ऑलिव्ह-हिरव्या वाळूचा खडक असलेले ग्लुकोनाइट,

greensand's Usage Examples:

It is typical of the strip tithings on the northern edge of Salisbury Plain: it extends from the greensand.

Glauconite particles are one of the main components of greensand, glauconitic siltstone and glauconitic sandstone.

The name derives from the distinctive outcropping of golden greensand rock present at the very top of the cliff.

HistoryMuch of Cottenham parish lies on a lower greensand ridge around 8 metres above sea level, which until the 17th century draining of the Fens was the only dry land in between Cambridge and the Isle of Ely around 12 miles to the north-east of the village.

Geology The hill is formed from upper greensand which is more resistant to erosion than the surrounding clay.

Thus references to "greensand marl" sometimes refer specifically to glauconite.

There are strong outflows of springs at various junctions of the upper greensand and gault.

The older parts of the church are in local greensand stone, while the restoration used limestone ashlar.

The Greensand Ridge, also known as the Wealden Greensand is an extensive, prominent, often wooded, mixed greensand/sandstone escarpment in south-east England.

300 to 500 metres (980 to 1,640 ft) of much less-resistant clays and greensands; Wealden clays, Gault and Upper Greensand.