Small rivers and streams around the Colorado River drain into the river and eventually to the ocean.
Explanation:
The Colorado River is a major river in the United States. This river runs through the southwestern part of the country, mostly through semi-arid and arid areas. The Colorado River starts its flow in the state of Colorado, continues its flow through Utah and Arizona, then leaving the United States and having a short span in Mexico until it enters the Gulf of Mexico. The river is fed with water through numerous smaller rivers and streams, which makes it larger and larger gradually, and all that water enters the ocean at the end.
- Some of the tributaries of the Colorado River and Green, San Juan, Little Colorado, and Gila.
- All of these rivers have their own watersheds, all of which are small, but they all together fall into the large watershed of the Colorado River.
- The Colorado River is very important river in the region, especially when it comes to agriculture.
- The most famous thing about the Colorado River is that in one part of it is located the world famous Grand Canyon, which is a major tourist attraction.
Learn more about the Grand Canyon brainly.com/question/3157117 #learnwithBrainly
Answer:
Extensional faulting observed in southwestern Mexico has been related to the incipient rifting of the Jalisco block from the Mexican mainland since the Pliocene. On the basis of new structural and geophysical data, we propose that (1) the continental boundaries of the Jalisco block are ancient structures reactivated since the Pliocene at a low (<1 mm/yr) rate of deformation, and (2) Pliocene-Quaternary extensional faulting at the edges of Jalisco block is a basement-controlled intraplate deformation related to plate boundary forces rather than to active continental rifting. The Jalisco block boundaries first developed in response to the uplift of the Puerto Vallarta batholith in pre-Neogene time and underwent a complex contractile deformation before the Pliocene. During Pliocene-Quaternary times north-northeast extension reactivated the northern boundary, forming the Tepic-Zacoalco rift, whereas east-southeast extension formed the northern Colima rift. South of the Colima volcano, active extension is found only west of the so-called southern Colima rift and partly reactivates old northeast-trending basement faults. The parallelism between the subducted Rivera-Cocos plate boundary zone and the eastern neotectonic boundary of the Jalisco block supports eastsoutheastward motion of the southern Mexican blocks induced by the differential motion and oblique subduction of the Cocos and Rivera plates. On the other hand, we envisage Pliocene-Quaternary extension along the northern boundary as an upper-plate response to the low convergence rate and the steep subduction angle of the Rivera plate.
Answer:
Tropic of Capricorn
Explanation:
The Tropic of Capricorn which is also known as the Southern tropic is the furthest direction south of the Equator where the Sun can be located vertically overhead as it the location of the subsolar point at the southern solstice. In the middle of June, the Tropic of Capricorn reaches a position of an angle of 90° below the horizon at midnight
The latitude of the Tropic of Capricorn is 23°26'11.8'' south of the Equator, while the location of the Tropic of Capricorn is shifting northward at a rate of 15 meters annually.
The real question is...can a box match?
