Notes, summaries, assignments, exams, and problems for Geology

Magma Classification and Characteristics

Magmas are molten rock materials found beneath the Earth's surface, characterized by their temperature, silica content, and viscosity. These properties dictate their behavior and the types of igneous rocks they form.

Basic Magmas

• Temperature: High, typically 1000-1200°C.
• Silica Content: Low (around 50%).
• Viscosity: Low, allowing them to easily reach the surface.
• Resulting Rocks: Dark-colored, with densities around 3000 kg/m³. Examples include basalt (extrusive) and gabbro (intrusive).

Acid Magmas

• Temperature: Lower, typically around 700°C.
• Silica Content: High (around 75%).
• Viscosity: Very high, often preventing them from reaching the surface easily.
• Resulting Rocks: Lighter-colored, with densities around 2600

Roman Memorials

Roman memorials were usually located in the forum or on the access roads to the cities.

Triumphal Arches

Triumphal arches were built for parades of victorious troops, dedicated to victorious generals or emperors. They were often placed in strategic locations such as road crossings, near bridges, and especially at the ends of forums.

• Primarily known from the Imperial period, they must have also existed in the Republican period.
• Their typology was diverse:
  • They usually consist of one or three openings, called "eyes," with the central one being the broadest. Above the entablature, a second body called the "attic" or "penthouse" was available, on which inscriptions were placed. The entire structure was completed with architectural and

Binders

Binders are materials that, when mixed with water, produce a chemical reaction that gives cohesion to particles. They are used to join construction pieces.

Chalk

• A naturally occurring calcium sulfate.
• Cooked to 180 °C, it becomes soft.
• Cannot be used outdoors as it becomes solid quickly and oxidizes iron.
• Uses: Wall cladding and ceilings.
• Variety: Plaster, used for plasterboard, decoration, molds, prosthetics, and orthopedic arts.

Lime

• Calcium carbonate, obtained by heating to about 900 °C.
• Highly reactive with water, which can raise the reaction temperature to 150 °C.
• Replaced cement until its discovery.
• Applications: Additive in mortars, whitewashed walls, purification tanks.

Cement

• A mixture of clay and limestone, heated to about 1600 °C.
• Properties

Factors Influencing the Peninsular Rivers

The characteristics of peninsular rivers are influenced by several factors, including:

• Climate: Rainfall and temperature patterns significantly impact river flow.
• Relief: The topography of the land affects the direction and speed of water flow.
• Lithology: The underlying rock type influences water absorption and erosion.
• Vegetation: Plant life can affect water flow and sediment levels.
• Human Action: Activities such as dam construction and irrigation alter river regimes.

River regimes can be classified as rain-fed, snow-fed, or a combination of both (mixed).

Basin Types

• Exorheic Basin: Characterized by water flowing into the open sea.
• Endorheic Basin: Refers to landlocked water bodies.
• Arheic Basin: Describes areas

Biodiversity in Spain

Location: Southwest Europe. Spain has two large biogeographic regions: Atlantic and Mediterranean. The Canary Islands have a tropical climate. The Iberian Peninsula served as a refuge during glaciations. Many animal and plant species evolved, forming new species. The presence of mountain ranges allows species to reproduce at high altitudes, creating a gradation between northern and southern Europe.

Human Impact on Biodiversity

Biodiversity has been affected by human actions, which have transformed the natural landscape (forests replaced by arable fields, etc.). This has led to a loss of vegetation and an increase in urban and industrial sites.

Landscapes of Plants

Oceanic Plant Landscape

Found in the Galician and Biscay regions.... Continue reading "Spain's Biodiversity: Habitats and Threats" »

Weathering of Rocks by Atmospheric Agents

Clasts are fragments of rock torn from a larger rock mass. The fragmentation of rocks is caused by atmospheric agents such as rain and snow. These agents wet the rock, dissolving minerals and reacting with them. Temperature changes also contribute: the expansion of rocks as the sun heats them contrasts with the contraction caused by freezing. Water seeps into cracks in rocks, subjecting them to pressure during freezing (gelifraction).

Weathering is the set of processes due to atmospheric agents that produce the alteration and disintegration of rocks.

• Mechanical Weathering: The rock is fragmented due to expansion and contraction, the freezing of water, or the impact of falling rocks.
• Chemical Weathering:

1. Geological Processes: Origin and Types

1.1 External Geological Processes

• Source:
  • Solar energy
• Type:
  • Weathering: Action of the atmosphere
  • Erosion: Separation of fragments and soil disturbance
  • Transport: Movement of these fragments in favor of gravity

1.2 Internal Geological Processes

• Source:
  • Geothermal energy inside the Earth
• Type:
  • Orogenic Movements: Horizontal displacement
  • Epirogenic Movements: The rise and decline with increasing mass of the Earth's crust

2. Plate Tectonics

• Structure based on geochemical and dynamic models:

• Source of plate movement:
  • Two scenarios:

1. Convection currents or flaring rims creating constructive

Earth's Dynamic Processes and Landforms

The displacement of lithospheric plates is responsible for the construction of Earth's relief, through the formation of mountain ranges and mid-ocean ridges. This movement also causes significant deformation of rocks.

Lithospheric Plate Movement

Formation of Mountain Ranges

Areas of collision between two plates are subjected to immense pressure, which compresses sediments, causing them to fold and form towering mountains.

Mid-Ocean Ridges

Mid-ocean ridges are large submarine elevations located in the middle of oceans, where magma flows through a central groove called a rift.

Oceanic Trenches

Oceanic trenches are deep depressions found along the coasts of oceanic islands and continents, representing the deepest... Continue reading "Earth's Geological Dynamics: Landforms, Rocks, and Cycles" »

Wilson Cycle

1. Hot mantle materials rise, causing the crust to fracture due to its rigidity. The fractures allow magma to output, and blocks of the lithosphere move, initiating the formation of an intracontinental rift valley.
2. The expansion of the ocean floor creates a narrow sea.
3. The growth of the seafloor allows the development of a mature ocean basin. Stable continental margins are limited by the basin's floor, where an important place of sediment deposition occurs.
4. The stable continental margins become active when the oceanic lithosphere begins to sink in subduction.
5. The reduction of the ocean is very evident. Marginal ranges are formed on active continental margins.
6. The oceanic lithosphere continues to subduct and sink until the ocean is completely

Classifying Energy Sources

Non-Renewable Energy

Energy sources available in limited quantities that are consumed much faster than they form.

Fossil Fuels

• Coal: A mineral fossil fuel originating from the decomposition of buried plant matter, accumulated over millions of years. Today, it's primarily used as fuel to produce thermal energy.
• Oil: A thick, dark, oily liquid formed from the decomposition of plant and animal remains buried for millions of years. It has a high calorific value, is relatively easy to extract and transport, and is used to generate electricity and produce materials like plastics and paints.
• Natural Gas: Has a similar origin and formation process to oil, often found together in deposits (jaciments). It's used as fuel or as a feedstock