Notes, abstracts, papers, exams and problems of Geology

Relative Dating Methods

The Formation of Minerals

The atoms will come apart, change themselves, and then form a new mineral.

Types of Metamorphic Rocks

Metamorphic rocks are divided into two categories: foliated and non-foliated. Be able to determine which rock is foliated and which is not.

Foliated Rocks

Foliated rocks are patterned rocks where you can see changes in the rock.

Non-foliated Rocks

Non-foliated rocks are solid color rocks.

Size, Shape, Site, Shadow, Texture, Pattern, Association, Tone.

Understanding Maps

Map: A representation usually on a flat surface of the whole or a part of an area.

Scale: Map Scale = Map distance/Earth distance

Be able to give a U.S.P.L.S. description of certain features/locations.

From the left to the right.

R7E, T14S, Sec.1, NE, SW, SE.

Non-Renewable Energy Sources

The Theory of Plate Tectonics: Global Tectonic

This theory states that:

• The lithosphere is divided into plates that cover the Earth's surface and fit together like a puzzle.
• The internal geological activity (volcanoes and earthquakes) is located in the boundaries between the plates.
• The ocean bottoms are generated in the ridges, by the magma that comes from the mantle and are destroyed in the trenches by subduction.
• When the plates move, they drag the continents. Where the plates separate, an ocean is formed, and where they collide, mountain ranges are formed.

Wegener said that the continents were those that moved on the ocean floor. LITHOSPHERE = CRUST + UPPER MANTLE.

ASTENOSPHERE allows plates to move vertically/horizontally.

Plates move with respect... Continue reading "The Theory of Plate Tectonics: Global Tectonic and Plate Movements" »

SYSTEMS

Can be small or large, living or non-living.

Types: open, close and isolated

• Open: exchanges both energy and matter
• Close: only exchange energy
• Isolated: Energy and matter is not exchange

Transfer: Basic flow through a system. Change in location of energy or matter.

Transformation: A new product is created. Change of state.

First law or thermodynamics: energy in an isolated system can be transformed but cannot be created or destroyed.

Second law or thermodynamics: is lost in the different levels of a system.

Entropy: is a measure of the amount of disorder in a system.

Negative feedback:

Positive feedback:

PRODUCTIVITY

Is the conversion of energy into biomass over a given period of time.

Biomass: is the living mass of an organism

Gross: total amount... Continue reading "Understanding Systems, Productivity, Global Warming, and Photochemical Smog" »

Echo sounding: is a type of sonar used to determine the depth of water by transmitting sound waves into water.

Trieste: is a city and a seaport in northeastern Italy. What is Trieste famous for? In the 19th century the monarchy was one of the Great Powers of Europe and Trieste was its most important seaport.

Deep sea winch: Fishing rod, mechanism

drift bottle : a bottle containing a record of the time and place at which it was set adrift in the ocean for supplying when recovered data to aid in determining the circulation of surface waters in the ocean

drogue: a device, typically conical or funnel-shaped with open ends, towed behind a boat, aircraft, or other moving object to reduce speed or improve stability.

Swallow Float: A tubular buoy used to... Continue reading "Exploring Oceanography: Tools and Techniques" »

Chapter 8 – Earthquakes

What is the elastic rebound theory? Is it possible for energy building up in the lithosphere to be released in a sequence of earthquakes?

Rocks “spring back” – a phenomenon called elastic rebound

Energy is released in a sequence of earthquakes (one earthquake can trigger slip on a nearby fault)

What is a seismic body wave, and what characterizes each of the two types of body waves (i.e. type of motion, velocity)?

1. Primary(P) waves(spring)=push&pull motion, greatest velocity, arrive first, travel solid, liquid, gases.
2. Secondary(S) waves (rope)=up&down motion, slower velocity, arrive after P at seismograph, travel only solid.

What is a seismic surface wave, and what characterizes each of the two types of surface

Chapter 5 - River Systems

How rivers and streams work – Gradient (know this!)

• Streamflow
  • Factors that determine velocity
  • Gradient, or slope
  • Channel characteristics
    • Shape
    • Size
    • Roughness
    • Discharge – volume of water flowing in the stream (generally expressed as cubic feet per second)
• Gradient highest nearest river source, where is it lowest?
• Upstream-downstream changes
  • Profile
  • Cross-sectional view of a stream
  • From head (source) to mouth
  • Profile is a smooth curve
  • Gradient decreases from the head to the mouth
  • Factors that increase downstream
    • Velocity
    • Discharge

Base level

Rivers flow and/or erode to the lowest level, ultimately to sea level

• Base level
  • Lowest point a stream can erode to
  • Two general types
    • Ultimate – sea level
    • Temporary, or local
  • Changing causes readjustment

THE WATER OR RIVERS:

The route of the rivers is determined by the relief. The characteristic differentiated sides are the Atlantic side and Mediterranean.

Atlantic:

Here are the longest rivers. This vertiente pertenece the longest river and the mighty of the region Guadalquivur along with its main tributary, the Genil basin is regulated by Gualdalkibir numbers embalses. Other rivers of the red side are the Guadalete, Odiel, and Barbate.

Mediterranean:

Is composed of rivers that pour their waters into the Mediterranean Sea. These rivers are born on the mountain rivers Penibética neighborhoods so they are small and short with irregular flow. Some of these rivers remain dry most of the year. Among Andalusian Mediterranean rivers can stand the walking... Continue reading "Geography and Climate of Andalusia: Rivers, Climate Variations, and Environmental Issues" »