Geological Regions: Siliceous, Limestone, and Shale

Siliceous terrain comprises ancient rocks from the Precambrian and Primary eras. It is mostly in the western peninsula (Galicia, León, Extremadura) and has ramifications to the western part of the Cantabrian mountain range, the CS, Montes de Toledo, and Sierra Morena. It is also located in isolated areas such as the axial zone and some sectors of the Pyrenees, Iberian system, coastal mountain range, and the Catalan-Penibético system. The prevailing rock is granite, and the landscape is determined

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Types of Sedimentary Deposits and Soil Genesis

Types of Sedimentary Deposits

Lacustrine deposits: These occur when earth is moved or transported by rivers and streams and deposited on lake bottoms.

Proluvial deposits: These are materials occupying the bed of dry streams.

Fluvial deposits: These are formed by sediments that accumulate from the activity of rivers and the processes associated with gravity sliding.

Wind deposits: These are formed through the accumulation of transported material, forming dunes and sand dune materials.

EOI: A special material

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Geological Eras and Landforms of the Iberian Peninsula

Geological Eras of the Iberian Peninsula

Paleozoic Era: Began 570 million years ago and lasted until 230 million years ago. During this era, two plates, or continents, were separated by the Sea of Tethys. Two orogenies occurred: the older Caledonian, which barely affected peninsular space, and the Hercynian, which developed during the Carboniferous period. As a consequence, a great mountain range arose in a NW-SE direction, becoming a massif called the Hesperian Massif, which occupies much of central

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Ibn Tulun Mosque: A Masterpiece of Islamic Architecture in Cairo

The Grand Mosque of Ibn Tulun

From his palace, al-Katai, Ibn Tulun governed with authority. His time in Samarra, where he grew up, is remembered for its giant brick mosques, built in the Iraqi tradition. He decided to build a similar prayer structure in Fostat (near the future city of Cairo), of monumental proportions. Unlike the Nile Valley, where stone was widely used since the Pharaohs for temples and tombs, Ibn Tulun used brick and stucco cladding, a technique common in Mesopotamia. The construction

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Earth’s Atmosphere: Layers, Phenomena, and Pollution

Earth’s Atmosphere: Layers and Composition

Troposphere

The troposphere is the layer that is in contact with the soil. Here, the temperature drops to -55ºC. This layer contains approximately 90% of the atmosphere’s upper interface.

Stratosphere

The stratosphere has a thickness of 30 km. At the top, ultraviolet rays of the sun collide with oxygen molecules (O2). The reaction releases heat, so the top is about -17ºC. In addition, the stratosphere is a region rich in ozone, the ozonosphere.

Mesosphere

The

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Renewable Energy, Material Properties, and Sustainable Development

Nuclear Transfer: Generating New Individuals

The following scheme observes nuclear transfer, a process where a new individual is generated using a somatic cell and an egg.

Renewable Energy Sources

Which are the sources of renewable energy?

  • Solar: Energy that reaches Earth as electromagnetic radiation from the sun.
  • Wind: Energy obtained from the wind, harnessing its kinetic energy.
  • Tidal: Energy derived from the movement of marine tides.
  • Geothermal: Energy that utilizes the internal heat of the Earth.
  • Biomass:
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