Glossary
Definitions from the Soil Science Society of America (SSSA)
A B C D E F G H I J K L M N O P Q R S T U V W X Y Z
| Back slope | The steepest inclined surface and principle element of many hillslopes Back slopes in the profile typically range from gently sloping to very steep and linear and descend to a foot slope. They are erosional forms produced mainly by mass wasting and running water. |
| Base saturation | The degree to which material having cation-exchange properties is saturated with exchangeable bases (sum of Ca, Mg, Na, K), expressed as a percentage of the total cation-exchange capacity. |
| Bedding planes | Fine stratifications, less than 5 millimeters thick, in unconsolidated alluvial, eolian, lacustrine, or marine sediments. |
| Bedrock | The solid rock that underlies the soil and other unconsolidated material or that is exposed at the surface. |
| Bench terrace | A raised, level or nearly level strip of earth constructed on or nearly on the contour, supported by a barrier of rocks or similar material, and designed to make the soil suitable for tillage and to prevent accelerated erosion. |
| Blowout | A shallow depression from which all or most of the soil material has been removed by wind A blowout has a flat or irregular floor formed by a resistant layer or by an accumulation of pebbles or cobbles. In some blowouts the water table is exposed. |
| Bottom land | The normal flood plain of a stream, subject to flooding. |
| Boulders | Rock fragments larger than 2 feet (60 centimeters) in diameter. |
| Broad-base terrace | A ridge-type terrace built to control erosion by diverting runoff along the contour at a nonscouring velocity. The terrace is 10 to 20 inches high and 15 to 30 feet wide and has gently sloping sides, a rounded crown, and a dish-shaped channel along the upper side. It may be nearly level or have a grade toward one or both ends. |
