Los Mandatos Informales (parte 2) - YouTube. Julie Jezuit. Los mandatos. Screen 3 on FlowVella - Presentation Software for Mac iPad and iPhone' See more. 'A2/B1 - Imperativos: Fluye como el agua. Consejos para sentirse a gusto con la vida. [De Typewear.]' See more. Descargar o inscribirse en un curso gratuito de Dawson Education Services Co-op, What's In. Detectores de movimiento, sensores de agua, sensores de temperatura. Comparte tu URL de FlowVella para que cualquiera con un iPad o un. Here is where you can respond to the questions you posted on screen 4. Also use this space to explain if your hypothesis was correct. Why or why not?
This workshop is developed for school administrators, technology coaches, etc. To assist in providing professional development for state specialists, administrators, and classroom teachers on how to use the iPad for classroom learning and how to use it as a technology tool. The apps used in this course are free and paid. Feel free to choose what best works with your audience. There are built in assignments for each post to provide hands-on applications for the participants. It is a self-paced workshop that can also be presented in a 6-hour fast paced face-to-face setting.
I would suggest breaking it into several days.
The large 'waterfall' at Hierve el Agua Hierve el Agua ( for 'the water boils') is a set of natural rock formations in the of that resemble cascades of water. The site is located about 70 km east of, past, in the municipality of, with a narrow, winding unpaved road leading to the site. The site consists of two rock shelves or cliffs which rise between fifty and ninety metres from the valley below, from which extend nearly white rock formations which look like waterfalls. These formations are created by fresh water springs, whose water is over-saturated with and other minerals. As the water scurries over the cliffs, the excess minerals are deposited, much in the same manner that are formed in caves.
One of the cliffs, called the 'cascada chica' (small waterfall) or the Amphitheatre, contains two large artificial pools for swimming as well as a number of small natural pools. One of the artificial pools is very near the edge of the cliff.
Looking out over the valley The site is located in a very isolated region with rough terrain, dominated principally by forest, cactus and other semi desert vegetation. The 'waterfalls' or rock formations are on cliffs of mountains that rise abruptly from the narrow valley floor below.
It is located in ethnic Mixe territory, with the two closest and most populous communities being San Lorenzo Albarradas and with populations of 1403 and 320 respectively (2005). The springs that produce the rock formations are one of the few water sources in the area. 'Waterfall' rock formations and springs.
Rock formation as it 'goes over' the cliff at the Amphitheater The site consist of two waterfall-like rock formations which have been formed over thousands of years. Both cliffs rise over fifty meters from the valley floor, with one rock formation reaching down twelve metres and the other reaching down thirty metres. The twelve meter one is called 'cascada chica' (small waterfall) and 'flows' off a base which is about sixty metres wide. The other, 'cascada grande' (large waterfall), extends down from a base with which is about ninety metres wide and eighty metres above the valley floor.
Natural and lower artificial pool The more easily accessible and more often visited of the two waterfalls is the 'cascada chica,' also called the Amphitheatre. This cliff rises over fifty metres above the valley floor, where there is a natural platform about sixty meters wide. This platform has four springs. The water from three of the four springs is captured by a number of small natural pools and two large artificial pools in which visitors can swim. The lower of the two pools is very close to the cliff edge and was built in 2007.
In these pools, the water appears a turquoise green due to the mineral concentration. The fourth spring is located closest to the edge and responsible for most of the waterfall rock formation.
Pagar El Agua On Line
Two of the four springs on the Amphitheatre side rise from the level floor and appear to bubble up, which is the source of the name. The bubbling action of these and some other springs is thought to occur due to construction of underground water currents. This bubbling action leads to the name of the area, Hierve el Agua (the water boils).
Water constantly flows out of the springs and the process of depositing the calcium carbonate is ongoing, which can be seen on the walls of the artificial pools. Trails lead from the cascada chica to the cascada grande, the valley floor and other areas in the vicinity. The cascada grande is just to the south of the cascada chica and easily visible from it. This waterfall rock formation is more vertical than the cascada chica. Similarly, it is a rock shelf from which flows mineral laden water over the side. This shelf is ninety metres above the valley floor, eighty metres wide with the waterfall extending down for about thirty metres.
This shelf does not have artificial pools. Ancient canals. One of the springs that bubbles up The area is also of archeological interest because of the extensive system of irrigation and terraces built by the as many as 2,500 years ago. It was also most likely a sacred site to the ancient peoples of the Oaxaca valley.
The canals are part of an irrigation system which was created more than 2,500 years ago, most of which extend from the Amphitheatre side. Researchers have studied the terraces and canals which have been cut into the sides of the mountains these cliffs are on and have concluded that they were an irrigation system, unique in Mexico. Only vestiges of these irrigation canals remain; however, the archeological area has not been completely explored. These irrigation canals are considered to be unique in, not only because irrigation was not common in pre-Hispanic Mexico but because they are the only example of lined irrigation canals. It is not known why does not appear outside of the Hierve el Agua area, and here the lining develops naturally. While seepage and bank erosion were indeed problems with irrigation farming in other parts of Mesoamerica, the nearest example of anything similar is with the of southern in 650 C.E.
The tourist attraction. Part of Turis Yu'u In addition to the artificial pools on the Amphitheatre side, a number of other services have been built for visitors such as food stands, small markets, cabins and a regular swimming pool. The cabin area, called 'Turis Yu’u,' with its pool was built in the 1990s and offer areas to change clothes, shower, eat in an open-air restaurant and for overnight stays although the accommodations are very basic. This complex, as well as many of the other stalls are owned by residents of the Roeguia community. However, despite the development, the nearby communities of San Lorenza Albarradas and San Isidro Roaguia still suffer from poverty. One reason for this is that visitors are charged between fifty and sixty each by the state of Oaxaca to enter the site.
Entrance fees can bring in anywhere from $1000 to $5000 pesos per day depending on the season. Another is that there is a dispute between the two nearby communities as to who should administer it. Disputes over administration and income led to the closing of the site between 2005 and 2007. Since then, promises by state officials were made to invest the money earned at the site to raising living standards in the area, but residents claim that this has never happened. The disputes have also led to tourists being charged twice to access the site, once on the road and once at the entrance to the park.
Wikimedia Commons has media related to. Wikivoyage has a travel guide for. References.