Current climate models base their operations on how much CO2 will be emitted in the future. Considering the actual trend, most models shows a rise in temperature in between 4/6<span> centigrade. Considerable change are possible with significace changes in the emission of co2.</span>
Earthquakes can occur at depths of over 700 km.
Explanation:
The earthquakes are a natural hazard which is associated with boundaries of the tectonic plates. The majority of the earthquakes occur at convergent and transforming plate boundaries. The reason as to why the earthquakes occur at these places is because of the pressure between the colliding or sliding plates, where the crust cracks and during the adjustment the force created is manifested with strong vibrations.
In general, the earthquakes occur at depths between 20 and 50 km, which is usually the depth where the plates create the most pressure upon each other. That is not to say that that is the only range where earthquakes occur, as they can occur anywhere from the surface of Earth and down to 800 km in depth. With other words, the earthquakes occur anywhere from the top of the lithosphere to the top of the astenosphere. Earthquake hot-spots are:
- Ring of Fire
- Mediterranean
- northern Turkey
- western Southwest Asia
Learn more about the astenosphere and lithosphere brainly.com/question/9259535
#learnwithBrainly
Active solar energy is solar panels or other mechanical energy systems from the sun, while passive are things like the sun heating your house from south facing windows (greenhouse affect).
Answer:
Para salvar el ecosistema.
Explicación:
La comunidad decide combinar actividades agrícolas con proyectos como el centro de ecoturismo para salvar el ecosistema de actividades humanas como la agricultura y la minería. Con la ayuda del ecoturismo podemos salvar el hábitat de diferentes organismos y hacer que el ecosistema sea más saludable. Entonces, para salvar los organismos y hacer un ecosistema saludable, la comunidad combina las actividades agrícolas con el ecoturismo.
