Dolerite hills form from the cooling and solidification of magma that intrudes into existing rock layers and then crystallizes underground. Over time, erosion removes the overlying sedimentary rocks, exposing the more resistant dolerite, which typically manifests as rugged hills or outcrops. The process involves geological uplift and weathering, which contribute to the formation of distinctive topographies in areas where dolerite is prevalent.
A bluestone is any of a variety of types of stone, including a form of dolerite which appears blue when wet, or a feldspathic sandstone in the United States.
The Sandhills are bigger, both in the height of the hills and the size of the region.
The Ngong Hills (Kenya) The Cheviot Hills (England)
Dawn Hills goes by Dawny, and Dawny Hills.
Nate Hills's birth name is Floyd Nathaniel Hills.
Dolerite is very rough.
Dolerite is not naturally magnetic. It does not possess magnetic properties on its own.
A dolerite dyke is a sheet-like igneous intrusion that cuts across the surrounding rock formations. It is composed mainly of medium-grained dolerite rock that solidified from magma that intruded into existing rock layers. Dolerite dikes are common in areas with volcanic activity or tectonic movement.
Dolerite rocks are a type of igneous rocks (formed as a result of cooling of magma or lava). They are mafic (45-52% SiO2), and subvolcanic (formed within the earth's crust). Within this characterisation there is considerable variation. Please see the link.
It wuz used for pounding into a rock. the dolerite ball was very. very hard.
Dolerite is a type of volcanic rock that is commonly found in dikes and sills. It is formed from the slow cooling of magma underground. Dolerite can be found in various regions around the world where there has been volcanic activity in the past.
Igneous Rock :)
A bluestone is any of a variety of types of stone, including a form of dolerite which appears blue when wet, or a feldspathic sandstone in the United States.
A dolerite occurs in dikes and sills. These are dark, medium-grained igneous rocks that are typically containing olivine, plagioclase, and pyroxene.
hills change shape and form from erosion
hornblende
Well really the valleys BETWEEN hills form by glacial and/or other erosion. The hills are what's left behind.