@singl.musicv: Ni Si Quiera - Antonio Cartagena #salsa #antoniocartagena #nisiquiera #🎧 #letrasdecanciones #fyp #parati #viral #siguiendo #musica #music #lyrics #dedicar #foryoupage #apoyo

🎧ꜱɪɴɢʟ.ᴍᴜꜱɪᴄᴠ🎶
🎧ꜱɪɴɢʟ.ᴍᴜꜱɪᴄᴠ🎶
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Region: CO
Wednesday 27 March 2024 20:19:27 GMT
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brayanfranco72
Brayan Franco :
"Qué nisiquiera dejaste que el sudor de mi cuerpo, secara en el tuyoooo"
2024-06-21 01:07:36
9
anairoby08
🍀Nairoby08🍀 :
Uf esta salsa duele 💔
2024-07-17 01:25:34
5
davidsalinasg38
Guerrero_Sayayin_BSC ❤️‍🔥 🔥 :
ganas de llorar 😕😕
2024-05-17 12:30:12
17
katito.mc
Katito🖤Moon :
🥺no hay otra oportunidad 😡😡😮‍💨
2024-07-11 02:25:25
4
jesusaguirre9470
RICARDO AB :
NI SIQUIERA 🎵
2024-08-31 15:54:56
0
melizhiitahlopez2416
Melizhiitah López :
Mi Canción Favorita 🥺♥️
2024-04-19 02:27:19
18
patostar77
Patricio Fuentes :
Todo lo que se va es para mejor!!!! Mejor es esta canción ❤️❤️❤️
2024-05-20 14:19:28
9
yesicarrasco07
Yesi Carrasco :
duele aún 💔
2024-04-26 00:47:04
12
edna.cerra3
Edna Cerra :
Hermosa salsa me fascina gracias 😍❤️❤️❤️😍🇨🇴
2024-04-28 21:42:17
4
palomagarcia768
Dios hasido bueno :
mi cancion favorita🥰❤
2024-05-17 12:01:16
5
untipo_serio70
Un tipo serio 70 :
dónde estaba yo metido que no había escuchado este tremendo tema? espectacular tema🥰🥰🥰 gracias a Dios mi corazón está sano y libre. viva la salsa mi gente bella 🔥🔥
2024-09-15 05:41:02
0
laura.rondon07
María Laura Rondón :
me reencanta está canción ❤️❤️🫶🫶❤️❤️
2024-05-14 02:04:28
2
ireibys01
iré❤️ :
amo esta canción
2024-04-14 02:33:49
7
roxanita.h3
Roxi🖤 :
me paso tal cual la canción 😭
2024-06-29 15:09:58
1
dnl.lax
dnl.lax :
Salsero Peruano p👌🔥
2024-06-27 04:13:53
1
amandareyes090
amandareyes090 :
uffff hermoso tema
2024-04-20 18:09:22
3
bettyhidalgo70
bettyhidalgo70 :
linda salsita 😞😞😞
2024-06-23 21:42:18
2
corina.barreto
corinabarreto760 :
Unas de mis favoritas ❤
2024-04-17 04:15:16
5
apolinargonzalez56
apolinargonzalez56 :
y los 2lo quisimos asi...
2024-04-20 13:17:56
3
ruijvg
Dani :
Dueles aún M
2024-05-19 20:56:49
1
natfal.24_96
Natividad Falcón :
canciones que llegan al 💔
2024-05-24 02:44:38
3
escalantevelasquez1
tu blanquita, 🥹❤️‍🩹🐷🐷 :
mi canción favorita 😍
2024-04-21 19:47:49
2
user9539805836931
user9539805836931 :
🤗❤🙏que triste verdad
2024-07-02 22:36:39
1
eduardomujica927
Eduardo Mujica :
tremenda canción
2024-04-29 19:06:59
1
luis.david.castro72
Tibisay julio morales :
temazo 🍻🍻🍻🍻
2024-06-28 12:15:17
1
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The solid, outermost shell of the Earth is called the lithosphere. This includes the crust and the upper, solid part of the mantle. On average, it is 50 km thick beneath the oceans and 70-100 km thick under the continents. The continental lithosphere and the oceanic lithosphere also differ in composition. The continental crust floats on the asthenosphere, the viscous upper part of the mantle that lies beneath the lithosphere The movement of the lithosphere, which can be observed in a great number of places, is the reason behind earthquakes and volcanic activity. These movements do not take place randomly, but along longitudinal belts. Volcanic activity and earthquakes mostly occur at the edge of continents, in oceanic island arcs, oceanic trenches, and mid-ocean ridges. These motion processes mark the boundaries of tectonic plates. The lithosphere is not uniform, it is broken up into tectonic plates of different sizes. Today, we know of seven major tectonic plates and a number of other, smaller ones, which all move in relation to each other. The seven major tectonic plates are: the African plate, the Eurasian plate, the North American plate, the South American plate, the Pacific plate, the Indo-Australian plate and the Antarctic plate. The theory that describes the motion of the lithosphere is called plate tectonics. There are three types of tectonic movement: convergence, divergence and subduction Mid-ocean ridges represent an example of divergent plate boundaries. As magma that is, molten rock, rises from the asthenosphere and penetrates the oceanic lithosphere, it reaches the surface, where it cools down and solidifies, forming new lithosphere at the edge of the crack. That is how mid-ocean ridges are formed.
The solid, outermost shell of the Earth is called the lithosphere. This includes the crust and the upper, solid part of the mantle. On average, it is 50 km thick beneath the oceans and 70-100 km thick under the continents. The continental lithosphere and the oceanic lithosphere also differ in composition. The continental crust floats on the asthenosphere, the viscous upper part of the mantle that lies beneath the lithosphere The movement of the lithosphere, which can be observed in a great number of places, is the reason behind earthquakes and volcanic activity. These movements do not take place randomly, but along longitudinal belts. Volcanic activity and earthquakes mostly occur at the edge of continents, in oceanic island arcs, oceanic trenches, and mid-ocean ridges. These motion processes mark the boundaries of tectonic plates. The lithosphere is not uniform, it is broken up into tectonic plates of different sizes. Today, we know of seven major tectonic plates and a number of other, smaller ones, which all move in relation to each other. The seven major tectonic plates are: the African plate, the Eurasian plate, the North American plate, the South American plate, the Pacific plate, the Indo-Australian plate and the Antarctic plate. The theory that describes the motion of the lithosphere is called plate tectonics. There are three types of tectonic movement: convergence, divergence and subduction Mid-ocean ridges represent an example of divergent plate boundaries. As magma that is, molten rock, rises from the asthenosphere and penetrates the oceanic lithosphere, it reaches the surface, where it cools down and solidifies, forming new lithosphere at the edge of the crack. That is how mid-ocean ridges are formed.

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