Isobath - a contour line linking regions of the same depth.

The total area of the bank within the 100 metre isobath measures 8 040 km2.

Drift ice extends 15-20 nm, roughly to the 10-15 m isobath.

It is 27.5 km long from safe water (12 m isobath) to the mouth of the Haihe.

The map also depicts the Brunei-Malaysian border as only running up to the 100 fathom isobath.

The bank is about 16 km in diameter as defined by the 200 m isobath, which correspondents to an area of more than 200 km.

Using current culture technologies, much farmed cultivation of marine plants and animals can be applied within the 10 metre isobath in marine environments.

Of these, 12 blocks were deepwater (beyond 400m isobath), 26 shallow offshore and 10 were onshore blocks.

"Contour line" is the most common usage in cartography, but isobath for underwater depths on bathymetric maps and isohypse for elevations are also used.

The canyon is located near the 100 meter isobath on the continental shelf and is 2,200 m (7,217 ft) deep at the base of the continental slope.

It extends from the shelf break zone an approximately 200m isobath for about 150 km downslope and reaches the depth of about 2,200 m within the abyssal plain.

Rosalind is 101 km long in a north-south direction, and 56 km wide, as defined by the 200 m isobath, which corresponds to an area of roughly 4 500 km2.

Until 2009, Malaysia did not recognise Brunei's EEZ claim and stated that Brunei's maritime territories ended at the 100 fathom isobath.

With little information on bottom type, a simple, one-off, spatial impact study like that shown in Figure 5 with eight sites along an isobath, taking three replicate grabs from each, is fairly common and moderately powerful.

In its 1979 territorial waters and continental shelf map, Malaysia claimed the area to be part of its continental shelf and depicted the Brunei-Malaysian border as running up to the 100 fathom isobath.

The last major regression, about 20,000 years ago, lowered the sea level to the present 130m isobath, which is south of Cape Point and Cape Hangklip, leaving the entire bottom of False Bay exposed.

The 2,000 m isobath follows more or less the course of the Garonne River and divides the basin into a relatively shallow northern platform, the so-called Aquitaine Plateau, and into a much deeper, tightly folded, southern region.

Of these, 9 blocks were deepwater (beyond 400m isobath), 7 shallow offshore and 11 were onland blocks The PSC's were signed for 23 exploration blocks comprising 9 deepwater, 6 shallow offshore and 8 onland.

There are three major basins contained within the Gulf of Maine: Wilkinson Basin to the west, Jordan Basin in the northeast, and Georges Basin in the south, which are isolated from each other beneath the 650 foot (200 m) isobath.

This littoral zone is wide and slopes gently: the 0 m isobath (the intertidal flats) extends to 3-8 km from shore at a slope of 0.71-1.28%, the 5 m isobath extends 14-18 km from shore, and the 10 m isobath reaches 22-36 km from shore.