Minerals are what cause water to be hard, tap water in east coast(NJ) is harder than tap water in CA. More minerals=harder water
Apatite has a hardness of 5 on the Mohs scale, meaning that minerals with a hardness greater than 5 can scratch it. Examples of such minerals include quartz (hardness 7), topaz (hardness 8), corundum (hardness 9), and diamond (hardness 10). These minerals, due to their higher hardness, can effectively scratch apatite.
Apatite has a hardness of 5 on the Mohs scale, so minerals with a hardness greater than 5 will scratch it. This includes minerals such as quartz (hardness 7), topaz (hardness 8), and corundum (hardness 9). Additionally, diamonds, which have a hardness of 10, will also easily scratch apatite.
Orthoclase has a hardness of 6 on the Mohs scale. This scale ranges from 1 (talc) to 10 (diamond), measuring the scratch resistance of various minerals. Orthoclase, a type of feldspar, can be scratched by minerals with a hardness greater than 6, such as quartz.
The Mohs Scale of Hardness determines the hardness of minerals by scratching them with commonly found objects. The minerals are assigned a number which corresponds to their hardness; higher numbers indicate higher hardness.
There is a scale of mineral hardness therefore obviously some will be softer than "4" and others harder because "4" is jut one point on that scale.
Apatite has a hardness of 5 on the Mohs scale, meaning that minerals with a hardness greater than 5 can scratch it. Examples of such minerals include quartz (hardness 7), topaz (hardness 8), corundum (hardness 9), and diamond (hardness 10). These minerals, due to their higher hardness, can effectively scratch apatite.
Apatite has a hardness of 5 on the Mohs scale, so minerals with a hardness greater than 5 will scratch it. This includes minerals such as quartz (hardness 7), topaz (hardness 8), and corundum (hardness 9). Additionally, diamonds, which have a hardness of 10, will also easily scratch apatite.
A steel nail cannot scratch minerals that are harder than itself, which has a Mohs hardness of about 4.5. This means it cannot scratch minerals such as quartz (hardness 7), topaz (hardness 8), corundum (hardness 9), and diamond (hardness 10). These minerals possess greater hardness and will resist scratching by a steel nail.
The scale used to measure the hardness of minerals is called the Mohs scale. It ranges from 1 (softest) to 10 (hardest). The hardness of a mineral affects its properties by determining how easily it can be scratched or damaged. Minerals with higher hardness are more resistant to abrasion and have a greater ability to maintain their shape and structure.
There are many minerals with hardness above 5.5 but the standard ones are feldspar,quartz, topaz, corundum and diamond.
Orthoclase has a hardness of 6 on the Mohs scale. This scale ranges from 1 (talc) to 10 (diamond), measuring the scratch resistance of various minerals. Orthoclase, a type of feldspar, can be scratched by minerals with a hardness greater than 6, such as quartz.
Any mineral with a hardness greater than that of fluorite which is 4 on the Mohs scale of hardness. Examples include quartz, orthoclase, garnet, diamond, etc.
The Mohs Scale of Hardness determines the hardness of minerals by scratching them with commonly found objects. The minerals are assigned a number which corresponds to their hardness; higher numbers indicate higher hardness.
Copper sulfide minerals, such as chalcocite and bornite, can be scratched by a penny but not a fingernail. This is due to the Mohs hardness scale, where these minerals have a hardness greater than a penny (3.5) but less than a fingernail (2.5).
There is a scale of mineral hardness therefore obviously some will be softer than "4" and others harder because "4" is jut one point on that scale.
The mineral that is softer than apatite is fluorite. On the Mohs scale of mineral hardness, apatite has a hardness of 5, while fluorite has a hardness of 4. This means that fluorite can be scratched by minerals with a hardness greater than 4, including apatite.
The hardness of MINERALS.