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  2. Joint (geology) - Wikipedia

    en.wikipedia.org/wiki/Joint_(geology)

    Systematic joints are planar, parallel, joints that can be traced for some distance, and occur at regularly, evenly spaced distances on the order of centimeters, meters, tens of meters, or even hundreds of meters. As a result, they occur as families of joints that form recognizable joint sets.

  3. Fracture (geology) - Wikipedia

    en.wikipedia.org/wiki/Fracture_(geology)

    Conjugate Joints occur when the joints intersect each other at angles significantly less than ninety degrees. Systematic Joints are joint systems in which all the joints are parallel or subparallel, and maintain roughly the same spacing from each other. Columnar Joints are joints that cut the formation vertically in (typically) hexagonal ...

  4. Columnar jointing - Wikipedia

    en.wikipedia.org/wiki/Columnar_jointing

    Columnar jointing is a geological structure where sets of intersecting closely spaced fractures, referred to as joints, result in the formation of a regular array of polygonal prisms (basalt prisms), or columns. Columnar jointing occurs in many types of igneous rocks and forms as the rock cools and contracts.

  5. Discontinuity (geotechnical engineering) - Wikipedia

    en.wikipedia.org/wiki/Discontinuity...

    In geotechnical engineering, a discontinuity (often referred to as a joint) is a plane or surface that marks a change in physical or chemical characteristics in a soil or rock mass. A discontinuity can be, for example, a bedding , schistosity , foliation , joint , cleavage , fracture , fissure , crack, or fault plane.

  6. Tessellated pavement - Wikipedia

    en.wikipedia.org/wiki/Tessellated_pavement

    In geology and geomorphology, a tessellated pavement is a relatively flat rock surface that is subdivided into polygons by fractures, frequently systematic joints, within the rock. This type of rock pavement bears this name because it is fractured into polygonal blocks that resemble tiles of a mosaic floor, or tessellations. [1]

  7. Tension (geology) - Wikipedia

    en.wikipedia.org/wiki/Tension_(geology)

    Tensile stress forms joints in rocks. A joint is a fracture that forms within a rock, whose movement to open the fracture is greater than the lateral movement that takes place. Joints are formed in the direction perpendicular to the least principal stress, meaning that they are formed perpendicular to the tensile stress. [ 1 ]

  8. How (And Why) To Tuck Turkey Wings - AOL

    www.aol.com/why-tuck-turkey-wings-185747104.html

    Step 2. Locate and tuck the wings: Locate the joint where each wing meets the body of the turkey by gently lifting the wings. Now imagine you're laying back on the grass with your arms tucked ...

  9. Structural geology - Wikipedia

    en.wikipedia.org/wiki/Structural_geology

    Structural geology is the study of the three-dimensional distribution of rock units with respect to their deformational histories. The primary goal of structural geology is to use measurements of present-day rock geometries to uncover information about the history of deformation ( strain ) in the rocks, and ultimately, to understand the stress ...