I Can’t Sleep - Crystals | Peaceful Bedtime Reading for Sleep

Episode Date: October 31, 2024

Relax with this calm bedtime reading about crystals, the naturally formed solids whose structures and beauty have fascinated people for centuries. Benjamin’s soothing narration gently explores how crystals form, their scientific properties, and their presence in nature and culture. With a steady, comforting cadence, this episode offers fact-filled storytelling—no whispers, no hypnosis—just calm education to ease insomnia and help quiet restless thoughts. Perfect for reducing stress, relieving anxiety, and guiding you into deep rest. Press play, unwind, and let your mind settle like the still beauty of crystals. Want More? Request a Topic: https://www.icantsleeppodcast.com/request-a-topic Ad-Free Episodes: https://icantsleep.supportingcast.fm/ Shop Sleep-Friendly Products: https://www.icantsleeppodcast.com/sponsors Join the Discussion on Discord: https://discord.gg/myhGhVUhn7 This content is derived from the Wikipedia article on Crystals, available under the Creative Commons Attribution-ShareAlike (CC BY-SA) license. Read the full article: Wikipedia – Crystals. Happy sleeping! Learn more about your ad choices. Visit megaphone.fm/adchoices

You're listening to a Glassbox Media podcast. What if I told you that most of the modern day self-help advice you've been hearing could actually make you worse? The key to a better life isn't about feel-good gimmicks that sound catchy. The Mentally Stronger Podcast gives you access to a licensed therapist who shares science-backed tools that will actually change your life. Hi, I'm Amy Morin, psychotherapist, mental strength trainer, and international best-selling author. In each episode, we cover research-back strategies, like how to stop relying on willpower and start creating habits for lasting change. And the five mental strength-building exercises you can do from your couch. I also speak to world-class experts like Dr. Nicole Kane, who shares how to permanently heal anxiety by addressing the root cause.

With over 200 episodes in our catalog, this podcast is for you if you're ready to crush self-doubt, conquer challenges, become stronger than ever with therapist-approved strategies that can change your life. Listen to Mentally Stronger with Therapist Amy Morin, wherever you get your podcasts. Welcome to the I Can't Sleep Podcast, where I read random articles from across the web to bore you to sleep with my soothing voice. I'm your host, Benjamin Boster. Today's episode is from a Wikipedia article titled, Crystal. A crystal or crystalline solid is a solid. solid material whose constituents, such as atoms, molecules, or ions, are arranged in a highly

ordered microscopic structure, forming a crystal lattice that extends in all directions. In addition, macroscopic single crystals are usually identifiable by their geometrical shape, consisting of flat faces with specific characteristic orientations. The scientific study of crystals in crystal formation is known as crystallography. The process of crystal formation via mechanisms of crystal growth is called crystallization or solidification. The word crystal derives from the ancient Greek word crustalos, meaning both ice and rock crystal, from Cruos, icy cold frost. Examples of large crystals include snowflakes, diamonds, and table salt.

Most inorganic solids are not crystals, but polycrystals, i.e. many microscopic crystals fused together into a single solid. Polycrystals include most metals, rocks, ceramics, and ice. A third category of solids is amorphous solids, where the atoms have no period structure whatsoever. Examples of amorphous solids include glass, wax, and many plastics. Despite the name, lead crystal, crystal glass, and related products are not crystals, but rather types of glass, i.e. amorphous solids. Crystals or crystalline solids are often used in pseudoscientific practices, such as crystal therapy. and, along with gemstones, are sometimes associated with spellwork and wicken beliefs and related religious movements. The scientific definition of a crystal is based on the microscopic arrangement of atoms inside it, called the crystal structure. A crystal is a solid where the atoms form a periodic arrangement.

Quasi-crystals are an exception. Not all solids are crystals. For example, when liquid water starts freezing, the phase change begins with small ice crystals that grow until they fuse, form in a polychristling structure. In the final block of ice, each of the small crystals, called crystallites or grains, is a true crystal with a periodic arrangement of atoms. But the whole polycrystal does not have a periodic arrangement of atoms,

because the periodic pattern is broken at the grain boundaries. Most macroscopic inorganic solids are polycrystalline, including almost all metals, ceramics, ice, rocks, etc. Solids that are neither crystalline nor polychristylene, such as glass, are called amorphous solids, also called glassy, vitreous, or non-crystalline. These have no periodic order even microscopically. There are distinct differences between crystalline solids and amorphous solids.

Most notably, the process of forming a glass does not release the latent heat of fusion, but forming a crystal does. A crystal structure, an arrangement of atoms in a crystal, is characterized by its unit cell, a small imaginary box containing one or more atoms in a specific spatial arrangement. The unit cells are stacked in three-dimensional space to form the crystal. The symmetry of a crystal is constrained by the requirement

that the unit cells stack perfectly with no gaps. There are 219 possible crystal symmetries. 230 is commonly cited, but this treats chiral equivalence as separate entities, called crystallographic space groups. These are grouped into seven crystal systems, such as cubic crystal system, where the crystals may form cubes or rectangular boxes, such as halide, or hexagonal crystal system, where the crystals may form hexagons, such as ordinary water ice.

Crystals are commonly recognized macroscopically by their shape, consisting of flat faces with sharp angles. These shape characteristics are not necessary for a crystal. A crystal is scientifically defined by its microscopic atomic arrangement, not its macroscopic shape. But the characteristic macroscopic shape is often present in easy to see. Eugel crystals are those that have obvious, well-formed flat faces. Anheedral crystals do not,

usually because the crystal is one grain in a polychristylene solid. The flat faces, also called facets of a eugedral crystal, are oriented in a specific way relative to the underlying atomic arrangement of the crystal. They are planes of relatively low Miller index. This occurs because some surface orientations are more stable than others, low surface energy. As a crystal grows, new atoms attach easily to the rougher and less stable parts of the surface, but less easily to the flat, stable surfaces. Therefore, the flat surfaces tend to grow larger and smoother, until the whole crystal surface consists of these plain surfaces. One of the oldest techniques in the science of crystallography consists of measuring the three-dimensional

orientations of the faces of a crystal, and using them to infer the underlying crystal symmetry. A crystal's crystallographic forms are sets of possible faces of the crystal that are related by one of the symmetries of the crystal. For example, crystals of Galena often take the shape of cubes, and the six faces of the cube belong to a crystallographic form that displays one of the symmetries of the isometric crystal system. Galena also sometimes crystallizes as octahedrons, and the eight faces of the octahedron belong to another crystallographic form, reflecting a different symmetry of the isometric system.

The crystallographic form is described by placing the Miller indices of one of its faces within brackets. For example, the octahedral form is written as open bracket, one one, close bracket, and the other faces in the form are implied by the symmetry of the crystal. Forms may also be closed, meaning that the form can completely enclose a volume of space or open, meaning that it cannot. The cubic and octahedral forms are examples of closed forms. All the forms of the isometric system are closed, while all the forms of the monoclinic and tric crystal systems are open.

A crystal's faces may all belong to the same closed form, or they may be a combination of multiple open or closed forms. The crystal's habit is its visible external shape. This is determined by the crystal structure which restricts the possible facet orientations, the specific crystal chemistry and bonding, which may favor some facet types over others, and the conditions under which the crystal formed. By volume and weight, the largest concentrations of crystals in the earth are part of its solid bedrock.

found in rocks typically range in size from a fraction of a millimeter to several centimeters across, although exceptionally large crystals are occasionally found. As of 1999, the world's largest known natural occurring crystal is a crystal of barrel from Malagialina Madagascar, 18 meters long and 3.5 meters in diameter, and weighing 380,000 kilograms. Some crystals have formed by magmatic and metamorphic processes, giving origin to large masses of crystalline rock. The vast majority of igneous rocks are formed from molten magma, and the degree of crystallization depends primarily on the conditions under which they solidified. Such rocks as granite, which have cooled very slowly and under great pressures, have completely crystallized. But many kinds of lava were poured out at the surface and cooled very rapidly,

and in this latter group, a small amount of amorphous or glassy matter is common. Other crystalline rocks, the metamorphic rock, such as marbles, mycoschists, and quartzites, are recrystallized. This means that they were at first fragmental rocks like limestone, shale, and sandstone. and have never been in a molten condition, nor entirely in solution. But the high temperature and pressure conditions of metamorphism have acted on them by erasing their original structures and inducing recrystallization in the solid state. Other rock crystals have formed out of precipitation from fluids,

commonly water, to form druses or quartz veins, Evaporites such as halite, gypsum, and some limestones have been deposited from aquaous solution, mostly owing to evaporation in arid climates. Water-based ice in the form of snow, sea ice, and glaciers are common crystalline, polycrystalline structures on Earth and other planets. A single snowflake is a single crystal or a collection of crystals, while an ice cube is a polycrystal. Ice crystals may form from cooling liquid water below its freezing point,

such as ice cubes or a frozen lake. Frost, snowflakes, or small ice crystals suspended in the air, ice fog, more often grow from a super-saturated gaseous solution of water vapor and air. When the temperature of the air drops below its dew point, without passing through a liquid state. Another unusual property of water is that it expands rather than it contracts when it crystallizes. Many living organisms are able to produce crystals grown from an aqua solution. For example, calcite or argonite in the case of most mollus or hydroxylapitite,

in the case of bones and teeth and vertebrates. The same group of atoms can often selects, solidify in many different ways. Polymorphism is the ability of a solid to exist in more than one crystal form. For pure chemical elements, polymorphism is known as allotropy. For example, diamond and graphite are two crystalline forms of carbon, while amorphous carbon is a non-crystalline form. Polymorphs, despite having the same atoms, may have very different properties. For example, diamond is the hardest substance known, while graphite is so soft that it is used as a lubricant.

Chocolate can form six different types of crystals, but only one has the suitable hardness and melting point for candy bars and confections. Polymorphism in steel is responsible for its ability to be heat-treated, giving it a wide range of properties. Polyamorphism is a similar phenomenon where the same atoms can exist in more than one amorphous solid form. Crystallization is the process of forming a crystalline structure from a fluid or from materials dissolved in a fluid. More rarely, crystals may be deposited directly from gas. Crystallization is a complex and extensively studied field, because depending on the conditions,

a single fluid can solidify into many different possible forms. It can form a single crystal, perhaps with various possible phases, stoichiometries, impurities, defects, and habits. Or it can form a polycrystal with various possibilities for the size, arrangement, orientation, and phase of its grains. The final form of the solid is determined by the conditions under which the fluid is being solidified,

such as the chemistry of the fluid, the ambient pressure, the temperature, and the speed with which all these parameters are changing. Specific industrial techniques to produce large single crystals include the Chakralski process and the Bridgman technique. Other less exotic methods of crystallization may be used, depending on the physical properties of the substance, including hydrothermal synthesis, sublimation, or simply solvent-based crystallization. Large single crystals can be created by geological processes. For example, selenite crystals in excess of 10 meters are found in the cave of the crystals in Nica, Mexico. Crystals can also be formed by biological processes.

Conversely, some organisms have special techniques to prevent crystallization from occurring, such as antifreeze proteins. An ideal crystal has every atom in a perfect, exactly repeating pattern. However, in reality, most crystalline materials have a variety of crystallographic defects, places where the crystals pattern is interrupted. The types and structures of these defects may have a profound effect on the properties of the materials. A few examples of crystallographic defects include vacancy defects, an empty space where an atom should fit,

interstitial defects, an extra atoms squeezed in where it does not fit, and dislocation. Dislocations are especially important in material science, because they help determine the mechanical strength of materials. Another common type of crystallographic defect is an impurity, meaning that the wrong type of atom is present in a crystal. For example, a perfect crystal of diamond would only contain carbon atoms, but a real crystal might perhaps contain a few boron atoms as well.

These boron impurities change the diamond's color to slightly blue. Likewise, the only difference between ruby and sapphire is the type of impurities present in a corundum crystal. In semiconductors, a special type of impurity called a dopand. T drastically changes the crystal's electrical properties. Semiconductor devices, such as transistors, are made possible largely by putting different semiconductor properties into different places in specific patterns. Twinning is a phenomenon somewhere between a crystallographic defect and a grain boundary. Like a grain boundary, a twin boundary has different crystal orientations on its two sides. But unlike a grain boundary, the orientations are not random, but related in a specific mirror image way.

Mosaicity is a spread of crystal plane orientations. A mosaic crystal consists of some. smaller crystalline units that are somewhat misaligned with respect to each other. In general, solids can be held together by various types of chemical bonds, such as metallic bonds, ionic bonds, covalent bonds, van dervales bonds, and others. None of these are necessarily crystalline or non-crystalline. However, there are some general trends as follows. metals crystallize rapidly and are almost always polycrystalline,

though there are exceptions like amorphous metal and single crystal metals. The latter are grown synthetically, for example fighter jet turbines, are typically made by first growing a single crystal of titanium alloy, increasing its strength and melting point over polycrystalline titanium. A small piece of metal may naturally form into a single crystal, such as type 2 telluric iron. But larger pieces generally do not unless extremely slow cooling occurs. For example, iron meteorites are often composed of single crystal, or many large crystals that may be several meters in size due to very slow cooling in the vacuum of space.

the slow cooling may allow the precipitation of a separate phase within the crystal lattice, which form its specific angles determined by the lattice, called Vidmanstadtin patterns. Ionic compounds typically form when a metal reacts with a non-metal, such as sodium with chlorine. These often form substances called salts, such as sodium chloride, table salt, or potassium nitrate, saltpeter. with crystals that are often brittle and cleave relatively easily. Ionic materials are usually crystalline or polycrystalline. In practice, large salt crystals can be created by solidification of a molten fluid or by crystallization out of a solution.

Some ionic compounds can be very hard, such as oxides like aluminum oxide found in many gemstones, such as ruby and synthetic sapphire. Covalently bonded solids, sometimes called covalent network solids, are typically formed from one or more non-metals, such as carbon or silicon and oxygen, and are often very hard, rigid, and brittle.

These are also very common, notable examples being diamond and quartz, respectively. Weak van derval's forces also help hold together certain crystals, such as crystalline molecular solids, as well as the interlayer bonding and graphite. Substances such as fats, lipids, and wax form molecular bonds because the larger molecules do not pack as tightly as atomic bonds. This leads to crystals that are much softer and more easily pulled apart or broken. Common examples include chocolate, candles or viruses.

Water ice and dry ice are examples of other materials with molecular bonding. Polymer materials generally will form crystalline regions, but the lengths of the molecules usually prevent complete crystallization, and sometimes polymers are completely amorphous. A quasi-crystall consists of arrays of atoms that are ordered, but not strictly periodic. They have many attributes in common with ordinary crystals, such as displaying a discrete pattern in x-ray diffraction, and the ability to form shapes with smooth flat faces. Quasi-crystals are most famous for their ability to show five-fold symmetry, which is impossible for an ordinary periodic crystal.

The International Union of Crystallography has redefined the term crystal, to include both ordinary periodic crystals and quasi-crystals, any solid having any essentially discrete diffraction diagram. Quasi-crystals, first discovered in 1982, are quite rare in practice. Only about 100 solids are known to form quasi-crystals, compared to about 400,000 periodic crystals known in 2004. The 2011 Nobel Prize in Chemistry was awarded to Dan Shackman for the discovery of quasi-crystals. Crystals can have certain special electrical, optical, and mechanical properties

that glass and polycrystals normally cannot. These properties are related to the anisotropy of the crystal, i.e. the lack of rotational symmetry in its atomic arrangement. One such properties is the Piazoa electric effect where a voltage across the crystal can shrink or stretch it. Another is birefringence, where a double image appears when looking through a crystal. Moreover, various properties of a crystal, including electrical conductivity, electrical permittivity, and Young's modules, may be different in different directions in a crystal. in a crystal. For example, graphite crystals consist of a stack of sheets, and although each individual sheet is mechanically very strong, the sheets are rather loosely bound to each other. Therefore,

the mechanical strengths of the material is quite different depending on the direction of stress. Not all crystals have all of these properties. Conversely, these properties are not quite exclusive to crystals. They can appear in glasses or polycrystals that have been made anisotropic by working or stress. For example, stress-induced by refringents. Crystallography is the science of measuring the crystal structure, in other words, the atomic arrangement of a crystal. One widely used crystallography technique is x-ray diffraction. Large numbers of known crystal structure are stored in crystallographic databases. In physics, the terms order and disorder designate the presence or absence of some symmetry or correlation

in a many-particle system. In condensed matter physics, systems typically are ordered at low temperatures. Upon heating, they undergo one or several phase transitions and to less ordered states. Examples for such an order-disorder transition are The melting of ice, solid liquid transition, loss of crystalline order, the demagnetization of iron by heating above the curie temperature, ferromagnetic, paramagnetic transition, loss of magnetic order. The degree of freedom that is ordered or disordered can be transitional,

crystalline ordering, rotational, rotational, ferroelectric ordering, or a spin state, magnetic ordering. The order can consist either in a full crystalline space group symmetry or in a correlation. Depending on how the correlations decay with distance, one speaks of long-range order or short-range order. If a disordered state is not in thermodynamic equilibrium, one speaks of quenior. Disorder. For instance, a glass is obtained by quenching a liquid. By extension, other quenched states are called spin glass, orientational glass. In some contexts, the opposite of quenched disorder is an healed disorder. The strictest form of order in a

solid is lattice periodicity. A certain pattern, the arrangement of atoms in a unit cell is repeated again and again to form a translationally invariant tiling of space. This is the defining property of a crystal. Possible symmetries have been classified in 14 brevet lattices and 230 space groups. Latus periodicity implies long-range order. If only one unit cell is known, then by virtue of of the translational symmetry, it is possible to accurately predict all atomic positions at arbitrary distances. During much of the 20th century, the converse was also taken for granted, until the discovery of quasi-crystals in 1982 showed that there are perfectly deterministic

tilings that do not possess lattice periodicity. Besides structural order, one may consider charge ordering, spin ordering, magnetic ordering, and compositional ordering. Magnetic ordering is observable in neutron diffraction. It is a thermodynamic entropy concept often displayed by a second-order phase transition. Generally speaking, high thermal energy is associated with disorder and low-thermal energy with ordering, although there have been violations of this. ordering peaks become apparent in diffraction experiments at low energy