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Calf

Calf most commonly refers to the young of domestic or other bovine species. It may also refer to: Detailed information on calves as young animals is covered in the section.

Zoology

Bovine calves

A bovine calf refers to the young of domestic (Bos taurus), encompassing both sexes from birth until or approximately one year of age. This period marks the transition from complete dependence on maternal to partial rumination and solid feed intake, with definitions varying slightly by production system—dairy calves often weaned earlier than calves. At birth, bovine calves typically weigh 60–100 pounds (27–45 kg), depending on breed; for example, Holstein dairy calves average 90–100 pounds, while Jersey calves average 60 pounds with a range of 42–72 pounds. Newborns are initially unable to stand independently, with most achieving this within 30 minutes, though some may take up to two hours, requiring maternal or human assistance to nurse. Growth is rapid during the neonatal phase, with calves often doubling their by 60 days of age through high intake and emerging function. Bovine calf development progresses through distinct life stages: the neonatal period (first week), characterized by total reliance on for and energy; the suckling phase (up to 6–8 weeks in systems or 7–8 months in systems), where calves consume while the develops via starter feeds; and , a gradual 1–2 week to solid diets like hay and concentrates to avoid digestive upset and growth setbacks. In operations, occurs when calves consume at least 1 kg of starter daily, ensuring rumen maturity. Breeding and birth in cattle involve a gestation period averaging 283 days, influenced by , calf , and prior selection history. The calving unfolds in three stages: preparatory (2–6 hours, involving and membrane rupture), delivery (30–90 minutes, with fetal expulsion via ), and placental expulsion (6–12 hours). Dystocia, or difficult calving, affects 5–13% of births, particularly in first-calf heifers, due to fetal malposition or oversized calves, increasing risks of injury and infection. Post-birth, intake within 2–12 hours is vital, providing approximately 150-200 g of immunoglobulins (IgG) to bolster immunity against pathogens. Care practices for bovine calves emphasize , , and monitoring to promote . Newborns are housed in individual hutches or pens (providing 28–32 ft² per calf) to minimize transmission, with hutches offering protection from and drafts. schedules typically begin at 2–4 months with clostridial (7–8 way) and respiratory vaccines (IBR, , PI3, BRSV), followed by boosters at . A primary health challenge is scours (diarrhea), often caused by infectious agents like or E. coli, which can be prevented through maternity pen sanitation, early feeding, navel disinfection with , and isolating sick calves while providing electrolytes. Historically, domestic and their calves trace origins to the wild (Bos primigenius), domesticated around 10,000 years ago in the through two primary events leading to and indicine lineages. since the period has reduced overall body size from (up to 1,800 pounds) and tailored calf traits: dairy breeds like Holsteins yield smaller, faster-maturing calves optimized for milk systems, while beef breeds like produce larger calves for enhanced meat growth potential.

Calves in other species

The term "calf" originates from cealf, a Common Germanic word derived from the *gelh₂- meaning "to swell," initially referring to the young of bovine animals due to the swelling associated with . Over time, the term extended by analogy to the young of other large mammals, particularly those with similar reproductive traits to , such as extended periods and substantial birth sizes. This nomenclature applies to the offspring of various non-bovine species, including elephants, cetaceans like whales, rhinoceroses, and hippopotamuses. Elephant calves, for instance, are born after a gestation of approximately 22 months, weighing up to 250 pounds (113 kg) and standing about 3 feet (1 m) tall at birth. Blue whale calves emerge after 10–12 months of gestation, measuring 20–25 feet (6–7.6 m) in length and weighing 4,000–6,000 pounds (1,800–2,700 kg). Rhinoceros calves, depending on the species, follow a 15–18 month gestation and weigh 88–143 pounds (40–65 kg) at birth. Hippopotamus calves are born after an 8-month (227–240 day) gestation, typically weighing 55–120 pounds (25–55 kg). Across these species, calf development varies between precocial and more dependent (semi-altricial) patterns, reflecting adaptations to their environments. Elephant calves exemplify precociality, standing and walking within minutes to hours of birth to keep pace with , though they remain nutritionally reliant on maternal for up to two years. In contrast, whale calves, such as those of baleen species, are mobile at birth—capable of immediately—but exhibit prolonged dependence on , for 6–12 months while gaining hundreds of pounds weekly to support rapid growth in marine habitats. Conservation efforts highlight the vulnerability of these calves in endangered populations, where their survival critically influences species dynamics. For North Atlantic right whales, a cetacean, calf mortality exceeds 50% in recent years due to threats like vessel strikes, with around 10-15 calves born in recent calving seasons (e.g., 11 in 2024-2025) against a need for at least 50 to stabilize the of approximately 370-380 individuals as of 2025. Ship strikes alone account for up to 20% of documented deaths, often targeting calves during , underscoring their role as population bottlenecks. Culturally, non-bovine calves hold symbolic value in various traditions, particularly elephant calves in Asian folklore. In Hindu and Buddhist narratives, such as those in , elephant calves represent innocence, familial bonds, and humble strength, often depicted as embodiments of divine protection and the challenges of growth within supportive herds. These motifs appear in Southeast Asian myths, where white elephant calves signify auspicious births and royal lineage, reinforcing elephants' status as symbols of and community.

Anatomy

Structure of the human calf

The human calf, also known as the sura, refers to the muscular region of the posterior lower leg situated between the and the ankle, primarily comprising the posterior compartment of the leg. This area is dominated by two major muscles: the gastrocnemius and the soleus, which together form the triceps surae group and are essential components of the leg's structural framework. The gastrocnemius is the superficial, bi-articular muscle of the calf, consisting of two heads—the medial and lateral—that originate from the posterior aspects of the medial and lateral femoral condyles, respectively. It crosses both the and ankle joints, inserting via the . The soleus lies deeper and is mono-articular, originating from the posterior surfaces of the and , as well as the tendinous arch between them, and also converging into the . A smaller accessory muscle, the plantaris, contributes to the calf's composition; it arises from the lateral supracondylar line of the and features a long, slender tendon that runs alongside the , though it is absent in approximately 10% of individuals. Supporting structures integral to the calf include the , a robust fibrous cord that unites the gastrocnemius and soleus muscles and inserts onto the ( ), providing a critical connection for force transmission. The encases the posterior compartment, dividing the leg into distinct muscular sections and contributing to overall stability. Innervation is supplied by the , a branch of the originating from spinal segments S1 and S2, which provides motor supply to the calf muscles and sensory branches like the . Blood supply derives from the , which branches from the and nourishes the region through perforating vessels. Anatomical variations in the calf include differences in muscle fiber composition, with the soleus predominantly consisting of slow-twitch (type I) fibers for endurance (approximately 70-85%), while the gastrocnemius features a more balanced mix of slow-twitch and fast-twitch (type II) fibers (around 50% slow-twitch). Sex differences are evident, as males typically exhibit a larger cross-sectional area of calf muscles, such as the gastrocnemius, compared to females, influenced by factors like overall body size and hormonal profiles. Embryologically, the calf muscles originate from the during lower limb development, which begins around the fourth week of with the formation of limb buds. By weeks 8 to 10, the limb structures differentiate, with the gastrocnemius specifically deriving from the paraxial in the post-otic , establishing the basic muscular patterns of the posterior . In adults, calf serves as a for muscle , with typical values ranging from 34-36 cm for women and 35-38 cm for men, varying by , activity level, and ; population studies report averages varying by and , for example, in adults approximately 39 cm for men and 38 cm for women (NHANES), while in older Asian cohorts around 35-36 cm.

Function and disorders

The calf muscles, primarily the gastrocnemius and soleus, play a crucial role in locomotion by facilitating plantarflexion, the action of pointing the foot downward, which is essential for pushing off during cycles in walking and running. These muscles also assist in knee flexion, helping to bend the during activities like climbing stairs or sprinting. Furthermore, they contribute significantly to shock absorption, contributing significantly to propulsion force in the lower limb during dynamic movements such as jumping or accelerating. Biomechanically, the calf muscles support venous return through their muscle pump action, where rhythmic contractions compress the deep veins of the leg to propel blood upward against gravity and prevent pooling, which is vital for cardiovascular health during prolonged standing or exercise. They also aid in maintaining balance and stability in upright posture by counteracting forward sway and stabilizing the ankle joint. Common disorders affecting the calf include , an inflammation of the often resulting from overuse, characterized by pain and stiffness exacerbated by dorsiflexion (pulling the foot upward). Calf strains, ranging from grade 1 (mild overstretching) to grade 3 (complete tears), frequently occur due to sudden or eccentric loading, leading to sharp pain, swelling, and reduced mobility. Another prevalent condition is deep vein thrombosis (DVT), where blood clots form in the calf's deep veins, often linked to immobility or hypercoagulability, potentially causing unilateral swelling, warmth, and risk of embolization if untreated. Diagnosis typically involves clinical assessment combined with imaging; for instance, is the gold standard for proximal DVT with sensitivity over 95%, but sensitivity for isolated calf DVT is lower, around 57%. Treatment for calf strains often follows the protocol—rest, ice, compression, and elevation—to reduce inflammation and promote healing, with physical therapy for rehabilitation. may require eccentric strengthening exercises, while severe ruptures, with incidence increasing with age to around 20-30 per 100,000 annually in adults over 40 and higher in athletes, sometimes necessitate surgical repair followed by immobilization. Prevention strategies emphasize regular routines to maintain flexibility and reduce risk, as inadequate warm-ups can increase susceptibility by up to 30%. Proper that supports neutral alignment also minimizes excessive calf loading during repetitive activities. Epidemiologically, calf injuries show higher incidence among runners, affecting up to 20% annually, particularly in those increasing mileage rapidly. Age-related atrophy, known as , leads to a progressive decline in calf muscle mass by approximately 1-2% per year after age 50, impairing function and elevating fall risk.

Glaciology

Ice calving process

, also known as calving, refers to the mechanical detachment of masses from the of glaciers, shelves, or floating extensions of sheets into surrounding water bodies, resulting in fragments termed ice calves or . This process is a primary of mass loss for marine-terminating glaciers and contributes significantly to global by transferring directly into the ocean. Calving occurs through several distinct types, each driven by specific environmental and glaciological conditions. Tidal calving is modulated by fluctuations in due to cycles, which induce stresses at the grounding line and accelerate ice by up to 4% for every 1% change in depth. calving involves undercutting at the ice- , where warmer melts the submerged portion of the front, forming notches that can deepen at rates of 10-30 cm per day and destabilize the overlying . Mechanical calving, the most prevalent type, arises from internal stresses leading to propagation, where fractures extend through the under tensile forces until reaching the , triggering detachment. The physical processes underlying calving begin with stress accumulation from the glacier's forward motion, primarily driven by basal sliding rates typically ranging from 10 to 100 m per year in tidewater settings, which concentrates strain at the terminus. This leads to fracture initiation at surface or basal crevasses, where tensile stresses exceed the ice's tensile strength, allowing cracks to propagate vertically and horizontally; models like those of Nye (1957) estimate crevasse depths based on local strain rates. Once detached, the falling ice calf generates splashes, waves, and underwater pressure pulses that can further fracture adjacent ice, amplifying the event. Contributing environmental factors include climate warming, which has accelerated calving rates by approximately 20% since the 1980s through enhanced surface melting that lubricates basal sliding and increases water pressure. currents play a key role by delivering warmer water to fronts, promoting undercutting and basal melt that reduces buttressing support. These factors interact with geometry, such as water depth and width, to modulate calving frequency and magnitude. Notable global examples illustrate the scale of calving events. In , the 2002 collapse of the Larsen B Ice Shelf involved rapid disintegration and calving of approximately 2,717 km² of ice over a few weeks, driven by surface ponding and hydrofracturing. In , tidewater glaciers contribute an average annual frontal volume of approximately 510 Gt (2010–2020), accounting for about half of the ice sheet's total mass loss. Monitoring calving relies on , such as Landsat missions, which capture positions and event extents with resolutions sufficient to detect changes over days to weeks. Seismic networks complement this by detecting precursory cracks and calving impacts through ground vibrations, enabling real-time alerts for large events.

Characteristics of ice calves

Ice calves, the detached fragments from glacier , exhibit a broad range of physical attributes. They span sizes from small bergy bits, typically under 5 m in height and 5–15 m in length, to massive tabular icebergs over 100 m thick and kilometers across. These structures consist primarily of freshwater with a of approximately 917 kg/m³, significantly lower than seawater's 1025 kg/m³, resulting in roughly 89% submersion and only 11% exposure above the surface. The morphology of ice calves varies based on calving conditions. Dry calving, occurring in air without , produces irregular, jagged shapes due to brittle . In contrast, wet calving into yields flatter, more tabular forms with smoother tops, often from edges. Post-detachment, calves may flip or roll due to uneven density distribution or wave action, altering their orientation and exposing new surfaces. Once afloat, ice calves' stability and drift are governed by environmental forces. , typically at speeds of 10–20 km/h in polar regions, imparts about 2% of its to the calf, while currents dominate longer-term movement, yielding average drift speeds of 0.2–0.8 m/s. In waters, their persistence is limited by , with summer rates of 0.5–2 m/day at the surface and higher basal , leading to half-lives of weeks to months depending on size and location. Ecologically, ice calves foster unique habitats by shading waters and releasing nutrient-rich , supporting marine such as aggregations beneath their edges for refuge from predators. However, they pose significant hazards to shipping, as exemplified by the 1912 collision of the RMS with a calf-derived , which caused the vessel's sinking and over 1,500 deaths. Measurement of ice calves relies on advanced and systems. Radar altimetry, such as from CryoSat-2 or TanDEM-X, enables estimation by mapping surface and inferring submerged portions via contrasts. Visual and size-based follows International Ice Patrol scales, categorizing calves by height (e.g., bergy bits 1–5 m) and length for hazard assessment. As of the 2010s, observations indicated heightened calving activity linked to amplification, where regional warming exceeds global averages, accelerating ice loss. At Jakobshavn Isbræ, Greenland's fastest-flowing , flow speeds had increased by approximately 50–150% since 2000, contributing to front retreat rates exceeding 10 km and speeds doubling to over 17 km/year (as of 2012). However, speeds at Jakobshavn slowed after 2015, with the experiencing variable annual mass loss, including a low of 55 Gt in 2024 due to above-average snowfall, though long-term dynamic losses from calving persist.

Proper names

Geographical locations

The name "Calf" in geographical locations often derives from kálfr, referring to a young bovine or, in topographic contexts, a rounded hill resembling the shape of a calf's leg, reflecting Scandinavian influences on place names in regions like the . One prominent example is the , an uninhabited island of approximately 2.5 square kilometers located off the southwest coast of the Isle of Man in the , separated by the narrow Calf Sound. This rugged, low-lying island reaches a highest point of 128 meters and serves as a key managed by Manx National Heritage, hosting significant seabird colonies including Manx shearwaters and providing habitat for and other . Historically, the island supported hermits, monks, farmers, and lighthouse keepers until the mid-20th century. The surrounding Calf of Man and Wart Bank area was designated a Marine in 2018, with conservation efforts emphasizing protection of breeding seabirds and wetlands, aligning with international standards under the framework since initial proposals in the early 2000s. Access is restricted to guided visits from April to September via boat from Port St Mary, with coordinates at approximately 54°03′N 04°49′W, to minimize disturbance to wildlife. In the , several hills bear the name "Calf," often linked to the topographic sense. The Calf in the Howgill Fells, within the , stands at 676 meters and is the highest point in this upland area of north-west , offering panoramic views and popular routes such as the 13-kilometer circuit from , which includes a 860-meter elevation gain. Nearby, Calf Top, at 610 meters on Middleton Fell near Sedbergh, marks the boundary between and and was as a mountain in 2016 after precise surveying confirmed its height just above the 610-meter threshold, making it a notable unnamed fell in local until its recognition. These sites attract hikers for their grassy summits and remote paths, with Calf Top accessible via trails from Barbon or Dentdale. Across the Atlantic, Calf Island lies in as part of the Islands , a small, marshy outcrop known for its tidal pools, wildflowers, and views of the harbor. Historically, it was granted to early colonists like William Brewster in the and later served as a private estate; in 1845, James Turner constructed a home using materials from a , while in 1902, it became the summer retreat of businessman Benjamin P. Cheney and actress Julia Arthur, featuring a colonial-style destroyed by fire in 1971. The island's past includes use by lobster fishermen and, during the 19th century, occasional roles in harbor activities, though not a primary site like neighboring Rainsford or Gallops Islands. Today, it remains largely undeveloped, accessible only by private boat, emphasizing its ecological value within the . In Utah, Calf Creek refers to a scenic canyon in Grand Staircase-Escalante National Monument, carved by the creek and famous for its waterfalls, including the 38-meter Lower Calf Creek Falls, which cascades into a turquoise pool amid desert sandstone. The 10-kilometer round-trip trail to the lower falls is a moderate hike through riparian greenery, passing ancient pictographs and slot canyons, while the upper falls, at 27 meters, offer a shorter, steeper 2-kilometer descent to additional pools. Named possibly for its calf-like bends or historical cattle grazing, the area supports diverse flora and fauna, drawing visitors for its contrast of arid plateaus and lush oases. Further afield in , the Calf associated with Cow and Islands forms a small in Newfoundland and Labrador's coastal waters, part of a minor at 56°38′N 60°49′W, traditionally used for seasonal amid the province's rich marine grounds. This remote feature, amid thousands of similar islets, reflects the rugged, fog-shrouded terrain supporting , , and fisheries, with limited modern access by small boats from nearby communities.

People and surnames

The surname Calf is of English origin, derived from the Middle English word "calf," meaning a young cow, which itself stems from Old English "cealf" and ultimately from Old Norse "kalfr." It likely originated as a nickname for someone resembling a calf in appearance or manner, or as a metonymic occupational name for a herder or tender of calves. Variants include Calfe and Colfe, the latter appearing in historical records. The remains rare globally, with fewer than 500 bearers estimated in the , ranking it as the 722,496th most common worldwide. It is most concentrated in the , particularly , where it accounts for about 37% of occurrences, followed by the at around 20%. Genealogical records on platforms like Ancestry trace Calf families primarily to rural areas in these regions from the 1800s onward, reflecting ties to farming heritage. Notable individuals bearing the surname include Abraham Colfe (1580–1657), an English clergyman and philanthropist who served as vicar of and founded in 1652 to provide education for local boys. In modern times, (born 1959) is a known for roles in films such as (1994) and television series including . Historical records also mention figures like Richard Calf, Bishop of Down in Ireland in 1354, though the surname's prominence remains limited outside minor ecclesiastical and artistic contexts. As a , Calf is uncommon in contemporary usage but traces back to the personal name Kalfr, used as a byname meaning "calf," occasionally appearing in or as a . Its rarity as a first name underscores the surname's stronger association with familial identity rather than standalone nomenclature. Culturally, the name evokes rural and agricultural roots, often linked to England's pastoral history without major celebrity associations, and appears frequently in 19th-century databases documenting farming communities. Demographic trends show its adoption influenced by Viking-era migrations from to , where elements integrated into Anglo-Saxon naming practices, later spreading via 19th- and 20th-century emigration to the .

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