Unit 4: Basics of Geological Field Work

Table of Contents


Uses of Field Tools

Geological field work is the foundation of geology. It requires a specific set of tools for observation, measurement, and collection.

Basic Geological Field Tools
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.

Clinometer

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.


Brunton Compass

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:

  1. Magnetic Compass: For navigation. The needle points to magnetic north, allowing you to orient your map and find your bearing.
  2. Sighting Compass: Using the sights and mirror, you can measure the precise horizontal bearing (azimuth) from you to a distant object. This is used for mapping and traversing.
  3. Clinometer: It has a built-in clinometer (a "bubble level" attached to a rotating scale) used to measure vertical angles, most importantly, the dip angle of a rock layer.
Primary Use: The Brunton Compass is the standard instrument used to measure Dip and Strike.

Planning Traverse

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.

Principles of Traverse Planning:


Locating Outcrops

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.

Where to Find Outcrops:

Locating on a Map:

When you find an outcrop, you must record its location accurately:


Concept of Bed, Dip, and Strike

These are the fundamental measurements used to describe the orientation of planar structures (like sedimentary beds, faults, or metamorphic foliation) in 3D space.

Bed

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

Strike: The compass direction (bearing) of a horizontal line on the surface of an inclined plane (the bed).

Dip

Dip: The maximum angle of inclination of the bed, measured perpendicular to the strike.

Dip has two parts:

  1. Dip Angle: The angle (from 0° to 90°) between the bedding plane and a horizontal plane.
    • A horizontal bed has 0° dip.
    • A vertical bed has 90° dip.
    • This is measured using the clinometer.
  2. Dip Direction: The compass direction *towards which* the bed is sloping (the "downhill" direction). This direction is always 90° (perpendicular) to the strike direction.
Recording Dip and Strike: A full measurement combines both and is written in a specific format.
Example: Strike N45°E, Dip 30° SE
This means the horizontal line runs NE-SW, and the bed is sloping downwards at 30° towards the Southeast.