Since January, another weekly group brings together patients and staff. This reduces institutional tension. The number of patients who did not complete treatment was significantly reduced. This is an opportunity for active training by staff.
Cairn making as a therapy. Inclusion of these groups in the proposed treatment took some time before patients could truly prescribe the final ritual and make it a departure ceremony for those who leave the next day. Gradually, this influence is confirmed, especially in the form of spontaneous development of cultural activity between patients.
For my part, since 2006 I have been engaged in public therapy with children. I am a psychologist at the therapeutic training institute in Toulon. I work with very restless children who are expelled due to expulsion because they know that they express their emotions better by beating or insulting than with balanced and reasoned words.
The very rigorous and structured community therapy methodology is especially suitable for children who need specific rules, frameworks and limitations. The topics offered in the classroom are numerous, but the difficulty for children, at least for these children, is to identify and express emotions. Admission and graduation rituals are highly regarded and often more dynamic than in adult groups. I try to use their limitless energy to fuel the dynamics in the group, and this becomes an asset, not a brake, causing reminders to order. This exercise bores me, and sometimes it happens that I overwhelm myself. But the methodology of this technique helps me stay on track.
The end of the ritual. At the end of the session, the participants stand up and form a circle, holding their shoulders. This is a very intimate moment when we share our feelings in a session.
In order to illustrate the state of social therapy for the last time, I would like to tell you this Brazilian proverb: “A spider without a web is like an Indian without his own land, he looks like an unconnected community. solidarity. Public therapy destroys isolation and isolation, enhances the sense of belonging to a group, community, creates connections, the exchange of experience, knowledge, know-how.
Careful observation of the “vertical” stratigraphic sequence of the mound for the first time led us to conclude that there were a split formation in two large sedimentary episodes. On the other hand, insisting on the nature and “horizontal” arrangement of the two families of sediments that make up the monument without interfering, we wanted to draw attention to the previous radical choice in favor of two pedological sources.
Quite distinctly: the surrounding land and the wet zone can form whitish hydromorphic silts located on the periphery of the outer shell, as well as in direct contact with the arch. Therefore, one of the goals of this chapter will be to collect information on other mounds that can report both on the nature of the land or materials used by builders, and on the dynamics of construction. If they repeat the order of the data obtained in the study, this information may thus enable us to establish particularly important correspondences between these various studied sites.
Interesting facts about cairns. Large-scale processes that generate metamorphic rocks move rocks through various geological environments: these processes are recorded by the mineralogical transformations of the rocks, which are reflected in the pressure space. temperature (and time).
DT routes are determined by the type of thermal installation in a given region and / or the geological environment (for example, subduction zones in the direction of mid-oceanic environments) and the type of geological process that determines the depth to which material and type are transported. translations suffered. During these events, the rocks can continuously recrystallize, and new minerals can replace old minerals in accordance with a complex time sequence.
Older minerals (or mineral associations) can survive continuous recrystallization due to low and / or adverse reaction kinetics. Therefore, it becomes important to study the geometric relationships between the constituent minerals of metamorphic rocks in order to identify groups of minerals that developed simultaneously with the equilibrium between them (mineralogical paragenesis), and to identify the relationships of reactions and / or imbalances between different groups of minerals in order to restore the time sequence of paragenesis and, therefore, a series of metamorphic events recorded by rocks during their evolution.
Comparison of these petrographic observations with experimental modeling (reproduced in the laboratory using chemical systems approximating the composition of real rocks) allows us to trace the pressure and temperature conditions for the formation of various mineralogical associations observed in rocks and, therefore, to conduct a quantitative assessment. metamorphic process.