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Deciduous Forests, Mediterranean Vegetation, and Soil Types

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1 - The Deciduous Forest

It consists of tall trees with straight trunks, smooth bark, and large leaves that fall in autumn. This forest type has relatively few species, often forming large masses. The most common features are Carballo oak and beech. In the understory, ferns and mosses thrive in a somber mood created by the treetops.

2 - The Heath and Grasslands

The Landa is a dense shrubland, whose height can be low or reach 4 feet. Its most abundant species are heather, gorse, and broom. The heath is considered a form of deciduous forest degradation or supraforestal vegetation. It is often used for animal bedding and then as fertilizer.

The meadows are herbaceous vegetation occupying large tracts of land with ocean views.

The Vegetation of the

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Plate Tectonics: Evidence, Types, and Interactions

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Plate Tectonics: Key Concepts

  • Biological Puzzles

    The existence of land bridges or island chains that connected the ancient continents.

  • Geographic Enigmas

    The outer edge of the continent is under the sea where the continental shelf terminates.

  • Geological Riddles

    There is a correspondence between geological structures present on both sides of the Atlantic Ocean.

Scenarios of Continental Drift

According to Wegener, all continents were part of a large landmass (supercontinent called Pangea).

  • Paleomagnetic Tests

    During the cooling of lava, ferrous minerals align. Studying these minerals indicates the position of the north pole.

  • Oceanographic Evidence

    The discovery of the oceanic ridge system that splits the great oceans.

  • Seafloor Spreading Hypothesis

    Harry Hess

... Continue reading "Plate Tectonics: Evidence, Types, and Interactions" »

Understanding River Systems: Gradient, Discharge, and Base Level

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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
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Understanding Natural Resources: Types, Sustainability, and Challenges

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Understanding Natural Resources

In human terms, a resource is anything we obtain from the environment to satisfy our needs and desires. All living things require basic resources such as food, water, and shelter. Some resources are directly usable, while others require effort or technology to become useful.

Types of Natural Resources

Perpetual Resources

These resources are virtually inexhaustible on human timescales. Examples include direct and indirect solar energy (wind, running water).

Non-Renewable Resources

Non-renewable resources exist in a fixed amount within the Earth's crust. They may form through natural processes, but over millions or billions of years (e.g., oil takes 600 million years to form). While complete exhaustion is rare, economic... Continue reading "Understanding Natural Resources: Types, Sustainability, and Challenges" »

Landforms and Geological Agents: Shaping Our Environment

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Landforms and Geological Agents

Forms of relief are shaped by geological agents and influenced by weather patterns.

Factors Influencing Landforms

  • Weather
  • Human population density
  • Vegetation and fauna
  • Ground viewpoint
  • Subjective aspects

Geological Agents and Relief Modeling

Geological agents, such as rivers, play a crucial role in modeling relief:

  • Rivers: Modeling river waters originates wild streams, U-shaped karst waters.
  • Coastal wind: Wind modeling.

Climate is a significant factor influencing the type of landscape.

Geologic agents include weather, vegetation, wildlife, and human activities.

The atmosphere influences weather phenomena, climate temperature, and rainfall. Air tends to flow from anticyclones towards depressions, causing wind.

Weathering Processes

Weathering... Continue reading "Landforms and Geological Agents: Shaping Our Environment" »

Environmental and Weather Terms Defined

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Environmental Terms Defined

Environment

It's the natural world that surrounds us.

Drought

It's the lack of water and it's related to environmental problems.

Supply

It's the place where I obtain certain resources.

Population

People that live in a determinate place.

Dams

Constructions that are prepared to contain water.

Recycling

It is the process by which you use old material to create a new product.

Environmental Problems

Pollution

It's when the air, water, or earth are damaged or spoiled by gases, toxic waste, or garbage.

Famine

When there is a lack of water.

Species Becomes Extinct

The species disappear completely.

Deforestation

When trees are cut down massively.

The Greenhouse Effect

The gradual warming of the Earth's surface caused by an increase in pollution... Continue reading "Environmental and Weather Terms Defined" »

Understanding Igneous, Metamorphic, and Sedimentary Rocks

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Igneous Rock

Igneous rocks are formed by the cooling of magma that reaches the crust. They are rocks created by the solidification of molten magma from the mantle.

Types of Igneous Rocks

  • Extrusive: Formed by eruptions when magma rises quickly from the mantle.
  • Intrusive: Formed when the magma in the mantle does not reach the surface.

Metamorphic Rock

Metamorphic rocks originate from the transformation of other types of rocks under high temperature and great pressure.

Formation

Metamorphic rocks form inside the Earth's surface.

Sedimentary Rocks

Sedimentary rocks form when sediments are pressed and cemented together.

Processes of Sedimentary Rock Formation

  • Sedimentation: Layers of sediments are deposited over millions of years.
  • Compaction: The weight on top
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Materials: History, Types, and Properties

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Materials: A Historical Perspective

Material is anything used to create something, any conglomeration of matter and mass. The history of civilization is linked to the history of materials.

The Stone Age

The Stone Age is the prehistoric period in which humans created tools from natural materials like stone, leather, and wood.

The Bronze Age

The Bronze Age marks the period when humans developed and created the first metal tools.

The Iron Age

The Iron Age represents a significant leap forward, with humans creating more advanced tools and weapons like spears and knives.

The Industrial Revolution

The Industrial Revolution, spanning the 19th and 20th centuries, was driven by discoveries such as plastics, silicon derivatives, computers, and textile fibers.... Continue reading "Materials: History, Types, and Properties" »

Lithosphere Dynamics, Plate Tectonics, and Seismic Activity

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Lithosphere Dynamics: Creation and Destruction

Oceanic vs. Continental Lithosphere

In the oceanic lithosphere, processes involving creation at divergent boundaries and destruction at convergent boundaries (subduction zones) generally balance each other. In contrast, the continental lithosphere is typically older because its creation rate is faster than its destruction rate, and growth primarily occurs at divergent boundaries.

Consequences of Plate Tectonics

Climate and Living Things

The movement of tectonic plates varies the arrangement of continents and oceans. This variation determines local climates and the distribution of different climatic zones across the planet, significantly impacting living organisms.

Geological Processes

The movement of... Continue reading "Lithosphere Dynamics, Plate Tectonics, and Seismic Activity" »

Topographic Maps, Erosion, and Landforms: Key Concepts

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Elements of a Topographic Map

  • Contours: These are the lines connecting points at the same altitude.
  • Dimension: Sea level is the reference altitude.
  • Equidistance: The difference in elevation between each contour line and the next.
  • Scale: The relationship between the real size and the represented size.
  • Orientation: An indication of the direction in which North lies.

Factors Influencing Water Erosion

  • Climate
  • The type of materials
  • The slope
  • Vegetation

Torrent

A stream with a fixed channel, short length, steep slopes, and irregular flow.

  • Receiving area
  • Drainage channel
  • The alluvial fan

River Erosion

  • Flow: A river erodes more when its flow is greater.
  • The speed of the water: The more slope, the more erosion.

Transportation of Materials

  • In solution
  • In solid form: rolling,
... Continue reading "Topographic Maps, Erosion, and Landforms: Key Concepts" »