located on the Land's End Granite, one of the five major granite batholiths that make up the spine of Cornwall ( see Geology of Cornwall ).
Geologically the archipelago is one of the most active volcanic regions in the world.
Geologically and geographically Pirin is divided into three parts: a north, central and south one, which are however not equal in size and tourist attractivity.
Geologically, Twente is one of the most interesting areas of the Netherlands.
Geologically and more
Geologically the district is predominantly greywacke of Late Jurassic to Late Cretaceous age, draped by wind-blown loess during the Pleistocene Ice Ages and more recently covered in volcanic ash and pumice from the Rotorua and Taupo volcanic centres.
Geologically, the Bass Islands are distinguished from the Austral Islands in that their vulcanism appears to be much more recent.
Geologically and interesting
Geologically interesting, the island is visited by many students engaged in mapping projects.
Geologically interesting parts of the Valley are the basalt flows and dinosaur tracks in South Hadley and Holyoke, Massachusetts, a chain of basaltic traprock ridges known as Metacomet Ridge along the ancient tectonic rift including the Mount Holyoke and Mount Tom ranges, layers of rock deposit laid down by the river, and varves and deltas
Geologically and places
Geologically, Holderness is underlain by Cretaceous chalk but in most places it is so deeply buried beneath glacial deposits that it has no influence on the landscape.
Geologically and region
Geologically, the region lies mostly within the Colorado Piedmont, in the valley of the South Platte and Arkansas rivers on the east side of the Rockies.
Geologically, Evans County lies in the coastal plain region of Georgia, an area consisting mostly of sedimentary rocks.
Geologically, this region is similar to the main Cascade Range, dominated by volcanism.
Geologically, the Catskills are a mature dissected plateau, a once-flat region subsequently uplifted and eroded into sharp relief by watercourses.
Geologically, the Little Sioux rises in a region of glacial potholes near the " Iowa Great Lakes " ( Spirit Lake, and East and West Okoboji ).
Geologically, Muswellbrook is situated in the northern parts of the Sydney basin, bordering the New England region.
Geologically the entire region is a part of the Deccan Trap of the Cretaceous Eocene period.
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