It is called a syncline.
A syncline is a downward curving fold in a rock formation, where the strata dip toward the center of the structure. An anticline is an upwardly curving fold, with the strata rise upward toward the center of the structure.
A FOLD has a strata on both limbs dipping inward toward the axis.
Strata can be found in sedimentary rocks, which form in layers over time as sediments accumulate and compact. Igneous rocks, which form from molten magma cooling and solidifying, do not typically have distinct layers or strata.
syncline, forming a structure known as a paired fold. This structure represents the opposite curvature to the anticline and can be found in fold-thrust mountain belts. The shared limb often marks a hinge point, where the folding of the rock strata changes direction.
A downward fold in a rock is called a syncline. It is a type of fold in which the rock layers are bent downward in a trough-like shape.
a trough or fold of stratified rock in which the strata slope upward from the axis.
A syncline is a downward curving fold in a rock formation, where the strata dip toward the center of the structure. An anticline is an upwardly curving fold, with the strata rise upward toward the center of the structure.
A syncline is a downward curving fold in a rock formation, where the strata dip toward the center of the structure. An anticline is an upwardly curving fold, with the strata rise upward toward the center of the structure.
As the Eurasian plate and the African plate converged, the two plates collided. The rock strata along the boundary was compressed, resulting in the rock strata to fold and buckle. Over time, these folded rock strata formed a fold mountain range known as the Atlas Mountains.
A syncline fold has strata on both limbs dipping inward toward the axis. This type of fold is characterized by a trough-like structure where the youngest layers are located in the center. It is the opposite of an anticline fold.
A FOLD has a strata on both limbs dipping inward toward the axis.
Strata can be found in sedimentary rocks, which form in layers over time as sediments accumulate and compact. Igneous rocks, which form from molten magma cooling and solidifying, do not typically have distinct layers or strata.
Strata is base where foundation is to laid' and depends weather it is soft soil, hard rock strata
Strata
strata
strata
The law that suggests that older rock strata are at the bottom and younger rock strata are at the top is the law of superposition. This principle states that in an undisturbed sequence of sedimentary rocks, the oldest rocks will be at the bottom and the youngest at the top due to the natural layering process over time.