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Where is Weathered Sandstone found?

Sandstone (with biological growth)

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Weathered Sandstone 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 Weathered Sandstone

Colorado Plateau, USA

Extensive sandstone formations (e.g., Navajo Sandstone, Entrada Sandstone) exhibit significant weathering and biological colonization, particularly by desert varnish and cryptobiotic crusts.

Australian Deserts

Sandstone outcrops and inselbergs (e.g., Uluru) show pronounced weathering features and diverse biological growth, including lichens and cyanobacterial mats.

Mediterranean Basin

Ancient sandstone structures and natural outcrops often display extensive biological colonization due to humid climates and long exposure times.

Tropical Rainforests

Sandstone in humid tropical regions can be heavily weathered and covered by dense biological growth, including mosses, ferns, and biofilms.

Collecting tips

  1. Look for surface discoloration and textures. Identify areas where the sandstone's original color is obscured by green, black, orange, or grey patches, indicating biological growth. Feel for friable or powdery surfaces, or crusty/velvety textures from organisms.
  2. Examine exposed outcrops. Weathering and biological growth are most pronounced on surfaces directly exposed to rain, wind, sunlight, and temperature changes. Look at cliffs, boulders, and rock faces.
  3. Consider the environment. Humid environments, areas with frequent wetting and drying cycles, and regions with significant temperature fluctuations are conducive to both weathering and biological colonization.
  4. Observe micro-features. Look for signs of bio-erosion, such as pitting or etching, and the presence of distinct biological structures like lichen thalli, moss cushions, or algal films.

Quick Check

Color:
Variable, often stained or covered by biological growth (green, black, orange, grey).
Luster:
Dull to earthy.
Streak:
Typically white or the color of the dominant cementing agent (e.g., reddish-brown for iron oxides), but often difficult to obtain due to friability and biological coating.

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