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What else can I help you with?
Which caves do you go through on graal classic to find the witch?
When u enter the forest there's a white monster guy who talks to u about the witch. Go thru any Cave. If you enter a new place where there is no monster, ur on the right track. If u see the monster again u have to start a different pattern coz u got it wrong. Keep going like this and u should end up at the witch's place. Talk to her and she will give u the rat spell. Hope I helped! Rubz:) (that's my name on graal)
Who was the first person to die exploring caves?
Frankly, no-one really knows because it depends on your criteria and the records available. A few intrepid souls tried to explore caves back in the 17th, even 16th Century; and metal-ore miners broke into caves from their mines, from time to time. It's entirely possible some of these people met their end underground, but mining was so dangerous it would probably have been recorded as a mining accident, and then rather scantily. Of modern explorers, in caves to explore out of curiosity, I suppose you could count a 19C quarryman called Joe Plumley who died in a vertical cave the quarry had opened up in Burrington Coombe (Somerset, SW England). None of the team were cavers as we would know then now. His work-mates lowered him on a rope but managed to break his neck in trying to pull him back up. The hole was covered over and is now lost, but was near the geological feature now known by the famous hymn that it inspired, "Rock of Ages".
Do caves change?
Yes. Sticking to the vast majority, which are limestone karst features,any cave passage carrying a stream is still developing. Changes in the region's hydrology or in sea-levels can alter the cave's water flows, e.g. drowning passagespreviously partly air-filled, or bringing about rejuventation processes and effects. Floods may build up sediment deposits in parts of the cave. When passages lose their formative streams entirely they can start to decay as percolation waterweakens roof and wall rock and bring about collapses that can fill the passage. Such collpases can occur at any time in a mature cave, but flowing water gradually removes the fallen material. (Note: to scotch a common misunderstanding, collapses do not form caves, though they may create a void above that already existing for the roof tofall into.) Calcium carbonate dissolved in percolation water may be deposited to form stalactites, stalagmites and related formations. Isostatic rebound after the cave's region has been de-glaciated at the end of an Ice Age glacial phase may modify the cave or influence its development in various more subtle ways. River or glacial valleys may cut across or below a cave, removing its feed water as well as removing parts of the passages. Caves in coastal areas may be destroyed by general cliff retreat. Eventually general lowering of the landscape will breach and destroy at least shallow-lying cave passages.
How caves are made?
by water and air combining to build pressure +++ Tht'as not correct and it's hard to see what the respondent had in mind. Most caves are formed in limestone by naturally-acidic groundwater dissolving it as it passes through the joints, bedding-planes and faults in the rock mass.
How are caves built?
The vast majority of the worl'd caves are in limestone. How Caves Form in Limestone That is such a common question on ‘Answers’ I wrote this single reply! The technical terms are introduced by capital initials. Most of the world’s caves are in Limestone. Caves need three materials: a soluble rock like Limestone or Gypsum, water and Carbon-dioxide (CO2). Their host limestone also needs to be of appropriate physical structure and raised into hills, then subjected to reasonably consistent precipitation for many tens or hundreds of thousands of years. Limestone is a sedimentary rock of which the world’s greater proportion was laid down in warm, relatively shallow, seas. The rock was laid in horizontal layers – Beds – separated by Bedding-planes which generally reflect geologically-brief changes in the environment. The suite of beds is known as a Formation, generally named after its “type area”. Later continental uplift (tectonic processes) raise the formation along with its underlying rocks, usually tilting and folding it to at least some extent in the process. Since most rocks are brittle they cannot take much stress, and limestone beds crack into grids of fine fractures called Joints. The uplift and folding often also causes Faulting – major breaks with the rock mass one side of the Fault Plane being raised, lowered or moved horizontally past that on the opposite side. (Note: Plane – the “Fault Line” sometimes misused as a political metaphor is that of the fault-plane cutting the land surface.) Now we have the hills, next we need rain-water that has absorbed atmospheric CO2 to create Carbonic Acid (weak, natural soda water in fact!). It may be augmented by acids from the soil, too. This solvent permeates through all those joints, bedding-planes and faults; flowing very, very slowly under considerable pressure applied by its depth, from its sinks on the surface to its springs at the base of the formation. In doing so, it dissolves the limestone (chemical weathering), creating meshes of tiny micro-conduits that over many tens of thousands of years coalesce and capture each other to form cave passages. Once this happens, the rate of erosion can increase – though still to perhaps only a few millimetres per thousand years under generally temperate climates. A cave, or a series within a cave system, that still carries its formative stream is called “Active”, and is still being developed. Surface changes such as the valley floor being lowered by erosion, or down-cutting within the cave by its stream, changes the water’s route and the original, now dried-out, stream-way is called “Fossil” or “Abandoned”. Such passages may be filled with silt left by floods as the main flow gradually abandons them; or may become richly decorated with Speleothems – calcite deposits such as stalactites and stalagmites precipitated from ground-water still oozing through the joints in the limestone above the cave. In time such passages may start to break down as there is no stream to dissolve away slabs falling from the roof as permeating ground-water attacks the rock above. In the end, surface lowering of the landscape as a whole, breaches and destroys the cave. Nothing is permanent in Nature! Caves in limestone are also parts of Karst Landscape. i.e. a landscape developed by the dissolution of limestone, giving surface features like Dolines, Limestone Pavement, and in the tropics, distinctive hills such as those represented in Chinese Willow-pattern images. ‘Karst’ is from the Slavic word ‘Kras’, the name for its world type-area. @@@@@ The above is purely an introduction to a vastly more complex and subtle series of processes, of course, and you need to refer to appropriate text-books on geology and cave studies to learn them. The scientific study of caves is Speleology – embracing geology, hydrology, biology, archaeology and other disciplines. Simply visiting caves to enjoy them for their scenery and the physical and mental challenges they present, is called Caving, though you can’t study a cave unless you can negotiate its obstacles. The enthusiasts are simply Cavers throughout the English-speaking world –you see “spelunkers” sometimes on ‘Answers’ but it's an old slang word not found in caving literature.. .
Why are the Mongol caves called caves of thousands?
cave had 4 trees the end
Who is powerful this the end secret?
That is Jommer meaning people can't see from God, then end secret more than top secret.
When did Think Secret end?
Think Secret ended in 2007.
When was End of Green - band - created?
End of Green - band - was created in 1992.
When did Deadly Secret end?
Deadly Secret ended on 1989-07-07.
When did Secret Agent X end?
Secret Agent X ended in 1939.
When did The Secret Lovers end?
The Secret Lovers ended on 2005-11-01.
When did The Secret Service end?
The Secret Service ended on 1969-12-14.
When did Secret Cabaret end?
Secret Cabaret ended on 1992-02-19.
When did Mission Top Secret end?
Mission Top Secret ended in 1995.
When did Secret of the Heart end?
Secret of the Heart ended on 1998-05-10.
When did The Secret Storm end?
The Secret Storm ended on 1974-02-08.
