Lecture 13 - Weathering and Erosion Flashcards
What is the Definition of Weathering?
-Series of processes that happen to rock as it is exposed to Earth’s surface; this may be physical, chemical or biological
What is the Definition of Erosion?
-The transportation of rock away from its exposure to another location
What is the Definition of Denudation?
-The removal of rock either by chemical decomposition or physical removal that wears down the Earth’s surface
-Erosion + chemical dissolution
What is Chemical Weathering?
-Involves chemical reactions with minerals, new minerals are formed and they may be soluble in water and easily transported
What is Physical Weathering?
-Rocks broken up into smaller pieces by mechanical force
What is Biological Weathering?
-Rocks altered chemically and or physically by the presence of plants, animals and bacteria
Factors Affecting Weathering: What is Lithology?
-Mineralogical composition and structure of rock
Factors Affecting Weathering: What is Climate?
-Rainfall and temperature are both important
-The same rock changes its weathering resistance depending on climate (tropical rainforests tend to have higher rates of weathering due to higher temperatures and rainfall)
Factors Affecting Weathering: What is Length of Exposure?
-The longer a rock is exposed at surface, the more weathered it will be
-Weathering is strong when erosion is low (material stays in place for longer)
Chemical Weathering: What is Solution?
-Simplest form of chemical weathering
-Minerals are decomposed with water acting as a solvent
Chemical Weathering: What is Carbonation?
-CO2 reacts directly with a mineral to from new minerals and releases bicarbonate ions (HCO3-)
-E.g. weathering of feldspars to form clay is a carbonation process (works quicker with higher temperatures)
Chemical Weathering: What is Oxidation?
-Process whereby an atom or ion loses an electron, increasing its positive charge
-Main oxidising agent is oxygen dispersed in water
-E.g. the Banded Iron Formation:
-formed when oxygen appeared
in oceans produced as waste by
cyanobacteria
-Oxygen entered contact with Fe-
rich waters (possibly from the
deep ocean)
-Fe was rusted and deposited
forming the BIF
What is Regolith and Soil?
-As rock reaches the Earth’s surface, it undergoes physical and chemical weathering
-Weathering can penetrate at depth, creating a weathered profile; a continuum from fresh rock to fractured and weathered rock, with soil at the top
-Regolith constitutes this entire layer of unconsolidated material