a rock specimen of a particular depositional enviroment
Yes, sedimentary rocks can be formed at the bottom of lakes through the accumulation and compression of deposited sediments over time. Processes like lithification can occur in lake environments, leading to the formation of sedimentary rocks such as shale or limestone.
sedimentary facies
They are called clastic sedimentary rocks.
Subduction and high pressure.
No, sedimentary rocks formed from fragments of other rocks are called clastic sedimentary rocks. Chemical sedimentary rocks form from minerals that are dissolved in water and precipitate out to form rocks like limestone or halite.
Most regional metamorphic rocks are formed in conditions within this range of geothermal gradients, passing through the greenschist facies to the amphibolites
Philip R. Royce has written: 'Stratigraphy, provinance and facies analysis of the Albian-Turonian Virginian Ridge Formation and Winthrop Sandstone, Methow Basin, northeastern Cascades, Washington' -- subject(s): Facies (Geology), Geology, Stratigraphic, Rocks, Sedimentary, Sedimentary Rocks, Sedimentation and deposition, Sediments (Geology), Stratigraphic Geology
Yes, sedimentary rocks can be formed at the bottom of lakes through the accumulation and compression of deposited sediments over time. Processes like lithification can occur in lake environments, leading to the formation of sedimentary rocks such as shale or limestone.
sedimentary facies
weathering erosion transportation deposition compaction/cementation and lithification changes sediments to sedimentary rocks. High pressure and temperatures changes them to metamophic rocks
yes
metamorphic
They are called clastic sedimentary rocks.
Subduction and high pressure.
False Sedimetary rocks can be formed from changes in igneous rock, and igneous rock can be from changes in sedimentary rock.
Heat and pressure from tectonic forces can metamorphose sedimentary rocks into metamorphic rocks. Weathering and erosion can break down sedimentary rocks into smaller particles or clasts. Hydrothermal fluids can alter the mineral composition of sedimentary rocks through processes like recrystallization.
Heating and pressurization changes igneous and sedimentary rocks into metamorphic rock.