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As discussed in previous lessons, strain energy in a material is the energy stored when it is elastically deformed, a concept crucial in materials science and mechanical engineering. This energy results from the internal work done against the cohesive forces within the material. When a material undergoes shearing stress and corresponding shearing strain, the strain energy density, which is the energy stored per unit volume, is calculated. Within the elastic limit, where the stress is...
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Related Experiment Video

Updated: Oct 12, 2025

Synchrotron X-ray Microdiffraction and Fluorescence Imaging of Mineral and Rock Samples
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Sand spikes pinpoint powerful palaeoseismicity.

Elmar Buchner1,2, Volker J Sach3,4, Martin Schmieder5,3

  • 1HNU - Neu-Ulm University of Applied Sciences, Wileystrasse 1, D-89231, Neu-Ulm, Germany. elmar.buchner@hnu.de.

Nature Communications
|November 19, 2021
PubMed
Summary

Sand spikes, enigmatic sandstone formations, are now understood to form from high-energy events like earthquakes or impacts. Their orientation reveals the direction of these powerful geological forces.

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Area of Science:

  • Geology
  • Sedimentology
  • Tectonics

Background:

  • Sand spikes are unusual sandstone formations, long interpreted as sedimentary concretions.
  • Their formation mechanism has remained a scientific mystery for nearly two centuries.

Purpose of the Study:

  • To present a novel high-energy formation mechanism for sand spikes.
  • To re-interpret sand spikes as a new type of seismite.

Main Methods:

  • Analysis of sand spike occurrences in the North Alpine Foreland Basin (Germany) and Mount Signal (USA).
  • Examination of seismite horizons and dewatering structures in Mid-Miocene Molasse sediments.
  • Stratigraphic and structural context analysis of sand spike orientation.

Main Results:

  • Sand spikes in Germany are linked to the Ries impact event, with tails oriented away from the crater.
  • Sand spikes at Mount Signal show tails pointing away from the San Andreas Fault.
  • Both occurrences exhibit characteristics of seismites, formed by seismic activity.

Conclusions:

  • Sand spikes are formed by high-energy, seismically induced processes, not typical concretionary growth.
  • Sand spikes serve as valuable indicators of past impact-induced or tectonic paleo-earthquakes.
  • Their systematic orientation provides a tool to identify the source regions of ancient seismic events.