Instruct: Given a question, retrieve relevant documents that can help answer the question.
Query: Can lava kill you?
A volcanic bomb is a mass of molten rock (tephra) larger than 64mm (2.5inches) in diameter, formed when a volcano ejects viscous fragments of lava during an eruption. They cool into solid fragments before they reach the ground. Because volcanic bombs cool after they leave the volcano, they are extrusive igneous rocks. Volcanic bombs can be thrown many kilometres from an erupting vent, and often acquire aerodynamic shapes during their flight. Bombs can be extremely large; the 1935 eruption of Mount Asama in Japan expelled bombs measuring 5–6m in diameter up to 600m from the vent. Volcanic bombs are a significant volcanic hazard, and can cause severe injuries and death to people in an eruption zone. One such incident occurred at Galeras volcano in Colombia in 1993; six people near the summit were killed and several seriously injured by lava bombs when the volcano erupted unexpectedly. On July 16, 2018, 23 people were injured on a tour boat near the Kilauea volcano as a result of a basketball-sized lava bomb from the 2018 lower Puna eruption.[1][2]
On 10 March 2016, Kumar was manhandled and abused on the JNU campus by a man who accused him of being a "deshdrohi" (traitor). The man was later identified as Vikas Chaudhary of Gaziabad, who stated that he wanted to "teach Kanhaiya a lesson". Addressing students later in the day, Kumar said such incidents couldn't scare him. "You can kill me, you can silence me but you cannot scare me. But before you kill me, think about Rohith Vemula. When you killed one Rohith, several Rohiths came forward. If you kill someone else now, many others will stand up. This is all happening as part of a plan." 
Sarkar (Ronit Roy), who is seeking to take revenge on Ravan for his win in the election, stops the car. Sarkar thinks that there are only twins and says that whoever reveals their identity as Ravan will be killed and the other will be spared. Both Lava and Kusa pretend to be Ravan, and Sarkar shoots Lava. As Kusa is screaming Lava's name after he is shot, Sarkar thinks that Kusa is actually Ravan. A fight ensues to try and kill them both. Ravan comes and save Lava and Kusa by killing Sarkar and his goons, though he is hurt repeatedly and dies after the fight.
Lava domes grow by endogenic dome growth or exogenic dome growth. The former implies the enlargement of a lava dome due to the influx of magma into the dome interior, and the latter refers to discrete lobes of lava emplaced upon the surface of the dome. It is the high viscosity of the lava that prevents it from flowing far from the vent from which it extrudes, creating a dome-like shape of sticky lava that then cools slowly in-situ. Spines and lava flows are common extrusive products of lava domes. Domes may reach heights of several hundred meters, and can grow slowly and steadily for months (e.g. Unzen volcano), years (e.g. Soufrière Hills volcano), or even centuries (e.g. Mount Merapi volcano). The sides of these structures are composed of unstable rock debris. Due to the intermittent buildup of gas pressure, erupting domes can often experience episodes of explosive eruption over time. If part of a lava dome collapses and exposes pressurized magma, pyroclastic flows can be produced. Other hazards associated with lava domes are the destruction of property from lava flows, forest fires, and lahars triggered from re-mobilization of loose ash and debris. Lava domes are one of the principal structural features of many stratovolcanoes worldwide. Lava domes are prone to unusually dangerous explosions since they can contain rhyolitic silica-rich lava.
The Lava Cast Forest area includes cinder cones and various lava flows, with the youngest flow at 6,000 years old. It created casts of tree trunks when lava flowed around the trees creating molds. The molds can be vertical or horizontal, with some horizontal casts being up to 50 to 60 feet long. The molds were created when hot lava came into contact with trees, chilling the lava and created a protective covering, or mold. The trees then burnt completely out leaving a hollow interior. In some of the molds, the imprint of tree bark can be seen. Even ancient charcoal are still in some of the molds, and rings of annual tree growth can be seen in some. Originally, lumber company employees thought the molds were lava gas blowouts, until Walter J. Perry discovered the imprints of lava bark. Lava "drippings" found in the molds were created in freshly formed molds where lava dripped into the interior cavity.
A lava tube is a natural conduit formed by flowing lava which moves beneath the hardened surface of a lava flow. Tubes can drain lava from a volcano during an eruption, or can be extinct, meaning the lava flow has ceased, and the rock has cooled and left a long cave.
Kusa makes a deal with Simran that she has to act like Ravan's lover so that Kusa can get his money back and Simran can take her revenge on Ravan. Kusa tells the truth to Lava and Priya about his deal with Simran. Ravan overhears the plan and angrily tries to kill Lava and Kusa. Just then, he receives a call in which he is told that he is the frontrunner for winning the election. Lava and Kusa hatch a plan to bring their brother back with them. They do a play in which emotional breakdowns occur in trying to convince Ravan to be their brother again. Later, it is known that Ravan is trying to kill his brothers. The next day, Lava and Kusa drive a car that has a bomb attached to it. After they leave, Ravan reveals his plan to kill Lava and Kusa. The uncle begs Ravan to save Lava and Kusa, but Ravan does not listen. Then, the uncle asks Kaka to tell Ravan to not kill Lava and Kusa. Kusa tells the plan to Lava while they are driving, and they understand Ravan and decide to die.
He lectured: "You can go to India, and if you see a Hindu walking down the road you are allowed to kill him and take his money, is that clear, because there is no peace treaty between us." He also suggested that power plants could use the dead bodies of Hindus as fuel. "Jews," el-Faisal said, "should be killed ... as by Hitler." He said: "People with British passports, if you fly into Israel, it is easy. Fly into Israel and do whatever you can. If you die, you are up in paradise. How do you fight a Jew? You kill a Jew. In the case of Hindus, by bombing their businesses."
"Mafic" or basaltic lavas are typified by their high ferromagnesian content, and generally erupt at temperatures in excess of . Basaltic magma is high in iron and magnesium, and has relatively lower aluminium and silica, which taken together reduces the degree of polymerization within the melt. Owing to the higher temperatures, viscosities can be relatively low, although still thousands of times higher than water. The low degree of polymerization and high temperature favors chemical diffusion, so it is common to see large, well-formed phenocrysts within mafic lavas. Basalt lavas tend to produce low-profile shield volcanoes or "flood basalt fields", because the fluidal lava flows for long distances from the vent. The thickness of a basalt lava, particularly on a low slope, may be much greater than the thickness of the moving lava flow at any one time, because basalt lavas may "inflate" by supply of lava beneath a solidified crust. Most basalt lavas are of "ʻAʻā" or "pāhoehoe" types, rather than block lavas. Underwater, they can form pillow lavas, which are rather similar to entrail-type pahoehoe lavas on land.
A Firax is a Lava Monster that appears in the 2010 Power Miners line. Firax has a trans-orange carapace with black arms. Firax is the same orange color as Firox. Firax is included in two sets, as shown below. He seems to have scratches all over his fiery body. Also, Firax is said to be a Firox on fire. What happens when you put a Firox in super heat? You get an even trickier Firax to deal with!. This explains that Lava Monsters might be Rock Monsters somehow modified by high levels of volcanic heat to create Lava Monsters. Apparently, Firax likes to trap Power Miners and take their vehicles for joyrides- melting the seats in the process! They're mischievous like they're Firox cousins, and love trapping the power miners. Once they eat orange lava crystals, he can create a flood of lava in the chambers, much to the pleasure of the Infernox. He has a cousin and a brother, the Firox, a rock version of the Firax, and the Eruptorr, a larger version of the Firax.
Effusive eruptions involve a relatively gentle, steady outpouring of lava rather than large explosions. They can continue for years or decades, producing extensive fluid mafic lava flows. For example, Kīlauea on Hawaii has continued erupting from 1983 to the present, producing of lava covering more than . Despite their ostensibly benign appearance, effusive eruptions are no less dangerous than explosive ones: one of the largest effusive eruptions in history occurred in Iceland during the 1783–1784 eruption of Laki, which produced about of lava and killed one fifth of Iceland's population. The ensuing disruptions to the climate may also have killed millions elsewhere. Still larger were the Icelandic eruptions of Katla (the Eldgjá eruption) circa 934, with of erupted lava, and the Þjórsárhraun eruption of Bárðarbunga circa 6700 BC, with lava erupted, the latter being the largest effusive eruption in the last 10.000 years. The lava fields of these eruptions measure 565 km (Laki), 700 km (Eldgjá) and 950 km (Þjórsárhraun).
Hawaiian eruptions often begin as a line of vent eruptions along a fissure vent, a so-called "curtain of fire." These die down as the lava begins to concentrate at a few of the vents. Central-vent eruptions, meanwhile, often take the form of large lava fountains (both continuous and sporadic), which can reach heights of hundreds of meters or more. The particles from lava fountains usually cool in the air before hitting the ground, resulting in the accumulation of cindery scoria fragments; however, when the air is especially thick with clasts, they cannot cool off fast enough due to the surrounding heat, and hit the ground still hot, the accumulation of which forms spatter cones. If eruptive rates are high enough, they may even form splatter-fed lava flows. Hawaiian eruptions are often extremely long lived; Puʻu ʻŌʻō, a cinder cone of Kilauea, has been erupting continuously since 1983. Another Hawaiian volcanic feature is the formation of active lava lakes, self-maintaining pools of raw lava with a thin crust of semi-cooled rock; there are currently only 6 such lakes in the world, and the one at Kīlauea's Kupaianaha vent is one of them.
Flows from Hawaiian eruptions are basaltic, and can be divided into two types by their structural characteristics. Pahoehoe lava is a relatively smooth lava flow that can be billowy or ropey. They can move as one sheet, by the advancement of "toes," or as a snaking lava column. A'a lava flows are denser and more viscous than pahoehoe, and tend to move slower. Flows can measure thick. A'a flows are so thick that the outside layers cools into a rubble-like mass, insulating the still-hot interior and preventing it from cooling. A'a lava moves in a peculiar way—the front of the flow steepens due to pressure from behind until it breaks off, after which the general mass behind it moves forward. Pahoehoe lava can sometimes become A'a lava due to increasing viscosity or increasing rate of shear, but A'a lava never turns into pahoehoe flow.
The lava river sometimes ran through lava tubes before emerging again. The lava front had a height of up to 15 m. On 15 and 16 June, a branch of lava flow to the south of Melfell traveled over 1 km in 30 hours before slowing and stopping by 21 June, 7.8 km from the Lava Crater. The longest lava stream produced was 8 km long and stopped in Stóraskógsbotnar. A scientist filming one of the lava streams on 2 November was hit by a block of lava and was killed.
Each players can join alliances and progress the game by carrying out missions, assignments and other processes, such as research and construction. This creates might, a point-index each player has, which indicates their strength. The maximum level of the champion is 75. Once you reach level 75, you can participate in the altanis event. Which involves killing each other troops and to occupy the emperor seat. When you win the altanis event, you can earn reward. You can press the "help" button when you join an alliance to speed the progress of research, troop training, set or repair traps, and upgrading structures. You can help your alliance to upgrade the capital buildings, like the watchtower, regional walls, vault, mason guilt...By upgrading these structures, you are able to increase the strength of your alliance. The stronger the alliance is, the more capable you can attract strong players to join. Players can attack each other capitals when they do not put on their peace shield. You attack players for resources and killed their troops if you won. If your attack failed, you may lead to your troops killed in the defenders capitals and are not able to heal them, no resources could be get from the attack.
The Byaduk Caves, lava tubes from the volcanic eruption of Mount Napier, are nearby. You can also see extensive views of the lava flow at Harmans Valley and the tumuli lava blisters off Old Crushers Road. 
A lava flow is a moving outpouring of lava created during a non-explosive effusive eruption. When it has stopped moving, lava solidifies to form igneous rock. The term "lava flow" is commonly shortened to "lava". Although lava can be up to 100,000 times more viscous than water, lava can flow great distances before cooling and solidifying because of its thixotropic and shear thinning properties.
Flows from Hawaiian eruptions can be divided into two types by their structural characteristics: pāhoehoe lava which is relatively smooth and flows with a ropey texture, and ʻaʻā flows which are denser, more viscous (and thus slower moving) and blockier. These lava flows can be anywhere between thick. Aa lava flows move through pressure—the partially solidified front of the flow steepens due to the mass of flowing lava behind it until it breaks off, after which the general mass behind it moves forward. Though the top of the flow quickly cools down, the molten underbelly of the flow is buffered by the solidifying rock above it, and by this mechanism aa flows can sustain movement for long periods of time. Pāhoehoe flows, in contrast, move in more conventional sheets, or by the advancement of lava "toes" in snaking lava columns. Increasing viscosity on the part of the lava or shear stress on the part of local topography can morph a pāhoehoe flow into an a'a one, but the reverse never occurs.
There are different forms of effusive lava that can provide different hazards. Pahoehoe lava is smooth and ropy while Aa lava is blocky and hard. Lava flows normally follow the topography, sinking into depressions and valleys and flowing down the volcano. Lava flows will bury roads farmlands and other forms of personal property. This lava could destroy homes, cars, and lives standing in the way. Lava flows are dangerous, however, they are slow moving and this gives people time to respond and evacuate out of immediate areas. People can mitigate this hazard by not moving to valleys or depressed areas around a volcano.
Littoral cones not primary volcanic vents and distinguishing between a littoral cone and a primary vent can be difficult. A littoral cone forms when lava flows from land into water. Interaction between the water and the lava leads to steam explosions. These explosions throw lava fragments into the air; under favourable circumstances these fragments pile up on land and form a cone. This activity may resemble that of fire fountaining. Repeated phases of magma-water mixing lead to the formation of bedded deposits. The steam explosions can lead to the formation of Pele's hair. The forming lava flows need to be sufficiently large; the minimum size of lava flows that have formed such cones in Hawaii is . Of these, about 5-6% of their volume is converted to fragments. Usually littoral cones are formed by aa lava as their fragmented nature allows ideal water-lava interactions, but pahoehoe and intermediary lavas can also form littoral cones. Other properties such as the speed of the lava flow and the structure of the flow front also influence the formation of littoral cones. Larger lava flow rates generate larger cones. In some littoral cones on Hawaii that were formed by pahoehoe lava flows, the collapse of a lava bench and subsequent steam explosions formed the cones instead. Pyroclastic flows can also form littoral cones, one such cone has been found on Lombok and formed during the 1257 Samalas eruption.
Bomber Royale is a mode you can access though options (Ps4) and though Geode. You can pick up different power-ups, which have varying effects:
Lava bomb: turns your rubber bomb into lava.
Sticky bomb: a big chain bomb that creates a large explosion.
Bomb jump: does a super high bomb jump.
Heal: Heals the player a significant amount.
A lava bench is a volcanic landform with a horizontal surface raised above the level of the surrounding area. They are created when molten lava travels away from a volcanic vent and expands an old shoreline. This is the process that creates new land in the ocean that life can eventually grow on. The Hawaiian islands are an example of land that was formed this way, and the Big Island is currently still expanding due to lava benches. The Kilauea Volcano releases lava that flows down the slope of the volcano and eventually encounters the ocean; this lava flow hardens when it comes into contact with the significantly cooler water of the ocean and forms an unstable lava bench. Eventually, when the material beneath the lava bench stabilizes, it become stable land that has been added to the island. If a newly formed lava bench rests on sediments, it may pose hazards due to its extremely unstable structure. Oftentimes, these benches are so unstable that they collapse into the sea, exposing the water to the hot lava on the interior of the bench and releasing acres of land into the ocean. When the hot lava hits the water, violent explosions of steam can shoot large rocks and molten lava up to inland. These collapses are extremely dangerous because they can happen without warning, and anyone or anything on the bench will be caught in the collapse. For safety, people are advised not to walk on lava benches because of their unstable nature, and they must maintain a safe distance from the lava bench.
In 1993, a photographer attempting to take pictures of a lava ocean entry died, and several tourists were injured, when a lava bench collapsed. In 2000, two people were found dead near a lava ocean entry from Kīlauea, likely killed by laze. Sulfur Dioxide emissions can also be fatal, especially to people suffering from respiratory ailments. In 2018 lava spatter from Kīlauea broke a man's leg, and another 23 people on a tour boat were injured by a steam explosion at a lava ocean entry from the same eruption.
Sullivan Bay is especially fascinating for those who are interested in geology and volcanology. You can walk over the uneroded, black lava flow covered with lava bubbles and tree-trunk molds in the surface. There are two small beaches where turtles come for nesting.
Lava Men have a high resistance to extreme heat and flame. They continually generate intense heat from their bodies and can increase the amount of heat at will, enough to be able to melt a weapon in its vicinity. They have a mystical ability to cause large amounts of volcanic ash to appear, seemingly from nowhere, and to transform metal into ash. They also have immunity to aging. Some Lava Men can mystically transform themselves into giants composed of hardened lava. Some Lava Men can mystically command molten lava to do their bidding by performing a ritual prayer to the demons they worship. The golden Lava Men can transform their shapes, and in doing so, even merge their bodies with one another. They once formed themselves into a large sphere that could defy gravity. Jinku has mystically created non-sentient Lava Men which possess the superhuman powers of the real Lava Men. Lava Men had unusually acute hearing and night vision to enable them to function more easily in the darkness of Subterranea.
Several different mechanisms have been invoked to explain the genesis of lava balloons. Water that penetrates the lava can boil and the resulting vapours can inflate the balloons and make them float, although for Terceira a non-water gas composition has been inferred. They are usually observed when lava flows enter the sea. They appear to form when water is trapped in lava as it flows onto a beach with waves or enters lava tubes; in the latter case, entrained water can be transported through the tube and eventually end up in developing pillow lavas which are rendered buoyant by water vapour bubbles.