lacustrine ,

Lacustrine means "of a lake" or "relating to a lake".

Lacustrine plain: A nearly level land area that was formed as a lakebed.

Lacustrine species reported from Teraina include fish.

Lacustrine material is well sorted and fine-textured, having finer silts and clays.

Lacustrine deposits are those deposited in lake water, and only when the lake drains or the land rises does it become dry land.

The shores of all Siberian lakes which filled the depressions during the Lacustrine period abound in remains dating from the Neolithic age.

Lacustrine vole (M. limnophilus)

Lacustrine wetlands generally occur on river floodplains and along lakeshores and are influenced by seasonal variations in groundwater levels.

Lacustrine shales consist of Lamosite and Torbanite.

Lacustrine fluvial whitefish (Coreganus megalops)

Lacustrine tufas are generally formed at the periphery of lakes and build up phytoherms (freshwater reefs) and stromatolites.

Lacustrine mud that is interbedded with salt and saturated with brine underlies the surface of Salar de Uyuni.

Lacustrine sediments filling these depressions contain a record of the Allerød warming, Younger Dryas cooling, and other climatic events.

Lacustrine plain, a plain that originally formed in a lacustrine environment, that is, as the bed of a lake.

Lacustrine silt deposits replaced soil scraped away by the glaciers, leaving behind deep, productive soil after the river breached the obstructing moraine and the lake disappeared.

Although many lovely lakes can be found in the Andean and coastal regions of central Chile, the south (Sur de Chile) is definitely the country's most lacustrine area.

Lacustrine sediments and associated terraces provide evidence for the past existence of five major prehistoric lakes that occupied the Tinajani Basin during the Pliocene and Pleistocene.

Rocks from Turkana containing Rimasuchus fossils are usually poorly lithified fluvial or lacustrine sandstones or mudstones that were deposited in lakes and rivers.

Lacustrine sediments deposited by the glacial lake are parent to the present soils of peats, silt, and sand; the peats are in marshes which form large parts of the park.

Lacustrine sediments of the Lower Tinajani Formation, which are exposed within the Tinajani Basin, demonstrate the presence of a pre-Quaternary, ancestral Lake Titicaca within it between 18 and 14 million years ago.