greater dependence on technology as a means of survival
Explanation:
One of the things that can occur as a result of technological progress is the greater dependence on technology as a means of survival.
- Technology is simply the practical application of science. It is science at work.
- Improved technology shifts attention to the deployment of innovations as life hacks.
- Robots nowadays have become errand boys and are gradually disrupting the ways in which work is done.
- Technology will reduce the time spent relating with others as people will prefer social media and games.
- Our world will become synthetic and not based on agriculture again if technology growth continues to accelerate.
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Wind carries heat, moisture, pollutants, and pollen to new areas. Many daily weather patterns depend on wind. A coastal region, for instance, undergoes changes in wind direction daily. The sun heats the land more quickly than the water.
Thank you for posting your question here at brainly. Among the chocies provided above, the quechua still present in modern-day south america because it <span>was imposed on every tribe conquered by the Incas. I hope the answer will help you. </span>
Answer:
The continuous process in which hot, molten material coming to the surface of the Earth from the interior forms igneous rocks, which are then broken down by weathering to create soil and sedimentary rocks.
Lava flows are the least hazardous of all processes in volcanic eruptions. How far a lava flow travels depends on the flows temperature, silica content, extrusion rate, and slope of the land. A cold lava flow will not travel far and neither will one that has a high silica content. Such a flow would have a high viscosity<span> (a high resistance to flow). A basalt flow like those in Hawai'i have low silica contents and low viscosities so they can flow long distances. Such a flow can move as far away as 4 km from its source and have a thickness of 10 m (Bryant, 1991). These flows can move at rates of several kilometers per hour (Scott, 1989). </span><span>More silica-rich flows can move as far away as 1.3 km from their sources and have thicknesses of 100 m (Bryant, 1991). These flows can move at rates of a few to hundreds of meters per hour (Scott, 1989). If a lava flow is channelized or travels underground in a lava tube then the distance it travels is greatly extended.</span>
