convergent boundary of two continental crusts
The erosion of a mountain range would primarily lead to the formation of sedimentary rocks. These rocks are formed from the accumulation and compaction of sediments that erode from the mountains and are deposited in layers over time. Magma could also be formed if the eroded sediments are subjected to high temperatures and pressures deep within the Earth, leading to the formation of igneous rocks. Metamorphic rocks could form from existing rocks within the mountain range that undergo changes due to heat and pressure during the mountain-building process.
A sedimentary rock could undergo further compaction and cementation to become a metamorphic rock due to increased heat and pressure. It could also melt and solidify into an igneous rock through volcanic activity. If exposed to erosion, it could break down into sediments and form new sedimentary rocks through deposition and lithification.
Sedimentary rocks form from the accumulation of sediment such as sand, silt, or clay. For sedimentary rocks to form, there must be pre-existing rocks that weather and erode to produce sediment. Therefore, sedimentary rocks could not have been the first rocks on Earth as they require the presence of older rocks to form.
Well, isn't that just a happy little question! A geologist can tell that a mountain chain was formed by the folding of rock layers by looking at the patterns and angles of the rocks. When rocks are folded, they create unique shapes and structures that help geologists understand how the mountains were formed. It's like nature's way of leaving us clues to unravel its beautiful mysteries.
Landforms that could be created at convergent boundaries would include: volcanoes, mountains, trenches, volcanic islands, and even deserts could result from the effects of converging boundaries.the landforms are mountains
The Pyrenees and the Alps could be the answer.
This mountain is in Turkey, and it is said that Noah's ark could be there.
Another term for diverting boundary could be a redirecting boundary or a deflecting boundary.
They are mostly found in Sedimentary Rocks
it could have sand in it
A natural boundary that is not a body of water could be formed by physical features such as mountains, deserts, or forests. These features act as barriers and define the limits of a region or country.
Natural boundaries can include landforms like rivers, mountains, and oceans that divide territories or regions. These boundaries are formed by natural features of the Earth's landscape and can be used to separate countries, states, or other geographical areas.
The sedimentary rock could, for instance, be found on a mountain and be crushed to dust by a huge ice glacier moving over it. The resulting dusty (or bigger) rock particles much later reach the lower end of the glacier and are washed into a lake or into the ocean where they sink to the bottom. Wait, oh, maybe half a million years, and the particles that sank to the bottom might turn into another sedimentary rock, altogether.
The erosion of a mountain range would primarily lead to the formation of sedimentary rocks. These rocks are formed from the accumulation and compaction of sediments that erode from the mountains and are deposited in layers over time. Magma could also be formed if the eroded sediments are subjected to high temperatures and pressures deep within the Earth, leading to the formation of igneous rocks. Metamorphic rocks could form from existing rocks within the mountain range that undergo changes due to heat and pressure during the mountain-building process.
A sedimentary rock could undergo further compaction and cementation to become a metamorphic rock due to increased heat and pressure. It could also melt and solidify into an igneous rock through volcanic activity. If exposed to erosion, it could break down into sediments and form new sedimentary rocks through deposition and lithification.
Yes, millions of years ago, Australia, North America, and other continents were part of a supercontinent called Pangaea. The Appalachian Mountains in the US and the Great Dividing Range in Australia were once connected as part of a larger mountain chain.
Sedimentary rocks, and foliated metamorphic rocks form in layers.