Mainly through expansion of cracks and fissures from frost expansion which leads to further and deeper cracks and fissures. Plant roots seeking moisture may extend roots into limestone cracks and fissures, prying the rock apart.
False
A xenocryst is a mineral crystal which is imbedded in igneous rock. The crystal is formed by exotic chemical and structural reactions in the tremendous pressure and temperature of the Earth's mantle, below the crust. The crystal is then picked up by liquid magma rock, and carried up cracks and fissures into the crust, where it solidifies into igneous rock. If the magma makes it all the way to the Earth's surface (where it is called lava), it solidifies into igneous rock either as a lava flow or a volcanic eruption. A classic example is the inclusion of xenocystic diamonds in fissures of igneous Kimberlite rock in the famous diamond mines of Africa.
the plants roots sink into the rock and cracks the rock.
places where groundwater bubbles or flows out of cracks in the rock is called springs.
Mainly through expansion of cracks and fissures from frost expansion which leads to further and deeper cracks and fissures. Plant roots seeking moisture may extend roots into limestone cracks and fissures, prying the rock apart.
Insects can perform their life functions in and around the cracks and fissures of exposed weathered metamorphic rock.
faults
fissures I'm 100% sure
such as rain and sleet and snow,
Vein minerals can contain deposits of metals and other minerals, and occur in fissures or cracks of rock.
That is known as an "intrusion". The magma (lava) is forced under pressure into cracks and fissures within the older rock. There are some good examples of this type of formation in Yellowstone caldera.
Cracks, splits, openings, crevasses.
They are called fissures.
These are typically called fumaroles, and can occur along cracks or fissures in the ground.
Groundwater seeping through the limestone rock over thousands of years dissolved the rock, creating cracks and fissures. Eventually, these cracks formed larger passageways that became the cave system of Lascaux.
the beds have cracks and fissures in them