
Color- the color of sample and minerals in thin section with polarized light.
Prominence- the extent to which the feature is conspicuous within the field of view. Contrast may be due to transparency, opacity, color, relief, interference color, size, shape, or distribution pattern.
Size- it is possible to divide minerals or features into
size classes. Although the exact size is indeterminate because
of the random cut of the thin section, approximations can be
made:
Shape
Very large >10,000µm (10mm) Large 2,000-10,000µm (2-10mm) Medium 200- 2000µm Small 60- 200µm Very small 2- 60µm Micro <2µm
- this inclueds the geometric forms, crystallographic forms and a number if irregular shapes. About 43 shape forms are listed in the book (see Bullock et al for some examples).
Frequency of occurrence as determined as percentage of
area. (NOTE - FitzPatrick breaks his frequency distribution into
more divisions than may be feasible without detailed counting of
grains or features)
Distribution patterns
Abrupt <100µm Sharp 100- 500µm Clear 500-1000µm Diffuse >1000µm
of a feature or the spatial relationship between individuals. All distribution patterns are relationship patterns.
Relationship between features includes the relationship
between different features, or how does one feature relate to
another.
Banded - the features occur in alternating bands.
Clustered - Occurring in clusters - the clusters vary in closeness of the individuals and may be dense, even, uneven, or wide.
Coated - Coated with a different material.
Inclined - The feature in inclined to some other feature.
Intimate - The two or more features present are intimately associated with each other.
Normal - The feature is arranged at right angles to some other feature.
Paired - the features occur as pairs (I am not sure how this differs from intimate)
Parallel - The features are parallel to each other.
Radial - The feature is distributed radially to some other component.
Unrelated - The feature has no fixed relationship with any other feature. The relationship may be defined as haphazard.
Orientation patterns may be due to soil forming processes or they may be inherited. The orientation should be described in terms of orientation direction, orientation degree (strongly to weakly oriented), and orientation relationships.

This page
(http://www.ces.ncsu.edu/plymouth/programs/properties.html)
created by
Vera MacConnell,
Research Technician, I
on February 6, 1998.
Last Updated on February 20, 1998.