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  2. Geology of Florida - Wikipedia

    en.wikipedia.org/wiki/Geology_of_Florida

    Florida is tied with North Dakota as having the fewest earthquakes of any US state. [7] Because Florida is not located near any tectonic plate boundaries, earthquakes are very rare, but not totally unknown. In January 1879, a shock occurred near St. Augustine. There were reports of heavy shaking that knocked plaster from walls and articles from ...

  3. File:Map of Tectonic Summary (Carribean).pdf - Wikipedia

    en.wikipedia.org/wiki/File:Map_of_Tectonic...

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  4. Geomorphology - Wikipedia

    en.wikipedia.org/wiki/Geomorphology

    The effects of tectonics on landscape are heavily dependent on the nature of the underlying bedrock fabric that more or less controls what kind of local morphology tectonics can shape. Earthquakes can, in terms of minutes, submerge large areas of land forming new wetlands.

  5. File:Interactions and feedback pathways for tectonics and ...

    en.wikipedia.org/wiki/File:Interactions_and...

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  6. Environment of Florida - Wikipedia

    en.wikipedia.org/wiki/Environment_of_Florida

    The environment of Florida in the United States yields an array of land and marine life in a mild subtropical climate. This environment has drawn millions of people to settle in the once rural state over the last hundred years. Florida's population increases by about 1,000 residents each day. [1]

  7. Tectonophysics - Wikipedia

    en.wikipedia.org/wiki/Tectonophysics

    Tectonophysics is concerned with movements in the Earth's crust and deformations over scales from meters to thousands of kilometers. [2] These govern processes on local and regional scales and at structural boundaries, such as the destruction of continental crust (e.g. gravitational instability) and oceanic crust (e.g. subduction), convection in the Earth's mantle (availability of melts), the ...

  8. Geology of the United States - Wikipedia

    en.wikipedia.org/wiki/Geology_of_the_United_States

    The richly textured landscape of the United States is a product of the dueling forces of plate tectonics, weathering and erosion. Over the 4.5 billion-year history of the Earth, tectonic upheavals and colliding plates have raised great mountain ranges while the forces of erosion and weathering worked to tear them down.

  9. Erosion and tectonics - Wikipedia

    en.wikipedia.org/wiki/Erosion_and_tectonics

    Understanding the principle of isostasy is a key element to understanding the interactions and feedbacks shared between erosion and tectonics. The principle of isostasy states that when free to move vertically, lithosphere floats at an appropriate level in the asthenosphere so that the pressure at a depth of compensation in the asthenosphere well below the base of the lithosphere is the same. [3]