How to identify River Pebbles
Sedimentary/Metamorphic/Igneous Rock Fragments
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Open the appTo correctly identify River Pebbles (Sedimentary/Metamorphic/Igneous Rock Fragments), check each of these features in order. Many rocks and minerals look alike, so cross-reference multiple properties before deciding.
Step-by-step identification
- 1
Color
Overall color and any zoning or banding
Extremely variable, depending on the constituent rock types. Can be white, black, grey, brown, red, green, or multicolored.
- 2
Luster
How the surface reflects light: metallic, vitreous, dull
Variable, typically dull to vitreous, depending on the lithology. Quartz pebbles may have a vitreous luster, while basalt pebbles might be dull.
- 3
Texture
Grain size and surface feel: coarse, fine, glassy
Smooth to slightly rough, often polished due to abrasion. The surface may show percussion marks or minor pitting.
- 4
Crystal Form
Shape of visible crystals or crystal faces
Not applicable to the aggregate as a whole. Individual clasts may exhibit relict crystal forms if they are crystalline rocks (e.g., granite, basalt).
- 5
Cleavage
How it breaks: flat cleavage planes vs irregular fracture
Not applicable to the aggregate. Individual clasts may exhibit cleavage if they are composed of minerals with good cleavage (e.g., feldspar in granite, calcite in limestone).
- 6
Geological Environment
The rock formation and setting where it occurs
Fluvial environments, including riverbeds, riverbanks, floodplains, and alluvial fans. Also found in ancient fluvial deposits that have been lithified into conglomerates.
Key Facts
- Hardness
- Variable, depending on the constituent lithologies (e.g., quartz ~7, limestone ~3).
- Specific Gravity
- Variable, typically ranging from 2.5 to 3.0 g/cm³ depending on the dominant lithologies.
- Crystal System
- Not applicable to the aggregate; individual clasts may be crystalline or amorphous.
- Color
- Highly variable, reflecting the diverse source rocks.
- Luster
- Variable, from dull to vitreous.
- Transparency
- Variable, from opaque to translucent (e.g., quartz pebbles).
- Fracture
- Variable, depending on the lithology (e.g., conchoidal for quartz, irregular for many others).
- Cleavage
- Not applicable to the aggregate; individual clasts may or may not exhibit cleavage.
- Composition
- Mixed, consisting of fragments of various igneous, metamorphic, and sedimentary rocks and minerals (e.g., quartz, feldspar, mica, calcite, rock fragments).
Physical characteristics
- Crystal Habit: Not applicable to the aggregate; individual clasts retain the habit of their source rock/mineral.
- Cleavage Type: Not applicable to the aggregate; depends on individual clasts.
- Fracture Type: Variable, depending on the lithology of individual clasts.
- Tenacity: Variable, depending on the lithology of individual clasts.
- Luster Type: Variable, from dull to vitreous, depending on the lithology.
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