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Bisecting the Southern Highlands is the Isthmus of Tehuantepec, a low-lying, narrow constriction of land that reaches an elevation of less than 900 feet (275 metres).
West of the Deotamura Range is the Agartala Plain, an extension of the lowlands of the Ganges (Ganga) and Brahmaputra river basins, with an elevation of less than 200 feet (60 metres).
The angle of the long axis of the concourse, following that of Manhattan's east-west streets, is not 90° but 119° east of north, and aligns with the sun through its "west" windows only from late May to early July, and then only at an elevation of less than 3°.
South of Lugnaquillia the range is not a significant barrier, but the Wicklow Mountains are nowhere crossed at an elevation of less than 1,000 feet (300 metres); the Military Road through the mountains, built after a rebellion in 1798, runs at an elevation of more than 1,000 feet for more than 20 miles (30 km).
Limestone low islands are those which are composed of at least 80%% calcareous rock types and rise to a maximum elevation of less than 30 m above mean sea level.
Volcanic low islands are those which are composed of at least 80%% igneous rock types and rise to a maximum elevation of less than 30 m above mean sea level.
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About half of this vast area lies at elevations of less than 650 feet (200 metres) above sea level, and the highest point (in the Valdai Hills, northwest of Moscow) reaches only 1,125 feet (343 metres).
The relief of the area is low having elevations of less than 10 50 m above sea level and is trending in the northward direction (Ugbaja and Edet 2004).
Most of Croatia is lowlands, with elevations of less than 200 m above sea level recorded in 53.42% of the country.
Lowlands make up the bulk of Croatia, with elevations of less than 200 m above sea level recorded in 53.42% of the country.
For elevation angles of less than 90° the forces agreed with many previous model-based calculations.
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