一个节理岩石被证明是由较高的渗透性组成的，而在不连续性的平面上的剪切应力的减少明显地增加了，描述了可忽略的抗拉强度。岩体在度方向上的断裂程度，并为控制提供方向上的关节数目提供了依据。因此，相邻点之间的间距对于增强单个块的大小至关重要，而对模式失败的控制可以很容易地描述。
它似乎对岩体的渗透性有影响，而且边坡的均匀流动破坏也很容易显现。不连续性的持续性定义在一起表示可以从坡面上滑动的块的间距和大小。完整岩石的小面积被认为是位于低持续间断点之间，岩石的强度可以很容易地描述为高得多的剪切应力，似乎是在作用于斜坡上。结合结构的粗糙度，可以看出其表面的不均匀性和表面的波纹度。该结构简单地说明了由两部分组成的粗糙表面，这两部分是岩石材料摩擦的组成部分，以及由在表面上进行的识别所产生的联锁。这些仅仅是增强了固有的不均匀性和影响表面波纹的不规则性，从而增强了对地理不连续的描述。
A jointed rock is shown to be consisting of higher permeability and the reduction in the shear stress along the planes of the discontinuity is clearly increased with depicting the negligible tensile strength. The degree of the fracturing of the rock mass in the direction of the degree and is being provided for the purpose of controlling the number of the joints at the provided direction. Thereby, the spacing between the adjacent points are very much crucial for the enhancement of the size of the individual blocks, and the controlling of the mode failure can be easily depicted
It seems to be influencing the permeability of the rock mass and the even flow failure of the slope can be easily shown. The persistence of the discontinuity is defined to be in together representing the spacing and the size of the blocks that can slide from the face of the slope. The small area of the intact rock is indicated to be lying between the low persistent discontinuities, and the strength of the rock can be easily depicted to be much higher that the shear stress that seems to be acting on the slope. The roughness of the joint structure is indicated to be measuring the inherent unevenness and the waviness of the surface of the discontinuity. The structure simply illustrates the rough surface that comprises of the two components which are the components of the friction of the rock material and the interlocking that is being produced by the help of the identification made on the surfaces. These simply enable the enhancement of the inherent unevenness and the irregularities that affect the waviness on the surface and it enables the enhancement of the description regarding the geographical discontinuities.