Geological field work is the foundation of geology. It requires a specific set of tools for observation, measurement, and collection.
| Tool | Primary Use(s) | 
|---|---|
| Geological Hammer | To break rocks for a fresh (unweathered) surface and to collect samples. (Pick end for hard rocks, chisel end for sedimentary rocks). | 
| Hand Lens (Loupe) | (Usually 10x magnification). To magnify rock grains to identify minerals, texture, and small fossils. | 
| Field Notebook & Pen/Pencil | To record all observations: locations, measurements (dip/strike), rock descriptions, sketches. | 
| Compass (Brunton/Clinometer) | For navigation and for measuring the orientation of geological structures (dip and strike). | 
| Map & GPS | Topographic map for navigation and plotting data. GPS for recording precise (X, Y) coordinates of outcrops. | 
| Acid Bottle (Dilute HCl) | To test for carbonate minerals. Calcite (limestone) will fizz vigorously. | 
| Sample Bags & Marker | To collect and label rock samples with location, date, and rock type. | 
A Clinometer is an instrument used to measure vertical angles. This includes:
It works using a simple pendulum or a weighted rotating wheel. When you align the instrument's sight with the slope, the pendulum hangs vertically (due to gravity), and the angle between the sight and the pendulum can be read. In most geological compasses, this function is built-in.
The Brunton Compass is the most essential and versatile tool for a geologist. It is a high-precision magnetic compass that combines three instruments in one:
Traverse: A traverse is a pre-planned route or path that a geologist walks to make observations and create a geological map.
Why Plan? You cannot just wander randomly. A planned traverse ensures you cover the area systematically and efficiently.
Outcrop (or "crop"): An exposure of bedrock at the Earth's surface. It is a place where the rock is not covered by soil, vegetation, water, or man-made structures.
Outcrops are the "data points" for a geologist. The rest of the geology is inferred (guessed) by connecting the data from outcrops.
When you find an outcrop, you must record its location accurately:
These are the fundamental measurements used to describe the orientation of planar structures (like sedimentary beds, faults, or metamorphic foliation) in 3D space.
A "bed" is a single, distinct layer of rock. In sedimentary rocks, this is a layer of sand, mud, or limestone deposited at one time. We measure the orientation of the bedding planes (the top and bottom surfaces of the bed).
Strike: The compass direction (bearing) of a horizontal line on the surface of an inclined plane (the bed).
Dip: The maximum angle of inclination of the bed, measured perpendicular to the strike.
Dip has two parts: