Rock can be defined as a natural aggregate of minerals connected by strong and permanent attractive forces and considered as a consolidated materials
Soil is defined as unconsolidated sediments and deposits of solid particles resulting from the disintegration of rock
Topsoil is the top layer of regolith.
Igneousrock results from the cooling and hardening of molten rock called magma, originating deep within the Earth
Sedimentary rock is formed from accumulated deposits of soil particles or remains of certain organisms that have become hardened by pressure or cemented by minerals
Two types of igneous rock:
Extrusive/Volcanic rock type: when molten materials cool rapidly at or near the Earth's surface (e.g., Basalts, Rhyolites, Andesites)
Intrusive/Plutonic type: when molten rock is trapped deep below the surface of the Earth and cools slowly (e.g., Granites, Syenites, Diorites, Gabbros)
Rocks with chief minerals as Quartz or Orthoclase (high in silica content) decompose to predominantly sandy or gravelly soil with little clay (e.g., Granite and Rhyolite)
Acidicrocks are light-colored, classified as acidic due to high silica content (e.g., Granite and Rhyolite)
Regolith protects the rock below from weathering because bedrock weathers easier than regular rock.
Most non organic materials that are identified as soil originated from rock as the parent material.
The source of soils.
Rock
Basicrock are very dark colored rock.
Rocks like granites, which are acidic, are considered good construction materials
Sedimentary rocks:
Shale: formed predominantly from deposited clay and silts soils, relatively stable when exposed to the environment but some expand or delaminate after contact with water or air.
Plastic flow refers to slow viscous movement and rearrangement within the rock mass as it changes and adjusts to the pressures created by external forces
Soil categories:
Residual soil: formed from weathering of rocks and remain at the location of their origin, the weathering process may be attributed to mechanical weathering or chemical and solution weathering.
Metamorphic rock results when igneous rock or sedimentary rocks are subject to a combination of heat, pressure, and plastic flow, changing the original rock structure and mineral composition
The rate of weathering is greater in warm humid regions than in cool dry regions
Sand stone is predominantly quartz cemented together with silica.
Which are generally considered good construction materials
Calcium carbonate or Iron compounds
Cemented sand and gravel
Conglomerate
Cemented rock fragments which are similar to sand stones.
Breccia
Predominantly crystalline calcium carbonate formed under water.
Limestone
A variety of limestone, but harder and more durable.
Dolomite
Softer forms of limestone.
Marl and Chalk
A good foundation material provided that the formation is sound and free of cavities.
Marl and Chalk
Refers to the effect of wind rain, running water and tectonic forces (such as earthquake)
Mechanical Weathering
Is a rock decomposition due to chemical changes in the rock minerals brought about by exposure to the atmosphere, temperature changes, water or other materials.
Chemical and Solution Weathering
Are those materials that have been moved from their place of origin.
Transported Soil
Most common example of intrusive/plutonic type of rock
Granites
When molten materials cooled rapidly at or near the Earth’s surface.
Extrusive or volcanic rock
Example of Extrusive or Volcanic rock
Basalts, Rhyolites, Andesites
Intrusive or Plutonic Rock is when molten rock trapped deep below the surface of the Earth and cooled slowly.