Its the Monocliens and Synclines
Folds which maintain uniform layer thickness are classed as concentric folds; those which do not are called similar folds. Similar folds tend to display thinning of the limbs and thickening of the hinge zone. Concentric folds are caused by warping which results from deformation of the layers, whereas similar folds usually form by some form of dislocation between the layers (sliding), with extension and contraction of the thickness of rock layers differently in the limb and hinge zones. -118 Team!
A syncline is a downward fold in rock layers where the youngest rocks are in the center and the oldest rocks are towards the edges. It forms a U shape, with the limbs of the fold dipping towards the center.
The two sides of a fold are called the limbs. The limb above the fold is referred to as the anticline limb, while the limb below the fold is known as the syncline limb.
A FOLD has a strata on both limbs dipping inward toward the axis.
you don't need a press to change the draw weight. there are hex key (allen wrench) bolts at the end of the riser where the limbs meet the riser. tighten them in equal increments or just go as tight as they both would go. (max draw weight) fyi. they both need to be the same. otherwise it can throw off the timing of the limbs. making it not as accurate.
folds that have parallel limbs are called isoclinal folds , in this case limbs dip at the same angle and direcrion.
A synclinal fold.
They can be called limbs, appendages, extremities, or members.
A fold where both ends of the rock layer are horizontal is known as a "recumbent fold." In this type of fold, the rock layers are bent over so that the axial plane is nearly horizontal, causing the limbs of the fold to lie parallel to the ground. Recumbent folds typically form under intense compressional forces, often associated with mountain-building events. They can indicate significant geological stress and deformation in the Earth's crust.
these are called flippers, I think
Symmetrical folds are formed when two tectonic forces compress rock layers from opposite sides, causing the layers to buckle and fold upwards in a wave-like pattern. This type of folding typically occurs in regions experiencing horizontal compressive stress, such as at convergent plate boundaries. The resulting structure features two limbs that dip away from the central axis, creating a symmetrical appearance. These folds are often indicative of significant geological processes and can be observed in mountain ranges.
fins
Folds which maintain uniform layer thickness are classed as concentric folds; those which do not are called similar folds. Similar folds tend to display thinning of the limbs and thickening of the hinge zone. Concentric folds are caused by warping which results from deformation of the layers, whereas similar folds usually form by some form of dislocation between the layers (sliding), with extension and contraction of the thickness of rock layers differently in the limb and hinge zones. -118 Team!
Lizards are sometimes called "sprawlers" because of the way they hold their limbs. In a neutral position, a lizard will hold its propodium (upper limb) pretty much horizontal and at a right angle with its spine. This places its feet far apart in a "sprawling" manner.
parapalegia
Arms, or limbs.
Like all animals, the limbs of a dragon could be legs, arms, and/or wings, depending on their function. Tails do not count as limbs in most cases.