👷AGY201. EARTH HISTORY

Earth History
🟢 *STRATIGRAPHY*
This is a branch of geology that deals with the study of rock layers and layering. Also used in the study of sedimentary and layered volcanic rocks.
   Its scientific discipline is concerned with the description of rock successions and their interpretation terms of a general time scale.

*PRINCIPLES OF STRATIGRAPHY*
All geologists use these principles in deciphering the spatial and temporal relationship of rock layers. The laws were developed in the 17th - 19th centuries based upon the work of *Nicolaus Steno (1669), James Hutton and William Smith*

(1) *PRINCIPLE OF UNIFORMITARIANISM*
This states that "the present is the key to the past".
It allows us to interpret the events of the past in rocks; it allows us to write the history of Earth.
   In addition to allowing the interpretation of the past, it allowed the prediction of the future.

(2). *PRINCIPLE OF SUPERPOSITION*
This states that " in any undisturbed sequence of rocks deposited in layers, the youngest layer is on top and the oldest on bottom; each layer being younger than the one beneath it and older than the one above it.
Nicolaus Steno in 1669 also formulated this law.

(3). *PRINCIPLE OF FLORAL AND FAUNA SUCCESSION*
Flora is plant life, while fauna refers to animals.
*Fossils* are physical evidence of preexisting organisms, either plant or animal. Obvious fossils are the preserved skeletal remains of animals.
  Other fossils which are also evidence of past organisms include tracks and trails, burrows, droppings and root casts.
  The principle states that *"faunas and floras succeed one another in a definite recognizable order"*
Faunal succession is the fundamental tool of stratigraphy and comprises the basis for the geologic time scale.

  


🟣 *MINERALS*
Geology deals with the physical and historical aspects of the Earth.

*Physical geology* is the study of the composition, behavior and processes that affect Earth's lithosphere

*MINERALS* are basic building blocks of nearly all Earth materials for most geological purposes. It is also a naturally occurring, solid, inorganic combination (compound) of one or more elements whose atoms are arranged in an orderly fashion (crystallinity) and has an established chemical composition that can vary slightly within specific limits.
Crystal structure is redundant.

Minerals like glass and opal have no particular geometric arrangement of their atoms (they are not true minerals because they lack crystallinity).
Mineraloid is used for these materials and some mineraloids are simply called rocks. (natural glass, obsidian is a kind if volcanic rock).

*MINERALS CHARACTERISTICS TO BE CLASSIFIED AS A MINERAL*
1. Naturally occurring
2. Solid
3. Inorganic
4. Geometric arrangement of its atoms
5. Chemical composition that can vary only according to  its specific limits

      *COMMON MINERALS*

*Quartz (SiO₂)* is most commonly known mineral. e.g Rose, Milky, Chart, Flint, Agate.

*Halite (NaCl)* is probably the most commonly used mineral and is found in most spice cabinets as table salt.

*PHYSICAL PROPERTIES OF MINERALS.*

1. *Hardness*: (vary from sample to sample of same mineral). e.g Magnetite ---- Hardness of 6. (5.5 - 6.5)

2. *Crystal form* is the geometric arrangement of plane(flat) surfaces on the outside of a mineral that reflect the internal crystallinity of the mineral.  Halite and Fluorite often has cubic crystal form. Corundum, Quartz and Calcite show different variations on the hexagonal crystal form.
Minerals without an external crystal form are referred to as *MASSIVE* (e.g. Chert, Limonite, e.t.c)

3. *Cleavage*: is the tendency of a mineral to break in a systematic way along planes of weakness determined by the type and strength of the chemical bonds between the atoms that make up the mineral.

4. *Fracture*:is the non- systematic and irregular way some minerals break. It is rough or uneven, unlike cleavage planes which are smooth and flat.
Conchoiddal fracture is a special kind of breakage that results in a curved parting surface. A homogeneous material that lack planes of weakness, equally strong in all directions.(e.g glass)

5. *Striations*: are very fine, parallel lines visible on the cleavage planes or crystal faces of some minerals due to their crystal structure and growth patterns.
Albite and Labradorite, both plagioclase feldspars---(1 cleavage plate). e.g. pyrite, quartz, garnet.
One direction cleavage: e.g. Biotite, Talc, Chlorite, Muscovite, Selenite, Gypsum

Two direction of cleavage: e.g. orthoclase and plagioclase

Three direction of cleavage:  e.g. Calcite

Four direction of cleavage:  e.g. Fluorite

Six direction of cleavage:  e.g. sphalerite


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