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Where is Iron-rich Sandstone with Trace Fossil found?

Sandstone (sedimentary rock) with possible Skolithos or similar trace fossil

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Iron-rich Sandstone with Trace Fossil occurs in specific geological environments. Knowing where to look, and in what kind of rock, is the difference between going home empty-handed and finding a great specimen.

Where to find Iron-rich Sandstone with Trace Fossil

Cambrian and Ordovician strata worldwide

Many Cambrian and Ordovician sandstone formations, such as the Potsdam Sandstone (North America), are renowned for abundant Skolithos trace fossils and often exhibit iron staining.

Western United States

Various Mesozoic and Cenozoic sandstone units in states like Utah, Arizona, and Colorado can be iron-rich and contain diverse trace fossil assemblages.

United Kingdom

Certain Paleozoic sandstones, particularly in Wales and Scotland, are known for their ichnofossil content and can be iron-stained.

Collecting tips

  1. Look for color variations. The iron enrichment often gives the sandstone a distinctive reddish, orange, or yellowish hue, which can be a good indicator.
  2. Examine weathered surfaces. Trace fossils are often more visible on weathered surfaces where differential erosion has highlighted their structure. Look for cylindrical or pipe-like features that cut across bedding planes.
  3. Check for bedding planes. While Skolithos are typically vertical to bedding, other trace fossils may be horizontal or oblique. Examine both bedding surfaces and cross-sections.
  4. Consider the geological context. Trace fossils are common in sedimentary rocks deposited in marine or marginal marine environments. Researching the local stratigraphy can help identify promising formations.

Quick Check

Color:
Reddish-brown, orange, yellow, purplish (due to iron oxides)
Luster:
Dull to earthy
Streak:
Reddish-brown (for hematite-rich), yellowish-brown (for goethite/limonite-rich)

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