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The intergluteal cleft or just gluteal cleft, also known by a number of synonyms, including natal cleft, butt crack, and cluneal cleft, is the groove between the buttocks that runs from just below the sacrum to the perineum,[1] so named because it forms the visible border between the external rounded protrusions of the gluteus maximus muscles. Other names are the anal cleft, crena analis, crena interglutealis, and rima ani. Colloquially the intergluteal cleft is known as bum crack (UK) or butt crack (US). The intergluteal cleft is located superior to the anus.
The anus is connected to the rectum by the anal canal. The anal canal has two ring-shaped muscles (called sphincter muscles) that keep the anus closed and prevent stool from leaking out. The anal canal is about 1-1/2 to 2 inches (about 3 to 5 cm) long and goes from the rectum to the anal verge. The anal verge is where the canal connects to the outside skin at the anus. This skin around the anal verge is called the perianal skin (previously called the anal margin).
Go beyond the iconic crack to learn how this State House bell was transformed into an extraordinary symbol. Abolitionists, women's suffrage advocates and Civil Rights leaders took inspiration from the inscription on this bell. Plan your visit to the Liberty Bell Center to allow time to view the exhibits, see the film, and gaze upon the famous cracked bell. No tickets are required and hours vary seasonally.
From Signal to Symbol The State House bell, now known as the Liberty Bell, rang in the tower of the Pennsylvania State House. Today, we call that building Independence Hall. Speaker of the Pennsylvania Assembly Isaac Norris first ordered a bell for the bell tower in 1751 from the Whitechapel Foundry in London. That bell cracked on the first test ring. Local metalworkers John Pass and John Stow melted down that bell and cast a new one right here in Philadelphia. It's this bell that would ring to call lawmakers to their meetings and the townspeople together to hear the reading of the news. Benjamin Franklin wrote to Catherine Ray in 1755, "Adieu, the Bell rings, and I must go among the Grave ones and talk Politicks." It's not until the 1830s that the old State House bell would begin to take on significance as a symbol of liberty.
The Crack No one recorded when or why the Liberty Bell first cracked, but the most likely explanation is that a narrow split developed in the early 1840s after nearly 90 years of hard use. In 1846, when the city decided to repair the bell prior to George Washington's birthday holiday (February 23), metal workers widened the thin crack to prevent its farther spread and restore the tone of the bell using a technique called "stop drilling". The wide "crack" in the Liberty Bell is actually the repair job! Look carefully and you'll see over 40 drill bit marks in that wide "crack". But, the repair was not successful. The Public Ledger newspaper reported that the repair failed when another fissure developed. This second crack, running from the abbreviation for "Philadelphia" up through the word "Liberty", silenced the bell forever. No one living today has heard the bell ring freely with its clapper, but computer modeling provides some clues into the sound of the Liberty Bell.
Ringworm on the skin starts as a red, scaly patch or bump. Over time, it may look like one or more rings with raised, bumpy, scaly borders (the center is often clear). This ring pattern gave ringworm its name, but not every infected person has it. The skin may flake, peel, or crack, and it can itch, sting, burn, or feel uncomfortable.
The round or bubble butt is in the shape of an "O" or "cherry-shaped." Typically, round butts have a fuller appearance with fat around the cheeks and top of the buttocks. Because of its fat distribution, the bubble butt has a rounded appearance. The bubble butt has a rounded effect when viewed from the backside and the side.
The square butt is the most common butt shape, especially in younger women. Square butts are equal in size from the waist to the hips. Square butts are called masculine-looking. The square butts also look flat. Square butts are common in patients with either high hip bones or excess "love handle" fat. As a result, the hip bone and outer thigh are in line, rather than tapering to the waist with a smooth curve. The result can be a flat, square butt. Poor gluteal muscle definition can also give the appearance of a flat butt. Square butts are very difficult to reshape with exercise and eating right. Often, square butts require plastic surgery to be reshaped. The Problem: Square butts cause the hip bones to become more prominent. Also, square butts become more prominent because of fat distributed around the "love handle" area. This "love handle" fat can give patients a square shape. Too much fat on the "love handle" area can make the butt appear large, even when the butt is small and flat. Because of the fat stored in the upper region of the hip bones, it is characteristic of square butt patients to have a flat butt. The fat that is carried on top of the hips of the square butt can be a worry for some men and women.
Patients with a V-shaped butt have a larger waist and small butt. Patients with a V-shaped buttock have full hips. Their buttocks are fuller at the top compared to the bottom of the buttocks. The large waist and small butt create the appearance of a "V." The V-shape butt is more frequently seen in older women. This is believed to occur due to reduced estrogen levels. The reduction in estrogen can change the location of fat storage areas. In aging women, butt fat disappears, and abdominal fat accumulates (not fair!). This change in fat distribution can lead to an inverted butt shape where the base of the butt is much smaller than the top of the butt. Unfortunately, due to loss of fat and volume, the inverted butt is also prone to drooping.
The Problem: The V-shape butt lacks volume in the mid and lower buttock. The butt cheek area may appear droopy and small compared to the overall circumference of the butt. Since there is no volume at the inferior border of the V-shaped butt, patients with a V-shaped buttock can have a very unhealthy appearing butt.
The COVID-19 pandemic has not just exposed the cracks in our global health systems but demonstrated how much health matters for our economies. Many developing economies are at risk of being hit hard by dual health and economic shocks with forecasts suggesting a cost of up to 8 percent in global GDP in 2020.
While plastic shrinkage cracks can happen anywhere in a slab or wall, they almost always happen at reentrant corners (corners that point into the slab) or with circular objects in the middle of a slab (pipes, plumbing fixtures, drains, and manholes). Since concrete cannot shrink around a corner, stress will cause the concrete to crack from the point of that corner.
An excessively wet mix is a contributing factor to shrinkage in concrete. While water is an essential ingredient in every concrete mix, there is such a thing as too much water. When the mix contains too much water, the slab will shrink more than if the correct amount of water was used. Hot weather is another big reason for plastic shrinkage cracks.
Just like a balloon, heat causes concrete to expand. When concrete expands, it pushes against anything in its way (a brick wall or adjacent slab for example). When neither has the ability to flex, the expanding force can be enough to cause concrete to crack.
Expansion joints are used as a point of separation (or isolation), between other static surfaces. Typically made of a compressible material like asphalt, rubber, or lumber, expansion joints must act as shock absorbers to relieve the stress that expansion puts on concrete and prevent cracking.
When the ground freezes, it can sometimes lift many inches before thawing and settling back down. This ground movement brought on by the freezing and thawing cycle is a huge factor contributing to concrete cracking. If the slab is not free to move with the ground, the slab will crack.
Although concrete is a very strong building material, it does have its limits. Placing excessive amounts of weight on top of a concrete slab can cause cracking. When you hear a concrete mix has a strength of 2000, 3000, 4000, or 5000+ PSI, it is referring to the pounds per square inch it would take to crush that concrete slab.
After a heavy rain or snowmelt when the ground below is soft and wet, excessive weight on the slab can press the concrete down and result in cracks. Residential homeowners who place large recreational vehicles or dumpsters on their driveways are more likely to see this type of cracking.
Crazing cracks are very fine, surface cracks that resemble spider webs or shattered glass. When the top of a concrete slab loses moisture too quickly, crazing cracks will likely appear. While unsightly, crazing cracks are not a structural concern.
If pain is not relieved by those changes,adjusting your weight by leaning forward slightly when seated may help. Sittingon a doughnut-shaped cushion or a V-shaped wedge cushion may help distributeweight away from the painful area. Using heat or ice on the painful area, aswell as taking over-the-counter pain relievers, also may offer some relief.
The consequences of plate movement are easy to see around Krafla Volcano,in the northeastern part of Iceland. Here, existing ground cracks have widenedand new ones appear every few months. From 1975 to 1984, numerous episodesof rifting (surface cracking) took place along the Krafla fissurezone. Some of these rifting events were accompanied by volcanic activity;the ground would gradually rise 1-2 m before abruptly dropping, signallingan impending eruption. Between 1975 and 1984, the displacements caused byrifting totalled about 7 m.
In East Africa, spreading processes have already torn Saudi Arabia awayfrom the rest of the African continent, forming the Red Sea. The activelysplitting African Plate and the Arabian Plate meet in what geologists calla triple junction, where the Red Sea meets the Gulf of Aden. A newspreading center may be developing under Africa along the East African RiftZone. When the continental crust stretches beyond its limits, tension cracksbegin to appear on the Earth's surface. Magma rises and squeezes throughthe widening cracks, sometimes to erupt and form volcanoes. The rising magma,whether or not it erupts, puts more pressure on the crust to produce additionalfractures and, ultimately, the rift zone. 2b1af7f3a8