2. FOLD, FAULT, AND JOINT GROUP 5

3. FOLD FOLDS ARE WAVE-LIKE IN SHAPE AND VARY ENORMOUSLY IN SIZE. THE TERM FOLD IS USED IN GEOLOGY WHEN ONE OR A STACK OF ORIGINALLY FLAT, LEVEL SURFACES, SUCH AS SEDIMENTARY STRATA, ARE BENT OR CURVED AS A RESULT OF PRESSURE AND HIGH TEMPERATURE. THE BASIC CAUSE IS LIKELY TO BE SOME ASPECT OF PLATE TECTONICS.

4. TYPES OF FOLD Anticline- is a fold that is convex up and has its oldest beds at its core. The term is not to be confused with antiform, which is a purely descriptive term for any fold that is convex up. Therefore if age relationships between various strata are unknown, the term antiform should be used.

5. SYNCLINE -IS A FOLD WITH YOUNGER LAYERS CLOSER TO THE CENTER OF THE STRUCTURE. SYNCLINES ARE TYPICALLY A DOWNWARD FOLD, TERMED A SYNFORMAL SYNCLINE (I.E. A TROUGH); BUT SYNCLINES THAT POINT UPWARDS, OR PERCHED, CAN BE FOUND WHEN STRATA HAVE BEEN OVERTURNED AND FOLDED (AN ANTIFORMAL SYNCLINE).

6. MONOCLINE- LOCAL WARPING IN HORIZONTAL STRATA. ROCK BEDS LYING AT TWO LEVEL SEPARATED BY STEEP INCLINED LIMBS. IT IS FORM BY VERTICAL MOVEMENT AND GENERALLY FOUND FAULT BELOW MONOCLINE. A STEP-LIKE FOLD IN ROCK STRATA CONSISTING OF A ZONE OF STEEPER DIP WITHIN AN OTHERWISE HORIZONTAL OR GENTLY-DIPPING SEQUENCE.

7. CHEVRON- FOLDS ARE A STRUCTURAL FEATURE CHARACTERIZED BY REPEATED WELL BEHAVED FOLDED BEDS WITH STRAIGHT LIMBS AND SHARP HINGES. WELL DEVELOPED, THESE FOLDS DEVELOP REPEATED SET OF V- SHAPED BEDS. THEY DEVELOP IN RESPONSE TO REGIONAL OR LOCAL COMPRESSIVE STRESS. INTER-LIMB ANGLES ARE GENERALLY 60 DEGREES OR LESS. CHEVRON FOLDING PREFERENTIALLY OCCURS WHEN THE BEDDING REGULARLY ALTERNATES BETWEEN CONTRASTING COMPETENCES.

8. RECUMBENT- FOLD HAS AN ESSENTIALLY HORIZONTAL AXIAL PLANE. LINEAR, FOLD AXIAL PLANE ORIENTED AT LOW ANGLE RESULTING IN OVERTURNED STRATA IN ONE LIMB OF THE FOLD.

9. ISOCLINAL- FOLDS ARE SIMILAR TO SYMMETRICAL FOLDS, BUT THESE FOLDS BOTH HAVE THE SAME ANGLE AND ARE PARALLEL TO EACH OTHER. 'ISO' MEANS 'THE SAME' (SYMMETRICAL), AND 'CLINE' MEANS 'ANGLE,' SO THIS NAME LITERALLY MEANS 'SAME ANGLE.' SO ISOCLINAL FOLDS ARE BOTH SYMMETRICAL AND ALIGNED IN A PARALLEL FASHION.

10. PLUNGING-A FOLD WHOSE AXIS PLANE IS NOT HORIZONTAL (NOT PARALLEL TO SEA LEVEL). DIRECTION OF PLUNGE - THE DIRECTION IN WHICH THE AXIS IS INCLINED NOSE - INDICATE THE DIRECTION OF PLUNGE. IN ANTICLINE, PLUNGE IS DIRECTED TOWARDS NOSE AND IN SYNCLINE IT IS DIRECTED AWAY FROM NOSE.

11. DOME AND BASIN- WE ALSO HAVE DOMES, WHICH ARE LIKE ANTICLINES BUT INSTEAD OF AN ARCH, THE FOLD IS IN A DOME SHAPE, LIKE AN INVERTED BOWL. SIMILARLY, THERE ARE ALSO BASINS, WHICH ARE LIKE SYNCLINES BUT AGAIN, INSTEAD OF A SINKING ARCH, THE FOLD IS IN A SHAPE OF A BOWL SINKING DOWN INTO THE GROUND. DOME: NONLINEAR, STRATA DIP AWAY FROM CENTER IN ALL DIRECTIONS, OLDEST STRATA IN CENTER. BASIN: NONLINEAR, STRATA DIP TOWARD CENTER IN ALL DIRECTIONS, YOUNGEST STRATA IN CENTER.

12. PTYGMATIC -FOLDS ARE CHAOTIC, RANDOM AND DISCONNECTED. TYPICAL OF SEDIMENTARY SLUMP FOLDING, MIGMATITES AND DECOLLEMENT DETACHMENT ZONES. PTYGMATIC FOLDS GENERALLY REPRESENT CONDITIONS WHERE THE FOLDED MATERIAL IS OF A MUCH GREATER VISCOSITY THAN THE SURROUNDING MEDIUM.

13. FAULT FAULT IS A PLANAR FRACTURE OR DISCONTINUITY IN A VOLUME OF ROCK, ACROSS WHICH THERE HAS BEEN SIGNIFICANT DISPLACEMENT AS A RESULT OF ROCK MASS MOVEMENT. LARGE FAULTS WITHIN THE EARTH'S CRUST RESULT FROM THE ACTION OF PLATE TECTONIC FORCES, WITH THE LARGEST FORMING THE BOUNDARIES BETWEEN THE PLATES. ENERGY RELEASE ASSOCIATED WITH RAPID MOVEMENT ON ACTIVE FAULTS IS THE CAUSE OF MOST EARTHQUAKES.CRUSTPLATE TECTONICACTIVE FAULTSEARTHQUAKES

14. TYPES OF FAULT STRIKE-SLIP, WHERE THE OFFSET IS PREDOMINATELY HORIZONTAL, PARALLEL TO THE FAULT TRACE.

15. DIP-SLIP, OFFSET IS PREDOMINATELY VERTICAL AND/OR PERPENDICULAR TO THE FAULT TRACE.

16. OBLIQUE-SLIP, COMBINING SIGNIFICANT STRIKE AND DIP SLIPSTRIKE AND DIP

17. JOINT JOINT IS A FRACTURE DIVIDING ROCK INTO TWO SECTIONS THAT HAVE NOT MOVED AWAY FROM EACH OTHER. A JOINT SEES LITTLE OR NO DISPLACEMENT. IN OTHER KINDS OF FRACTURING, LIKE IN A FAULT, THE ROCK IS PARTED BY A VISIBLE CRACK THAT FORMS A GAP IN THE ROCK.

18. NONSYSTEMATIC JOINTS -ARE JOINTS THAT ARE SO IRREGULAR IN FORM, SPACING, AND ORIENTATION THAT THEY CANNOT BE READILY GROUPED INTO DISTINCTIVE, THROUGH- GOING JOINT SETS

19. SYSTEMATIC JOINTS ARE PLANAR, PARALLEL, JOINTS THAT CAN BE TRACED FOR SOME DISTANCE, AND OCCUR AT REGULARLY, EVENLY SPACED DISTANCES ON THE ORDER CENTIMETERS, METERS, TENS OF METERS, OR EVEN HUNDREDS OF METERS. AS A RESULT, THEY OCCUR AS FAMILIES OF JOINTS THAT FORM RECOGNIZABLE JOINT SETS.

20. TYPES OF SYSTEMATIC JOINT: LONGITUDINAL JOINTS – JOINTS WHICH ARE ROUGHLY PARALLEL TO FOLD AXES AND OFTEN FAN AROUND THE FOLD. CROSS-JOINTS – JOINTS WHICH ARE APPROXIMATELY PERPENDICULAR TO FOLD AXES. DIAGONAL JOINTS – JOINTS WHICH TYPICALLY OCCUR AS CONJUGATE JOINT SETS THAT TREND OBLIQUE TO THE FOLD AXES. STRIKE JOINTS – JOINTS WHICH TREND PARALLEL TO THE STRIKE OF THE AXIAL PLANE OF A FOLD. CROSS-STRIKE JOINTS – JOINTS WHICH CUT ACROSS THE AXIAL PLANE OF A FOLD.