Glaciers pick up glacial till and sometimes run into moraines or other large objects. they deposit their till around these objects forming long deposits. this is called a(an)

drumlin

Explanation:

Drumlin

It is present in the streamlined scenery in the central lowland of the Scotland . The drumlin is in the form of a small hill , with steep slopes , summit at the up - ice end and tending an egg shape .

Drumlin always occurs in groups and is rarely found in single .

And the ends are tapered of each of the hill that points in the direction of the glacier flow .

kettle, moraine and till

Kettle, moraine and till are formed by the glacier deposition.

Kettle: It is formed when the blocks of ice comes out of the retreating glacier and gets submerged in the hole of sediments.

Moraine: It is a mass of rocks and sediments carried by a retreating glacier and deposited to other locations, typically in the form of ridges.

Till: It is formed when the materials like sediments in the form of clay, sand, gravel and boulders are frozen in the glacier.

the roman republic began to expand when rome fought the punic wars and defeated carthage. the punic wars refer to the series of 3 wars fought among rome and carthage, before it ended in carthage's defeat.

it being an ocean esketit where we droppin