A anhedral crystal is not well formed due to limited growth in environment. A euhedral crystal are well formed with recognizable faces from more space to grow.
no
Because they can take long to form resulting in a large crystal well-formed. And also remeber fast forming Crystal =small, slow forming Crystal =large
== == Many minerals have multiple crystal habits, which are the size and shape of a particular mineral crystals formation. Examples of crystal habit include boytroidal, stubby, blocky, radiating, wheat sheaf, columnar, acicular, foliated, subhedral, euhedral, drusy, dendritic, and bladed.
igneous is the texture of igneous rocks. The texture of igneous rocks is defined by 3 ways: a) Crystallinity- it expresses the degree of formation of crystals in an igneous rock. the texture of an igneous rock may be Holocyrstalline (Completely characterised by crystals, Hemicrystalline (partially having crystals) and holocrystalline (no crystals). b) Granularity- it is the size of the grains. it may be equigranular (when mineral grains are equal in size) or inequigranular (when mineral grains are not equal in size). c) shape of crystals- The shape of crystals may be Euhedral (When all crystals are of same shape), Subhedral (when they are partially similar in shape), Anhedral (when they are completely different in shape).
The crystals have abundant room to grow in their hollow surroundings also the crystals can form very easily in many places.
no
Because they can take long to form resulting in a large crystal well-formed. And also remeber fast forming Crystal =small, slow forming Crystal =large
Mineral crystals are divided into six distinct mineral crystal systems based on geometry and angles between axes. Crystals can further be subdivided into categories of 'habit', the crystals' variety of appearances in nature. Examples of habit are boytroidal, globular, massive, euhedral, drusy, acicular, and so on.
In a fluid (magma) they are free to grow in any direction, and therefore are able to grow into euhedral crystals.
== == Many minerals have multiple crystal habits, which are the size and shape of a particular mineral crystals formation. Examples of crystal habit include boytroidal, stubby, blocky, radiating, wheat sheaf, columnar, acicular, foliated, subhedral, euhedral, drusy, dendritic, and bladed.
Virtually all rock contains mineral crystals of various sizes. Most volcanic rocks such as granite contain crystals of quartz and other minerals. Crystal size varies depending on the speed of cooling.
igneous is the texture of igneous rocks. The texture of igneous rocks is defined by 3 ways: a) Crystallinity- it expresses the degree of formation of crystals in an igneous rock. the texture of an igneous rock may be Holocyrstalline (Completely characterised by crystals, Hemicrystalline (partially having crystals) and holocrystalline (no crystals). b) Granularity- it is the size of the grains. it may be equigranular (when mineral grains are equal in size) or inequigranular (when mineral grains are not equal in size). c) shape of crystals- The shape of crystals may be Euhedral (When all crystals are of same shape), Subhedral (when they are partially similar in shape), Anhedral (when they are completely different in shape).
The crystals have abundant room to grow in their hollow surroundings also the crystals can form very easily in many places.
Euhedral crystals forms [perfectly formed].
Beneficial to euhedral crystal shapes would be the proper temperature and length of time spent in ideal conditions for crystal formation for the particular mineral. Ideal conditions would include: space available for mineral crystal growth and availability or supply of mineral rich solutions bearing mineral components.
A mineral is always made up of crystals, but if the crystals are very small the mineral will not appear crystalline to the naked eye. A good example of this is quartz. Almost everyone is familiar with the colorless, transparent, 6 sided quartz crystal. But quartz also forms veins inside other rocks which don't appear crystalline at all. The quartz in the vein is still crystalline, it is just that the crystals are very, very small, because they formed too quickly to grow large enough to be visible to the naked eye.
No. A crystal garden my be made of crystals but it is no itself a crystal.