answersLogoWhite

0

The tendency of some minerals to break along certain planes is called, "Cleavage".

User Avatar

Wiki User

10y ago

What else can I help you with?

Continue Learning about Movies & Television

What property describes how a mineral breaks?

The property is referred to as cleavage or fracture, the tendency, or lack of tendency, of a mineral to break along planes of weakness. Some minerals have multiple planes of cleavage. Some have none, and are said to exhibit fracture.Cleavage is the tendency of a mineral to break along flat surfaces. The way in which a mineral breaks depends on how its atoms are bonded, or joined together. In a mineral that displays cleavage, the bonds of the crystal structure are weaker in the directions in which the mineral breaks.fracture is the tendency of a mineral to break into irregular pieces. Some minerals such as quartz break into pieces with curved surfaces. Other minerals may break differently-perhaps into splinters or into rough or jagged pieces. In a mineral that displays fracture, the bonds that join the atoms are fairly equal in strength in all directions. The mineral does not break along flat surfaces because there are no particular directions ofweakness in its crystal structure.


Is it possible for a mineral to have a prismatic habit without having a cleavage?

Yes, a mineral can have a prismatic habit without exhibiting cleavage. Prismatic habit refers to the crystal form of a mineral that resembles elongated, prism-like shapes. Cleavage, on the other hand, is the tendency of a mineral to break along specific planes of weakness in its structure. A mineral may grow in a prismatic shape while lacking defined cleavage planes, resulting in a more conchoidal or uneven fracture instead.


What is the Definition of Rock Cleavage?

A mineral's ability to split easily along planes of weakness, producing flat surfaces.


The tendency of a mineral to split easily along a flat surface is called?

It wil break & produce fragments of d same shape as d parent material bcos it broke on a flat surface


What are color cleavage and luster are examples of when classifying minerals?

Color, cleavage, and luster are physical properties used to classify minerals. Color refers to the appearance of a mineral, which can vary widely, while luster describes how light interacts with the mineral's surface, indicating whether it is metallic, glassy, or dull. Cleavage refers to the tendency of a mineral to break along specific planes of weakness, which helps in identifying the mineral's internal structure. Together, these properties assist geologists and mineralogists in accurately identifying and categorizing different minerals.

Related Questions

He strong tendency of certain minerals to break along smooth parallel planes is known as?

The strong tendency of certain minerals to break along smooth parallel planes is known as cleavage. Cleavage occurs due to the internal atomic arrangement of the mineral, which allows it to break along specific planes of weakness.


What is mineral's cleavage?

Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.


What is the tendency of a mineral to break along planes of weakness producing smooth parallel breaks known as?

Cleavage is the tendency of a minerals to break along flat surfaces. It means that the make up of the mineral is uneven, dense on one side and not dense in the other, causing the mineral to break along flat surfaces. The tendency of a mineral to break irregurlary is fracture.


What is a minerals cleavage?

Cleavage is the tendency of a mineral to break along smooth planes parallel to zones of weak bonding.


When a mineral breaks along a weakly bonded plane?

It exhibits cleavage, which is the tendency of a mineral to break along certain planes of weakness determined by its atomic structure. Cleavage is a property seen in minerals with strong bonds in certain directions but weaker bonds in other directions. The resulting flat, shiny surfaces are a result of the breakage along these weakly bonded planes.


What is the difference between fracture and cleavage in a mineral?

Cleavage is the breaking of a mineral along flat surfaces. Fracture, on the hand is just the chipping or "fracture" of a mineral.Cleavage is the tendency to break along flat surfaces, and fracture is the tendency of a mineral to break into irregular pieces.


The tendency of a mineral to break along flat surfaces?

The tendency of a mineral to break along flat surfaces is called cleavage. Cleavage occurs due to the alignment of weak atomic bonds within the mineral's crystal structure, allowing it to break easily along specific planes. The quality of cleavage can be described by the number and orientation of the cleavage planes in a mineral.


Is Zinc a cleavage or an fracture?

Zinc is a metal that exhibits a fracture rather than cleavage. Fracture refers to the way a mineral breaks when it is not along cleavage planes, while cleavage refers to the tendency of a mineral to break along flat planes.


Cleavage is the tendecy of some minarelsto break along?

Cleavage is the tendency of some minerals to break along smooth, flat planes. This is due to the arrangement of atoms within the mineral's structure, which allows for easy separation along specific crystallographic planes. Cleavage can help in mineral identification and classification.


How does a mineral break into smooth pieces when a tool is used to break it?

A mineral can have varying numbers of cleavage planes, areas where there exists an inclination to cleave when struck or force is applied.. Most mineral crystals exhibit a preferred cleavage in certain directions, but may have cleavage planes in other directions.


When a mineral breaks along a weakly bonded plane it is called blank?

When a mineral breaks along a weakly bonded plane, it is called cleavage. Cleavage is the tendency of a mineral to break along specific planes of weakness due to the arrangement of atoms in the crystal lattice.


Can rocks have cleavage?

Yes, rocks can have cleavage. Cleavage is the tendency of a mineral to break along smooth, parallel planes. It is a property commonly observed in minerals like mica and feldspar, which can be found in certain types of rocks such as schist and granite.