Welded tuff is forms when the ash deposited is so hot that it is still partially molten. The still liquid component then cools, fusing the deposit into a single solid mass. Cemented tuff becomes bound together from processes similar to those that form ordinary sedimentary rocks. Grains are bound together under pressure as minerals dissolved in water crystallize.
Yes, welded tuff and cemented tuff can result from the same volcano. Welded tuff forms when volcanic ash and debris are ejected at high temperatures and fuse together upon landing, forming a welded rock. Cemented tuff forms when loose volcanic ash and debris accumulate and are later compacted and cemented together. Both processes can occur in the same volcanic eruption, resulting in different types of tuff.
The grain size of welded tuff can vary depending on the specific conditions under which it was formed. Generally, welded tuff has a fine-grained to medium-grained texture due to the rapid cooling and solidification of the volcanic ash during welding. This process can result in a range of grain sizes, typically ranging from less than 1 millimeter to several millimeters in size.
Tuff is not always foliated. Foliation refers to the alignment of minerals in a rock due to pressure during metamorphism, whereas tuff is a type of rock made of volcanic ash that has been cemented together. Tuff typically does not exhibit foliation unless it has been subjected to intense pressure and heat during metamorphism.
The mountain built up by a volcano is essentially a pile of material that has erupted from it such as lava, ash, and welded tuff.
Tuff rocks are formed from volcanic ash and debris that have been compacted and cemented together. They are usually light in color and can contain fragments of volcanic glass, crystals, and other minerals. Tuff rocks are commonly found in areas with past volcanic activity and are often used for construction purposes due to their durability.
Yes, welded tuff and cemented tuff can result from the same volcano. Welded tuff forms when volcanic ash and debris are ejected at high temperatures and fuse together upon landing, forming a welded rock. Cemented tuff forms when loose volcanic ash and debris accumulate and are later compacted and cemented together. Both processes can occur in the same volcanic eruption, resulting in different types of tuff.
Welded tuff typically contains minerals such as quartz, feldspar, biotite, and hornblende. The exact mineral composition can vary depending on the specific geologic setting where the welded tuff formed.
Squashed pumice blobs in a welded tuff .
== == Rhyolite, basalt, pumice, obsidian, andesite, dacite, tuff, welded tuff, scoria.
Yes, tuff is an igneous rock. It is formed from volcanic ash and other volcanic debris that has been compacted and cemented together.
The grain size of welded tuff can vary depending on the specific conditions under which it was formed. Generally, welded tuff has a fine-grained to medium-grained texture due to the rapid cooling and solidification of the volcanic ash during welding. This process can result in a range of grain sizes, typically ranging from less than 1 millimeter to several millimeters in size.
Sandstone is a sedimentary rock formed when sand weathered from preexisting rock is cemented together. Tuff is an igneous rock formed from volcanic ash.
One characteristic that can help distinguish between sandstone and tuff is their composition. Sandstone is primarily composed of sand-sized mineral grains cemented together, while tuff is composed of volcanic ash and tephra fragments that have been compacted and cemented together. Tuff may also exhibit a finer texture due to the smaller size of volcanic particles compared to sand grains in sandstone.
Tuff is not always foliated. Foliation refers to the alignment of minerals in a rock due to pressure during metamorphism, whereas tuff is a type of rock made of volcanic ash that has been cemented together. Tuff typically does not exhibit foliation unless it has been subjected to intense pressure and heat during metamorphism.
== == Rhyolite, basalt, pumice, obsidian, andesite, dacite, tuff, welded tuff, scoria.
The mountain built up by a volcano is essentially a pile of material that has erupted from it such as lava, ash, and welded tuff.
If the process of cementation is volcanic you get a "tuff". If the cementation post sedimentation of rock clasts you get a sedimentary rock which may be a breccia or a conglomerate.