ഭൂമിയിലെ കല്ലുകൾ എങ്ങനെ ഉണ്ടാവുന്നു? | Rock fromation and types explained in Malayalam - video Dailymotion

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ഭൂമിയിലെ കല്ലുകൾ എങ്ങനെ ഉണ്ടാവുന്നു? ഏതൊക്കെ തരം കല്ലുകളാണ് ഭൂമിയിൽ ഉള്ളത് എന്നീ കാര്യങ്ങൾ വിശദീകരിക്കുന്ന വീഡിയോ. #rocks #geology #science

Transcript

00:00Good afternoon, I'm here with you.

00:04I'm dear to me, I'm here with you.

00:08How many times we learn these lessons are going to teach.

00:11We learn these lessons with you.

00:15I don't know how many new lessons are going to teach the lesson.

00:21Regarding these lessons, we learn how many new lessons are going to teach.

00:27That's why the trees are so simple and scientific.

00:33The trees are not living, minerals, and solid bodies are so simple.

00:39In this deep-eyed, we have many trees.

00:42That's why the trees are so small.

00:46That's why the trees are so small.

00:48That's why the trees are so small.

00:52The trees are very effective.

01:02That are the trees of science.

01:08The trees are very common.

01:11You should see outside of the forest.

01:15When we come to the forest, we have to see the trees in this forest.

01:19we are not now corresponding with the shape, color and texture

01:24formation is not tied

01:27as we don't have an emotional pattern

01:30not when these patterns are not set to present

01:34we are talking about the patterns of evolution

01:38as well as all the patterns of evolution

01:41this is the ageological activity

01:43and as I know the patterns of the patterns of

01:47This is an example of a rock cycle of rock, rock, rock, rock, rock, rock and rock

02:17this is the term and has a meaning

02:22the ignition is used as fire

02:27that is the ignition rock

02:28the ignition is used as the ignition rock

02:33let's just simplify it

02:36if we have to prepare our own water

02:40we have to prepare our own water

02:43we have to prepare our own water

02:46We have to use lava and magma.

02:48This lava and magma is basically one of the things we can use.

02:51I think it's very interesting.

02:53What we have to use is we have to use the rock.

02:56We have to use the rock and melt.

03:01We have to use the rock.

03:03We have to use the rock and melt.

03:06That's the thing we have to use lava.

03:09Because when we have to use lava and magma,

03:11we have to use the rock and melt.

03:14Lava, Magma and the two different things are different.

03:19In this case, we have a magma and this is the Lava and Magma.

03:27In this case, we have the Lava and Magma, we have the Ignis rocks.

03:32There are some examples of Basalt.

03:34Basalt is a place where we are going to go to Mumbai and Istanbul.

03:44This is the example of a granite and an example of the two ignees rocks

03:49This is the example of an ignees rock

03:53This is the example of a granite

03:57This is the form of a granite

04:02This is the basalt

04:04This is the name of ignees rocks

04:11It's intrusive and extrusive, and there are two categories of ignees rocks.

04:16We have two types of ignees rocks.

04:20Extrusive and extrusive, we have to walk in the exit.

04:24Exit, exterior and exterior meaning.

04:27It's an extrusive walk.

04:28It's an extrusive walk.

04:33It's an extrusive ignees rocks.

04:38It's an extrusive walk.

04:45It's an extrusive walk.

04:51It's an extrusive walk.

04:59This type of walk is a sedimentary walk.

05:02sedimentary rocks are the same as we are talking about the other side of the road

05:08sedimentation and sedimentary and walk in our daily life

05:16sedimentation process is very symbolic

05:19example of the example of the road

05:22Now that we're in a glass of water, we'll take it in a little bit

05:33We're going to have to take a few more

05:36We're going to have to take a few more

05:39We'll have to take a few particles in this area

05:44We can do sedimentation

05:47The sedimentary rocks are very important in our water bodys

05:51There are a lot of things in our water bodys

05:54There are many particles in our water bodys

05:59There are a lot of things in our water bodys

06:03Over time, there are a few days

06:05There are a lot of sediment that can be used

06:09We have a lot of pressure

06:14There are a lot of people in our water bodys

06:18In this area, we will have a lot of pressure

06:22We can press this rock and we can see this rock

06:27That is sedimentary rock

06:32We can see sedimentary rock

06:35We will be interested in the first fossil

06:39We have to make the first fossil formation

06:42That's why we used sedimentary rocks

06:46What are we doing here?

06:48There are lots of things

06:49We use limestone trees

06:51We use geothermal trees to form

06:55First of all, we use the sedimentary trees to form

07:01We use sedimentation to form

07:04We don't have to go to the river

07:07We have to go to the gulf

07:09We have to build a sandstone and build a new formation

07:13We build a shale, and we have to build a sandstone

07:18This is a sedimentary rock

07:20For the sedimentary rock as well

07:24For various types of rock, there is a sandstone

07:26and there is a sedimentary rock

07:28These are sedimentary rock

07:32We have to build a sedimentary rock

07:35We are talking about the two of these and the other types of new types

07:38We have some ideas

07:41When we talk about the metamorphic rock, we are thinking about the same idea

07:45Metamorphic rock is known, because we are talking about the metamorphic rock

07:49Let's explain about the rock that already exists

07:55We are learning the root of the rocks

07:59We are learning the root of the ignex rock and sediment rock

08:01This is already the root of the formation

08:03The geological activity, the area of the ground, is the deformation of the ground.

08:11That's why we call it the granite deformation.

08:16The conditions are very different.

08:19Every time, the conditions are very different.

08:23The conditions are very different, very different pressure.

08:26Already in the end of the rocks,

08:28the ground is the metamorphism.

08:32These trees are stretched out and stretched out and stretched out with the composition, texture, etc.

08:41That's why we have metamorphic rocks.

08:43That's why the rocks are already intact.

08:48I call it rock cycle.

08:51That's why the trees are very important.

08:54We have a lot of trees.

08:56Now we have one example.

08:58We have a sandstone.

09:00The name is a sedimentary stone

09:03The formation of the sandstone of the formation of the sandstone

09:07That or sediment is sediment

09:11The pressure is one of the references

09:13It is a sandstone

09:16Sand particles are mainly silica

09:20It is the same sand particles

09:23So it's set into the silica

09:24This is the sand particles

09:28This is actually the magma. This is the silicate formation of the silicate.

09:35One of the things that the igneous formation has to be built in the sandstone.

09:46This is the metamorphism. This is the metamorphic rock.

09:56You can work out the rock cycle, you can continue to work out, you can continue to work in a process

10:01We call it a metamorphic rock, it's a great deal

10:06It's not a rock cycle

10:08This is a metamorphic rock, it's a great geological activity

10:13It's a great deal, it's a great deal

10:17It's a great deal, it's a great deal

10:19It's a great deal

10:23It's a great deal, it's a great deal in making snow and gonna cry

10:34It's significant

10:35It's acceptable

10:37It's spectacular

10:40To add the rock cycle

10:45You already had a pictures

10:49This is a marble, which is a metamorphic rock, which is a metamorphic rock, which is a limestone, which is a limestone.

11:04This is a sedimentary rock site.

11:14This is a metamorphic rock site.

11:23This is a metamorphic rock site.

11:35This is a metamorphic rock site.

11:39This is a metamorphic rock site.

11:46This is a metamorphic rock site.

11:55This is a metamorphic rock site.

11:58This is a metamorphic rock site.

ഭൂമിയിലെ കല്ലുകൾ എങ്ങനെ ഉണ്ടാവുന്നു? | Rock fromation and types explained in Malayalam

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